[ { "text": "The Noribagaribao Formation originally refers to the gray-green thick layer of medium-fine-grained rock-cut feldspar sandstone feldspar quartz sandstone feldspar sandstone feldspar sandstone feldspar sandstone and feldspar sandstone, clay and mud crystal limestone, and only bivalve fossils are seen, which are continuous deposited with the ninety-superior teams.", "triple_list": [ [ "Nuoribagari protection group", "Lithology", "Gray gray-green thick layer - fine-grained rock-cut feldspar sandstone" ], [ "Nuoribagari protection group", "Lithology", "Feldspar quartz sandstone" ], [ "Nuoribagari protection group", "Lithology", "Feldstone sandstone intersects siltstone" ], [ "Nuoribagari protection group", "Lithology", "Clay rock" ], [ "Nuoribagari protection group", "Lithology", "Mud crystal limestone" ], [ "Nuoribagari protection group", "Paleontological", "Bivalves" ], [ "Nuoribagari protection group", "Integration of contacts", "Ninety teams" ] ] }, { "text": "The Qumocuo group test area only has a small amount of exposure in the southwest part of the picture Wangyongqu area, with an area of less than 10m2 and a thickness of more than 29.25m.", "triple_list": [ [ "Quemoduo Group", "Exposed", "Picture of the southwest character Wang Yong song" ], [ "Quemoduo Group", "area", "10m2" ], [ "Quemoduo Group", "thickness", "29.25m" ] ] }, { "text": "The grey thick-thick layered conglomerate of the Xinjinjiquguo Formation 37.63m Parallel and unconformity Yaxicuo Formation", "triple_list": [ [ "The grey thick-thick layered gravel rock of the New Jiquguo Formation", "thickness", "37.63m" ], [ "The grey thick-thick layered gravel rock of the New Jiquguo Formation", "Integration of contacts", "Yaxicuo Group" ] ] }, { "text": "Porcelain is mainly plagioclase and a small amount of quartz mica.", "triple_list": [ [ "Pyramid", "Contained", "Plagioclase" ], [ "Pyramid", "Contained", "Quartz Miscellaneous" ] ] }, { "text": "The colorful opale green mixed rock sub-belt volcanic rocks are located in the Dangjiang-Colorful area in the northern part of the survey area, and are generally distributed in a northwest-south eastward direction.", "triple_list": [ [ "Colorful opale green mixed rock sub-belt volcanic rocks", "Exposed", "Dangjiang, the northern part of the test area - colorful" ], [ "Colorful opale green mixed rock sub-belt volcanic rocks", "Distribution pattern", "Northwest-south eastward belt-shaped cloth" ] ] }, { "text": "Hecosmilia sp. scabbard coral was collected from limestone; Complexastraea sp. and Radulopccten sp. scraping sea fans; Oscillopha sp., the era was the Middle Jurassic.", "triple_list": [ [ "Limestone", "Paleontological", "hecosmilia sp.Sharpening coral" ], [ "Limestone", "Paleontological", "Complexastraea sp." ], [ "Limestone", "Paleontological", "Radulopccten sp.Scrape the sea fan" ], [ "Limestone", "Paleontological", "Oscillopha sp." ], [ "Limestone", "Age", "Middle Jurassic" ] ] }, { "text": "The late Triassic granite is mainly distributed in the area of Ladigonmaméria in the test area. The area is controlled by the NW-SE directional fracture in the tectonic mixed zone, and is distributed in a long strip shape. The invasive body has good group living and has very good band ductility. 8 invasive bodies are exposed, with an area of about 227m2.", "triple_list": [ [ "Late Triassic Granite", "Exposed", "Radigonmaméri Japanese" ], [ "Late Triassic Granite", "Distribution pattern", "Long strip shape" ], [ "Late Triassic Granite", "area", "227m2" ] ] }, { "text": "The main lithologies in Beiziqu area of Jieduo Township are a section of gray - dark gray is accompanied by brown medium-thin layered silty silty silty silty silty silty and coal seam limestone, and gray-purple medium-thick layered lithotris feldstone sandstone is relatively few.", "triple_list": [ [ "Jieduo Township Beiziqu", "Lithology", "Gray - dark gray with brown medium-thin layered silty slab" ], [ "Jieduo Township Beiziqu", "Lithology", "Carbon slate" ], [ "Jieduo Township Beiziqu", "Lithology", "Coal seam limestone" ], [ "Jieduo Township Beiziqu", "Lithology", "Gray-purple medium-thick layered lithotrix feldspar sandstone" ], [ "Jieduo Township Beiziqu", "Lithology", "Siltstone" ] ] }, { "text": "Rhyolites are less distributed, mostly in a lens-like manner.", "triple_list": [ [ "Rhyolite", "Distribution pattern", "Lens-like" ] ] }, { "text": "Light gray giant thick layered crystalline limestone 134.13m", "triple_list": [ [ "Light gray giant thick layered crystalline limestone", "thickness", "134.13m" ] ] }, { "text": "Dark gray thin-layered silty slate with gray medium-layered fine-grained feldquartz sandstone 19.10m", "triple_list": [ [ "Dark gray thin-layered silty slate with gray medium-layered fine-grained feldquartz sandstone", "thickness", "19.10m" ] ] }, { "text": "As early as 1970, the Qinghai Provincial Regional Test Team divided the Early Carboniferous Sediment in Tanggula Mountain from bottom to top into the upper coal-containing seam of the limestone formation in the lower clastic rock formation in the upper coal-bearing seam in the middle of the lower clastic rock formation.", "triple_list": [ [ "Early Carboniferous Sedimentation", "Contained", "Clastic rock formation" ], [ "Early Carboniferous Sedimentation", "Contained", "Central limestone formation" ], [ "Early Carboniferous Sedimentation", "Contained", "Coal-containing layer" ] ] }, { "text": "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone with mud calcareous silt sandstone and a small amount of fine-grained rock-cut quartz sandstone 242.55m", "triple_list": [ [ "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone with mud calcareous silt sandstone and a small amount of fine-grained rock-cut quartz sandstone", "thickness", "242.55m" ] ] }, { "text": "Discussion on the times, there are fossils in the middle of the Noribagaribao group, Martinia sp, Marginifera sp., Orthoticia indicaWaagen, Squamularia sp., Athyris sp.; Spirifer sp., Crurithyris sp., Dielasma sp., Coral Liangshanophyllum sp., Wentzella sp., Waagenophyllum sp.; Neoschwagerina douvilina Ozawa, Parafusulina cf. yabei Hanzawa, Yabeina wangsiania (Lee), Pseudofusulina yunnanensis Zhang; Pachyphloia sp., Reichelina sp; Ammonite Agathiceras suessi Gemmmellaro, Attinsia sp.", "triple_list": [ [ "Nuoribagari protection group", "Paleontological", "Martinia sp, Marginifera sp." ], [ "Nuoribagari protection group", "Paleontological", "Orthoticia indicaWaagen" ], [ "Nuoribagari protection group", "Paleontological", "Squamularia sp." ], [ "Nuoribagari protection group", "Paleontological", "Athyris sp." ], [ "Nuoribagari protection group", "Paleontological", "spirifer sp." ], [ "Nuoribagari protection group", "Paleontological", "Crurithyris sp." ], [ "Nuoribagari protection group", "Paleontological", "Dielasma sp." ], [ "Nuoribagari protection group", "Paleontological", "Coral Liangshanophyllum sp." ], [ "Nuoribagari protection group", "Paleontological", "Wentzella sp." ], [ "Nuoribagari protection group", "Paleontological", "Waagenophyllum sp." ], [ "Nuoribagari protection group", "Paleontological", "Neoschwagerina douvilina O zawa" ], [ "Nuoribagari protection group", "Paleontological", "Parafusulina cf. yabei Hanzawa" ], [ "Nuoribagari protection group", "Paleontological", "Yabeina wangsiania (Lee)" ], [ "Nuoribagari protection group", "Paleontological", "Pseudofusulina yunnanensis Zhang" ], [ "Nuoribagari protection group", "Paleontological", "Pachyphloia sp." ], [ "Nuoribagari protection group", "Paleontological", "Reichelina sp" ], [ "Nuoribagari protection group", "Paleontological", "Ammonite Agathiceras suessi Gemmellaro" ], [ "Nuoribagari protection group", "Paleontological", "Attinsia sp" ] ] }, { "text": "The Kaixin Ridge group is distributed in the area of Ziqudong Ziquyong-Lamei Qudongjiaoyong-Dongmoyong Zhaqingxiang-Saiquyong.", "triple_list": [ [ "Happy Ridge Group", "Exposed", "Ziqubei Dongziqu-Latitude Qudongjiaoyong-Dongmoyong Zhaqingxiang-Saiqu-Yuan" ] ] }, { "text": "Among them, Wentzelella is an important element in the Ipcipyllum-Wentzelella combination in the upper part of the lower south slope of the East Kunlun Mountains in our province, and is also found in the Xiqingshan and the South Qilianshan subdivisions.", "triple_list": [ [ "Wentzelella", "Belongs to", "Ippyllum-Wentzelella combination in the upper part of the Permian lower south slope of the East Kunlun Mountain" ], [ "Wentzelella", "Exposed", "The west is surrounded by mountains" ], [ "Wentzelella", "Exposed", "South Qilian Mountain" ] ] }, { "text": "It is reflected in the deep-sea-semi-deep-sea carbonate sedimentation, and there are fiber sponges Inozian and sea lily stem Cyclocyclicus sp., which was the early and middle Permian.", "triple_list": [ [ "Deep-semi-deep-carbonate rock", "Paleontological", "Fiber sponge Inozian" ], [ "Deep-semi-deep-carbonate rock", "Paleontological", "Sea lily stem Cyclocyclicus sp." ], [ "Deep-semi-deep-carbonate rock", "Age", "Early and Middle Permian" ] ] }, { "text": "Volcanic rocks are mainly distributed in the Tojiqubuqu area, and petrochemistry reflects the characteristics of alkaline volcanic rocks of high titanium.", "triple_list": [ [ "Volcanic rocks", "Exposed", "Tojiqubuqu" ], [ "Volcanic rocks", "Belongs to", "Characteristics of alkaline volcanic rocks" ] ] }, { "text": "Gray medium-layered medium-grained rock-cut sandstone sandstone intersected with dark gray thin-layered siltstone, producing brachiopod Martinia sp. fault Gadikao Formation, gray thick layered tuff", "triple_list": [ [ "Gray medium-layered medium-grained rock-cut sandstone sandstone with dark gray thin-layered siltstone", "Paleontological", "Brachiopod Martinia sp." ], [ "Gray medium-layered medium-grained rock-cut sandstone sandstone with dark gray thin-layered siltstone", "Fault contact", "Gadikao Group" ], [ "Gadikao Group", "Lithology", "Gray thick layered tuff" ] ] }, { "text": "In the area north of Jiangyong, the rocks have strong deformation, and the rocks are mainly eye-like strip-shaped neutral volcanic mylonite inanite mylonite.", "triple_list": [ [ "Dangjiang Chongbei", "Lithology", "Ocular band-like neutral volcanic mylonite" ], [ "Dangjiang Chongbei", "Lithology", "Ananite mylonite" ] ] }, { "text": "This strata area is distributed in the opal green mixed zone of Tongtian River. Its lithological metamorphosis and deformation are similar to the Beining multigroup strata in Changqingke Xiaosumang Township, Yushu County, Qinghai Province, southern Tongtian River. The rock strata units in Qinghai Province have not been cleaned up. The 1:200,000 Dengke area report shows the Ningduo Group. This article uses this strata unit - Ningduo Group. Since this strata is a set of hierarchical disordered tectonic rock strata, the report uses Ningduo Group, which is from the mid-Paleoproterozoic period.", "triple_list": [ [ "This strata", "Earth tectonic location", "Tongtian River opal green mixed belt" ], [ "Ningduoqun", "Distribution pattern", "Layered disordered tectonic rock formations" ], [ "Ningduoqun", "Age", "Ancient Proterozoic" ] ] }, { "text": "Gray-purple medium-thick layered mud calcium silty sandy medium-grained rock-cut feldspar sandstone sandstone and mud calcium silty sandstone and medium-layer complex fine conglomerate 11.20m", "triple_list": [ [ "Gray-purple medium-thick layered mud calcium silty sandy medium-grained rock feldspar sandstone sandstone intersected mud calcium silty sandstone and medium-layered complex fine gravel rock", "thickness", "11.20m" ] ] }, { "text": "Carbonate rock formation (C1Z2) The geographical distribution location of this group is basically in line with the clastic rock formation (C1Z1), with a distribution area of 45m2, and a section control thickness greater than 155.36m, but the maximum thickness in many layers is as high as 1005.58m.", "triple_list": [ [ "Carbonate rock formation", "area", "45m2" ], [ "profile", "thickness", "155.36m" ], [ "Multiple pictures", "thickness", "1005.58m" ] ] }, { "text": "Dangjiangrong volcanic rocks are mainly distributed in the south side of Duocai Township in the test area - the north of Dangjiangyong-Songmorong area. The exposed area is 520m2, and the maximum thickness is controlled to be 703.71m.", "triple_list": [ [ "Dangjiangrong Volcanic Rock", "Exposed", "South side of Duocai Township-North Dangjiang Yong-Songmorong" ], [ "Dangjiangrong Volcanic Rock", "area", "520m2" ], [ "Dangjiangrong Volcanic Rock", "thickness", "703.71m" ] ] }, { "text": "The lava composition is andesite, with a lava content of about 70%.", "triple_list": [ [ "Lava", "Lithology", "Andanyan" ] ] }, { "text": "The clastic rock grain size in the southern area of Xiaoxiang becomes thinner, and to the top is the regular grain rhythm layer of siltstone, the characteristics of quartz reflect the gradual deepening of seawater.", "triple_list": [ [ "Go to the south of Xiaoxiang", "Lithology", "Clastite" ], [ "Go to the south of Xiaoxiang", "Lithology", "Siltstone" ], [ "Go to the south of Xiaoxiang", "Develop", "Resolution" ] ] }, { "text": "The rocks are mainly fine-grained quartz sandstone sandstone silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty and thin layered biolimestone limestone. In the measurement area, they are mostly interspersed with medium-acid volcanic rocks and tuffs, and thin gypsum layers are interspersed with local areas.", "triple_list": [ [ "rock", "Lithology", "Fine-grained quartz sandstone" ], [ "rock", "Lithology", "Siltstone" ], [ "rock", "Lithology", "Silty slab" ], [ "rock", "Lithology", "Polygon" ], [ "rock", "Lithology", "Rock cuttings sandstone" ], [ "rock", "Lithology", "Calcium siltstone" ], [ "rock", "Lithology", "Calcium slab" ], [ "rock", "Lithology", "Thin layered biolimestone" ], [ "rock", "Lithology", "Limestone" ], [ "rock", "Lithology", "Medium-acid volcanic rock" ], [ "rock", "Lithology", "Tuff" ], [ "rock", "Lithology", "Gypsum layer" ] ] }, { "text": "It disintegrated from the Batang group of the late Triassic period of the Central Plains, belonging to the Western Jinwulan-Jinshajiang stratigraphic division.", "triple_list": [ [ "Batang Group of the Late Triassic World", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ] ] }, { "text": "Nuoriba Garibao Group (P2nr) Liu Guangcai (1993) created the famous Nuoriba Garibao Group in Nuoriba Garibao City.", "triple_list": [ [ "Nuoribagari protection group", "Exposed", "Golmud City Noriba Garibao" ] ] }, { "text": "There is a dense permeability cleavage in the rock.", "triple_list": [ [ "rock", "Develop", "Permeable cleavage" ] ] }, { "text": "The rocks in the south side of Duocai Township are mainly composed of flakes of physical and chemical Anshanyan Ying'an tuff, and the rock deformation is relatively weak, mainly mainly flakes of physical and chemical mylonite, with green mud schist, flakes of physical and chemical basalt, lithotripsy sandstone and slate.", "triple_list": [ [ "Colorful Township South", "Lithology", "Andesan rock" ], [ "Colorful Township South", "Lithology", "Yingan tuff" ], [ "Colorful Township South", "Lithology", "Physical and chemical mylonite" ], [ "Colorful Township South", "Lithology", "Green mud schist" ], [ "Colorful Township South", "Lithology", "Physical and chemical basalt" ], [ "Colorful Township South", "Lithology", "Rock cuttings sandstone" ], [ "Colorful Township South", "Lithology", "Slate" ] ] }, { "text": "Qinghai Province Second Region Transfer Team (1982) created a famous group of Zaduo Group in Zaduo County (Zhaduo County).", "triple_list": [ [ "Miscellaneous groups", "Exposed", "Zaduo County Area (Zhaduo County)" ] ] }, { "text": "The era of sedimentation of the saduo group was late Carboniferous-Early and Middle Permian.", "triple_list": [ [ "Miscellaneous groups", "Age", "Late Carboniferous-Early and Middle Permian" ] ] }, { "text": "The rock combination changes in the region are obvious, and the rocks in the southern part of the measurement area are mainly fine-grained sandstone and silt sandstone silt slate and limestone.", "triple_list": [ [ "South of the test area", "Lithology", "Fine-grained sandstone" ], [ "South of the test area", "Lithology", "Siltstone" ], [ "South of the test area", "Lithology", "Silty slab" ], [ "South of the test area", "Lithology", "Slate" ], [ "South of the test area", "Lithology", "Limestone" ] ] }, { "text": "The rock combination is mainly composed of rock-cut quartz sandstone and silty slate, with rock-cut sandstone containing conglomerate sandstone silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty", "triple_list": [ [ "rock", "Lithology", "Rock cutting quartz sandstone" ], [ "rock", "Lithology", "Silty slab" ], [ "rock", "Lithology", "Rock cuttings sandstone" ], [ "rock", "Lithology", "Contaminated rock" ], [ "rock", "Lithology", "Chop sandstone" ], [ "rock", "Lithology", "Siltstone" ], [ "rock", "Lithology", "Qianmeiyan" ], [ "rock", "Lithology", "Silicone rock" ] ] }, { "text": "This work follows the bipartite division plan for the rock formations of Qinghai Province (1997), namely two formal formation-level rock formation units, including the clastic rock formation (C1Z1) and carbonate rock salt formation (C1Z2) from bottom to top.", "triple_list": [ [ "Miscellaneous groups", "Outcrop", "Clastic rock formation" ], [ "Miscellaneous groups", "Outcrop", "Carbonate salt formation" ] ] }, { "text": "The Mixed Rock Belt Period of the Western Jinwulan Tectonics is considered to be the Carboniferous-Permian period.", "triple_list": [ [ "Mixed rock belt in Xijin Wulan tectonic", "Age", "Carboniferous-Permian" ] ] }, { "text": "Gray medium-layered fine-grained feldquartz sandstone sandstone with dark gray thin-layered silt sandstone 122.32m", "triple_list": [ [ "Gray medium-layered fine-grained feldquartz sandstone with dark gray thin-layered siltstone", "thickness", "122.32m" ] ] }, { "text": "The rock is characterized by physical and chemical mylonite and Ananite rhyolite tuff volcanic breccia lava, with green mud schist and physical and chemical basalt, lithotris sandstone and slate.", "triple_list": [ [ "rock", "Lithology", "Physical and chemical mylonite chemistry andshanite" ], [ "rock", "Lithology", "Ying'an rhyolite" ], [ "rock", "Lithology", "Tuff" ], [ "rock", "Lithology", "Volcanic breccia lava" ], [ "rock", "Lithology", "Green mud schist" ], [ "rock", "Lithology", "Physical and chemical basalt" ], [ "rock", "Lithology", "Rock cuttings sandstone" ], [ "rock", "Lithology", "Slate" ] ] }, { "text": "The maximum structural stacking thickness is 1039.52m.", "triple_list": [ [ "Maximum structural stacking", "thickness", "1039.52m" ] ] }, { "text": "This stratigraphic area is distributed in the Xijin Wulan-Jinshajiang stratigraphic area, which cannot be compared with previous information.", "triple_list": [ [ "Strata", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ] ] }, { "text": "The opale mixed rock assembly consists of colorful opalite components and basal cracked rock blocks as early as the mid-Middle Permian Obada limestone and Dangjiangrong volcanic rock.", "triple_list": [ [ "Ophiolure Mixed Rock Combination", "Lithology", "Colorful ophiolite" ], [ "Ophiolure Mixed Rock Combination", "Lithology", "Basement cracked rock blocks" ], [ "Ophiolure Mixed Rock Combination", "Lithology", "Obada limestone in the early and middle Permian" ], [ "Ophiolure Mixed Rock Combination", "Lithology", "Chelong Sandstone" ], [ "Ophiolure Mixed Rock Combination", "Lithology", "Dangjiangrong Volcanic Rock" ] ] }, { "text": "The opalae mixed rock era was the early Carboniferous era.", "triple_list": [ [ "Ophiolulu mixed rock", "Age", "Early Carboniferous" ] ] }, { "text": "Zhiduo County’s Administrative area is affiliated to Yushu Tibetan Autonomous Prefecture, Qinghai Province.", "triple_list": [ [ "Zhiduo County", "Administrative area", "Yushu Tibetan Autonomous Prefecture, Qinghai Province" ] ] }, { "text": "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone with fine-grained rock-cut miscellaneous sandstone 31.11m", "triple_list": [ [ "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone with fine-grained rock-cut miscellaneous sandstone", "thickness", "31.11m" ] ] }, { "text": "The vertical change is manifested as a degenerate stratigraphic structure from bottom to top from coarse to thin, and the horizontal change is in the west and fine trend in the east. The sedimentary era was the Middle Permian.", "triple_list": [ [ "Strata", "Age", "Middle Permian" ] ] }, { "text": "The bottom is in integrated contact with the clastic rock formation (C1Z1), in contact with the Kaixinling group fault, and the local Tuotuo River group angle is not integrated on it.", "triple_list": [ [ "bottom", "Integration of contacts", "Clastic rock formation" ], [ "bottom", "Fault contact", "Happy Ridge Group" ], [ "bottom", "Unconformity contact", "Tuotuo River Group" ] ] }, { "text": "Gray - light gray huge thick layered limestone, fiber-producing sponge Inozian and sea lily stem Cyclocyclicussp.", "triple_list": [ [ "Gray - light gray huge thick layered limestone", "Paleontological", "Fiber sponge Inozian" ], [ "Gray - light gray huge thick layered limestone", "Paleontological", "Sea lily stem Cyclocyclicusp" ] ] }, { "text": "The lower part of Kaixinling group is a carbonate rock with variegated clastic rock and limestone and volcanic rock, and the upper part is a carbonate rock with a little clastic rock.", "triple_list": [ [ "Happy Ridge Group", "Lithology", "Carbonate rock" ], [ "Happy Ridge Group", "Lithology", "Variegated clastic rock" ], [ "Happy Ridge Group", "Lithology", "Limestone" ], [ "Happy Ridge Group", "Lithology", "Volcanic rocks" ], [ "Happy Ridge Group", "Lithology", "Carbonate rock" ], [ "Happy Ridge Group", "Lithology", "Clastite" ] ] }, { "text": "The lithologic combination of the Noribagaribao Formation is a set of gray gray-green gray-purple lithotrix feldspar sandstone feldspar quartz sandstone mixed with a mud silt sandstone mud crystal biolimestone and gray-green basalt basalt medium-basalt medium acidic volcanic breccia interlayer.", "triple_list": [ [ "Nuoribagari protection group", "Lithology", "Gray gray-green gray-purple rock-cut feldspar sandstone" ], [ "Nuoribagari protection group", "Lithology", "Feldspar quartz sandstone" ], [ "Nuoribagari protection group", "Lithology", "Mud siltstone" ], [ "Nuoribagari protection group", "Lithology", "Mud crystal biolimestone" ], [ "Nuoribagari protection group", "Lithology", "Gray-green basalt andshan rock" ], [ "Nuoribagari protection group", "Lithology", "Basalt" ], [ "Nuoribagari protection group", "Lithology", "Medium-basic medium acidic pyroclastic rock" ], [ "Nuoribagari protection group", "Lithology", "Volcanic breccia" ] ] }, { "text": "Gray-purple thick layered calcareous complex fine conglomerate interlayer-thick layered medium-grained cuts feldspar sandstone (anticline structure) 90.01m", "triple_list": [ [ "Gray-purple thick layered calcareous complex fine conglomerate interlayer-thick layered medium-grained cuts feldspar sandstone", "thickness", "90.01m" ] ] }, { "text": "Ningduoyan Group Pt1-2N The southern side of this strata is Engulfeded by Jurassic granite, and the northern side is in contact with the colorful ophiogenic mixed rock fault, mainly a set of medium-deep metamorphic strata of gneis schist.", "triple_list": [ [ "Ningduoyan Group", "Engulfed", "Jurassic granite" ], [ "Ningduoyan Group", "Fault contact", "Colorful opal green mixed rocks" ], [ "Ningduoyan Group", "Lithology", "Gneis schist" ] ] }, { "text": "Dark gray thin layered silty slate with gray thin-medium layered fine-grained feldquartz sandstone and gray thin layered bioclastic limestone 11.23m", "triple_list": [ [ "Dark gray thin-layered silty slate with gray thin-medium-layered fine-grained feldquartz sandstone and gray thin-layered bioclad limestone", "thickness", "11.23m" ] ] }, { "text": "It is more appropriate to classify the Nuoribagaribao group into a middle Permian.", "triple_list": [ [ "Nuoribagari protection group", "Age", "Medium Perm" ] ] }, { "text": "Profile description The measured geological profile of the Permian Noribagaribao Group in Gongnayong Jiezha Township, Zaduo County, Qinghai Province VIII003P4.", "triple_list": [ [ "Gongnayong, Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Permian Noribagaribao Group" ] ] }, { "text": "Gray-purple medium-thick layered light metamorphic calcareous silty mudstone sandstone with fine-grained feldspar quartz sandstone 65.13m", "triple_list": [ [ "Gray-purple medium-thick layered light metamorphic calcareous silty mudstone with fine-grained feldspar quartz sandstone", "thickness", "65.13m" ] ] }, { "text": "The siliceous rocks are the radioworm Albaillella indebsis WonPylentonema sp.Entactinia variospina(Won)Pseudolbaillella chilensis Ling et Forsgthe; the dentate stone Gnathodus bilineatus (Round) is produced in the sea mountain flakes.", "triple_list": [ [ "Silicone rock", "Paleontological", "Albaillella indebsis WonPylentonema sp." ], [ "Silicone rock", "Paleontological", "Entactinia variospina(Won)Pseudolbaillella chilensis Ling et Forsgthe" ], [ "Haishan Rock", "Paleontological", "Gnathodus bilineatus (Round)" ] ] }, { "text": "The groups of shaduo distributed in the measurement area are mainly distributed in the northern area of Jieduo Township, Zhaqing Township, Zaduo County, the southern part of the measurement area, and are distributed along the northwest-south east-east tectonic line. It is tectonicly distributed in the Haduo Late Paleozoic active continental tectonic belt south of the Western Jinwulan-Jinsha River junction and north of the Lancang River junction.", "triple_list": [ [ "Miscellaneous groups", "Exposed", "Zaqing Township, Zaduo County, Zaduo County, Jieduo Township, Jieduo Township, Zaduo County" ], [ "Miscellaneous groups", "Distribution pattern", "Northwest-south east-east tectonic line" ], [ "Miscellaneous groups", "Earth tectonic location", "Zaduo Late Paleozoic Activity Land Frame Structural Belt" ], [ "Miscellaneous groups", "Earth tectonic location", "Zaduo Late Paleozoic active continental tectonic belt north of Lancang River Belt" ] ] }, { "text": "Gray-gray-brown medium-layered calcareous cemented complex conglomerate 212.11m", "triple_list": [ [ "Gray-gray-brown medium-layered calcareous cemented complex gravel", "thickness", "212.11m" ] ] }, { "text": "The fossils such as the hamstring coral and bivalves in the Gariba Formation of the Noribagaribao Formation have unclear contact with the Lower Vazzargen Formation. The disappearance of clastic rocks is the top level, and the large set of limestone appears as the boundary, and the integration of the limestone of the overlying ninety teams of limestones is in contact with.", "triple_list": [ [ "Nuoribagari protection group", "Paleontological", "Fly coral" ], [ "Nuoribagari protection group", "Paleontological", "Bivalves" ], [ "Nuoribagari protection group", "Lithology", "Clastite" ], [ "Nuoribagari protection group", "Lithology", "Limestone" ], [ "Nuoribagari protection group", "Integration of contacts", "Ninety teams of limestone" ] ] }, { "text": "There is less distribution in the Carboniferous strata survey area, only the Early Carboniferous Miscellaneous Group (C1Z) is distributed.", "triple_list": [ [ "Carboniferous strata", "Outcrop", "Early Carboniferous Worlds" ] ] }, { "text": "The early Carboniferous Era was the Middle Permian era.", "triple_list": [ [ "Early Carboniferous Worlds", "Age", "Middle Permian" ] ] }, { "text": "This section is distributed in the colorful opal green mixed rock belt and is produced in tectonic blocks. The section reflects the two strata, which are divided by the colorful opal green mixed rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock tectonic rock", "triple_list": [ [ "profile", "Earth tectonic location", "Colorful opal green mixed rock belt" ], [ "profile", "Distribution pattern", "Tectonic rock blocks" ], [ "profile", "Lithology", "Gneis" ], [ "profile", "Lithology", "Rock Schist" ] ] }, { "text": "The classification of the stratigraphic areas in the survey area is based on the rock formations of Qinghai Province. The Mado-Malkang Stratigraphic Area of Bayankala Stratigraphic Area belongs to the Xijinwulan-Jinshajiang Stratigraphic Area and the Tanggula-Changdu Stratigraphic Area of the Tanggula-Changdu Stratigraphic Area. The Yushu-Zhongdian plot was destroyed in the east outside the map area after this work and did not appear in the investigation area.", "triple_list": [ [ "Test area", "Stratigraphical zoning", "Bayankala stratigraphic area" ], [ "Test area", "Stratigraphical zoning", "Mado-Malcon Stratigraphic Zone" ], [ "Test area", "Stratigraphical zoning", "Qiangbei-Changdu-Simao stratigraphic area" ], [ "Test area", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ], [ "Test area", "Stratigraphical zoning", "Tanggula-Chambo stratigraphic division" ] ] }, { "text": "Discussion of the times This project has fossils of fiber sponges inozian and Cyclocyclicus sp. in Obada limestone, which was the early and middle Permian period. Among siliceous rocks, there are fossils of radioworms Pseudoalbaillella fusiformis (spindle-shaped pseudoalbaillella sp.) and Pseudoalbaillella sp. (many unspecified species of pseudoalbaillella). The era is P1-P2.", "triple_list": [ [ "Obada Limestone", "Paleontological", "Fiber sponge inozian" ], [ "Obada Limestone", "Paleontological", "Sea lily stem Cyclocyclicus sp." ], [ "Obada Limestone", "Age", "Early and Middle Permian" ], [ "Silicone rock", "Paleontological", "Radioworm Pseudoalbaillella fusiformis (spindle-shaped fake Albait)" ], [ "Silicone rock", "Paleontological", "Pseudoalbaillella sp. (Many undetermined species of fake Albait)" ], [ "Silicone rock", "Age", "P1-P2" ] ] }, { "text": "Grooved molds and particle sequence stratigraphic structures are seen in sandstone.", "triple_list": [ [ "sandstone", "Develop", "Slot mold" ], [ "sandstone", "Develop", "Granular Sequence Laminating" ] ] }, { "text": "Biocombination characteristics and discussion of the times The fossils in the measured area of the clastic rock formation are relatively small in size in the mixed counties, and fossils such as coral Arachnolasma.", "triple_list": [ [ "Miscellaneous clastic rock formation", "Paleontological", "Coral Arachnolasma." ] ] }, { "text": "The thickness of the clastic rock formation in the Hadot group is 481.10m", "triple_list": [ [ "Miscellaneous clastic rock formation", "thickness", "481.10m" ] ] }, { "text": "Light gray medium-thick layered bioclass limestone produces coralstone Syringopora sp.Diphyphyllum integrates heteromultigroup clastic rock formations", "triple_list": [ [ "Light gray medium-thick layered bioclastic limestone", "Paleontological", "Coral Fly Syringopora sp.Diphyphyllum" ], [ "Light gray medium-thick layered bioclastic limestone", "Integration of contacts", "Miscellaneous clastic rock formation" ] ] }, { "text": "The rock formation consists of the newly discovered and established deep metamorphic rock colorful opalene mixed rocks (CPd) and Chayong opalene mixed rocks (Ch) in the Ningduo group of the ancient Middle Proterozoic. The tectonic rock blocks are distributed in the Tongtian River opalene mixed belt in the measurement area.", "triple_list": [ [ "Rocky formations", "Lithology", "Deep metamorphic rocks in Ningduo group in ancient times" ], [ "Rocky formations", "Lithology", "Colorful opal green mixed rocks" ], [ "Rocky formations", "Lithology", "Chayong ophiolula mixed rock" ], [ "Rocky formations", "Distribution pattern", "Tectonic rock blocks" ], [ "Rocky formations", "Earth tectonic location", "Tongtian River opal green mixed belt" ] ] }, { "text": "Polila Formation Gray-blocked Algae-containing Gross Crystalline Limestone, Binoshaibiaganziensis Chen. Halobia sp", "triple_list": [ [ "Polila Formation Gray-block Layer Algae-containing Gross Microcrystalline Limestone", "Paleontological", "Bivalve Haiobiaganziensis Chen. Halobia sp" ] ] }, { "text": "The lava components are mainly plagioclase zoicle.", "triple_list": [ [ "Lava", "Contained", "南后后" ], [ "Lava", "Contained", "南后后" ] ] }, { "text": "Gray sheet physical and chemical medium-grain feldspar quartz sandstone and silty slate interlayer fault Dangjiangrong volcanic rock (CPdva).", "triple_list": [ [ "Gray sheet physical and chemical medium-grain feldspar quartz sandstone and silty slate interlayer", "Fault contact", "Dangjiangrong Volcanic Rock (CPdva)" ] ] }, { "text": "Off-white thick layered crystalline limestone 112.21m", "triple_list": [ [ "Off-white thick layered crystalline limestone", "thickness", "112.21m" ] ] }, { "text": "Physical and chemical altered andesite (Anshan mylonite) 11.21m", "triple_list": [ [ "Physical and chemical altered andesite (Anshan mylonite)", "thickness", "11.21m" ] ] }, { "text": "Physical and chemical alteration of gray-green medium-thick layered sheets and Anshan tuff lava 100.01m", "triple_list": [ [ "Physical and chemical alteration of Andesan tuff lava in gray-green medium-thick layered sheet", "thickness", "100.01m" ] ] }, { "text": "Physical and chemical altered andesite (Anshan mylonite) 20.31m", "triple_list": [ [ "Physical and chemical altered andesite (Anshan mylonite)", "thickness", "20.31m" ] ] }, { "text": "Light fleshy red medium-thick layered altered rhyolite 15.11m", "triple_list": [ [ "Light fleshy red medium-thick layered altered rheology", "thickness", "15.11m" ] ] }, { "text": "Physical and chemical alteration of Andan tuff lava (Anshan mylonite) fault Chrodon sandstone (CPdfw)", "triple_list": [ [ "Physical and chemical alteration of Andan tuff lava (Anshan tuff mylonite)", "Fault contact", "Cut Dragon Sandstone (CPdfw)" ] ] }, { "text": "Gray thin-layer sheet physical and chemical silt calcium silt sandstone 7.22m", "triple_list": [ [ "Gray thin-layer sheet physical and chemical silt calcium silt sandstone", "thickness", "7.22m" ] ] }, { "text": "The chedron sandstone (CPdfw) is mainly distributed in the Songmorong area south of Dangjiang Township in the test area, followed by the Dangjiangrong area, with a controlled thickness of 1565.70m.", "triple_list": [ [ "Cut Dragon Sandstone (CPdfw)", "Exposed", "Songmorong, south of Dangjiang Township" ], [ "Cut Dragon Sandstone (CPdfw)", "Exposed", "Dang Jiang Rong" ], [ "Cut Dragon Sandstone (CPdfw)", "thickness", "1565.70m" ] ] }, { "text": "The fine grains in marble have a grainy crystal structure, a directional structure, a main mineral calcite, a small amount of mica, and a chlorite (illustrated black mica).", "triple_list": [ [ "Dali Rock", "Distribution pattern", "Fine grains and grainy crystal structure" ], [ "Dali Rock", "Develop", "Directional construction" ], [ "Dali Rock", "Contained", "Calcite" ], [ "Dali Rock", "Contained", "muscovite" ], [ "Dali Rock", "Contained", "Celite (black mica illusion)" ] ] }, { "text": "Obadadong limestone (P1-2ca) is mainly distributed in the test area. The Dangagu and Songmorong first zone on the west side of Obadadongdangjiang Township, North. The main body is broken and distributed in the Chayong opal green mixed rock belt, and a small number of tectonic rock wood are distributed in the colorful opal green mixed rock belt. Exposed area 110m2 Control maximum thickness 537.36m. It is in fault contact with the Geren volcanic rock Dalong sandstone in the Chayong opalgreen mixed rock zone; it is in tough shear zone with the volcanic rock sandstone in the colorful opaln mixed rock, and it is covered by the angle of the Neojin Quguo Formation.", "triple_list": [ [ "Obada Limestone", "Exposed", "Chayong North Obadadong Dangjiang Township West side Dangagu and Songmorongdi" ], [ "Obada Limestone", "Distribution pattern", "Block break" ], [ "Obada Limestone", "Distribution pattern", "Tectonic rock blocks" ], [ "Obada Limestone", "Exposed", "Chayong ophiolure mixed rock belt" ], [ "Obada Limestone", "Exposed", "Colorful opal green mixed rock belt" ], [ "Obada Limestone", "area", "110m2" ], [ "Obada Limestone", "thickness", "537.36m" ], [ "Obada Limestone", "Fault contact", "Geren volcanic rock Dalong Sandstone in Chayong ophiolenic mixed rock zone" ], [ "Obada Limestone", "Integration of contacts", "Volcanic rock mixed sandstones in colorful opal green mixed rocks" ], [ "Obada Limestone", "Unconformity contact", "New Jiquguo Group" ] ] }, { "text": "Based on the analysis of the above-mentioned fossils and comparison with the fossils in Guizhou, this picture contains paleobiological fossils in the Early Carboniferous Era, which should be in the middle and late period of the Early Carboniferous Era.", "triple_list": [ [ "Paleobiological fossils in the Early Carboniferous Era", "Age", "Early Carboniferous Constitutional Period" ] ] }, { "text": "The measured profile of Niecha Quning Duoyan Group (Pt1-2N) in Duocai Township, Zhiduo County, Qinghai Province Ⅷ003P2. The geographical coordinates start at 95°28′17 east longitude, 33°46′05 north latitude; the end at 95°28′56 east longitude, 33°47′32 north latitude.", "triple_list": [ [ "Niecha Quning Duoyan Group, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "95°28'17 East longitude" ], [ "Niecha Quning Duoyan Group, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "33°46′05 North latitude" ], [ "Niecha Quning Duoyan Group, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "95°28'56 East longitude" ], [ "Niecha Quning Duoyan Group, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "33°47′32 North latitude" ] ] }, { "text": "New Jiquguo Formation Brick-red conglomerate Obada Limestone (P1-2ca)", "triple_list": [ [ "New Jiquguo Group", "Lithology", "Brick red gravel" ], [ "New Jiquguo Group", "Lithology", "Obada Limestone" ] ] }, { "text": "The rock formation in Qinghai Province is used in this name and is defined as a stratigraphic body distributed on the northern slope of the Tanggula Mountain and located below the ninety-two teams. It is composed of variegated clastic rocks with mudstone limestone and unstable volcanic rocks.", "triple_list": [ [ "Rocky Formation in Qinghai Province", "Exposed", "The northern slope of Tanggula Mountain" ], [ "Rocky Formation in Qinghai Province", "Integration of contacts", "Ninety teams" ], [ "Rocky Formation in Qinghai Province", "Lithology", "Variegated clastic rock" ], [ "Rocky Formation in Qinghai Province", "Lithology", "Mudstone" ], [ "Rocky Formation in Qinghai Province", "Lithology", "Limestone" ], [ "Rocky Formation in Qinghai Province", "Lithology", "Volcanic rocks" ] ] }, { "text": "The Xiaduo Group Clarification Rock Formation produces plant fragments of 66.13m in gray-black medium-layer carbonaceous silty fine sandstone with gray-black argillite feldspar quartz silty sandstone with coal seams", "triple_list": [ [ "The gray-black medium-layered carbonaceous silt fine sandstone with gray-black argillite quartz silt sandstone with coal layer", "Paleontological", "Plant fragments" ], [ "The gray-black medium-layered carbonaceous silt fine sandstone with gray-black argillite quartz silt sandstone with coal layer", "thickness", "66.13m" ] ] }, { "text": "The geographical location of the section is 95°22′20 east longitude, 33°56′11 north latitude, and Elevation is 4943m; the end point is 96°20′20 east longitude, 33°53′44 north latitude, and an elevation is 4464m.", "triple_list": [ [ "profile", "Coordinates", "95°22'20 East longitude" ], [ "profile", "Coordinates", "33°56′11 North latitude" ], [ "profile", "Elevation", "4943m" ], [ "profile", "Coordinates", "96°20′20 East longitude" ], [ "profile", "Coordinates", "33°53′44 North latitude" ], [ "profile", "Elevation", "4464m" ] ] }, { "text": "This group belongs to a set of carbonate salt formations deposited in shallow sea environment. Due to the damage of later faults, the formation is incompletely exposed, and the lithophagophyllum changes in the transverse direction. Only in the Talongjuesa area on the western map, the lens body of breccia-shaped limestone marble has increased significantly. The vertical and lower part is mainly gray-thick-thick layered sand-clad limestone and oval-grained limestone microcrystalline limestone, with a small amount of mud-grained limestone, and the upper carbonate salt crystal grain size becomes thinner. The limestone generally Contained mud-carbon and biological clastic limestone, among which sand-grained interlaced stratigraphic horizontal stratigraphic stratigraphic horizontal stratigraphic stratigraphic limestone is developed in sand-clad limestone.", "triple_list": [ [ "This group", "Belongs to", "Sedimentation in shallow sea environment" ], [ "This group", "Belongs to", "Carbonate salt formation" ], [ "This group", "Exposed", "The Dragon-Powering Area in Xitubian" ], [ "This group", "Lithology", "Breccia limestone" ], [ "This group", "Develop", "Marble lens body" ], [ "This group", "Lithology", "Gray thick-timbered layered sand chip limestone" ], [ "This group", "Lithology", "Oxygen limestone microcrystalline limestone" ], [ "This group", "Lithology", "Mixed limestone" ], [ "This group", "Lithology", "Carbonate salt" ], [ "Limestone", "Develop", "Sludge carbon and bioclastic limestone" ], [ "Sand chip limestone", "Develop", "Sand pattern interlaced layering" ], [ "Sand chip limestone", "Develop", "Horizontal stratification" ] ] }, { "text": "The stratigraphic zone belongs to the Xijinwulan-Jinshajiang stratigraphic zone.", "triple_list": [ [ "Strata", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ] ] }, { "text": "The Zaduo group strata in the test area are most fully exposed in the Zaqing Township, Zaduo County, Qinghai Province, with the main body being in the Zaduo County in the south of the test area.", "triple_list": [ [ "Miscellaneous groups", "Exposed", "Zaqing Township, Zaduo County, Qinghai Province" ] ] }, { "text": "1:250,000 I46C003004 (Zhiduo County) Regional geological survey project is located on the northern slope of Tanggula Mountain in Qinghai Province, with geographical coordinates of 94°30′-96°00′ East longitude; 33°00′-34°00′ North latitude.", "triple_list": [ [ "Zhiduo County", "Located at", "The northern slope of Tanggula Mountain in Qinghai Province" ], [ "Zhiduo County", "Coordinates", "East longitude 94°30′-96°00′" ], [ "Zhiduo County", "Coordinates", "North latitude 33°00′-34°00′" ] ] }, { "text": "Gray thin layered limestone with white thin layered gypsum layer 222.33m", "triple_list": [ [ "Gray thin layered limestone with white thin layered gypsum layer", "thickness", "222.33m" ] ] }, { "text": "This rock formation produces new halberds Neochones sp. slim pattern halberds eauicones sp.", "triple_list": [ [ "The rock formation", "Paleontological", "New halberd Neochones sp." ], [ "The rock formation", "Paleontological", "slim patterned halberd eauiconetes sp." ] ] }, { "text": "This 1:25 Wanzhiduo County regional geological survey collected abundant stratigraphic data, and newly discovered or established three informal rock formation units, including three groups, namely, Bayan Kala Mountain Group (B), Sandstone Formation (2-3B), and Sandstone and Slate Interstratigraphic Sections (3B), and the Early Triassic Triassic Volcanic Formation (P3h); Carboniferous-Permian Colorful Ophiolen Mixed Rock (CPd); Triassic Chayong Ophiolen Mixed Rock (ch).", "triple_list": [ [ "Zhiduo County", "Contained", "Ningduoyan Group in the Proterozoic Period" ], [ "Zhiduo County", "Contained", "Bayan Kala Mountains in the Mid-End Triassic" ], [ "Zhiduo County", "Contained", "Sandstone Formation" ], [ "Zhiduo County", "Contained", "Interlayer section of the slate sandstone and slate" ], [ "Zhiduo County", "Contained", "Late Permian Early Triassic Volcanic Rock Formation" ], [ "Zhiduo County", "Contained", "Carboniferous-Permian colorful opalene mixed rock" ], [ "Zhiduo County", "Contained", "Triassic checks on ophiolula mixed rock" ] ] }, { "text": "The geographical coordinates of the Noribagaribao Group are 95°50′18 east longitude, 33°06′09 north latitude, and Elevation is 4829m; the end point is 95°53′15 east longitude, 33°07′03 north latitude, and elevation is 4674m.", "triple_list": [ [ "Nuoribagari protection group", "Coordinates", "95°50'18 East longitude" ], [ "Nuoribagari protection group", "Coordinates", "33°06'09 North latitude" ], [ "Nuoribagari protection group", "Elevation", "4829m" ], [ "Nuoribagari protection group", "Coordinates", "95°53'15 East longitude" ], [ "Nuoribagari protection group", "Coordinates", "33°07′03 North latitude" ], [ "Nuoribagari protection group", "Elevation", "4674m" ] ] }, { "text": "The metamorphic rock system in this test area is compared with the above metamorphic rocks. The lithology is similar to that of Ningduo Group, so it is also classified as Ningduo Group, and its era is temporarily classified as the mid-Proterozoic.", "triple_list": [ [ "Metamorphic rock system", "Belongs to", "Ningduoyan Group" ], [ "Metamorphic rock system", "Age", "Ancient Proterozoic" ] ] }, { "text": "The Tongtian River opaleum mixed rock is used in the rock formations of Qinghai Province (1997), which is defined as the Tongtian River opaleum mixed rocks. It is a geological body of multiple rocks that are striped or intermittently spread along the line of Xijin Wulan Lake-Tongtian River-Yushu. It mainly consists of slate thousand rock schist transformed sandstone gabbro gabbro gabbro gabbro sibrous siliceous basalite marble limestone and normal clastic rocks. The relationship between the rock blocks is unclear or is a fault contact, including radioworm relics, brachiopods and bivalve fossils, and its geological era is classified as Carboniferous-early Triassic.", "triple_list": [ [ "Tongtian River opal green mixed rock", "Exposed", "Xijin Wulan Lake-Tongtian River-Yushu" ], [ "Tongtian River opal green mixed rock", "Distribution pattern", "Belt or intermittent spread" ], [ "Tongtian River opal green mixed rock", "Lithology", "Slate" ], [ "Tongtian River opal green mixed rock", "Lithology", "Qianmeiyan" ], [ "Tongtian River opal green mixed rock", "Lithology", "Rock Schist" ], [ "Tongtian River opal green mixed rock", "Lithology", "Sandstone" ], [ "Tongtian River opal green mixed rock", "Lithology", "Gambling" ], [ "Tongtian River opal green mixed rock", "Lithology", "Glitter crystal rock" ], [ "Tongtian River opal green mixed rock", "Lithology", "Pillow-shaped basalt" ], [ "Tongtian River opal green mixed rock", "Lithology", "Silicone rock" ], [ "Tongtian River opal green mixed rock", "Lithology", "Dali Rock" ], [ "Tongtian River opal green mixed rock", "Lithology", "Limestone" ], [ "Tongtian River opal green mixed rock", "Lithology", "Clastite" ], [ "Tongtian River opal green mixed rock", "Paleontological", "Radioworm ruins, insects, brachiopods" ], [ "Tongtian River opal green mixed rock", "Paleontological", "Bivalves" ], [ "Tongtian River opal green mixed rock", "Age", "Carbonite-April Triassic" ] ] }, { "text": "Neoschwagerina douvilina Ozawa, Yabeina wangsiania is a standard molecule in the Middle Permian.", "triple_list": [ [ "Neoschwagerina douvilina Ozawa", "Age", "Middle Permian" ], [ "Yabeina wangsiania", "Age", "Middle Permian" ] ] }, { "text": "The measurement area is a mountainous area with high Elevation at mid-latitude, located in a high-Elevation, thin air, and a typical plateau continental climate with a variable climate, unknown seasons, long freezing period, the annual maximum temperature is 24, the lowest temperature is -30, and the temperature difference between day and night is large; there are many westerly winds from October to May of the following year, and there are many northerly winds from June to September.", "triple_list": [ [ "Test area", "Belongs to", "High-Elevation mountainous areas" ], [ "Test area", "Belongs to", "Typical plateau continental climate" ] ] }, { "text": "The test area era belongs to the early and middle Permian era.", "triple_list": [ [ "Test area", "Age", "Early and Middle Permian" ] ] }, { "text": "A set of clastic rock combinations in Nuoriba Garibao Group", "triple_list": [ [ "Nuoribagari protection group", "Lithology", "Clastic rock" ] ] }, { "text": "Gray medium-thick layered medium-fine grain quartz sandstone sandstone with grey-dark gray silty slate thickness 111.24m", "triple_list": [ [ "Gray medium-thick layered medium-fine grain quartz sandstone sandstone with grey-dark gray silty slab", "thickness", "111.24m" ] ] }, { "text": "In Jiang Rong saw a bauma sequence composed of particle sequence layer, horizontal stratigraphy and wrapping stratigraphy.", "triple_list": [ [ "Dang Jiang Rong", "Develop", "Granular Sequence Layer" ], [ "Dang Jiang Rong", "Develop", "Horizontal stratification" ], [ "Dang Jiang Rong", "Develop", "Cover lamination" ], [ "Dang Jiang Rong", "Contained", "Bauma Sequence" ] ] }, { "text": "The Kaixinling group exposed in the test area was only the upper Nuoribagaribao group and the Jiujidao team, and the lower Zharigen group did not show any exposure.", "triple_list": [ [ "Happy Ridge Group", "Outcrop", "Nuoribagari protection group" ], [ "Happy Ridge Group", "Outcrop", "Ninety teams" ], [ "Happy Ridge Group", "Outcrop", "Zharigen Group" ] ] }, { "text": "The average Elevation in Zhiduo County is mostly between 4600 and 5200m, and the relative height difference is large. The highest peak is located in the middle of the measurement area, with a maximum Elevation of 5876m.", "triple_list": [ [ "Zhiduo County", "Elevation", "4600-5200m" ], [ "The highest peak", "Located at", "Sell little sele" ], [ "The highest peak", "Elevation", "5876m" ] ] }, { "text": "The angle of the gray-green conglomerate is not integrated with the Nuoribagaribao group", "triple_list": [ [ "Gray green gravel rock", "Unconformity contact", "Nuoribagari protection group" ] ] }, { "text": "The lithology of the lower part is black cloud plagiaria gneiss containing pomegranates. The plagiaria gneiss containing diopterite. The plagiaria gneiss cordierite. The plagiaria gneiss striped dimica gneiss flanks gneiss flanks gneiss flanks gneiss flanks gneiss flanks and dark gray-green plagiaria gneiss; the main lithology of the upper part is gray-gray-green dimica quartz schist grey green angular mesquite schist quartz schist and gray-white flake calcite marble medium-gray marble, etc.", "triple_list": [ [ "Lower part", "Lithology", "Black clouds oblique gneis" ], [ "Lower part", "Lithology", "Pomegranate black cloud oblique length gneiss" ], [ "Lower part", "Lithology", "Ginsky with diopside mica" ], [ "Lower part", "Lithology", "Cordierite Mica Mesofeldspar Gins" ], [ "Lower part", "Lithology", "striped dimica feldsite gneis" ], [ "Lower part", "Lithology", "Off-white sugar-grained marble" ], [ "Lower part", "Lithology", "Dark gray-green oblique amphibolite" ], [ "Upper", "Lithology", "Gray-Grey-Grey-Grey-Grey-Grey-Grey-Micca Quartz Schist" ], [ "Upper", "Lithology", "Gray-green angular radicchi" ], [ "Upper", "Lithology", "Quartz schist" ], [ "Upper", "Lithology", "Off-white quartz rock" ], [ "Upper", "Lithology", "Off-white flake calcite marble" ], [ "Upper", "Lithology", "Medium marble" ] ] }, { "text": "In the early and middle Proterozoic Ningduo group, the area was in the Western Jinwulan tectonic mixed rock belt. Similar rocks were found in the Western Jinwulan Lake at the western end of the mixed belt and the Xiaosumang area of Yushuzhou, Qinghai Province. Most previous studies believed that it belonged to the Proterozoic territory.", "triple_list": [ [ "Early and Middle Proterozoic Ningduoqun", "Earth tectonic location", "Mixed rock belt in Xijin Wulan tectonic" ], [ "Early and Middle Proterozoic Ningduoqun", "Earth tectonic location", "Mixed Xijin Wulan Lake with the western end" ], [ "Early and Middle Proterozoic Ningduoqun", "Earth tectonic location", "Xiaosumang area, Yushuzhou, Qinghai Province" ], [ "Early and Middle Proterozoic Ningduoqun", "Belongs to", "Proterozoic" ] ] }, { "text": "Qinghai Provincial Geological Bureau (1991) used the Zaduo Group in the Qinghai Provincial Regional Geological Chronicle, and established the Oquga Group and the Charanning Group from the bottom up. However, these three groups have neither a profile basis nor a contact relationship, and the actual meaning is difficult to understand and apply.", "triple_list": [ [ "Miscellaneous groups", "Outcrop", "Narongpu Group" ], [ "Miscellaneous groups", "Outcrop", "Russian group" ], [ "Miscellaneous groups", "Outcrop", "Charanning Group" ] ] }, { "text": "The rocks in this section are designated by 1:200,000 zone adjustment data, and the results of this sheet identification are in brackets. The main body of the section is mylonite, and the Develop of rotary smear-like mylonide structure and other tough deformation characteristics.", "triple_list": [ [ "Mylonite", "Develop", "Myrgonal surface treatment of rotary splatter S-C composition" ] ] }, { "text": "The Zaduo group is in fault contact with the Gadikao Formation of the Permian Kaixinling Group, and is covered by the angle of the Paleo-Middle Tuotuohe Formation (Et) of the late Triassic ligation group.", "triple_list": [ [ "Miscellaneous groups", "Fault contact", "Permian Kaixinling Group Gadikao Group" ], [ "Miscellaneous groups", "Unconformity contact", "Late Triassic Ligation Group" ], [ "Miscellaneous groups", "Unconformity contact", "Jiapila Jurassic Yanshiping Group" ], [ "Miscellaneous groups", "Unconformity contact", "Tuotuohe Formation in the Paleo-Central" ] ] }, { "text": "Qinghai Provincial Regional Test Team (1970) classified the Lower Permian from bottom to top into the upper clastic rock formation and the volcanic rock formation in the lower clastic rock formation in a 1:1 million hot spring pattern.", "triple_list": [ [ "Lower Permian", "Outcrop", "Lower clastic rock formation" ], [ "Lower Permian", "Outcrop", "Limestone Formation" ], [ "Lower Permian", "Outcrop", "Upper clastic rock formation" ], [ "Lower Permian", "Outcrop", "Volcanic rock formation" ] ] }, { "text": "The geographical coordinates of the hot spring web start at 95°28′50 east longitude, 33°07′18 north latitude, and Elevation is 4888m; the end at 95°27′51 east longitude, 33°05′29 north latitude, and an elevation is 4790m.", "triple_list": [ [ "Hot spring web", "Coordinates", "95°28'50 East longitude" ], [ "Hot spring web", "Coordinates", "33°07'18 North latitude" ], [ "Hot spring web", "Elevation", "4888m" ], [ "Hot spring web", "Coordinates", "95°27'51 East longitude" ], [ "Hot spring web", "Coordinates", "33°05'29 North latitude" ], [ "Hot spring web", "Elevation", "4790m" ] ] }, { "text": "In the area of Chayong, only a small number of gray black clouds were found to be slanted gneiss distributed in the Late Triassic and Late Jurassic invasion rock mass.", "triple_list": [ [ "Check the rush", "Lithology", "Grey black clouds oblique gneis" ], [ "Grey black clouds oblique gneis", "Exposed", "Late Triassic" ], [ "Grey black clouds oblique gneis", "Exposed", "Late Jurassic invasion of rock bodies" ] ] }, { "text": "In 1980, the Qinghai Provincial Stratigraphy Preparation Team believed that the Tongtian River Group was composed of a medium-shallow metamorphic shallow marine-marine sedimentary clastic rocks and volcanic rocks, and the geological era was the Permian.", "triple_list": [ [ "Tongtianhe Group", "Lithology", "Clastite" ], [ "Tongtianhe Group", "Lithology", "Volcanic rocks" ], [ "Tongtianhe Group", "Age", "Permian" ] ] }, { "text": "Similar formations are also exposed along the Xijinwulan-Jinsha River suture belt to the northwest in the Saimaolakun area of Mingjing Lake. The lithology is mainly quartz schist, with black cloud slant gneiss and granular rocks. After comparing the 1:25 Wanke Xili Lake area adjustment report, it is classified as Ningduo Group.", "triple_list": [ [ "Xijin Wulan-Jinshajiang suture belt", "Lithology", "quartz schist" ], [ "Xijin Wulan-Jinshajiang suture belt", "Lithology", "Black clouds oblique gneis" ], [ "Xijin Wulan-Jinshajiang suture belt", "Lithology", "Granular rock" ], [ "Keke Xili Lake", "Belongs to", "Ningduoqun" ] ] }, { "text": "The early Carboniferous Clastogranular rock formation in this area is mainly composed of gray-dark gray-purple rock-cut feldspar sandstone feldspar quartz sandstone silt sandstone, and is sandwiched with carbonaceous slate limestone coal seams.", "triple_list": [ [ "Early Carboniferous Clastograft", "Lithology", "Gray - dark gray gray purple rock-cut feldspar sandstone" ], [ "Early Carboniferous Clastograft", "Lithology", "Feldspar quartz sandstone silt slab" ], [ "Early Carboniferous Clastograft", "Lithology", "Carbonite slate" ], [ "Early Carboniferous Clastograft", "Lithology", "Limestone" ] ] }, { "text": "The colorful opal green mixed rocks are in contact with each other in the tectonic interface of faults or tough shear zones, the north side is in contact with the tectonic interface of Triassic Chayong opal green mixed rocks (fault or strong-sliced physical and chemical belt), and the south side is in contact with the Batang Group fault of the late Triassic, spreading in the northwest-south eastward direction, and both ends extend out of the map area.", "triple_list": [ [ "Colorful opal green mixed rocks", "Fault contact", "Triassic checks on ophiolula mixed rock" ], [ "Colorful opal green mixed rocks", "Fault contact", "Batang Group of the Late Triassic World" ], [ "Colorful opal green mixed rocks", "Distribution pattern", "Northwest-South East-East" ] ] }, { "text": "Among them, the ophiolite components have not seen the complete stratigraphic sequence in the area, and they are all produced from tectonic blocks. For details, please refer to the Tongtianhe ophiolite part of Chapter 3, Section 1 of the report.", "triple_list": [ [ "Ophiolite Formation", "Distribution pattern", "Tectonic rock blocks" ] ] }, { "text": "Section a is 20-40cm thick, and is composed of grey-replacement medium-fine-grained feldspar quartz sandstone from bottom to top, and there is an incomplete heavy load mode at the bottom; section b is 10cm thick, and is horizontally laminated, composed of grey-replacement fine-grained feldspar quartz sandstone; section c is 15cm thick, composed of gray-replacement calcified silt sandstone, and develops wrapping lamination.", "triple_list": [ [ "Paragraph a", "thickness", "20-40cm" ], [ "Paragraph a", "Lithology", "Gray medium-fine-grained feldspar quartz sandstone" ], [ "Paragraph a", "Lithology", "Gray residual fine-grained feldspar quartz sandstone" ], [ "Section b", "thickness", "10cm" ], [ "Section b", "Develop", "Horizontal stratification" ], [ "Section b", "Lithology", "Gray remnant fine-grained feldspar" ], [ "Section b", "Lithology", "Chop sandstone" ], [ "Section c", "thickness", "15cm" ], [ "Section c", "Lithology", "Gray Calcium Siltstone" ], [ "Section c", "Develop", "Cover lamination" ] ] }, { "text": "This metamorphic rock system is compared with the above metamorphic rocks. The lithology is similar to that of the Ningduo group, so it is also classified as Ningduo group. Its era is temporarily classified as the Proterozoic. This work was obtained in the oblique long angle diazotite (VIII003P2JD6-4). The age of Sm-Nd isochronic pattern was 215661Ma, among which W (Sm) 10-64.45W (Nd) 10-613.71; 147Sm144Nd0.1963; 143Nd144Nd1б 0.5129030.000007, which should be the diagenetic age.", "triple_list": [ [ "Metamorphic rock system", "Belongs to", "Ningduoqun" ], [ "Metamorphic rock system", "Age", "Proterozoic" ] ] }, { "text": "In Buta Township, Dingqing County, Tibet, in the southern part of the project, the U-Pb zircon method 124524Ma isotope isotope isochronic crossing point age of the U-Pb zircon method 124524Ma isotope isotope isotope isochronic in the newly discovered metamorphic invasion group in the Proterozoic Jitang group of the Qiangtang continent block. The rock characteristics are also similar, and its era belongs to the Mesoproterozoic.", "triple_list": [ [ "Qiangtang land block Proterozoic Jitang Group", "Age", "Middle Proterozoic" ] ] }, { "text": "The newly discovered and established colorful opalgreen mixed rock (CPd) is distributed in the Tongtian River composite tectonic opalgreen mixed rock belt. It is a component of the Tongtian River opalgreen mixed rock established by the rock formations of Qinghai Province. It represents the material components of the upper western Jinwulan-Jinsha River Belt.", "triple_list": [ [ "Colorful opal green mixed rocks", "Earth tectonic location", "Tongtianhe composite structure ophiolula mixed rock belt" ], [ "Colorful opal green mixed rocks", "Belongs to", "Tongtian River opal green mixed rock" ], [ "Colorful opal green mixed rocks", "Earth tectonic location", "Xijinwulan-Jinshajiang River Belt" ] ] }, { "text": "The clastic rock formation of the Haddo group (C1Z1) was in integrated contact with the overlying carbonate salt formation (C1Z2), and in fault contact with the 90-way team (P2j) of the Noribagaribao group (P2nr) of the Kaixinling group of the Permian period, and in angle unconformity contact with the Jiapilatuotuohe Formation (Et) of the Late Triassic ligation group.", "triple_list": [ [ "Miscellaneous clastic rock formation", "Integration of contacts", "Carbonate salt formation" ], [ "Miscellaneous clastic rock formation", "Fault contact", "Permian Kaixinling Group Noribagari Bao Group" ], [ "Miscellaneous clastic rock formation", "Fault contact", "Ninety teams" ], [ "Miscellaneous clastic rock formation", "Unconformity contact", "Late Triassic Ligation Group Jiapilatuotuohe Formation" ] ] }, { "text": "A single-particle U-Pb zircon age of 70966Ma was obtained in black cloud slant gneiss (VIII003JD1858-7), reflecting the metamorphosis era of this set of strata in Jinning period.", "triple_list": [ [ "Black clouds oblique gneis", "Age", "Jinning period deterioration era" ] ] }, { "text": "In the Songmorong area, the rocks have relatively strong deformation, mainly mylonite mylonite.", "triple_list": [ [ "Matsumo Ryo", "Lithology", "Mylonite mylonite" ] ] }, { "text": "The contact between the faults of the Noribagaribao group and the lower Carboniferous Zaduo group was not bottomed out, and the angle of the Jiapila group was not integrated with the limestone of the overlying ninety teams was not integrated.", "triple_list": [ [ "Nuoribagari protection group", "Fault contact", "Carboniferous Miscellaneous Groups" ], [ "Nuoribagari protection group", "Integration of contacts", "Ninety teams of limestone" ], [ "Nuoribagari protection group", "Unconformity contact", "Ligation group Apira group" ] ] }, { "text": "The rock formation in Qinghai Province adopts the Liu Guangcai division plan, and defines the Miduo group as located on the northern slope of the Tanggula Mountain. The lower part is called the coal-containing clastic rock formation. It consists of lithotris sandstone siltstone carbogenic shale metamorphic clastic rock slate intersecting rocks and coal seams, and occasionally volcanic rocks; the upper part is called the carbonate rock formation, which consists of gray-dark gray limestone intersecting a little clastic rocks, containing brachiopod coral bryozo and plant fossils, which have not been seen, and is parallel and unconsistent with the overlying clastic rocks.", "triple_list": [ [ "Miscellaneous groups", "Exposed", "The northern slope of Tanggula Mountain" ], [ "Miscellaneous groups", "Outcrop", "Coal-containing clastic rock formation" ], [ "Miscellaneous groups", "Outcrop", "Carbonate Formation" ], [ "Coal-containing clastic rock formation", "Lithology", "Rock cuttings sandstone" ], [ "Coal-containing clastic rock formation", "Lithology", "Siltstone" ], [ "Coal-containing clastic rock formation", "Lithology", "Carbonaceous shale" ], [ "Coal-containing clastic rock formation", "Lithology", "Metamorphic clastic rock" ], [ "Coal-containing clastic rock formation", "Lithology", "Slate" ], [ "Coal-containing clastic rock formation", "Lithology", "Huiyan" ], [ "Coal-containing clastic rock formation", "Lithology", "Coal layer" ], [ "Coal-containing clastic rock formation", "Lithology", "Volcanic rocks" ], [ "Carbonate Formation", "Lithology", "Gray - dark grey limestone" ], [ "Carbonate Formation", "Lithology", "Clastite" ], [ "Carbonate Formation", "Paleontological", "Brachiopod coral mossworm" ], [ "Carbonate Formation", "Paleontological", "Plant fossils" ], [ "Carbonate Formation", "Integration of contacts", "Gamay Nong Group" ] ] }, { "text": "This section consists of regional dynamic thermal flow metamorphic rocks and mixed rocks such as black cloud plagiaria and pomegranate black cloud plagiaria plagiaria plagiaria schist chlorite quartz schist pyroxene granite and striped mixed rocks.", "triple_list": [ [ "profile", "Lithology", "Black clouds oblique gneis" ], [ "profile", "Lithology", "Pomegranate black cloud oblique length gneiss" ], [ "profile", "Lithology", "Eryun oblique length gneis" ], [ "profile", "Lithology", "Black cloud quartz schist" ], [ "profile", "Lithology", "quartz schist" ], [ "profile", "Lithology", "Chlorite quartz schist" ], [ "profile", "Lithology", "Pyroxene Granular Rock" ], [ "profile", "Lithology", "Striped stripe-like mixed rock" ], [ "profile", "Lithology", "Metamorphic rock" ], [ "profile", "Lithology", "Mixed rock" ] ] }, { "text": "The actual measured profile of Niechaqu, Duocai Township, Zhiduo County, Qinghai Province (Figure 2-9). The geographical location of this profile starts at 95°28′17 east longitude, 33°46′05 north latitude, and Elevation is 4307m; the end point is 95°28′56 east longitude, 33°47′32 north latitude, and an elevation is 4268m.", "triple_list": [ [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "95°28'17 East longitude" ], [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "33°46′05 North latitude" ], [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Elevation", "4307m" ], [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "95°28'56 East longitude" ], [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Coordinates", "33°47′32 North latitude" ], [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Elevation", "4268m" ] ] }, { "text": "Zhiduo County Bendu District is located in Zaduo County, the source area of Lancang River and Zhiduo County, the first county in the Yangtze River. It belongs to the eastern extension of the Tanggula Mountain. It has snow-capped mountains all year round. The natural landform barrier forms the dividing line between Qinghai and Tibet. There are county-level highways and simple township-level highways in the district. Most areas have high mountains, valleys, deep rivers, lakes and marshes, and some seasonal walkways can only be transported by cartons and horses, which is extremely inconvenient for transportation.", "triple_list": [ [ "Zhiduo County", "Located at", "Zaduo County, Lancang River Source District" ], [ "Zhiduo County", "Located at", "Zhiduo County" ] ] }, { "text": "The black cloud plagiarite gneis rock has a semi-automorphic scale-grained crystal structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a main mineral plagiarite 28-47, mica 14-32, quartz 25-57, and some rocks Contained a small amount of garnet, cordierite, chlorite, chlorite and diopsides of about 8 diopsides, etc., and the silicon-line pyrolithic stone is a plagiarite-shaped scale-grained crystal structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure, a flaky scalyptus-shaped structure", "triple_list": [ [ "Black clouds oblique gneis", "Distribution pattern", "Semi-automorphic scale granular crystal structure" ], [ "Black clouds oblique gneis", "Distribution pattern", "Throat" ], [ "Silicon-line red columnar mica plagiarum gneis", "Distribution pattern", "Micro-grained semi-automorphic scales granular crystal structure" ], [ "Silicon-line red columnar mica plagiarum gneis", "Distribution pattern", "Throat" ] ] }, { "text": "The coarse grains of diopylate rock have a granular metacrystalline structure and a stripe-like structure. The main mineral components are diopylate 59, potassium feldspar 25, calcite 10, and a small amount of garnet.", "triple_list": [ [ "Diopylate", "Develop", "Striped structure" ] ] }, { "text": "The Noribagaribao Group in the district is mainly distributed in the Dongjiaoyong-Dongmoyong Zhaqingxiang area south of Narigongma-Ziqu. The distribution area is 2200m2, and the maximum thickness is controlled to be 1947.40m.", "triple_list": [ [ "Nuoribagari protection group", "Exposed", "The area of Dongjiaoyong-Dongmoyong Zhaqingxiang, south of Ziqu" ], [ "Nuoribagari protection group", "area", "2200m2" ], [ "Nuoribagari protection group", "thickness", "1947.40m" ] ] }, { "text": "Gray thin - Medium-layer fine-grained feldquartz sandstone sandstone with dark gray - Medium-layer silty slate 25.12m", "triple_list": [ [ "Thin gray - Medium-layer fine-grained feldquartz sandstone with dark gray - Medium-layer silty slab", "thickness", "25.12m" ] ] }, { "text": "The geographical coordinates of the profile start at 95°07′03, latitude 33°15′30, and the elevation is 4608m; the end at 95°06′07, latitude 33°14′15, and the elevation is 4463m.", "triple_list": [ [ "profile", "Coordinates", "95°07'03 East longitude" ], [ "profile", "Coordinates", "33°15'30 North latitude" ], [ "profile", "Elevation", "4608m" ], [ "profile", "Coordinates", "95°06'07 East longitude" ], [ "profile", "Coordinates", "33°14′15 North latitude" ], [ "profile", "Elevation", "4463m" ] ] }, { "text": "The fine-grained elongated pyroschist is semi-self-shaped column-grained metamorphic structure, strip-shaped, and flaky structure. The main minerals are plagioclase 40-47, amphibole 48-58, some rocks Contained mica 5, monoclinic pyroxene 6, quartz 5, and a small amount of potassium feldspar. The angular pyroxene rock has a medium-fine semi-self-shaped-grained metamorphic structure, with a flaky structure. The main mineral components are plagioclase 91-99, plagioclase 1-8, and some rocks Contained mica and a small amount of spinel.", "triple_list": [ [ "Fine-grained semi-self-shaped column-like metamorphic structure of oblique long angle flashesch", "Distribution pattern", "Strip shape" ], [ "Fine-grained semi-self-shaped column-like metamorphic structure of oblique long angle flashesch", "Distribution pattern", "Flake-like" ], [ "horned schist rock", "Distribution pattern", "Medium fine grain semi-self-forming-self-forming granular crystal structure" ], [ "horned schist rock", "Distribution pattern", "Flake-like" ] ] }, { "text": "This strata is a newly discovered and established tectonic rock formation unit in this district adjustment work. The 1:2000 Wanzhiduo County area area adjustment will be divided into the late Triassic Batang Group (3Bt).", "triple_list": [ [ "Zhiduo County", "Outcrop", "Batang Group of the Late Triassic World" ] ] }, { "text": "In 1959, the South-to-North Water Diversion Expedition Team of the Chinese Academy of Sciences named the metamorphic rock system on both sides of the Tongtian River as the Tongtian River Group, and the era was classified as the Paleozoic.", "triple_list": [ [ "Tongtianhe Group", "Age", "Paleozoic" ] ] }, { "text": "The 1:200,000-area data of this strata are classified into the Triassic Bayankala Mountains. The rock combination is composed of gray-thick-block layered limestone, and there are few biological fossils in the rock layer.", "triple_list": [ [ "This strata", "Belongs to", "The Triassic Bayankara Mountains" ], [ "This strata", "Lithology", "Gray thick-block layered limestone" ] ] }, { "text": "Therefore, this strata is classified as the Early and Middle Permian.", "triple_list": [ [ "Strata", "Age", "Early and Middle Permian" ] ] }, { "text": "The ancient protozoa strata of Ningduoyan Group Measurement Area of the ancient protozoa is a newly discovered rock strata unit in this work. It is only found in the area of Riariqu, southwest of Zhiduo County. The data of the previous generation belongs to the Batang Group of the Late Triassic Period (3Bt).", "triple_list": [ [ "Ningduoyan Group in the Proterozoic Period", "Exposed", "Zhiduo County Southwest Chaqu Ria Riqu" ], [ "Ningduoyan Group in the Proterozoic Period", "Belongs to", "Batang Group of the Late Triassic World" ] ] }, { "text": "In the ancient Proterozoic Ningbo rock group, the lithologic nature of medium-thick layered lithotrix feldstone sandstone silt sandstone slate sandstone limestone and coal line routes were obtained on the 1:200, Wanzaduo County area.", "triple_list": [ [ "Ningduoyan Group in the Proterozoic Period", "Lithology", "Medium-thick layered rock" ], [ "Ningduoyan Group in the Proterozoic Period", "Lithology", "Chissite sandstone" ], [ "Ningduoyan Group in the Proterozoic Period", "Lithology", "Siltstone" ], [ "Ningduoyan Group in the Proterozoic Period", "Lithology", "Slate sandstone" ], [ "Ningduoyan Group in the Proterozoic Period", "Lithology", "Limestone" ], [ "Zaduo County", "Paleontological", "Early Carboniferous" ], [ "Zaduo County", "Paleontological", "Bivalve fossil" ] ] }, { "text": "This strata is mainly exposed in the Niechaqu area, and the rock types are also relatively complex, mainly a rock combination of gneiss schist quartzite and marble.", "triple_list": [ [ "This strata", "Exposed", "Nie Chaqu" ], [ "This strata", "Lithology", "Gneis" ], [ "This strata", "Lithology", "Rock Schist" ], [ "This strata", "Lithology", "Quartzite" ], [ "This strata", "Lithology", "Dali Rock" ] ] }, { "text": "Zhiduo County Bend Survey Area is located in the hinterland of the Qinghai-Tibet Plateau. The Tanggula Mountain runs across the entire area. The mountains are steep and the valleys are crisscrossing. The snow-capped mountains in the middle and south of the Tu District are towering all year round. Most of them are continuous and steep peaks, and few sedimentary basins with wide and shallow river valleys.", "triple_list": [ [ "Zhiduo County area survey area", "Located at", "Qinghai-Tibet Plateau" ], [ "Zhiduo County area survey area", "Located at", "Tanggula Mountain" ] ] }, { "text": "Early and Middle Permian strata ㈠ Colorful opale green mixed rock (CPd) This tectonic rock formation unit is an informal tectonic rock formation unit newly discovered and established in this work, mainly distributed in the colorful township - the middle tour of Niechaqu - Dangjiang Township and other places.", "triple_list": [ [ "Colorful opal green mixed rocks", "Exposed", "Colorful Township - Nie Chaqu Middle Tour - Dangjiang Township" ] ] }, { "text": "The Kaixinling group is rich in fossils such as brachiopods and corals, and has not seen the bottom boundary. It is bounded by the top level of the limestone in the upper part of this group as the boundary and the integrated contact with the coal-containing clastic rock of the overlying Wuli Group or parallel to the ligation group.", "triple_list": [ [ "Happy Ridge Group", "Paleontological", "Brachiopod" ], [ "Happy Ridge Group", "Paleontological", "coral" ], [ "Limestone", "Integration of contacts", "Wuliqun coal-containing clastic rock" ], [ "Limestone", "Integration of contacts", "Ligation group" ] ] }, { "text": "Dark gray silty mud slate with dark gray calcareous slate (anticline structure) thickness 306.12m", "triple_list": [ [ "Dark gray silty mud slate with dark gray calcified slate", "thickness", "306.12m" ] ] }, { "text": "The clastic rock formation is in tectonic contact with other stratigraphic units, and there is an unconsolidation of the Paleo-Neocentric Tuohe Formation.", "triple_list": [ [ "Clastic rock formation", "Unconformity contact", "Ancient and Neo-Tuotuohe Formation" ] ] }, { "text": "In 1988, Liu Guangcai analyzed the rock characteristics of each rock formation and the total appearance of the fossils contained in each rock formation and the contact relationship between each rock formation, and divided the mixed groups into two rock formations, namely the (lower) coal-containing clastic rock formation and the (upper) carbonate rock formation.", "triple_list": [ [ "Miscellaneous groups", "Outcrop", "Coal-containing clastic rock formation" ], [ "Miscellaneous groups", "Outcrop", "Carbonate rock formation" ] ] }, { "text": "The semi-automorphic scale grainy metamorphic structure of quartz schist is flaky, with mineral components quartz 60-91, plagioclase 2-7, mica 7-11, and mica 0-22.", "triple_list": [ [ "quartz schist", "Distribution pattern", "Semi-automorphic scale granular crystal structure" ], [ "quartz schist", "Distribution pattern", "Flake-like" ] ] }, { "text": "Gray medium-layered medium-grained rock-cut feldspar sandstone sandstone with gray medium-thin layered fine grained quartz sandstone and dark gray thin-layered silt sandstone 198.67m", "triple_list": [ [ "Gray medium-layered medium-grained rock-cut feldspar sandstone with gray medium-thin-thin layered fine grains and dark gray thin-layered silt sandstone", "thickness", "198.67m" ] ] }, { "text": "The Zaduo County area includes the lower clastic rock formation, the lower carbonate rock formation, the upper coal-containing clastic rock formation and the upper carbonate rock formation.", "triple_list": [ [ "Zaduo County", "Outcrop", "Clastic rock formation" ], [ "Zaduo County", "Outcrop", "Carbonate Formation" ], [ "Zaduo County", "Outcrop", "Coal-containing clastic rock formation" ], [ "Zaduo County", "Outcrop", "Carbonate Formation" ] ] }, { "text": "Late Carboniferous Strata 1:200. Wanzaduo County area is divided into the northern area of Jieduo Township, Zaduo County. There are very few late Carboniferous Gamay Nong Group. This work has obtained many early and middle Permian fossils in this strata and are classified as the Permian Kaixinling Group, so it has not been exposed.", "triple_list": [ [ "Zaduo County", "Outcrop", "Late Carboniferous Family Gamay Nong Group" ], [ "Permian fossils", "Belongs to", "Permian Happy Ridge Group" ] ] }, { "text": "Dark gray silty slate fault Obada limestone (P1-2ca)", "triple_list": [ [ "Dark gray silty slab", "Fault contact", "Obada Limestone" ] ] }, { "text": "Gray thick-block layered crystalline limestone thickness 537.36m", "triple_list": [ [ "Gray thick-block layered crystalline limestone", "thickness", "537.36m" ] ] }, { "text": "This district adjustment work disintegrates some of the strata of the original late Triassic Batang group in the survey area into colorful opalene mixed rocks, and further divides them into four informal map-filling units, colorful opalene (CPdop), dragon sandstone (CPdop), Dangjiangrong volcanic rock (CPdva), and Obada limestone (P1-2ca).", "triple_list": [ [ "Batang Group of the Late Triassic World", "Lithology", "Colorful opal green mixed rocks" ], [ "Batang Group of the Late Triassic World", "Lithology", "Colorful ophiolite" ], [ "Batang Group of the Late Triassic World", "Lithology", "Chelong Sandstone" ], [ "Batang Group of the Late Triassic World", "Lithology", "Obada Limestone" ] ] }, { "text": "The rocks in the Songmorong area on the south side of Dangjiang Township are mainly gray mylonized feldspar quartz sandstone feldspar sandstone feldspar silt sandstone silt sandy slate with gray-green medium-acid volcanic limestone lenses in the weak deformation zone. They are all mylonite tectonic schist in the strong deformation zone, and are distributed in the Dangjiangrong volcanic rocks in the contact with the ductile shear zone.", "triple_list": [ [ "Song Morong, south of Dangjiang Township", "Lithology", "Gray mylonite feldspar quartz sandstone" ], [ "Song Morong, south of Dangjiang Township", "Lithology", "Feldspar rock" ], [ "Song Morong, south of Dangjiang Township", "Lithology", "Chop sandstone" ], [ "Song Morong, south of Dangjiang Township", "Lithology", "Silty slate with gray-green medium acidic volcanic rock" ], [ "Song Morong, south of Dangjiang Township", "Lithology", "Limestone" ], [ "Mylonite tectonic schist", "Distribution pattern", "Tough shear belt" ], [ "Mylonite tectonic schist", "Integration of contacts", "Dangjiangrong Volcanic Rock" ] ] }, { "text": "Ninety-Dao Team Light gray thick-block layered limestone Integrated Nuoribagaribao Group Thickness 498.88m", "triple_list": [ [ "Ninety teams", "Lithology", "Light gray thick-block layered limestone" ], [ "Ninety teams light gray thick - layered limestone", "Integration of contacts", "Nuoribagari protection group" ], [ "Nuoribagari protection group", "thickness", "498.88m" ] ] }, { "text": "Gray-brown medium-layered calcareous cemented medium-fine-grained rock-cut feldspar sandstone sandstone with gray-brown thin-medium-layered mud calcium silty sandstone 144.21m", "triple_list": [ [ "Gray-brown medium-layered calcareous cemented medium-fine-grained rock-cut feldspar sandstone with gray-brown thin-medium-layered mud calcareous silt sandstone", "thickness", "144.21m" ] ] }, { "text": "The lateral lithology of the Noribagaribao Formation in this area does not change much. The spatially bounded by the fault is fault blocks and is produced in the fault zone. Its overall shows a monoclinic structure that is tilted southward from northwest to southward. Its lithological components are gray medium-grained lithostone, gray medium-fine feldspar quartz sandstone, gray black thin-layer fine sandy complex mineral silt sandstone gray black silt silt silt silt sandstone, and gray thick-layered mud crystal bioclass lithostone intersected with gray-green altered basalt Ying'anite tuff lava.", "triple_list": [ [ "Nuoribagari protection group", "Distribution pattern", "Faulted block" ], [ "Nuoribagari protection group", "Distribution pattern", "Northwest-South east-to-south" ], [ "Nuoribagari protection group", "Lithology", "Gray medium-grained sandstone" ], [ "Nuoribagari protection group", "Lithology", "Gray medium-fine-grained feldspar quartz sandstone" ], [ "Nuoribagari protection group", "Lithology", "Gray-black thin layered fine sandy complex mineral silt sandstone" ], [ "Nuoribagari protection group", "Lithology", "Gray black silty slab" ], [ "Nuoribagari protection group", "Lithology", "Gray fine gravel" ], [ "Nuoribagari protection group", "Lithology", "Gray thick layered mud crystal bioclass limestone" ], [ "Nuoribagari protection group", "Lithology", "Gray-green altered basalt" ], [ "Nuoribagari protection group", "Lithology", "Ying'an Rock" ], [ "Nuoribagari protection group", "Lithology", "Tuff lava" ] ] }, { "text": "In 1989, the Qinghai Provincial and Regional Comprehensive Geological Brigade divided the Kaixinling Group from bottom to top into the lower carbonate rock formation and the upper carbonate rock formation in the 1:20 Wantuotuohe band Zhanggang Risong Siemens.", "triple_list": [ [ "Tuotuo River Strip Zhanggang Sun Pine", "Outcrop", "Happy Ridge Group" ], [ "Happy Ridge Group", "Outcrop", "Lower carbonate rock formation" ], [ "Happy Ridge Group", "Outcrop", "Clastic rock formation" ], [ "Happy Ridge Group", "Outcrop", "Upper carbonate rock formation" ] ] }, { "text": "The particle size of the rock from south to north becomes coarse, and conglomerate interlayers appear. The limestone is mostly limestone with breccia-like structures or biological clastic limestone.", "triple_list": [ [ "rock", "Lithology", "Conglomerate interlayer" ], [ "Limestone", "Lithology", "Breccia-like limestone" ], [ "Limestone", "Lithology", "Bioclastic limestone" ] ] }, { "text": "Dimica schist semi-self-shaped grain-scale crystalline structure, flake-like structure, mineral composition, black mica 35-38.", "triple_list": [ [ "Dimica schist", "Distribution pattern", "Semi-self-shaped granular-scale crystal structure" ], [ "Dimica schist", "Develop", "Flake-like structure" ], [ "Dimica schist", "Contained", "Black Mouse" ] ] }, { "text": "The Carboniferous-Permian Kaixinling Group (CPK) was created by Team 632 of Qinghai Provincial Petroleum Bureau (1957) in Kaixinling, Tanggula Mountain. It originally refers to the light gray dense block limestone on the upper part, the black gray sandstone shale in the middle, with thin layers of conglomerate and muddy sandstone in the lower part, and the black gray thick layer and gray-white thin layer-thick layer of dense shale, rich in flies and fossil traces. The bottom is a green sandstone with gray black shale and a coal seam of up to 1m thick.", "triple_list": [ [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Light gray dense blocky limestone" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Black-gray sandstone shale" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Thin layer of gravel" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Mud sandstone" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Black and gray thick layer and off-white thin layer - thick layer of dense shale" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Cyan sandstone" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Grey-black shale" ], [ "Carboniferous period - Permian Kaixin Ridge Group", "Lithology", "Coal layer" ] ] }, { "text": "According to the above-mentioned cross-section and route data analysis, the maximum thickness is 787.22m.", "triple_list": [ [ "profile", "thickness", "787.22m" ] ] }, { "text": "The measured geological tectonic profile of Chayong ophiolite in Duocai Township, Zhiduo County, Qinghai Province Ⅷ003P9.", "triple_list": [ [ "Zhiduo County Duocai Township, Qinghai Province", "Lithology", "Chayong ophiolula mixed rock" ] ] }, { "text": "The opalae mixed rock era was the early Carboniferous era.", "triple_list": [ [ "Ophiolulu mixed rock", "Age", "Early Carboniferous" ] ] }, { "text": "Ophthalmospheric strip-like neutral volcanic mylonite pellet-like structure, the matrix is a scale-grained metacrystalline structure, and an ophthalmospheric strip-like structure.", "triple_list": [ [ "Ocular band-like neutral volcanic mylonite", "Distribution pattern", "Scale grainy metamorphic structure" ], [ "Ocular band-like neutral volcanic mylonite", "Develop", "Eyeball strip-like structure" ] ] }, { "text": "Dark gray silty mud slate with dark gray medium-thick layered fine-grained rock thickness 231.22m", "triple_list": [ [ "Dark gray silty mud slate with dark gray medium-thick layered fine-grained rock", "thickness", "231.22m" ] ] }, { "text": "The Kaixinling group and the Carboniferous Miscellaneous groups were in fault contact. Within a small area of the area around Zhaqing Beiranzheyong, it was covered by the angle of the late Permian Early Triassic Volcanic Formation established by this work. The angle of the Tuotuohe Formation in the Paleogene Triassic ligation group is not integrated.", "triple_list": [ [ "Happy Ridge Group", "Fault contact", "Carboniferous Miscellaneous Groups" ], [ "Happy Ridge Group", "Unconformity contact", "Late Permian Early Triassic Volcanic Rock Formation" ], [ "Happy Ridge Group", "Unconformity contact", "The late Triassic ligation group was erected in the ancient Tuotuohe Formation" ] ] }, { "text": "The Tibetan District Transfer Team (1:200,000 Deng Kefang District Transfer Report) obtained U-Pb method isotope age measurement data, with the metamorphic age of 1680390Ma1870280Ma1780150Ma, that is, the first metamorphic period may be the Luliang movement at the end of the Paleoproterozoic, and it was therefore determined that it was formed in the Paleoproterozoic.", "triple_list": [ [ "Deng Keteng", "Age", "Ancient Proterozoic" ] ] }, { "text": "The strata are mainly distributed in the area of Zhageyongqu, Diyakandoga Qingma Zageyongqu in the south and west corner of the Ma area. It is exposed in the Beiziqu area of Jieduo Township. It is a fault block produced in the fault zone with a distribution area of 200m2.", "triple_list": [ [ "Strata", "Exposed", "Land, Kandoga Qingma Zageyong Qu" ], [ "Strata", "Exposed", "Jieduo Township Beiziqu" ], [ "Strata", "Distribution pattern", "Faulted block" ], [ "Strata", "area", "200m2" ] ] }, { "text": "The measured area belongs to the alpine cold area of the Qinghai-Tibet Plateau. The soil type is mainly alpine desert soil, mostly herbs, and the grass cover rate accounts for 30-80. Some areas have abundant water and grass.", "triple_list": [ [ "Test area", "Belongs to", "The Qinghai-Tibet Plateau Alpine Area" ] ] }, { "text": "Gray thin-medium-layered medium-grained rock-cut sandstone sandstone with dark gray thin-layered silt sandstone thickness 1947.40m", "triple_list": [ [ "Gray thin-medium-layered medium-grained rock-cut sandstone sandstone with dark gray thin-layered siltstone", "thickness", "1947.40m" ] ] }, { "text": "The rock types of this formation are also relatively complex. The following sections are mainly gneiss, and the upper section is schist and quartzite, which are distributed in the opal green mixed zone of Tongtian River.", "triple_list": [ [ "This strata", "Lithology", "Gneis" ], [ "This strata", "Lithology", "Rock Schist" ], [ "This strata", "Lithology", "Quartzite" ], [ "This strata", "Distribution pattern", "Constructed block" ], [ "This strata", "Earth tectonic location", "Tongtian River opal green mixed belt" ] ] }, { "text": "The strata from old to new have the ancient protoproterozoic Ningdoyan group (Pt1-2N); the early Carboniferous Aduo group (C1Z) and the late Carboniferous Gamayong group (C2J); the middle Permian Kaixinling group Noribagaribao group (P2nr) ninety-way team ( P2j); Gadikao Formation in the Early and Middle Permian Permian (P1-2gd); Late Permian Early and Triassic Volcanic Formation (P31h); Carboniferous-Permian Colorful Ophiogenic Mixed Rock (CPd) Triassic Chayong Ophiogenic Mixed Rock (Ch); Early and Middle Triassic Jilong Formation (1-2j); Middle and Late Triassic Bayan Kala Mountain Formation (B) Late Triassic Batang Formation (3Bt) and Ligation Group Jiapila Formation (3jp) Poli La Formation (3b) Bagong Formation (3bg); Jurassic Yanshiping Group Qumocuo Formation (Jq), Buqu Formation (Jb) Xiali Formation (Jx); Paleocene-Oligocene Tuotuohe Formation (Et), Oligocene-Midocene Chabaoma Formation (ENc), Eocene-Midocene Yaxicuo Formation (ENy) and Miocene Wudaoliang Formation (Nw), Pleistocene Quguo Formation (Nq), etc., as well as Quaternary strata of various causes.", "triple_list": [ [ "Strata", "Outcrop", "Ningduoyan Group in the Proterozoic Period" ], [ "Strata", "Outcrop", "Early Carboniferous Worlds" ], [ "Strata", "Outcrop", "Late Carboniferous Family Gamay Nong Group" ], [ "Strata", "Outcrop", "The Kaixinling Group of the Middle Permian Noribagari Bao Group" ], [ "Strata", "Outcrop", "Ninety teams" ], [ "Strata", "Outcrop", "Early and Middle-aged Permian Gadikao Group" ], [ "Strata", "Outcrop", "Late Permian Early Triassic Volcanic Rock Formation" ], [ "Strata", "Outcrop", "Carboniferous-Permian colorful opalene mixed rocks" ], [ "Strata", "Outcrop", "Triassic checks on ophiolula mixed rock" ], [ "Strata", "Outcrop", "The Triassic Triassic Jilong Formation" ], [ "Strata", "Outcrop", "Bayan Kala Mountains in the Mid-End Triassic" ], [ "Strata", "Outcrop", "Batang Group of the Late Triassic World" ], [ "Strata", "Outcrop", "Ligation group Apira group" ], [ "Strata", "Outcrop", "Polira group" ], [ "Strata", "Outcrop", "Bagong Group" ], [ "Strata", "Outcrop", "Jurassic Yanshiping Group of Birds Moduo Group" ], [ "Strata", "Outcrop", "Button group" ], [ "Strata", "Outcrop", "Xiali Group" ], [ "Strata", "Outcrop", "The Paleoplecent-Oligocene Tuotuohe Formation" ], [ "Strata", "Outcrop", "Oligocene-Middle Chopoma Group" ], [ "Strata", "Outcrop", "Eocene-Middle Eocene Yaxicuo Group" ], [ "Strata", "Outcrop", "Mid-Episode Five Daoliang Formation" ], [ "Strata", "Outcrop", "Pliocene orchid group" ], [ "Strata", "Outcrop", "The Fourth Age" ] ] }, { "text": "Gray yellow medium-thick layered silty-containing microcrystalline limestone with blue-gray medium-layered silty-silty shiny sand-clay limestone 21.33m", "triple_list": [ [ "Gray-yellow Medium-thick layered silty-containing microcrystalline limestone with blue-gray medium-layered silty-containing shiny sand-clay limestone", "thickness", "21.33m" ] ] }, { "text": "The main body of the sedimentary strata is the Triassic strata, accounting for about 80% of the strata in the measured area.", "triple_list": [ [ "Sedimentary strata", "Belongs to", "Triassic strata" ] ] }, { "text": "The formation is distributed in tectonic blocks along the northwest-southeast tectonic line in the Carboniferous-Permian colorful opalgreen mixed zone. The exposed area is very small, less than 5m2, and the maximum control thickness is greater than 1039.52m.", "triple_list": [ [ "Strata", "Distribution pattern", "Constructed block" ], [ "Strata", "Earth tectonic location", "Carboniferous-Permian colorful opalgreen mixed belt" ], [ "Strata", "area", "5m2" ], [ "Strata", "thickness", "1039.52m" ] ] }, { "text": "Fossils such as corals produced in the Carbonate Rock Formation in the Early Carboniferous Apora sp.Diphyphyllum.", "triple_list": [ [ "Early Carbonate Group Carbonate Group", "Paleontological", "Coral Syringopora sp.Diphyphyllum" ] ] }, { "text": "Gray medium-layered limestone sandstone and gray medium-layered marlstone, producing insecticidal Reichelinasp; foraminifer Pachyphloiasp., Brachipods Spirifer sp., Crurithyris, Dielasmasp._Line newlines_", "triple_list": [ [ "Gray medium-layered limestone with dark gray thin layered siltstone and gray medium-layered marlstone", "Paleontological", "Reichelinasp" ], [ "Gray medium-layered limestone with dark gray thin layered siltstone and gray medium-layered marlstone", "Paleontological", "Foraminifera Pachyphloiasp." ], [ "Gray medium-layered limestone with dark gray thin layered siltstone and gray medium-layered marlstone", "Paleontological", "Brachiopod Spirifer sp." ], [ "Gray medium-layered limestone with dark gray thin layered siltstone and gray medium-layered marlstone", "Paleontological", "Crurithyris" ], [ "Gray medium-layered limestone with dark gray thin layered siltstone and gray medium-layered marlstone", "Paleontological", "Dielasmasp." ] ] }, { "text": "Among them, the colorful opale green mixed rocks, the late Permian-early Triassic volcanic rock formation contacts the Kaixinling group formation in the early and middle Permian by angle disorganization, which is an important geological achievement determined by the new discovery of this work.", "triple_list": [ [ "Colorful opal green mixed rocks", "Unconformity contact", "Happy Ridge Group in the Permian" ], [ "Late Permian-early Triassic Volcanic Formation", "Unconformity contact", "Happy Ridge Group in the Permian" ] ] }, { "text": "The clastic rock formation (C1Z1) is distributed in the area of Zhageyongqu, Diyakandoga Qingma Zageyongqu in the south and west corner of the map area.", "triple_list": [ [ "Clastic rock formation", "Exposed", "Land, Kandoga Qingma Zageyong Qu" ] ] }, { "text": "The actual measured geological profile of Noribagaribao Group and Jiujidao Team in Jiezha Township, Zaduo County, Qinghai Province was Ⅷ003P7 (Figure 2-13).", "triple_list": [ [ "Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Permian Noribagaribao Group" ], [ "Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Ninety teams" ] ] }, { "text": "The group consists of the old and the newest team including the Noribagari protection group of the Zharigen Group and the Ninety-Da team.", "triple_list": [ [ "This group", "Outcrop", "Zharigen Group" ], [ "This group", "Outcrop", "Nuoribagari protection group" ], [ "This group", "Outcrop", "Ninety teams" ] ] }, { "text": "The early Carboniferous Ages Belongs to to the Tanggula-Chambo stratigraphic division.", "triple_list": [ [ "Early Carboniferous Worlds", "Stratigraphical zoning", "Tanggula-Chambo stratigraphic division" ] ] }, { "text": "Tuff is mainly crystalline tuff, and glicillary tuff appears locally.", "triple_list": [ [ "Tuff", "Lithology", "Crystal tuff" ], [ "Tuff", "Lithology", "Glassic tuff" ] ] }, { "text": "Dark gray fragmented silty slate with gray fragmented thin-medium layered fine-grained feldquartz sandstone faults Early Carboniferous group of gray thick layered limestone", "triple_list": [ [ "Dark gray crushed silty slate with gray crushed thin-medium layered fine-grained feld quartz sandstone", "Fault contact", "Early Carboniferous Groups of Grey Thick Laminated Limestone" ] ] }, { "text": "Gray medium-layer fine-grained feldquartz sandstone sandstone with dark gray thin-layered silty slate 11.22m", "triple_list": [ [ "Gray medium-layered fine-grained feldquartz sandstone with dark gray thin-layered silty slab", "thickness", "11.22m" ] ] }, { "text": "Gray thin-layered silt mud slate sand-containing coal seam produces plant fragments", "triple_list": [ [ "Gray thin layered silt mud slate coal layer", "Paleontological", "Plant fragments" ] ] }, { "text": "The Permian strata in the Tanggula area of Qinghai Province are rich in paleontological fossils, mainly including worm-like brachiopod coral plant fossils.", "triple_list": [ [ "Tanggula area of Qinghai Province", "Outcrop", "Permian strata" ], [ "Permian strata", "Paleontological", "insects" ], [ "Permian strata", "Paleontological", "Brachiopod" ], [ "Permian strata", "Paleontological", "Coral plant fossils" ] ] }, { "text": "The original rock face is retained in the local weak deformation zone. When the area on the north side of Jiangrong is composed of gray two-cloud tectonic schist mylonite, the original rock is sandstone slate, and residual sedimentary structures such as particle sequence layer and horizontal stratigraphic and rolled stratigraphic are seen in the weak deformation zone, and colorful ophiolite tectonic rocks form a colorful ophiolite mixed rock (Figure 26).", "triple_list": [ [ "Dangjiangrong North Side", "Lithology", "Gray two-cloud tectonic schist mylonite" ], [ "Gray two-cloud tectonic schist mylonite", "Belongs to", "Sandstone slate" ] ] }, { "text": "The Permian strata in the area are distributed in the Western Jinwulan-Jinshajiang strata and the Tanggula-Changdu strata zone south of it.", "triple_list": [ [ "Permian strata", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ], [ "Permian strata", "Stratigraphical zoning", "Tanggula-Chambo stratigraphic division" ] ] }, { "text": "Andesite rocks are gray-green, with a doxoplasmic structure that changes to interwoven structures and sheet-like structures.", "triple_list": [ [ "Andesanite rocks", "Distribution pattern", "Spot-like structure" ], [ "Andesanite rocks", "Distribution pattern", "Variable interwoven structure" ], [ "Andesanite rocks", "Develop", "Flake-like structure" ] ] }, { "text": "Dark gray medium-thin layered argillic quartz silt sandstone with fine-grained feldspar quartz sandstone. Fossil production Cardium (ulongocardium) cf.submartini J.ChenUnionites Emeinsis Chen et Zhang 421.26m", "triple_list": [ [ "Dark gray medium-thin layered arable quartz silt sandstone with fine-grained feldspar quartz sandstone", "Paleontological", "Cardium (ulongocardium) cf." ], [ "Dark gray medium-thin layered arable quartz silt sandstone with fine-grained feldspar quartz sandstone", "Paleontological", "submartini J." ], [ "Dark gray medium-thin layered arable quartz silt sandstone with fine-grained feldspar quartz sandstone", "Paleontological", "ChenUnionites Emeinsis Chen et Zhang" ], [ "Dark gray medium-thin layered arable quartz silt sandstone with fine-grained feldspar quartz sandstone", "thickness", "421.26m" ] ] }, { "text": "Dark gray calcium slate with gray thin layered siliceous rock 14.51m", "triple_list": [ [ "Dark gray calcium slate with gray thin layered siliceous rock", "thickness", "14.51m" ] ] }, { "text": "Gray medium-layered medium-fine-grained feldspar quartz sandstone sandstone with dark gray silty slate 126.65m", "triple_list": [ [ "Gray medium-layered medium-fine-grained feldspar quartz sandstone with dark gray silty slab", "thickness", "126.65m" ] ] }, { "text": "The lithology of the Jielong Formation is gray silty silty silty silty silty silty silty medium-thin layered sandy limestone mud crystal limestone grey light gray medium-layered medium-fine-grained feldspar quartz sandstone, among which the silty is horizontally stratigraphic and contains pyrite crystals.", "triple_list": [ [ "Jilong Group", "Lithology", "Gray silty slab" ], [ "Jilong Group", "Lithology", "Thousand-shaped silty slab" ], [ "Jilong Group", "Lithology", "Gray medium-thin layered sandy limestone" ], [ "Jilong Group", "Lithology", "Mud crystal limestone" ], [ "Jilong Group", "Lithology", "Gray - light gray medium-layered medium-fine-grained feldspar quartz sandstone" ], [ "Jilong Group", "Lithology", "Slate" ], [ "Slate", "Develop", "Horizontal stratification" ], [ "Slate", "Develop", "Pyrite crystals" ] ] }, { "text": "Gray medium-thick layer metamorphic fine-grained rock fragment feldspar sandstone 14.21m", "triple_list": [ [ "Gray medium-thick layer metamorphic fine-grained feldspar sandstone", "thickness", "14.21m" ] ] }, { "text": "In the design, the informal stratigraphic unit volcanic rock formation was established in the late Permian.", "triple_list": [ [ "Late Permian", "Outcrop", "Volcanic rock formation" ] ] }, { "text": "Dark gray thin-layer iron feldspar quartz silt sandstone intersects thin-layer fine-grained quartz sandstone 152.88m.", "triple_list": [ [ "Dark gray thin layered iron feldspar quartz silt sandstone with thin layer fine-grained quartz sandstone", "thickness", "152.88m" ] ] }, { "text": "Gray yellow thick medium-grained rock-cut feldspar sandstone 35.91m", "triple_list": [ [ "Gray yellow thick medium-grained feldspar sandstone", "thickness", "35.91m" ] ] }, { "text": "This volcanic strata consists of 4 eruptions-eruption overflow cyclonic volcanic rhythms. There is an eruption interruption period in the middle. Among them, 1-5 layers are sedimentary-eruption-eruption overflow. 6-7 layers are eruptions-eruption overflow. 8-9 layers are eruptions-eruption overflow. There is an eruption interruption period. There is an eruption overflow. The eruption overflow period is a long time. The single layer of lava consists of a rhythmic layer of basic-neutral volcanic rock.", "triple_list": [ [ "Volcanic strata", "Contained", "Eruption-eruption overflow cyclonic volcanic rhythm" ], [ "Volcanic strata", "Contained", "Deposition-Eruption-Eruption overflow" ], [ "Volcanic strata", "Contained", "Eruption - Eruption overflow" ], [ "Volcanic strata", "Lithology", "Basal-neutral volcanic rock" ] ] }, { "text": "The lithologies of the Gadikao Formation are gray-green Andesanite Andesan basalt midbasalt medium acidic volcanic clastic rocks intersect limestone and sandstone siltstone.", "triple_list": [ [ "Gadikao Group", "Lithology", "Gray green Andesan rock" ], [ "Gadikao Group", "Lithology", "Anshan basalt" ], [ "Gadikao Group", "Lithology", "Basalt" ], [ "Gadikao Group", "Lithology", "Medium-basic medium acidic pyroclastic rock" ], [ "Gadikao Group", "Lithology", "Limestone" ], [ "Gadikao Group", "Lithology", "sandstone" ], [ "Gadikao Group", "Lithology", "Siltstone" ] ] }, { "text": "Gray Fluid Crystal Shaped Wave Tuff Lava 18.66m", "triple_list": [ [ "Gray Fluid Crystal Shaped Tuff Lava", "thickness", "18.66m" ] ] }, { "text": "Gray thin-medium-layered powdered sand chip tuff lava 11.8m", "triple_list": [ [ "Gray thin-medium-layered powdered sand chip tuff lava", "thickness", "11.8m" ] ] }, { "text": "Gray-green thin-medium-layered Ying'an fluidic glass-crack tuff 87.31m", "triple_list": [ [ "Gray-green thin-medium-layered Ying'an fluid-grained glass-crash tuff", "thickness", "87.31m" ] ] }, { "text": "Purple-red medium-thick layered fine-grained feldspar rock-cut sandstone with light gray-green medium-thick layered fine-grained feldspar quartz sandstone fault lower section of Jielong Formation (2j1)", "triple_list": [ [ "Purple-red medium-thick layered fine-grained feldspar fragment sandstone with light gray-green medium-thick layered fine-grained feldspar quartz sandstone", "Fault contact", "Jilong Group" ] ] }, { "text": "The field outcropping of this section of the Jiapila Formation is good, and the bottom is integrated with the dark gray calcareous silt sandstone gray feldstone sandstone, and is not integrated with the Tuotuohe Formation.", "triple_list": [ [ "Kapila Group", "Integration of contacts", "Dark gray calcium silt sandstone" ], [ "Kapila Group", "Integration of contacts", "Gray feldstone sandstone" ], [ "Kapila Group", "Unconformity contact", "Tuotuohe Formation" ] ] }, { "text": "Therefore, it is undoubtedly true that the era in the sandstone formation should be the Middle Triassic-Late Triassic Camian period.", "triple_list": [ [ "Sandstone Formation", "Age", "Middle Triassic - Late Triassic Camian Period" ] ] }, { "text": "The rock combination of the Bagong Formation is mainly composed of feldspar quartz sandstone quartz sandstone siltstone carbonaceous shale and limestone lens body and coal seam, which produces a large number of animal and plant fossils, and the exposed thickness of the rock formation can reach 2234.26m.", "triple_list": [ [ "Bagong Group", "Lithology", "Feldspar quartz sandstone" ], [ "Bagong Group", "Lithology", "Quartz sandstone" ], [ "Bagong Group", "Lithology", "Siltstone" ], [ "Bagong Group", "Lithology", "Carbon shale" ], [ "Bagong Group", "Lithology", "Limestone lens body" ], [ "Bagong Group", "Lithology", "Coal layer" ], [ "Bagong Group", "Paleontological", "Fossils of animals and plants" ], [ "Bagong Group", "thickness", "2234.26m" ] ] }, { "text": "Gray-gray-green thick-titanium layered tuff 66.57m", "triple_list": [ [ "Gray-gray-green-thick layered tuff", "thickness", "66.57m" ] ] }, { "text": "Yellow-brown medium-layered medium-fine-grained feldspar sandstone 148.82m", "triple_list": [ [ "Yellow-brown medium-layered medium-fine-grained feldspar sandstone", "thickness", "148.82m" ] ] }, { "text": "In the area of Geo-Zijisai, volcanic tuff is mainly interspersed with a small amount of lava. Clastite interlayers are rare or missing. The lithology is Andesite rhizome tuff, and rhizome tuff crystalline tuff wave tuff volcanic breccia and sandstone siltstone, with a thickness greater than 1614.37m.", "triple_list": [ [ "False - Zijisai", "Lithology", "Volcanic tuff" ], [ "False - Zijisai", "Lithology", "Lava" ], [ "False - Zijisai", "Lithology", "Clastic rock mezzanine" ], [ "False - Zijisai", "Lithology", "Andanyan" ], [ "False - Zijisai", "Lithology", "Flow-grained tuff" ], [ "False - Zijisai", "Lithology", "Flowing Ying'an Rock" ], [ "False - Zijisai", "Lithology", "Tuff" ], [ "False - Zijisai", "Lithology", "Crystal chip tuff" ], [ "False - Zijisai", "Lithology", "Feixiyan" ], [ "False - Zijisai", "Lithology", "Volcanic breccia" ], [ "False - Zijisai", "Lithology", "sandstone" ], [ "False - Zijisai", "Lithology", "Siltstone" ], [ "False - Zijisai", "thickness", "1614.37m" ] ] }, { "text": "The horizontal lamina is developed in slate, with flat and smooth layers, and there is granular lamina in a single coarse sandstone.", "triple_list": [ [ "Slate", "Develop", "Horizontal stratification" ], [ "Coarse sandstone", "Develop", "Granular Sequence Laminating" ] ] }, { "text": "In the test area, 1:20 million Wanzhi was transferred to the sandstone formation of Bayankala Mountains. Only two six-shot coral fossils were collected, and they were identified as Montlivaltia sp.", "triple_list": [ [ "Bayankala Mountain Sandstone Formation", "Paleontological", "Six-Shock Coral Fossils" ], [ "Bayankala Mountain Sandstone Formation", "Paleontological", "Montlivaltia sp." ] ] }, { "text": "The Triassic strata are widely distributed in the survey area, consisting of the early and middle Triassic Jielong Formation of the Triassic Chayong ophiolin mixed rocks, the late Triassic Batang Group and the ligation group of the Triassic Bayankara Mountain Group.", "triple_list": [ [ "Triassic strata", "Outcrop", "Triassic period Chayong ophiolenic mixed rocks Early and Middle Triassic period Jielong Formation" ], [ "Triassic strata", "Outcrop", "The Triassic Bayankara Mountains" ], [ "Triassic strata", "Outcrop", "Batang Group of the Late Triassic World" ], [ "Triassic strata", "Outcrop", "Ligation group" ] ] }, { "text": "Gray-green medium-layer crystal chip tuff 4.57m", "triple_list": [ [ "Gray-green medium-layered crystal chip chip tuff", "thickness", "4.57m" ] ] }, { "text": "Andesite rocks are gray-green, with a doxoplasmic structure that changes to interwoven structures and sheet-like structures.", "triple_list": [ [ "Andanyan", "Distribution pattern", "Spot-like structure" ], [ "Andanyan", "Distribution pattern", "Variable interwoven structure" ], [ "Andanyan", "Develop", "Flake-like structure" ] ] }, { "text": "Slate Formation Sandstone and Slate Interlayer Section (3B) Thickness 2417.17m", "triple_list": [ [ "Interlayer section of the slate sandstone and slate", "thickness", "2417.17m" ] ] }, { "text": "In the same year, in the above report, the Batang group was divided into volcanic rocks in the lower clastic rocks (carbonate rocks) and upper clastic rocks, which became the basis of the three-part plan of the Batang group.", "triple_list": [ [ "Batang Group", "Lithology", "Clastite" ], [ "Batang Group", "Lithology", "Volcanic rocks" ], [ "Batang Group", "Lithology", "Carbonate rock" ], [ "Batang Group", "Lithology", "Clastite" ] ] }, { "text": "Gray sericary cune schist 167.41m", "triple_list": [ [ "Gray sericary mud schist", "thickness", "167.41m" ] ] }, { "text": "The lithologic monotony and single color, clear stratigraphic layout, and stable strata, mainly gray silty slate with horizontal stratigraphic stratigraphic and pyrite crystals, with limestone sandy limestone and sandstone", "triple_list": [ [ "Jilong Group", "Develop", "Horizontal stratification" ], [ "Jilong Group", "Develop", "Inclined layering" ], [ "Jilong Group", "Develop", "Pyrite crystals" ], [ "Jilong Group", "Lithology", "Gray silty slab" ], [ "Jilong Group", "Lithology", "Limestone" ], [ "Jilong Group", "Lithology", "Sandy limestone" ], [ "Jilong Group", "Lithology", "sandstone" ] ] }, { "text": "The lava components are mainly composed of plagioclase zoicle and yangqi stone. In addition, there are a small amount of quartz chlorite titanium magnetite and later quartz fine veins, and some plagioclase appear as porcine.", "triple_list": [ [ "Lava", "Contained", "plagiarite" ], [ "Lava", "Contained", "Yang Qishi" ], [ "Lava", "Contained", "Quartz green clay stone" ], [ "Lava", "Contained", "Titanium magnetite" ], [ "Lava", "Contained", "Quartz vein" ], [ "Lava", "Contained", "Plagioclase" ] ] }, { "text": "Dark gray silty slate with rock cuttings feldstone 251.18m", "triple_list": [ [ "Dark gray silty slate with rock cuttings feldstone sandstone", "thickness", "251.18m" ] ] }, { "text": "Light gray medium layered fine-grained quartz sandstone 166.14m", "triple_list": [ [ "Light gray medium layered fine-grained quartz sandstone", "thickness", "166.14m" ] ] }, { "text": "Gray-green altered olive basalt with a small amount of thin layered siliceous rock 197.29m", "triple_list": [ [ "Gray-green altered olive basalt with a small amount of thin layered siliceous rock", "thickness", "197.29m" ] ] }, { "text": "Gray silty slate feldspar transformed into sandstone sandstone (oblique core) 375.6m", "triple_list": [ [ "Gray silty slate feldspar into sandstone limestone", "thickness", "375.6m" ] ] }, { "text": "Gray-green thick layered coarse-grained rock fragment sandstone 20.82m", "triple_list": [ [ "Gray-green thick layered coarse-grained rock fragments sandstone", "thickness", "20.82m" ] ] }, { "text": "Bagong Formation (3bg) Li Pu et al. (1951) called the coal-containing sand shale formation in Chayabagong the Bagong coal system, and the era was Jurassic.", "triple_list": [ [ "Bagong Group", "Exposed", "Chayabagong" ], [ "Bagong Group", "Lithology", "Coal-containing sand shale" ], [ "Bagong Group", "Age", "Jurassic" ] ] }, { "text": "Gray thin-layer sheet physical and chemical fine-grained feldspar crushed sandstone sandstone intersected with gray thin-layer slate 45.14m", "triple_list": [ [ "Gray thin-layer sheet physical and chemical fine-grained feldspar crushed sandstone sandstone intersected with gray thin-layer slab", "thickness", "45.14m" ] ] }, { "text": "Dark gray block layered bio-clad powder crystal thin layer of crustal limestone, produced by Pseudofusulinavulgaris Megasphaericatorigama", "triple_list": [ [ "Dark gray block layered bioclad powder crystal thin layer of clastic limestone", "Paleontological", "可以中国 Pseudofusulinavulgaris Megasphaericatorigama" ] ] }, { "text": "The clastic rock formation (3Bt1) has a grey medium-thin layered medium-fine-grained feldspar sandstone with gray medium-layered mud crystal limestone", "triple_list": [ [ "Clastic rock formation", "Lithology", "Gray Medium-Thin Laminate Medium-Fine Grained Feldspar" ], [ "Clastic rock formation", "Lithology", "Chop sandstone" ], [ "Clastic rock formation", "Lithology", "Gray medium-layer mud crystal limestone" ] ] }, { "text": "Horizontal stratigraphy develops in slate, contains calcium tuberculosis, plant fragments, bordering Qumalai County in the north, and is equivalent to the south bank of Tongtian River.", "triple_list": [ [ "Slate", "Develop", "Horizontal stratification" ], [ "Slate", "Develop", "Calcium tuberculosis" ], [ "Slate", "Paleontological", "Plant fragments" ] ] }, { "text": "Off-white gravel limestone 19.31m", "triple_list": [ [ "Off-white gravel limestone", "thickness", "19.31m" ] ] }, { "text": "Inclined stratigraphy is seen in sand chip limestone and sandstone interlayers.", "triple_list": [ [ "Sand chip limestone and sandstone interlayer", "Develop", "Inclined layering" ] ] }, { "text": "The Bayankala Mountain Group in the area did not see the top and bottom. According to the profile route data, it was divided into sandstone formation (2-3B) and slate and sandstone interlayer sections (3B). The two were in a integrated contact, and incorrectly contacted with Chayong ophiolite in the south of Zhiduo County, and it was covered by the angle of the Xinjin Jiquguo Formation.", "triple_list": [ [ "Bayankala Mountain Group", "Outcrop", "Sandstone Formation" ], [ "Bayankala Mountain Group", "Outcrop", "Interlayer section of slate and sandstone in the Slate Formation" ], [ "Bayankala Mountain Group", "Fault contact", "Chayong Ophiopolysite" ], [ "Bayankala Mountain Group", "Unconformity contact", "New Jiquguo Group" ], [ "Sandstone Formation", "Integration of contacts", "Interlayer section of slate and sandstone in the Slate Formation" ] ] }, { "text": "Gray thin-middle-physical and chemical fine-grained feldspar crushed sandstone 38.83m", "triple_list": [ [ "Thin gray-middle-sliced physical and chemical fine-grained feldspar crushed sandstone", "thickness", "38.83m" ] ] }, { "text": "Gray thin-layer medium-fine-grained rock-cut feldspar quartz sandstone sandstone-dark gray silty slate 244.67m", "triple_list": [ [ "Gray thin-layer medium-fine-grained rock fragment feldspar quartz sandstone intersected with grey-dark gray silty slab", "thickness", "244.67m" ] ] }, { "text": "Gray-green all-green mud petrochemical Yangqi petrochemical basalt (covered by the Quaternary flood alluvial) 4.31m", "triple_list": [ [ "Gray green all-green mud petrochemical Yangqi petrochemical basalt", "thickness", "4.31m" ] ] }, { "text": "Sandstone Formation (2-3B) has limited exposure, mainly distributed on both sides of Tongtian River in the northeast corner of the map area. The core of the band-shaped formation is a complex anticline or spread between the fault zones. It is not integrated on it in the Tertiary period. The distribution area in the area is about 330m2. It is integrated with the slate sandstone formation upward, and has no bottoming. The maximum thickness is controlled at 2959.61m. The lithology is mainly gray-light gray-green medium-fine-grain feldspar quartz sandstone rock-cuts feldspar quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone rock-cuts quartz sandstone pyrite medium-fine-grain feldspar quartz sandstone silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt s", "triple_list": [ [ "Sandstone Formation", "Exposed", "Tongtian River" ], [ "Sandstone Formation", "Distribution pattern", "The strip-shaped group has a complex anticline core or spreads in the fault zone" ], [ "Sandstone Formation", "Unconformity contact", "Third period" ], [ "Sandstone Formation", "area", "330m2" ], [ "Sandstone Formation", "Integration of contacts", "Slate sandstone formation" ], [ "Sandstone Formation", "thickness", "2959.61m" ], [ "Sandstone Formation", "Lithology", "Gray - Light gray-green medium-fine-grain feldspar quartz sandstone" ], [ "Sandstone Formation", "Lithology", "Lithic feldspar quartz sandstone" ], [ "Sandstone Formation", "Lithology", "Rock cutting quartz sandstone" ], [ "Sandstone Formation", "Lithology", "Pyrite-containing medium-fine feldspar quartz sandstone" ], [ "Sandstone Formation", "Lithology", "Siltstone" ], [ "Sandstone Formation", "Lithology", "Silty slab" ], [ "Sandstone Formation", "Lithology", "Silicone rock" ] ] }, { "text": "The Bagong Formation was first cited by the rock formation in Qinghai Province (1997), and the definition of the Bagong Formation was revised by Tibet Stratigraphic Cleaning Formation, referring to a set of coal-containing clastic rock formations integrated under the limestone of the Polila Formation, producing plant spores and other fossils.", "triple_list": [ [ "Bagong Group", "Integration of contacts", "Polila Formation limestone" ], [ "Bagong Group", "Lithology", "Coal-containing clastic rock" ], [ "Bagong Group", "Paleontological", "Plant spore powder" ] ] }, { "text": "Gray medium-layered lithotrix quartz sandstone with gray medium-thick layered gravel-containing coarse sandstone 18.48m", "triple_list": [ [ "Gray medium-layered lithotrix quartz sandstone with gray medium-thick layered gravel-containing coarse sandstone", "thickness", "18.48m" ] ] }, { "text": "The lithologic properties of the carbonate formation are composed of gray-white medium-thick layer of mud crystal limestone fragmented blocky limestone and a small amount of gray-black thin layer of limestone dark green andesite meso-basic lava dark gray sandstone slate, which is reflected in coastal-shallow marine carbonate platform-front sloped reef limestone. This section has rich fossils and many categories.", "triple_list": [ [ "Carbonate rock formation", "Lithology", "Off-white medium-thick layer of mud crystal limestone" ], [ "Carbonate rock formation", "Lithology", "Broken block limestone" ], [ "Carbonate rock formation", "Lithology", "Limestone" ], [ "Carbonate rock formation", "Lithology", "Dark green Andes" ], [ "Carbonate rock formation", "Lithology", "Medium-basic lava" ], [ "Carbonate rock formation", "Lithology", "Dark grey sandstone" ], [ "Carbonate rock formation", "Lithology", "Slate" ], [ "Carbonate rock formation", "Lithology", "Reef-like limestone" ] ] }, { "text": "The Gadikao Formation in the Permian Permian was divided into a clastic rock section from bottom to top. A set of purple-red hard sandstone quartz sandstone siltstone mudstone clay rocks with conglomerate impurity limestone and volcanic rocks. The upper carbonate rock section is a set of gray-gray-black breccia limestone biolimestone, with local flint strips and nodule limestone. It has not been seen bottoming out, and it has been in integrated contact with the overlying Zageyong Group.", "triple_list": [ [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Clastite" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Purple-red hard sandstone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Quartz sandstone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Siltstone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Mudstone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Clay rock" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Polygon" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Limestone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Volcanic rocks" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Carbonate rock" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Grey-grey-black breccia limestone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Biolimestone" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Flint strip" ], [ "Early and Middle-aged Permian Gadikao Group", "Lithology", "Tuberculous limestone" ], [ "Early and Middle-aged Permian Gadikao Group", "Integration of contacts", "Zag Yong Group" ] ] }, { "text": "The altered basalt is gray-green, with a spotty structure, a matrix interfilled structure, and a block-like structure.", "triple_list": [ [ "Alteration basalt", "Distribution pattern", "Spotted structure" ], [ "Alteration basalt", "Distribution pattern", "Filling room structure" ], [ "Alteration basalt", "Develop", "Blocky structure" ] ] }, { "text": "Gray-green-light gray-green flowing Ying'an rock 57.59m", "triple_list": [ [ "Gray-green-light gray-green flowing Ying'an rock", "thickness", "57.59m" ] ] }, { "text": "Many paleontological fossils of this combination are distributed in the limestone of the carbonate rock formation in the Batang Group, and are relatively rare in the profile. They are located in the upper strata of the actual measured profile of the Batang Group of the Sieo Gongma Evening Triassic Batang Group in Duocai Township, Zhiduo County, Qinghai Province.", "triple_list": [ [ "Batang Group Carbonate Formation Limestone", "Located at", "Shio Ogongma, Duocai Township, Zhiduo County, Qinghai Province" ], [ "Batang Group Carbonate Formation Limestone", "Integration of contacts", "Carbonate rock formation in the late Triassic Batang group" ] ] }, { "text": "The stomata of almonds in the rocks is unevenly distributed, with obvious eruption rhythm layers. The stomata and almond structures are developed in basalt. The colors of the volcanic rocks are gray-gray-brown, and there is brown-red locally, reflecting the characteristics of green bottom and red tops. They are the products of the volcanic eruption phase-eruption phase.", "triple_list": [ [ "rock", "Contained", "Eruption rhythm layer" ], [ "Basalt", "Develop", "Air hole" ], [ "Basalt", "Develop", "Almond structure" ], [ "Volcanic rocks", "Belongs to", "Land phase volcanic overflow phase-erupt phase" ] ] }, { "text": "Gray-Grey-Grey-Grey-Thick-layered almond-like quartz-containing basalt androstone 76.70m", "triple_list": [ [ "Gray-Grey-Grey-Grey-Thick-layered almond-like quartz-containing basalt andshan rock", "thickness", "76.70m" ] ] }, { "text": "The section position starts at 96°01′59 east longitude, 33°47′58 north latitude, and Elevation is 4015m; the end is 96°01′59 east longitude, 33°48′59 north latitude, and an elevation is 4218m.", "triple_list": [ [ "profile", "Coordinates", "96°01'59 East longitude" ], [ "profile", "Coordinates", "33°47′58 North latitude" ], [ "profile", "Elevation", "4015m" ], [ "profile", "Coordinates", "96°01'59 East longitude" ], [ "profile", "Coordinates", "33°48′59 North latitude" ], [ "profile", "Elevation", "4218m" ] ] }, { "text": "Based on geological characteristics, contact with fault contact with the Noribagaribao Formation and Jiujidao Team of Kaixinling Group and the petrochemical characteristics of island arc volcanic rocks", "triple_list": [ [ "Kaixinling Qun Noriba Gari Protection Group", "Fault contact", "Ninety teams" ] ] }, { "text": "Late Triassic Ligation Group (3J) was created by Qinghai Provincial Regional Test Team (1970). The original definition refers to the original definition of the clastic rock carbonate distributed in the Tanggula Mountain area and is mainly composed of a set of clastic carbonate deposited from coastal to shallow seas. It is divided into four rock groups: gray clastic rock formation of the lower limestone formation of the purple-red clastic rock formation and upper limestone formation. It is not integrated with the Permian system at angles and parallels, and is mostly not topped, and it can be seen locally that it has not integrated contact with the Jurassic Cretaceous and Third Systems.", "triple_list": [ [ "Late Triassic Ligation Group", "Exposed", "Tanggula Mountain area" ], [ "Late Triassic Ligation Group", "Lithology", "Clarinet rocks deposited from coastal to shallow sea" ], [ "Late Triassic Ligation Group", "Lithology", "Carbonate rock" ], [ "Late Triassic Ligation Group", "Outcrop", "Purple-red clastic rock formation" ], [ "Late Triassic Ligation Group", "Outcrop", "Lower limestone formation" ], [ "Late Triassic Ligation Group", "Outcrop", "Gray clastic rock formation" ], [ "Late Triassic Ligation Group", "Outcrop", "Upper limestone formation" ], [ "Late Triassic Ligation Group", "Unconformity contact", "Permian" ], [ "Late Triassic Ligation Group", "Unconformity contact", "Jurassic Cretaceous" ], [ "Late Triassic Ligation Group", "Unconformity contact", "The third series" ] ] }, { "text": "A set of gray-purple clastic rocks and gray carbonate rock formations were disintegrated in the original Triassic Batang group formation in the Boche area of Dangjiang Township. The rock combination characteristics are obviously different from those of the Triassic Batang group.", "triple_list": [ [ "Dangjiang Township Boche", "Outcrop", "The original Triassic Batang Group" ], [ "The original Triassic Batang Group", "Lithology", "Gray purple clastic rock" ], [ "The original Triassic Batang Group", "Lithology", "Grey carbonate rock" ] ] }, { "text": "Dark gray thin layer medium-fine-grained feldspar quartz sandstone sandstone formation (2-3B) gray thin layer medium-coarse-grained feldspar quartz sandstone 278.02m", "triple_list": [ [ "Dark gray thin layer medium fine-grained feldspar quartz sandstone sandstone formation (2-3B) gray thin layer medium coarse-grained feldspar quartz sandstone", "thickness", "278.02m" ] ] }, { "text": "Gray thick layered fluidic wave-shape slurry tuff 126.19m", "triple_list": [ [ "Gray thick layered fluidic wave-shape slurry tuff", "thickness", "126.19m" ] ] }, { "text": "The rocks of the Gadikao Formation are usually mainly gray-green, and the appearance of limestone interlayers reflects the environment of underwater eruption.", "triple_list": [ [ "Gadikao Group", "Lithology", "Limestone mezzanine" ] ] }, { "text": "Dark gray thin-medium-thick layered siltstone, fossilized Halobia sp.Cardium (ulongocardium) sp. 178.57m", "triple_list": [ [ "Dark gray thin-medium-thick layered siltstone", "Paleontological", "Halobia sp." ], [ "Dark gray thin-medium-thick layered siltstone", "Paleontological", "Cardium (ulongocardium ) sp." ], [ "Dark gray thin-medium-thick layered siltstone", "thickness", "178.57m" ] ] }, { "text": "Impression structures are seen on the bottom layer of rock debris sandstone, such as heavy core mold groove mold and flame-like structure. At the same time, small inclined layer, small hill-like layering, wrapping and lamination are developed.", "triple_list": [ [ "Rock cuttings sandstone", "Develop", "Impression structure" ], [ "Rock cuttings sandstone", "Develop", "Re-core model" ], [ "Rock cuttings sandstone", "Develop", "Grooving mold" ], [ "Rock cuttings sandstone", "Develop", "Flaming structure" ], [ "Rock cuttings sandstone", "Develop", "Small slant layer" ], [ "Rock cuttings sandstone", "Develop", "Small mound-like stratigraphy" ], [ "Rock cuttings sandstone", "Develop", "Cover lamination" ] ] }, { "text": "Among them, cephalopods are Longoborditides sp. , Paraceratites sp. , Voritesfalcatus sp. , Japonites yushuensis, J. sp. , Balatonites gracilis, B. disparicostatus B, Xizang ensis B. sp., Cuceoeras Cuccene, C. taramellii C. sp., Acrochordiceras cf, Carolinae, Beyrchites sp., Cymnoeoceras sp., Lsculites cf. meduoensis;", "triple_list": [ [ "Cephalopod", "Paleontological", "Longoborditides sp." ], [ "Cephalopod", "Paleontological", "Paraceratites sp." ], [ "Cephalopod", "Paleontological", "Voritesfalcatus sp." ], [ "Cephalopod", "Paleontological", "Japonites yushuensis" ], [ "Cephalopod", "Paleontological", "J. sp." ], [ "Cephalopod", "Paleontological", "Balatonites gracilis" ], [ "Cephalopod", "Paleontological", "B. disparicostatus B" ], [ "Cephalopod", "Paleontological", "Xizang ensis B.sp." ], [ "Cephalopod", "Paleontological", "Cuceoeras Cuccene" ], [ "Cephalopod", "Paleontological", "C. taramellii C. sp." ], [ "Cephalopod", "Paleontological", "Acrochordiceras cf" ], [ "Cephalopod", "Paleontological", "Carolinae" ], [ "Cephalopod", "Paleontological", "Beyrchites sp." ], [ "Cephalopod", "Paleontological", "Cymnoeoceras sp." ], [ "Cephalopod", "Paleontological", "Lsculites cf. meduoensis" ] ] }, { "text": "Gray rhyolite 31.75m", "triple_list": [ [ "Gray rhizome", "thickness", "31.75m" ] ] }, { "text": "Clexite Formation (3Bt1) This rock formation is mainly distributed in the line of Gengzhichun-Nichaqu-Zhengma, and is also distributed in the area of Sieogongma, with a controlled thickness of 1705.89m.", "triple_list": [ [ "Clastic rock formation", "Exposed", "More direct rush - Nie Chaqu - Zheng Mao Yong" ], [ "Clastic rock formation", "Exposed", "Scared Ogonma" ], [ "Clastic rock formation", "thickness", "1705.89m" ] ] }, { "text": "Gray-green gabbro (tectonic block) 15.62m", "triple_list": [ [ "Gray-green gabbro", "Distribution pattern", "Tectonic rock blocks" ], [ "Gray-green gabbro", "thickness", "15.62m" ] ] }, { "text": "The lava composition is andesite, with a lava content of about 70.", "triple_list": [ [ "Lava", "Lithology", "Andanyan" ] ] }, { "text": "The secondary minerals include particulate magnetite apatite and zircon, which are distributed in small inclusions in polsters.", "triple_list": [ [ "Sub-mineral", "Contained", "Particular magnetite apatite" ], [ "Sub-mineral", "Contained", "Zircon" ] ] }, { "text": "Light gray-brown-gray-green Anshan crystalline crystal sediment tuff sandwiched dark gray layered argillite limestone.", "triple_list": [ [ "Early and Middle Permian Noribagaribao Group", "Lithology", "Light gray-brown-gray green Anshan crystalline tuff" ], [ "Early and Middle Permian Noribagaribao Group", "Lithology", "Dark gray layered argillite" ] ] }, { "text": "The late Triassic brachiopod fossils are mainly distributed in the Batang group and the ligation group of the Porilla group. There are relatively few in the Bagong group of the ligation group. According to the fossil molecules and their combination characteristics and the Triassic paleontological strata of the rock formation in Qinghai Province, the late Triassic brachiopods can be divided into 2 paleontological combinations in the area.", "triple_list": [ [ "Late Triassic Brachiopod", "Located at", "Batang Group" ], [ "Late Triassic Brachiopod", "Located at", "Ligation group" ], [ "Late Triassic Brachiopod", "Located at", "Kapila Group" ], [ "Late Triassic Brachiopod", "Located at", "Polira group" ] ] }, { "text": "Sandstone slate interlayer section of the Slate Formation (3B) This group is mainly distributed on the north and south banks of Tongtian River. The strata direction is consistent with the direction of the main tectonic line of the region. It is spread in the northwest-southeast belt, extending to the northwest-southeast into the neighboring area respectively. The fold fault structure and joint splitting in the rock formation are very developed, forming a complex oblique structure", "triple_list": [ [ "Sandstone slate interlayer section of Slate Formation", "Exposed", "Tongtian River North and South" ], [ "Sandstone slate interlayer section of Slate Formation", "Distribution pattern", "Northwest-Southeast Belt Distribution" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Wrinkles" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Fracture structure" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Procedure" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Severing" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Complex tilt structure" ] ] }, { "text": "There are wave marks in the sandstone, and there are grooved mold groove mold structures on the level.", "triple_list": [ [ "sandstone", "Develop", "Groove mold structure" ] ] }, { "text": "Purple-red - light gray-green medium-thick layered feldspar quartz sandstone 42.24m", "triple_list": [ [ "Purple-red - light gray-green medium-thick layered feldspar quartz sandstone", "thickness", "42.24m" ] ] }, { "text": "Fossil strata such as carpopod corals in the limestone can be compared with the Gadikao Formation.", "triple_list": [ [ "Limestone", "Paleontological", "Insect" ], [ "Limestone", "Paleontological", "Brachiopod" ], [ "Limestone", "Paleontological", "coral" ] ] }, { "text": "In this work, Parahalobia sp (parasalis clams) of the early and middle triassic periods were found in this strata, and it was determined as the Jielong Group.", "triple_list": [ [ "Strata", "Belongs to", "Jilong Group" ], [ "Early and Middle Triassic", "Paleontological", "Parahalobia sp(生生生生生生生)" ], [ "Early and Middle Triassic", "Paleontological", "Claraia sp(Keria clam) wrist foot" ] ] }, { "text": "Gray-light gray-green rhyolite 78.66m", "triple_list": [ [ "Gray-light gray-green rhyolite", "thickness", "78.66m" ] ] }, { "text": "Gray-green giant thick layered complex volcanic breccia 123.45m", "triple_list": [ [ "Grey-green giant thick layered complex volcanic breccia", "thickness", "123.45m" ] ] }, { "text": "Gray-purple thin-medium-layered rock-cut feldspar sandstone 11.43m", "triple_list": [ [ "Gray-purple thin-medium-layered lithotrix feldspar sandstone", "thickness", "11.43m" ] ] }, { "text": "The gravel components include siliceous rock sandstone and limestone, which are mostly subcircular and subangular, with poor sorting and mixed sizes. The largest gravel diameter is 13cm, the smallest is 2cm, and generally 4-5cm.", "triple_list": [ [ "gravel", "Lithology", "Silicone rock" ], [ "gravel", "Lithology", "sandstone" ], [ "gravel", "Lithology", "Limestone" ], [ "gravel", "Distribution pattern", "Secondary circle - secondary edge" ] ] }, { "text": "The highly altered olive basalt is gray-green, with a spotty structure, a matrix with interstitial structure and an almond-like structure.", "triple_list": [ [ "Alive basalt", "Distribution pattern", "Spotted structure" ], [ "Alive basalt", "Distribution pattern", "Interstellar structure" ], [ "Alive basalt", "Develop", "Almond-like structure" ] ] }, { "text": "Gray-green medium-grained gabbro (tectonic block) 72.89m", "triple_list": [ [ "Gray green medium-grained gabbro", "Distribution pattern", "Tectonic rock blocks" ], [ "Gray green medium-grained gabbro", "thickness", "72.89m" ] ] }, { "text": "Gray-green thick layered flow-grained complex chip melted tuff 81.26m", "triple_list": [ [ "Gray-green thick layered flow-grained complex chip melted tuff", "thickness", "81.26m" ] ] }, { "text": "Gray medium-thick layered medium-grained rock-cut quartz sandstone 18.67m", "triple_list": [ [ "Gray medium-thick layered medium-grained quartz sandstone", "thickness", "18.67m" ] ] }, { "text": "Combined with the rich biological fossils such as the rocks of the Gapila Formation, it can be seen that its sedimentary environment is a stable high-energy environment with a shallow and land-sea sea.", "triple_list": [ [ "Kapila Group", "Paleontological", "dragonfly" ], [ "Kapila Group", "Paleontological", "Wrist foot" ], [ "Kapila Group", "Paleontological", "coral" ], [ "Kapila Group", "Belongs to", "Stable coastal shallow - high-energy environment of land sheds and seas" ] ] }, { "text": "Rock cuttings 25-30 are Anshan basalt cuttings, with a spot-like structure and a matrix with an interfilled structure.", "triple_list": [ [ "Anshan basalt rock chips", "Distribution pattern", "Spotted structure" ], [ "Anshan basalt rock chips", "Distribution pattern", "Filling room structure" ] ] }, { "text": "Light gray-green sheet physical and chemical tuff with dark gray-green sheet physical and chemical tuff 89.24m", "triple_list": [ [ "Light gray-green sheet physical and chemical tuff with dark gray-green sheet physical and chemical Andesan rock", "thickness", "89.24m" ] ] }, { "text": "Porcelain consists of plagioclase and ordinary pyroxene, and the matrix is composed of plagioclase and iron.", "triple_list": [ [ "Pyramid", "Contained", "Plagioclase" ], [ "Pyramid", "Contained", "Ordinary pyrosine" ], [ "Substrate", "Contained", "Plagioclase" ], [ "Substrate", "Contained", "Pyrox" ], [ "Substrate", "Contained", "Iron" ] ] }, { "text": "The Kapila Group took root in the area of Donoda - Russia and Bangladesh - Sobao Chaya - Longmari - Polyri Cha Riyong Qu - However, it also rang Qu Gao Yong Wali Yong - Ge Chong Jia Ye - Squeezing Erpuma and other places.", "triple_list": [ [ "Kapila Group", "Exposed", "Dominant" ], [ "Kapila Group", "Exposed", "Russia and Bangladesh can take root" ], [ "Kapila Group", "Exposed", "Sobao check teeth" ], [ "Kapila Group", "Exposed", "Longmari" ], [ "Kapila Group", "Exposed", "Refuting the poor day to check the sunrise song" ], [ "Kapila Group", "Exposed", "However, it also rushes high and strong" ], [ "Kapila Group", "Exposed", "Add leaves" ], [ "Kapila Group", "Exposed", "Suffering Erpoma" ] ] }, { "text": "Gray thick layered fluid tuff lava 13.48m", "triple_list": [ [ "Gray thick layered flow tuff lava", "thickness", "13.48m" ] ] }, { "text": "The Bayankala Mountains in the test area are only located in the area of Zhiduo County, downstream of Chaqu and Dengequ, and the main body is located outside the picture.", "triple_list": [ [ "Bayankala Mountain Group", "Exposed", "Zhiduo County Town - Downstream of Chaqu - Deng'erqu" ] ] }, { "text": "Light gray thick-block layered powder crystals Contained bioclass thin layer limestone under the Vuloribagaribao Formation gray medium-layered fine-grained feldspar quartz sandstone.", "triple_list": [ [ "Light gray thick-block layered powder crystals Contained thin layer of limestone", "Integration of contacts", "Grey medium-layered fine-grained feldspar quartz sandstone of Nuoribagaribao Formation" ] ] }, { "text": "Gray medium-thick layered medium-grained cuts quartz sandstone fault Geren volcanic rock (chva) 6.63m", "triple_list": [ [ "Gray medium-thick layered medium-grained quartz sandstone", "Fault contact", "Geren Volcano Rock" ], [ "Geren Volcano Rock", "thickness", "6.63m" ] ] }, { "text": "The newly discovered Jielong Formation strata in the Triassic Batang Group in the area are in fault contact with the Triassic Batang Group and the ligation group strata, with a distribution area of 200m2 and a maximum control thickness greater than 796.23m.", "triple_list": [ [ "The Triassic Batang Group", "Outcrop", "Jilong Group" ], [ "Jilong Group", "Fault contact", "The Triassic Batang Group" ], [ "Jilong Group", "Fault contact", "Ligation group" ], [ "Jilong Group", "area", "200m2" ], [ "Jilong Group", "thickness", "796.23m" ] ] }, { "text": "Gray Fluid Breccia Lava 294.97m", "triple_list": [ [ "Gray Breccia lava", "thickness", "294.97m" ] ] }, { "text": "Gray thin-layer plate-like silt sandstone, producing plant fossil fragments 1026.34m", "triple_list": [ [ "Gray thin-layer plate-like siltstone", "Paleontological", "Plant fossil fragments" ], [ "Gray thin-layer plate-like siltstone", "thickness", "1026.34m" ] ] }, { "text": "The slate is horizontal stratigraphic, reflecting the Bauma sequence formed by the turbid currents of the deep-sea-semi-deep sea phase.", "triple_list": [ [ "Slate", "Develop", "Horizontal stratification" ], [ "Slate", "Contained", "Bauma Sequence" ] ] }, { "text": "Taking the disappearance of the clastic rock of the Jiapila Formation, the emergence of the large limestone is as the base boundary, and the disappearance of the large limestone is as the integrated contact with the overlying Bagong Formation, the control thickness is greater than 1789.98m.", "triple_list": [ [ "Kapila Group", "Lithology", "Clastite" ], [ "Kapila Group", "Lithology", "Limestone" ], [ "Kapila Group", "Integration of contacts", "Bagong Group" ], [ "Kapila Group", "thickness", "1789.98m" ] ] }, { "text": "The Polila Formation gray medium-layer mud crystal limestone with gray thin-layer limestone integrated Jiapila Formation Thickness 220.75m", "triple_list": [ [ "Polila Formation Gray Medium-layered Mud Crystal Limestone with Gray Thin-layered Lithospark Sandstone", "Integration of contacts", "Kapila Group" ], [ "Polila Formation Gray Medium-layered Mud Crystal Limestone with Gray Thin-layered Lithospark Sandstone", "thickness", "220.75m" ] ] }, { "text": "Chayong opalienite mixed rocks are further divided into three informal tectonic rock formation units, namely Chayong opalienite (chop), Geren volcanic rocks (chva), Dalong sandstone (chd).", "triple_list": [ [ "Chayong ophiolula mixed rock", "Lithology", "Chayong Ophiopolysite" ], [ "Chayong ophiolula mixed rock", "Lithology", "Geren Volcano Rock" ], [ "Chayong ophiolula mixed rock", "Lithology", "Dalong Sandstone" ] ] }, { "text": "Gray-green medium-thin layered crystal chip tuff 27.43m", "triple_list": [ [ "Gray-green medium-thin layered crystal chip chip tuff", "thickness", "27.43m" ] ] }, { "text": "Gray-green giant thick layered crystal chip tuff 183.53m", "triple_list": [ [ "Gray-green giant thick layered crystal chip chip tuff", "thickness", "183.53m" ] ] }, { "text": "Dark gray thin layered medium-fine-grained feldspar quartz sandstone with dark gray silty slate interlayer 261.40m", "triple_list": [ [ "Dark gray thin layered medium-fine-grained feldspar quartz sandstone with dark gray silty slate interlayer", "thickness", "261.40m" ] ] }, { "text": "Qinghai Provincial Geological Survey Institute (2001) has obtained abundant bivalves in this strata in the Kokoxili region. Mainly include Myophoria (costaoria) mansuyi, Plagiostoma sp., Placunopsis remuensis. The main spores include Cyathidites minor, Conrerrlcosis Porites sp. fossils of remains Cnondrites sp., Phycosiphon incertum, Megagraphon irregeulare, Planolites montanus, etc.", "triple_list": [ [ "Kekexili area", "Paleontological", "Bivalves" ], [ "Kekexili area", "Paleontological", "Myophoria (costaoria) mansuyi" ], [ "Kekexili area", "Paleontological", "Plagiostoma sp." ], [ "Kekexili area", "Paleontological", "Placunopsis remuensis" ], [ "Kekexili area", "Paleontological", "Spore powder" ], [ "Kekexili area", "Paleontological", "Cyathidites minor" ], [ "Kekexili area", "Paleontological", "Conrerrlcosis Porites sp." ], [ "Kekexili area", "Paleontological", "Ruins fossils" ], [ "Kekexili area", "Paleontological", "Cnondrites sp." ], [ "Kekexili area", "Paleontological", "Phycosiphon incertum" ], [ "Kekexili area", "Paleontological", "Megagraphon irregeulare" ], [ "Kekexili area", "Paleontological", "Planolites montanus" ] ] }, { "text": "Gray-green thick-conducting layered complex conglomerate 22.97m angle unconsolidation Nuoribagaribao Formation Dark gray thin-layered silt sandstone with gray thin-layered medium-grained rock-cut feldstone sandstone", "triple_list": [ [ "Gray-green thick conductive layered complex gravel", "thickness", "22.97m" ], [ "Gray-green thick conductive layered complex gravel", "Unconformity contact", "Dark gray thin-layered silt sandstone with gray thin-layered medium-grained rock-cut feldstone sandstone" ] ] }, { "text": "There is a physical and chemical phenomenon in siltstone, and the thickness is greater than 1896.15m, including bivalves Halobia yunnanensis, H. cfconvesa, H. anliangbaensis, H. superba, H. rugosa, H. cf. yunnanensis. H. cf. conveezsa. H. austriaca, Cardium (ulongcardium) xizangense Krumbecia timorensis; ammonite Profrachyceras sp., rachyceras cf. aon; brachipods Aulacothyris sp. plant Clathropteris mongugaica, Neocalamites sp., etc.", "triple_list": [ [ "Siltstone", "Develop", "Physical and chemical phenomena of film" ], [ "Siltstone", "thickness", "1896.15m" ], [ "Siltstone", "Paleontological", "bivalve Halobia yunnanensis" ], [ "Siltstone", "Paleontological", "H.cfconvesa" ], [ "Siltstone", "Paleontological", "H. anliangbaensis" ], [ "Siltstone", "Paleontological", "H. superba" ], [ "Siltstone", "Paleontological", "H. rugosa" ], [ "Siltstone", "Paleontological", "H. cf. yunnanensis." ], [ "Siltstone", "Paleontological", "H. cf. conveezsa." ], [ "Siltstone", "Paleontological", "H. austriaca" ], [ "Siltstone", "Paleontological", "Cardium (ulongcardium) xizangense Krumbecia timorensis" ], [ "Siltstone", "Paleontological", "Ammonite Profrachyceras sp." ], [ "Siltstone", "Paleontological", "rachyceras cf. aon" ], [ "Siltstone", "Paleontological", "Brachiopod Aulacothyris sp." ], [ "Siltstone", "Paleontological", "Plant Clathropteris mongugaica" ], [ "Siltstone", "Paleontological", "Neocalamites sp." ] ] }, { "text": "In 1982, the second district transfer team of Qinghai Province named the Gadikao Group and the Zageyong Group. The former is divided into clastic rock sections and carbonate sections from bottom to top, and the latter is divided into clastic rock volcanic rock sections and carbonate sections from bottom to top. At the same time, these two groups are believed to represent the Maokou strata of the Qixia period respectively.", "triple_list": [ [ "Gadikao Group", "Lithology", "Clastite" ], [ "Gadikao Group", "Lithology", "Carbonate" ], [ "Gadikao Group", "Belongs to", "Qixia period" ], [ "Zag Yong Group", "Lithology", "Clastite" ], [ "Zag Yong Group", "Lithology", "Clastite" ], [ "Zag Yong Group", "Lithology", "Volcanic rocks" ], [ "Zag Yong Group", "Lithology", "Carbonate" ], [ "Zag Yong Group", "Belongs to", "Maokou period" ] ] }, { "text": "In this work, the brachiopod fossils in the early and middle triassic triassic were collected in this strata and classified into the Jielong Formation (1-2j), and further divided into the lower sandstone section (1-2j1) and the upper limestone section (1-2j2).", "triple_list": [ [ "Brachiopod fossils in the early and middle triassic", "Belongs to", "Jilong Group" ], [ "Brachiopod fossils in the early and middle triassic", "Contained", "Sandstone section" ], [ "Brachiopod fossils in the early and middle triassic", "Contained", "Limestone section" ] ] }, { "text": "Gray green medium-thick layered medium-fine-grained rock-cut feldspar sandstone with gray medium-layered mud crystal limestone 36.79m", "triple_list": [ [ "Gray-green medium-thick layered medium-fine-grained rock-cut feldspar sandstone with gray medium-layered mud crystal limestone", "thickness", "36.79m" ] ] }, { "text": "Among the volcanic rocks, there are overflowing lava and erupting volcanic clastic rocks.", "triple_list": [ [ "Volcanic rocks", "Lithology", "Lava" ], [ "Volcanic rocks", "Lithology", "Pyroclastic rock" ] ] }, { "text": "The plagioclase is semi-self-shaped and has sericite-shaped.", "triple_list": [ [ "Plagioclase", "Distribution pattern", "Semi-self-shaped granular" ] ] }, { "text": "Developed wave-shaped interlaced stratigraphy, parallel stratigraphy in sandstone", "triple_list": [ [ "sandstone", "Develop", "Wavy interlaced layering" ], [ "sandstone", "Develop", "Parallel layering" ] ] }, { "text": "Gray thick layered gray matter fine egg rock 114.11m", "triple_list": [ [ "Gray thick layered gray matter fine egg rock", "thickness", "114.11m" ] ] }, { "text": "Volcanic lava and volcanic clastic rocks are commonly found in the late Permian strata. For example, the Jiashanite in the Tuoba Formation in the Changdu area is distributed in the area of Tronsai-Banaseranzhegawacheji-Jilayong, which is not integrated with the Lower Noribagaribao Formation, and the ligated group is not integrated.", "triple_list": [ [ "Late Permian strata", "Lithology", "Volcanic lava" ], [ "Late Permian strata", "Lithology", "Pyroclastic rock" ], [ "Chamdo", "Contained", "Tuoba Group" ], [ "Tuoba Group", "Lithology", "Andanyan" ], [ "Tuoba Group", "Exposed", "Tronsai-Banaseran Gawacheji-Girardong" ], [ "Tuoba Group", "Unconformity contact", "Nuoribagari protection group" ], [ "Tuoba Group", "Unconformity contact", "Ligation group" ] ] }, { "text": "The Batang group and ligation group in the late Triassic period (Polira group of the Gapila group) produce a large number of brachiopod bivalve fossils", "triple_list": [ [ "Batang Group of the Late Triassic World", "Paleontological", "Brachiopod" ], [ "Batang Group of the Late Triassic World", "Paleontological", "Bivalves" ], [ "Ligation group", "Outcrop", "Kapila Group" ], [ "Ligation group", "Outcrop", "Polira group" ], [ "Ligation group", "Paleontological", "Brachiopod" ], [ "Ligation group", "Paleontological", "Bivalves" ] ] }, { "text": "The measured profile of the Tronsai Late Permian-Early Triassic Volcanic Formation in Zhaqing Township, Zaduo County, Qinghai Province Ⅷ003P12.", "triple_list": [ [ "Tron Tournament in Zhaqing Township, Zaduo County, Qinghai Province", "Outcrop", "Late Permian-early Triassic Volcanic Formation" ] ] }, { "text": "Gray medium-thick layered powder shiny crystal containing biological clastic algae sand limestone with a small amount of dark gray medium-layered biological clastic limestone with gray green sandstone 151.30m", "triple_list": [ [ "Gray medium-thick layered powder shiny crystal containing biological clastic algae sand limestone with a small amount of dark gray medium-layered bioclad limestone with gray-green sandstone", "thickness", "151.30m" ] ] }, { "text": "Light gray block layered limestone 698.16m", "triple_list": [ [ "Light gray block layered limestone", "thickness", "698.16m" ] ] }, { "text": "The Bagong group is mainly distributed in Zhonggenyonghe Ranyeyongqu in the area. A small amount is exposed downstream of Ziqu, with a distribution area of about 50m2 and a thickness of 2234.26m.", "triple_list": [ [ "Bagong Group", "Exposed", "All the roots" ], [ "Bagong Group", "Exposed", "Yet, it also surging" ], [ "Bagong Group", "Exposed", "Ziqu" ], [ "Bagong Group", "area", "50m2" ], [ "Bagong Group", "thickness", "2234.26m" ] ] }, { "text": "Carbonate rock formation (3Bt3) This rock formation is distributed in the colorful group land-Shimagang group and Obadadong-Gajike area. The control thickness is greater than 1580.75m. It is a fault block produced in the fault zone. It is partially in integrated contact with the lower volcanic rock formation (3Bt2), but most of it is fault contact.", "triple_list": [ [ "Carbonate rock formation", "Exposed", "Colorful Group - Scared Magang Group" ], [ "Carbonate rock formation", "Exposed", "Obada-Gagiko" ], [ "Carbonate rock formation", "thickness", "1580.75m" ], [ "Carbonate rock formation", "Distribution pattern", "Faulted block" ], [ "Carbonate rock formation", "Integration of contacts", "Volcanic rock formation" ] ] }, { "text": "The carbonate rock formation test area is only in the area of the Ceratopsia, because the exposed formation is very poor.", "triple_list": [ [ "Carbonate rock formation", "Exposed", "Ceratops tooth race" ] ] }, { "text": "The Batang group is spread in the north, west and west directions of the RiArijiqu-Colorful Music-Niekaqu-Middle Tour-Zhengmoyong-Songmoyong. The exposed width is about 5m, and the east and west ends extend into the adjacent space respectively.", "triple_list": [ [ "Batang Group", "Distribution pattern", "North West and west" ], [ "Batang Group", "Exposed", "Sun A Ri Song - Colorful Song - Nie Ka Song - Zheng Moyong - Song Moyong" ], [ "Batang Group", "thickness", "5m" ] ] }, { "text": "Light gray medium-layer crystalline limestone 145.55m", "triple_list": [ [ "Light gray medium-layer crystalline limestone", "thickness", "145.55m" ] ] }, { "text": "The Batang group consists of two groups: volcanic rock and carbonate rock at the upper lower clastic rock.", "triple_list": [ [ "Batang Group", "Lithology", "Clastite" ], [ "Batang Group", "Lithology", "Volcanic rocks" ], [ "Batang Group", "Lithology", "Carbonate rock" ] ] }, { "text": "The actual measured stratigraphic profile of the Permian Gadikao Formation in Gongnayong Early Middle and Middle Gadikao Formation in Jiezha Township, Zaduo County, Qinghai Province is Ⅷ003P4, the geographical coordinates are 95°50′18, the north latitude is 33°06′09, the Elevation is 4829m; the end point is 95°53′15, the north latitude is 33°07′03, the elevation is 4674m.", "triple_list": [ [ "Gongnayong, Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Early and Middle-aged Permian Gadikao Group" ], [ "Early and Middle-aged Permian Gadikao Group", "Coordinates", "East longitude 95°50′18" ], [ "Early and Middle-aged Permian Gadikao Group", "Coordinates", "North latitude 33°06′09" ], [ "Early and Middle-aged Permian Gadikao Group", "Elevation", "4829m" ], [ "Early and Middle-aged Permian Gadikao Group", "Coordinates", "95°53'15 East longitude" ], [ "Early and Middle-aged Permian Gadikao Group", "Coordinates", "North latitude 33°07′03" ], [ "Early and Middle-aged Permian Gadikao Group", "Elevation", "4674m" ] ] }, { "text": "Porcelain is mainly plagioclase, followed by amphibole, with a content generally 15-25 and a particle size generally 0.5-2mm.", "triple_list": [ [ "Pyramid", "Contained", "Plagioclase" ], [ "Pyramid", "Contained", "Azurite" ], [ "Pyramid", "thickness", "0.5-2mm" ] ] }, { "text": "The Jielong Group distributed in the southeast corner of Saiyinlong area of the test area. The main body extends eastward from the picture. It is an extension of the layered section, producing rich cephalopods and bivalve fossils.", "triple_list": [ [ "The Silver Dragon in the Southeast Corner", "Outcrop", "Jilong Group" ], [ "Jilong Group", "Paleontological", "Cephalopod" ], [ "Jilong Group", "Paleontological", "Bivalves" ] ] }, { "text": "The clastic rock formation of the underwater volcanic rock under Geren volcanic rock showed fault contact, with a control thickness greater than 619.57m.", "triple_list": [ [ "Geren Volcano Rock", "Fault contact", "Clastic rock formation" ], [ "Geren Volcano Rock", "thickness", "619.57m" ] ] }, { "text": "No fossils were found in the sandstone slate interlayer formation of Bayanrola Mountains, but outside the picture, the Qinghai Provincial Comprehensive Geological Brigade in 1990, 50m outside the northeast corner of the survey area, bivalves were found, Plagiostoma nuitoense, Unionites Rapezoidalis, Palaeocardita rhomboidalis, and Halobia sp. The remains were found in the Ria Plutoki Palahelicorhaphe sp., Lachrgmatichnus sp.", "triple_list": [ [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Exposed", "50m outside the northeast corner of the test area" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Bivalves" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Plagiostoma nuitoense" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Unionites Rapezoidalis" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Palaeocardita rhomboidalis" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Halobia sp" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Exposed", "Buqu Upstream Day" ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Palahelicorhaphe sp." ], [ "Sandstone slate interlayer formation in Bayanolala Mountains", "Paleontological", "Lachrgmatichnus sp." ] ] }, { "text": "This field survey believes that this volcanic rock combination exists and the lateral lithology is relatively stable. The lithology is mainly mesophisticated volcanic lava and is interposed with mesophisticated volcanic rocks. It has terrestrial volcanic rock characteristics and has unconformity contact relationships at the bottom. It is covered by the angle of the Jiapila group of the Kaixinling Group of the Early and Middle Permian period.", "triple_list": [ [ "Volcanic rocks", "Lithology", "Mesoplasmic volcanic lava" ], [ "Volcanic rocks", "Lithology", "Mesoplasmic pyroclastic rock" ], [ "Volcanic rocks", "Unconformity contact", "The Permian Kaixinling Qun Noriba Garibao Group" ], [ "Volcanic rocks", "Unconformity contact", "Ninety teams" ], [ "Volcanic rocks", "Unconformity contact", "Late Triassic Ligation Group Kapila Group" ] ] }, { "text": "The ninety teams in the district were integrated with the appearance of large sets of limestone as the base boundary above the Noribagaribao Formation. They did not see the top. The angle of the Jiapila Formation was not integrated. The lithology was mainly dark gray powder crystal mud crystal limestone and a small amount of gray sandstone silt sandstone, which was a set of shallow marine limestone.", "triple_list": [ [ "Ninety teams", "Lithology", "Limestone" ], [ "Ninety teams", "Integration of contacts", "Nuoribagari protection group" ], [ "Ninety teams", "Unconformity contact", "Kapila Group" ], [ "Ninety teams", "Lithology", "Dark gray powder crystal mud crystal limestone" ], [ "Ninety teams", "Lithology", "Gray sandstone" ], [ "Ninety teams", "Lithology", "Siltstone" ], [ "Ninety teams", "Lithology", "shallow marine limestone" ] ] }, { "text": "Dark gray medium-thick layered coarse-grained rock fragment sandstone sandstone with a small amount of dark gray silty slate 384.79m", "triple_list": [ [ "Dark gray medium-thick layered coarse-grained rock fragment sandstone with a small amount of dark gray silty slabs", "thickness", "384.79m" ] ] }, { "text": "The rock types of Gadikao Formation are complex, and the whole is volcanic rocks and pyroclastic rocks.", "triple_list": [ [ "Gadikao Group", "Lithology", "Volcanic rocks" ], [ "Gadikao Group", "Lithology", "Pyroclastic rock" ] ] }, { "text": "Dark gray medium-thick layered medium-coarse-grained feldspar rock-cut quartz sandstone 114.60m", "triple_list": [ [ "Dark gray medium-thick layered medium-coarse-grained feldspar cuttings quartz sandstone", "thickness", "114.60m" ] ] }, { "text": "The clastic rock combinations are gray medium-thick layer fine-grained quartz sandstone mud calcareous slate slate and feldspar quartz sandstone silt sandstone.", "triple_list": [ [ "Clastic rock formation", "Lithology", "Gray medium-thick layer of fine-grained quartz sandstone" ], [ "Clastic rock formation", "Lithology", "Calcium slab" ], [ "Clastic rock formation", "Lithology", "Slate" ], [ "Clastic rock formation", "Lithology", "Feldspar quartz sandstone" ], [ "Clastic rock formation", "Lithology", "Siltstone" ] ] }, { "text": "Sandstone Develop, deformation stratigraphy and heavy load structure, common sandstone contains slate gravel chips, and inter-middle fold Develop", "triple_list": [ [ "sandstone", "Develop", "Deformed layering" ], [ "sandstone", "Develop", "Heavy load touch structure" ], [ "sandstone", "Contained", "Slate gravel chips" ], [ "sandstone", "Develop", "Wrinkles" ] ] }, { "text": "The Bayankala Mountain group exposed in the measurement area is divided into sandstone formation (2-3B) slate formation sandstone and slate interlayer sections (3B) equivalent to the central sandstone formation established by the rock formation in Qinghai Province, and the upper slate formation informal formation, with the era of mid-late III.", "triple_list": [ [ "Bayankala Mountain Group", "Outcrop", "Sandstone Formation" ], [ "Bayankala Mountain Group", "Outcrop", "Slate Formation" ], [ "Bayankala Mountain Group", "Outcrop", "Sandstone and slate interlayer sections" ], [ "Bayankala Mountain Group", "Age", "Third generation" ] ] }, { "text": "Gray contains silty slate, and produces cephalopod fossil Paraceratitesp. 259.6m", "triple_list": [ [ "Gray silty slabs", "Paleontological", "Paraceratitesp." ], [ "Gray silty slabs", "thickness", "259.6m" ] ] }, { "text": "A large number of bivalves represented by Halobia, fossils such as six-shot corals and well-preserved spore powder combinations were found on the southern edge of the Bayankala Basin along the southern part of the Tongtian River. Among the remains, the common genus Helminthopsis, Helminthoda, Megagraphton, Chondrites, etc. are important molecules in the Nereites phase divided by Seilacher (1963). They are produced together with the above fossils, reflecting that they may mainly represent the slope environment.", "triple_list": [ [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Bivalves" ], [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Six-shoot coral" ], [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Helminthopsis" ], [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Helminthoida" ], [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Megagraphon" ], [ "The southern edge of Bayankala Basin is along the southern part of Tongtian Henan", "Paleontological", "Chondrites" ] ] }, { "text": "Rocks are composed of porcine and matrix.", "triple_list": [ [ "rock", "Develop", "Pyramid" ], [ "rock", "Develop", "Substrate" ] ] }, { "text": "The wavy stratum of the Develop of slate is a basic sequential sequential sequence, with paleogenesis Develop, generally from 120°-270°.", "triple_list": [ [ "Slate", "Develop", "Corrugated stratum" ] ] }, { "text": "Therefore, the chronological stratigraphic units of the Jielong Formation are the Indian mid-Asian order of the Early and Middle Triassic.", "triple_list": [ [ "Jilong Group", "Age", "Early and Middle Triassic Indian Middle-Anisian Order" ] ] }, { "text": "The Dalong sandstone (chd) and the Chayong opalite (chop) Geren volcanic rock (chva) in the early and mid-Permian Obada limestone were in fault contact or tectonic interface of the physical and chemical belt. The north side was in fault contact with the Bayankara Mountains of Triassic, and the south side was in fault contact with the colorful opalene mixed rock (CPd), with a control thickness greater than 1110.04m.", "triple_list": [ [ "Dalong Sandstone", "Fault contact", "Chayong Ophiopolysite" ], [ "Dalong Sandstone", "Fault contact", "Geren Volcano Rock" ], [ "Dalong Sandstone", "Fault contact", "Obada limestone in the early and middle Permian" ], [ "Dalong Sandstone", "Fault contact", "The Triassic Bayankara Mountains" ], [ "Dalong Sandstone", "Lithology", "Colorful opal green mixed rocks" ], [ "Dalong Sandstone", "thickness", "1110.04m" ] ] }, { "text": "Gray block layered coarse-grained quartz sandstone 107.03m", "triple_list": [ [ "Gray block layered coarse quartz sandstone", "thickness", "107.03m" ] ] }, { "text": "Parallel stratification and a small amount of rolled stratification structure in siltstone", "triple_list": [ [ "Siltstone", "Develop", "Parallel layering" ], [ "Siltstone", "Develop", "Cover lamination" ] ] }, { "text": "Light gray block layered limestone 80.53m", "triple_list": [ [ "Light gray block layered limestone", "thickness", "80.53m" ] ] }, { "text": "Purple-red medium-thick layered complex conglomerate interlayer layered fine-grained feldspar quartz sandstone, partially intersected with a small amount of purple-red thin-layered submerged tuff, angle unconsolidated, 90 teams (P2j) of Kaixinling Group, Middle Permian 132.55m", "triple_list": [ [ "Purple-red medium-thick layered complex conglomerate interlayer layered fine-grained feldspar quartz sandstone", "Unconformity contact", "The 90-way team of the Kaixinling Group of the Middle Permian" ], [ "A small amount of purple-red thin layered tuff", "Unconformity contact", "The 90-way team of the Kaixinling Group of the Middle Permian" ], [ "The 90-way team of the Kaixinling Group of the Middle Permian", "thickness", "132.55m" ] ] }, { "text": "The newly established Chayong opalene mixed rock (ch) is a component of the Tongtian River opalene mixed rock established in the rock formations of Qinghai Province. It represents the material components of the Shangganzi-Litang Belt in the measurement area.", "triple_list": [ [ "Chayong ophiolula mixed rock", "Lithology", "Tongtian River opal green mixed rock" ], [ "Chayong ophiolula mixed rock", "Earth tectonic location", "Shangganzi-Litang Combination Belt" ] ] }, { "text": "The upper section is a large set of limestone, with a particularly horizontal stratigraphic Develop, and the basic stratigraphic sequence consisting of limestone and siltstone, reflecting that the shallow sea environment has fewer fossils and monotonous categories, mainly semi-plankton cephalopods. It belongs to the Tetis biota. Most of the fossils are found at the level and have the characteristics of different places. These characteristics indicate that this group is a semi-deep-sea sedimentary environment with reduced energy when sediment is deposited.", "triple_list": [ [ "Limestone", "Develop", "Horizontal stratification" ], [ "Limestone", "Lithology", "Siltstone" ], [ "Limestone", "Paleontological", "Cephalopod" ] ] }, { "text": "Dark gray thick layered silt sandstone silt silt silt silt sand with gray thick layered fine-grained quartz sand and gray thin layered limestone 263.57m", "triple_list": [ [ "Dark gray thick layered silt sandstone silt silt silt silt sand with gray thick layered fine-grained quartz sand and gray thin layered limestone", "thickness", "263.57m" ] ] }, { "text": "1:200,000 area adjusted the Carboniferous Clastozoic Clastodia group and the Kaixinling Jiujidao team contacted the Nuoribagaribao group, and the local ligation group Jiapila group did not integrate it.", "triple_list": [ [ "Carboniferous Clastozoic Rock Formation", "Integration of contacts", "Kaixinling Ninety Train Team" ], [ "Carboniferous Clastozoic Rock Formation", "Integration of contacts", "Nuoribagari protection group" ], [ "Carboniferous Clastozoic Rock Formation", "Unconformity contact", "Ligation group Apira group" ] ] }, { "text": "Light gray medium-thick layered breccia limestone 32.27m", "triple_list": [ [ "Light gray medium-thick layered breccia limestone", "thickness", "32.27m" ] ] }, { "text": "Gray-green sheet physical and chemical Qiangyangqi Petrochemical Green Mud Petrochemical Diaphragm Wall 143.08m", "triple_list": [ [ "Gray-green sheet physical and chemical Qiangyangqi Petrochemical Green Mud Petrochemical Diaphragm Wall", "thickness", "143.08m" ] ] }, { "text": "The rock formation in Qinghai Province (1997) continues to use this name and redefines the Jiujiu team as a stratigraphic body distributed on the northern slope of the Tanggula Mountains and is located between the Noribagaribao Formation and the Nayixiong Formation. It is composed of gray-dark gray carbonate rocks and a little clastic rocks, rich in fossils such as coral amaryllite bivalves and brachiopods.", "triple_list": [ [ "Ninety teams", "Exposed", "The northern slope of Tanggula Mountain" ], [ "Ninety teams", "Integration of contacts", "Nuoribagari protection group" ], [ "Ninety teams", "Integration of contacts", "Na Yixiong Group" ], [ "Ninety teams", "Lithology", "Ash - dark gray carbonate rock" ], [ "Ninety teams", "Lithology", "Clastite" ], [ "Ninety teams", "Paleontological", "dragonfly" ], [ "Ninety teams", "Paleontological", "coral" ], [ "Ninety teams", "Paleontological", "Chrysanthemum" ], [ "Ninety teams", "Paleontological", "Bivalves" ], [ "Ninety teams", "Paleontological", "Brachiopod" ] ] }, { "text": "The base boundary of the Jiapila Formation is bounded by the unconsolidation of complex conglomerates, and the emergence of large limestones is bounded by the integration of the Polila Formation.", "triple_list": [ [ "Kapila Group", "Unconformity contact", "Polygon" ], [ "Kapila Group", "Lithology", "Limestone" ], [ "Kapila Group", "Integration of contacts", "Polira group" ] ] }, { "text": "Geren volcanic rocks (chav) are mainly distributed in the Geren Kangba Rang Sairi Ariqu area in the test area. The volcanic rock formation in the Geren Kangba Rang Sairi Ariqu area is distributed in the Chayong Qu area. The lithogic gray-green andshanite volcanic breccia are acidic tuff lava and microcrystalline limestone and grey-thick layered metamorphic cleavage feldspar sandstone thousand-shaped slate feldspar sandstone limestone.", "triple_list": [ [ "Geren Volcano Rock", "Exposed", "Geren Kangba Ryan in Chayong area" ], [ "Geren Volcano Rock", "Lithology", "Gray green Andesan rock" ], [ "Geren Volcano Rock", "Lithology", "Volcanic breccia" ], [ "Geren Volcano Rock", "Lithology", "Medium acid tuff lava" ], [ "Geren Volcano Rock", "Lithology", "Microcrystalline limestone with gray thickness-medium-thin layered rock" ], [ "Geren Volcano Rock", "Lithology", "Chissite sandstone" ], [ "Geren Volcano Rock", "Lithology", "Thousand-shaped slabs" ], [ "Geren Volcano Rock", "Lithology", "Feldstone Sandstone" ], [ "Geren Volcano Rock", "Lithology", "Rock cuttings sandstone" ], [ "Volcanic rock formation", "Exposed", "Cha Yongqu" ] ] }, { "text": "The thickness of the upper section of the Jiapila Group (2j2) of the Jiapila Group is 590.07m", "triple_list": [ [ "Grey gray-purple fragmented sandstone of the Jiapila group", "Fault contact", "Jilong Group" ], [ "Jilong Group", "thickness", "590.07m" ] ] }, { "text": "Dark gray green almond-shaped basalt 51.91m", "triple_list": [ [ "Dark gray green almond-like basalt", "thickness", "51.91m" ] ] }, { "text": "Light gray thick-block layered limestone 82.85m", "triple_list": [ [ "Light gray thick-block layered limestone", "thickness", "82.85m" ] ] }, { "text": "Sandstone slate interlayer sections of the slate Formation (3B) According to the route and profile data, deformation slatting, coil slatting, heavy core model structure, groove model structure, and monotonous two-component interlayer structures, often with segments C and C-E in the Bauma sequence. No degeneration sequences representing segment A and segment B (developmental parallel slatting) that represent the dynamic products of the upper water flow are found.", "triple_list": [ [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Deformed layering" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Cover lamination" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Re-core model structure" ], [ "Sandstone slate interlayer section of Slate Formation", "Develop", "Groove model structure" ], [ "Sandstone slate interlayer section of Slate Formation", "Contained", "Bauma Sequence" ] ] }, { "text": "Carbonate rock formation (3Bt3) thickness 1580.75m", "triple_list": [ [ "Carbonate rock formation", "thickness", "1580.75m" ] ] }, { "text": "In the Qinghai Provincial Bureau of Geology and Minerals (1991), in the Qinghai Provincial Regional Geological Chronicle, the Batang Group (unspecified) was restricted to the northeast edge of the Tanggula Mountain, while the Kennan Group (unspecified) was divided into the Yushu-Zhongdian stratigraphic division.", "triple_list": [ [ "Batang Group", "Exposed", "Northeastern margin of Tanggula Mountain" ], [ "Kenan Group", "Stratigraphical zoning", "Yushu-Zhongdian Stratigraphic Zone" ] ] }, { "text": "Gray rhyolite sandwiched gray giant thick layered rhyolite tuff lava 164.46m", "triple_list": [ [ "Gray rhyolite with gray huge thick layered rhyolite tuff lava", "thickness", "164.46m" ] ] }, { "text": "Dark gray medium-thick layered fine-grained quartz sandstone with gray-black slate fault Carbonate rock formation (3Bt3) thickness 1149.44m", "triple_list": [ [ "Dark gray medium-thick layered fine-grained quartz sandstone with gray black slate", "Fault contact", "Carbonate rock formation" ], [ "Carbonate rock formation", "thickness", "1149.44m" ] ] }, { "text": "Late Permian-Early Triassic Volcanic Rock Formation geographical coordinates start at 95°07′03 east longitude, 33°15′30 north latitude, and Elevation is 4608m; end at 95°06′07 east longitude, 33°14′15 north latitude, and an elevation is 4463m. The overlying strata is the Late Triassic ligation group Jiapila Formation (3jp) The lithology is purple-red thick-layered complex medium conglomerate interspersed with purple-red medium-layered medium-fine-grained feldspar quartz sandstone. Angle unconsolidation Volcanic rock formation (P31h)", "triple_list": [ [ "Late Permian - Early Triassic Volcanic Formation", "Coordinates", "95°07'03 East longitude" ], [ "Late Permian - Early Triassic Volcanic Formation", "Coordinates", "33°15'30 North latitude" ], [ "Late Permian - Early Triassic Volcanic Formation", "Elevation", "4608m" ], [ "Late Permian - Early Triassic Volcanic Formation", "Coordinates", "95°06'07 East longitude" ], [ "Late Permian - Early Triassic Volcanic Formation", "Coordinates", "33°14′15 North latitude" ], [ "Late Permian - Early Triassic Volcanic Formation", "Elevation", "4463m" ], [ "Late Permian - Early Triassic Volcanic Formation", "Integration of contacts", "Late Triassic Ligation Group Kapila Group" ], [ "Late Triassic Ligation Group Kapila Group", "Lithology", "Purple-red thick layered complex gravel rock" ], [ "Late Triassic Ligation Group Kapila Group", "Lithology", "Purple-red medium-layered medium-fine-grained feldspar quartz sandstone" ], [ "Late Triassic Ligation Group Kapila Group", "Unconformity contact", "Volcanic rock formation" ] ] }, { "text": "The Bayankala Mountains have few fossils, monotonous species, and are mainly composed of bivalve brachiopods and cephalopods.", "triple_list": [ [ "Bayankala Mountain Group", "Paleontological", "Bivalves" ], [ "Bayankala Mountain Group", "Paleontological", "Brachiopod" ], [ "Bayankala Mountain Group", "Paleontological", "Cephalopod" ] ] }, { "text": "In this paper, an informal map filling unit, namely the Late Permian-Early Triassic Volcanic Rock Formation (P31h), is only distributed in the Ranzhawacheji-Gashaomunasa area in the measurement area. The rock combination is gray-green-gray-purple basalt andesite and mesobasic volcanic breccia breccia tuff with a small amount of rhyolite.", "triple_list": [ [ "Late Permian-early Triassic Volcanic Formation", "Exposed", "Ranzhe Gawacheji-Ga Shaomuna" ], [ "Late Permian-early Triassic Volcanic Formation", "Lithology", "Gray-green-gray-purple basalt" ], [ "Late Permian-early Triassic Volcanic Formation", "Lithology", "Mesoplasmic volcanic breccia" ], [ "Late Permian-early Triassic Volcanic Formation", "Lithology", "Breccia tuff with a small amount of rhizome" ] ] }, { "text": "Gray fine-grained conglomerate crushed sandstone sandstone with dark gray silty slate 180.31m", "triple_list": [ [ "Gray fine-grained conglomerate debris sandstone sandstone sandstone sandy slabs", "thickness", "180.31m" ] ] }, { "text": "Gray thick layered medium-fine-grained rock-cut feldspar sandstone 89.26m", "triple_list": [ [ "Gray thick layered medium-fine-grained feldspar sandstone", "thickness", "89.26m" ] ] }, { "text": "Dark purple medium-thick layered Ying'anite rock-crystal-crystal-crystal-tuff 54.85m", "triple_list": [ [ "Dark purple medium-thick layered Ying'anite crystalline tuff", "thickness", "54.85m" ] ] }, { "text": "In 1983, the Qinghai Second District Transfer Team conducted a 1:200,000-area transfer in Yushu. The lithology was a set of shallow-medium metamorphic clastic rocks and volcanic carbonate rocks with a thickness of up to 8189m.", "triple_list": [ [ "Yushu", "Outcrop", "Conan Group" ], [ "Conan Group", "Lithology", "shallow-medium metamorphic clastic rock" ], [ "Conan Group", "Lithology", "Volcanic rocks" ], [ "Conan Group", "Lithology", "Carbonate rock" ], [ "Conan Group", "thickness", "8189m" ] ] }, { "text": "The Carboniferous Clastozoic rock formation spreads in the northwest-south eastward direction in the measurement area.", "triple_list": [ [ "Carboniferous Clastozoic Rock Formation", "Distribution pattern", "Northwest-South East-East" ] ] }, { "text": "The ligation group in the test area from old to new is composed of the Porilla group and the Bagong group, with integrated contact between them, mainly distributed in the vast area of Kouqian Qu'angnong Quzijisai in the central and southern part of the test area.", "triple_list": [ [ "Ligation group", "Outcrop", "Kapila Group" ], [ "Ligation group", "Outcrop", "Polira group" ], [ "Ligation group", "Outcrop", "Bagong Group" ], [ "Ligation group", "Exposed", "Qu'ang'an's songs in front of the mouth" ] ] }, { "text": "Gray thick layered gray matter conglomerate sandwiched gray medium layered limestone 196.88m", "triple_list": [ [ "Gray thick layered gray matter conglomerate with gray medium layered limestone", "thickness", "196.88m" ] ] }, { "text": "Horizontal stratigraphy is particularly developed in sandstone. Due to the influence of tectonic transformation, the dense stratigraphy of the group tilted southward has been completely replaced in siltstone.", "triple_list": [ [ "sandstone", "Develop", "Horizontal stratification" ], [ "sandstone", "Develop", "Intensive cleavage" ] ] }, { "text": "Light gray green slime rock 51.32m", "triple_list": [ [ "Light gray green rock", "thickness", "51.32m" ] ] }, { "text": "The Jielong Formation is defined as gray (sticky) slate with limestone and sandstone. The lower limestone is more, and there is no top and bottom, including cephalopods and other fossils.", "triple_list": [ [ "Jilong Group", "Lithology", "Gray (touch) slate" ], [ "Jilong Group", "Lithology", "Limestone" ], [ "Jilong Group", "Lithology", "sandstone" ], [ "Jilong Group", "Paleontological", "Cephalopod" ] ] }, { "text": "The Qinghai Provincial Second Regional Transfer Team (1986) believed that in the 1:200, Wanzhiduo County area (I-46-[24]) regional geological survey report, the Batang Group was believed to be on top of the upper clastic rock, and accordingly, it divided the Batang Group into four points.", "triple_list": [ [ "Clastite", "Belongs to", "Batang Group" ], [ "Carbonate rock", "Belongs to", "Batang Group" ] ] }, { "text": "Brown-black strip-shaped magnetite-containing siliceous rock 115.31m", "triple_list": [ [ "Brown-black striped magnetite-containing siliceous rock", "thickness", "115.31m" ] ] }, { "text": "Ash-dark gray-thin-medium-thick layered medium-fine-grained quartz sandstone silt sandstone interlayer, containing plant fossils, 169.56m underlying strata Polila Formation gray-white block layered biological scale limestone.", "triple_list": [ [ "Gray-dark gray-thin-medium-thick layered medium-fine grain quartz sandstone silt sandstone interlayer", "Paleontological", "Plant fossils" ], [ "Gray-dark gray-thin-medium-thick layered medium-fine grain quartz sandstone silt sandstone interlayer", "thickness", "169.56m" ], [ "Gray-dark gray-thin-medium-thick layered medium-fine grain quartz sandstone silt sandstone interlayer", "Integration of contacts", "Polila Formation Ash-Oh-White Block Laminated Bioscale Limestone" ] ] }, { "text": "Paleozoites in the early and middle triassic periods are mainly distributed in the Jielong Group. The measurement area is the western extension of the group. There are relatively few paleozoite fossils, mainly distributed in the 1:25 million Yushu web on the east side of the map, producing abundant cephalopods and bivalve fossils.", "triple_list": [ [ "Paleontological of the Triassic Period in the Early and Middle Ages", "Located at", "Jilong Group" ], [ "Jilong Group", "Paleontological", "Cephalopod" ], [ "Jilong Group", "Paleontological", "Bivalves" ] ] }, { "text": "Gray-green all-green mud petrochemical Yangqi petrochemical olive pyroxene rock tectonics fault Dalong sandstone (chd) 83.28m", "triple_list": [ [ "Gray-green all-green petrochemical Yangqi petrochemical olive pyroxene rock", "Develop", "Structural sheet" ], [ "Gray-green all-green petrochemical Yangqi petrochemical olive pyroxene rock", "Fault contact", "Dalong Sandstone" ], [ "Dalong Sandstone", "thickness", "83.28m" ] ] }, { "text": "Triassic Bayankala Mountain Group (B) Beijing Institute of Geology (1961) established a strata composed of mud and sandy clastic rocks into the Bayankala Mountain Group in the Mado-Zhujie Temple area, which belongs to the Carboniferous period.", "triple_list": [ [ "Mado-Zhujie Temple", "Lithology", "mud sand clastic rock" ], [ "Mado-Zhujie Temple", "Outcrop", "Bayankala Mountain Group" ], [ "Bayankala Mountain Group", "Age", "Carboniferous period" ] ] }, { "text": "Slate is often weathered into sheet-like needle rod-like shape, and is intact with the sandstone formation of the underlying formation. The Neojin Quguo Formation is not integrated on it, with a control thickness greater than the thickness of 2417.17m and a distribution area of only 50m2. Its lithological combination is gray medium-thick layered medium-fine-grained feldspar rock-cut sandstone medium-thick layered fine-grained feldspar quartz sandstone gray thick layered coarse-grained rock-cut sandstone gray medium-thick layered fine-grained calcareous feldspar sandstone silt sandstone and dark gray silt slate argillary slate and calcareous slate. The rocks generally Contained pyrite crystals.", "triple_list": [ [ "Slate", "Integration of contacts", "Sandstone Formation" ], [ "Slate", "Unconformity contact", "New Jiquguo Group" ], [ "Slate", "thickness", "2417.17m" ], [ "Slate", "area", "50m2" ], [ "New Jiquguo Group", "Lithology", "Gray medium-thick layer medium-fine-grained feldspar" ], [ "New Jiquguo Group", "Lithology", "Chop sandstone" ], [ "New Jiquguo Group", "Lithology", "Medium-thick layered fine-grained feldspar quartz sandstone gray thick layered coarse-grained rock" ], [ "New Jiquguo Group", "Lithology", "Chop sandstone" ], [ "New Jiquguo Group", "Lithology", "Gray medium-thick layered fine-grained rock" ], [ "New Jiquguo Group", "Lithology", "Chissite sandstone" ], [ "New Jiquguo Group", "Lithology", "Gray medium layered fine-grained calcareous feldspar sandstone" ], [ "New Jiquguo Group", "Lithology", "Siltstone" ], [ "New Jiquguo Group", "Lithology", "Dark gray silty slab" ], [ "New Jiquguo Group", "Lithology", "Mud slate" ], [ "New Jiquguo Group", "Lithology", "Calcium slate" ], [ "New Jiquguo Group", "Develop", "Pyrite crystals" ] ] }, { "text": "Gray-gray-green-thick layered fog rock 85.98m", "triple_list": [ [ "Gray-gray-green-thick-titanium layered rock", "thickness", "85.98m" ] ] }, { "text": "Light gray male thick layered breccia limestone with light gray thick layered dolomite limestone 100.48m", "triple_list": [ [ "Light gray male thick layered breccia limestone with light gray thick layered dolomite limestone", "thickness", "100.48m" ] ] }, { "text": "Gray limestone 60.00m", "triple_list": [ [ "Gray limestone", "thickness", "60.00m" ] ] }, { "text": "The rock cuttings are composed of porcine crystals and matrix. The porcine crystal is composed of pyroxene and chlorite petrochemical plagioclase. The tuff matter 40-53 is mainly composed of Anshan basalt fragments less than 2mm, followed by plagioclase crystal chips, and a small amount of chlorite petrochemical pyroxime crystal chips are seen.", "triple_list": [ [ "Rock chips", "Contained", "Pyramid" ], [ "Rock chips", "Contained", "Substrate" ], [ "Pyramid", "Contained", "Pyrox" ], [ "Pyramid", "Contained", "Green mud petrochemical plagioclase" ], [ "Tuff", "Contained", "Anshan basalt rock chips" ], [ "Tuff", "Contained", "Platyrospar crystal chips" ], [ "Tuff", "Contained", "Celite petrochemical pyroxene crystal chips" ] ] }, { "text": "The distribution area of the Bayan Kala Mountains is about 789m2, and the maximum thickness is controlled at 5275.38-7458.27m.", "triple_list": [ [ "Bayankala Mountain Group", "area", "789m2" ], [ "Bayankala Mountain Group", "thickness", "5275.38-7458.27m" ] ] }, { "text": "Gray Flowing Ying'an Rock 68.63m", "triple_list": [ [ "Gray flowing Ying'an rock", "thickness", "68.63m" ] ] }, { "text": "There are granular stratigraphy and the bottom erosion surfaces in sandstone, there are parallel stratigraphy and a small amount of rolled stratigraphy structures in siltstone, and horizontal stratigraphy in slate.", "triple_list": [ [ "sandstone", "Develop", "Granular Sequence Laminating" ], [ "sandstone", "Develop", "Wash the surface" ], [ "Siltstone", "Develop", "Parallel layering" ], [ "Siltstone", "Develop", "Cover lamination" ], [ "Slate", "Develop", "Horizontal stratification" ] ] }, { "text": "The test area era was in the early stage of the late Triassic period.", "triple_list": [ [ "Test area", "Age", "Early Late Triassic" ] ] }, { "text": "Gray-green medium-thin layered crystal chip tuff 69.52m", "triple_list": [ [ "Gray-green medium-thin layered crystal chip chip tuff", "thickness", "69.52m" ] ] }, { "text": "Dark gray thin-layer silt sandstone is mixed with shale thin-layer quartz sandstone 57.30m.", "triple_list": [ [ "Dark gray thin layered silt sandstone with shale thin layered quartz sandstone", "thickness", "57.30m" ] ] }, { "text": "The late early Triassic granite developed on the southern side of this opaleum mixed rock. It is a set of arc granite in the subduction period of the opaleum mixed rock zone. It is a product of the concurrent tectonic action with the Dalong Sandstone (chd) Geren volcanic rock (chav). Its U-Pb isotope age is 214.88Ma, which can also represent the formation era of the Dalong Sandstone (chd) Geren volcanic rock (chav).", "triple_list": [ [ "Ophiolulu mixed rock", "Lithology", "Early Late Triassic Granite" ], [ "Subduction period of ophiolite mixed rock belt", "Lithology", "Arc granite" ] ] }, { "text": "In the 1986 regional geological survey report of the Qinghai Provincial Second Regional Serve Team (1986) divided the late Triassic strata on both sides of the Tongtian River into three rock groups: volcanic rocks in the middle of the lower clastic rock and carbonate rock and upper clastic rock.", "triple_list": [ [ "Late Triassic strata", "Lithology", "Clastite" ], [ "Late Triassic strata", "Lithology", "Volcanic rocks" ], [ "Late Triassic strata", "Lithology", "Carbonate rock" ], [ "Late Triassic strata", "Lithology", "Clastite" ] ] }, { "text": "Gray medium-thick layered bioclastic siliceous strip limestone with gray medium-layered limestone 231.29m", "triple_list": [ [ "Gray medium-thick layered bioclastic siliceous strip limestone with gray medium-layered limestone", "thickness", "231.29m" ] ] }, { "text": "Dark gray silt sandstone with gray medium-thick layered fine-grained quartz sandstone 836.96m", "triple_list": [ [ "Dark gray silt sandstone with gray medium-thick layered fine-grained quartz sandstone", "thickness", "836.96m" ] ] }, { "text": "Gray medium-layered biological clastic mud crystal limestone with gray layered mud crystal limestone, Weiyuanla sp., Unionite sp., Arestes cf.rothpletzi Welter 263.34m", "triple_list": [ [ "Gray medium-layered mud crystal limestone containing biological clastics and gray layered mud crystal limestone", "Paleontological", "Weiyuanla sp." ], [ "Gray medium-layered mud crystal limestone containing biological clastics and gray layered mud crystal limestone", "Paleontological", "Unionite sp." ], [ "Gray medium-layered mud crystal limestone containing biological clastics and gray layered mud crystal limestone", "Paleontological", "Arestes cf.rothpletzi Welter" ], [ "Gray medium-layered mud crystal limestone containing biological clastics and gray layered mud crystal limestone", "thickness", "263.34m" ] ] }, { "text": "The lithologies of the volcanic rock formation are mainly basalt Andshan basalt flux tuff lava flexural breccia tuff lava turtious lava turtious glazed clastic crystal tuff lava almond-like basalt sandstone siliceous rock mud limestone feldstone sandstone.", "triple_list": [ [ "Volcanic rock formation", "Lithology", "Basalt" ], [ "Volcanic rock formation", "Lithology", "Anshan basalt" ], [ "Volcanic rock formation", "Lithology", "Flow-grained tuff lava" ], [ "Volcanic rock formation", "Lithology", "Fluid breccia tuff lava" ], [ "Volcanic rock formation", "Lithology", "Ying'an glass chip tuff lava" ], [ "Volcanic rock formation", "Lithology", "Almond-shaped basalt" ], [ "Volcanic rock formation", "Lithology", "Pyroclastic rock" ], [ "Volcanic rock formation", "Lithology", "Silicone rock" ], [ "Volcanic rock formation", "Lithology", "Mud crystal limestone" ], [ "Volcanic rock formation", "Lithology", "Feldstone Sandstone" ] ] }, { "text": "Gray-brown rhizomorphic volcanic breccia 4.67m", "triple_list": [ [ "Gray-brown rhizomorphic volcanic breccia", "thickness", "4.67m" ] ] }, { "text": "Among them, the Claraia sp (Ker's clam) brachiopod fossils in the region are standard fossil molecules from the Early Triassic period and are distributed in the middle of the Xiahuancang Formation in Qilian, southern Qinghai.", "triple_list": [ [ "Claraia sp (Kerthy clam) brachiopod fossil", "Age", "Early Triassic" ], [ "Claraia sp (Kerthy clam) brachiopod fossil", "Located at", "Qinghai South Qilian Xiahuancang Group" ] ] }, { "text": "The rock combination is gray medium-thick layer of mud calcareous slate slate light purple-red (gravel-containing) coarse-medium-coarse-grained feldspar quartz sandstone with gray-red silt shale and volcanic rock.", "triple_list": [ [ "rock", "Lithology", "Gray medium-thick layer of mud calcium slab" ], [ "rock", "Lithology", "Slate" ], [ "rock", "Lithology", "Light purple-red (gravel-containing) coarse-medium coarse feldspar quartz sandstone" ], [ "rock", "Lithology", "Grey-red siltstone" ], [ "rock", "Lithology", "shale" ], [ "rock", "Lithology", "Volcanic rocks" ] ] }, { "text": "Local basalt and tuff are exposed layer by layer.", "triple_list": [ [ "Basalt", "Integration of contacts", "Tuff" ] ] }, { "text": "In 1959, the South-to-North Water Diversion Geological Brigade named a set of medium-shallow metamorphic rock system by Tongtian River in the Niantong River, and the era was included in the Early Paleozoic.", "triple_list": [ [ "Tongtian River", "Lithology", "shallow metamorphic rock system" ], [ "Tongtian River", "Outcrop", "Tongtianhe Group" ], [ "Tongtian River", "Age", "Early Paleozoic" ] ] }, { "text": "Early and Middle Permian Gadikao Group (P1-2gd) Thickness 1614.37m", "triple_list": [ [ "Early and Middle-aged Permian Gadikao Group", "thickness", "1614.37m" ] ] }, { "text": "The rock formation of Qinghai Province (1997) was revised by the Baiyankala Mountain Group after the Qinghai Provincial Survey Team in 1970, and defined it as a huge-thick strata distributed in the Kekexili-Bayankala area, which is almost entirely composed of sand slate. It is difficult to see the top and bottom. Occasionally, it is not integrated under the Nianbao Group above the Buqing Mountain Group.", "triple_list": [ [ "Bayankala Mountain Group", "Exposed", "Kekexili-Bayankala area" ], [ "Bayankala Mountain Group", "Lithology", "Sand slab" ], [ "Bayankala Mountain Group", "Unconformity contact", "Buqingshan Group" ], [ "Bayankala Mountain Group", "Unconformity contact", "Nianbao Group" ] ] }, { "text": "Ash-Gray-Grey-Grey-Grey-Grey-Alternated Pyroxene (Tectonic Block) 35.58m", "triple_list": [ [ "Ash-Grey Green Alternating Pyroxene", "Distribution pattern", "Tectonic rock blocks" ], [ "Ash-Grey Green Alternating Pyroxene", "thickness", "35.58m" ] ] }, { "text": "According to the above fossil combination, the era of the Batang group should be the late Triassic.", "triple_list": [ [ "Batang Group", "Age", "Late Triassic" ] ] }, { "text": "In 1997, the book on Rock Strata in Sichuan Province divided it into the Gangdagui Formation, and the era was classified as the Permian. This set of strata is widely compared with the lithologic Formation of Gadikao Formation in this area, so it is reasonable to classify this set of strata as the Early and Middle Permian.", "triple_list": [ [ "Gunda Overview Group", "Age", "Permian" ], [ "Gunda Overview Group", "Age", "Early and Middle Permian" ] ] }, { "text": "The Kapila Group era belongs to the early triassic period.", "triple_list": [ [ "Kapila Group", "Age", "Early Late Triassic" ] ] }, { "text": "The Jiushidao Team (P2j) is composed of Liu Guangcai (1993)'s Creation of Jiushidao Team is located in the Jiushidao area of Tanggulashan Township, Golmud City. It originally refers to gray dark gray powder crystal limestone biological shiny gravel gravel gravel limestone and dark gray thick layer of medium-fine-grain feldspar rock sandstone.", "triple_list": [ [ "Ninety teams", "Exposed", "Jiushidaoban area, Tanggulashan Township, Golmud City" ], [ "Ninety teams", "Lithology", "Gray dark gray powder limestone" ], [ "Ninety teams", "Lithology", "Bio-glitter gravel limestone" ], [ "Ninety teams", "Lithology", "Dark gray thick layer of medium-grained feldspar" ], [ "Ninety teams", "Lithology", "Chop sandstone" ] ] }, { "text": "The measurement area is only distributed in the area of the ceratopsia, extending to the northeast. Its main body is in the Yushu County area facing the east, with lithogenic gray slate sandstone sandstone and limestone conglomerates.", "triple_list": [ [ "Test area", "Located at", "Ceratops tooth race" ], [ "Test area", "Distribution pattern", "Block break" ], [ "Test area", "Distribution pattern", "Northeast extension" ], [ "Test area", "Lithology", "Gray slate" ], [ "Test area", "Lithology", "sandstone" ], [ "Test area", "Lithology", "Limestone" ], [ "Test area", "Lithology", "Polygon" ] ] }, { "text": "The ninety-dao teams were integrated on the Nuoribagaribao Formation, which was not integrated by the ligation group or the Tuotuohe Formation. The lithology in the test area was gray-black - gray thick layered limestone gray-black - dark gray bioclass limestone gray-class limestone sandstone sandstone and small amounts of medium-layer fine-grained feldspar quartz sandstone and siltstone.", "triple_list": [ [ "Ninety teams", "Integration of contacts", "Nuoribagari protection group" ], [ "Ninety teams", "Unconformity contact", "Ligation group" ], [ "Ninety teams", "Unconformity contact", "Tuotuohe Formation" ], [ "Ninety teams", "Lithology", "Gray-black - gray thick layered limestone" ], [ "Ninety teams", "Lithology", "Gray-black - dark gray bioclass limestone" ], [ "Ninety teams", "Lithology", "Gray clastic limestone" ], [ "Ninety teams", "Lithology", "Sand chip limestone" ], [ "Ninety teams", "Lithology", "Medium-layer fine-grained feldspar quartz sandstone" ], [ "Ninety teams", "Lithology", "Siltstone" ] ] }, { "text": "The pyrite crystals contained in rocks generally have a particle size of 0.5mm-1cm.", "triple_list": [ [ "rock", "Contained", "Pyrite crystals" ], [ "Pyrite crystals", "thickness", "0.5mm-1cm" ] ] }, { "text": "Gray-green pillow-shaped basalt 293.48m", "triple_list": [ [ "Gray-green pillow-shaped basalt", "thickness", "293.48m" ] ] }, { "text": "The Bagong Formation was in integrated contact with the Lower Bolila Formation and had a fault contact with the Gadikao Formation of the Kaixinling Group of the Permian period.", "triple_list": [ [ "Bagong Group", "Integration of contacts", "Polira group" ], [ "Bagong Group", "Fault contact", "Permian Kaixinling Group Gadikao Group" ] ] }, { "text": "The Jielong Group distributed in the southeast corner of Saiyinlong area of the test area, extending eastward from the picture.", "triple_list": [ [ "The Silver Dragon in the Southeast Corner", "Outcrop", "Jilong Group" ] ] }, { "text": "Gray medium-thick layer of physical and chemical fine-grained feldspar sandstone sandstone with gray thin layer of sericite 127.40m", "triple_list": [ [ "Gray medium-thick layer of physical and chemical fine-grained feldspar fragments sandstone with gray thin layer of sericite thousand rock", "thickness", "127.40m" ] ] }, { "text": "In 1993, the Qinghai Provincial and Regional Comprehensive Geological Brigade captured bivalve corals and remains fossils in the Yege area, which stretched 4m from the northeast corner of the test area.", "triple_list": [ [ "Ye Ge", "Paleontological", "Bivalves" ], [ "Ye Ge", "Paleontological", "coral" ], [ "Ye Ge", "Paleontological", "Ruins fossils" ] ] }, { "text": "The thickness of the sandstone monolayer is generally 10-30 cm, and the horizontal layer is developed in slate, containing mud sand and calcium tuberculosis.", "triple_list": [ [ "sandstone", "thickness", "10－30 ㎝" ], [ "Slate", "Develop", "Horizontal stratification" ], [ "Slate", "Develop", "Mud sand and calcium tuberculosis" ] ] }, { "text": "The lithology of the upper section of the Jielong Formation is gray-white thick-block layered shiny crystals containing biological clastic algae sand limestone.", "triple_list": [ [ "Jilong Group", "Lithology", "Off-white thick-layered shiny crystals containing biological detritus algae sand limestone" ] ] }, { "text": "The measured geological tectonic profile of Chayong ophiolite in Duocai Township, Zhiduo County, Qinghai Province is Ⅷ003P9. The starting point of the geographical coordinates is 95°22′20 east longitude, 33°56′11 north latitude, and Elevation is 4943m; the end point is 96°20′20 east longitude, 33°53′44 north latitude, and Elevation is 4464m.", "triple_list": [ [ "Zhiduo County Duocai Township, Qinghai Province", "Lithology", "Chayong ophiolula mixed rock" ], [ "Cha Yong Ophio-green mixed", "Coordinates", "95°22'20 East longitude" ], [ "Cha Yong Ophio-green mixed", "Coordinates", "33°56′11 North latitude" ], [ "Cha Yong Ophio-green mixed", "Elevation", "4943m" ], [ "Cha Yong Ophio-green mixed", "Coordinates", "96°20′20 East longitude" ], [ "Cha Yong Ophio-green mixed", "Coordinates", "33°53′44 North latitude" ], [ "Cha Yong Ophio-green mixed", "Elevation", "4464m" ] ] }, { "text": "Dark gray medium-thick layered fine-grained feldspar quartz sandstone with gray black silty carbonaceous slate thickness 1896.15m", "triple_list": [ [ "Dark gray medium-thick layered fine-grained feldspar quartz sandstone with gray black silty carbonaceous slate", "thickness", "1896.15m" ] ] }, { "text": "Due to the limited exposure area, the vertical and horizontal changes are not large. The rocks of the Jiapila Formation basically did not show recrystallization, and only local fragmentation caused by tectonic extrusion was seen near the segmental fracture zone and inside the rock. Therefore, the degree of metamorphism was slight. The rock type was internal clastic biological clastic limestone, and a small amount of sand clastic oligite limestone was seen, and a small amount of mesoplasmic volcanic rock was partially interspersed with a small amount of mesoplasmic volcanic rock.", "triple_list": [ [ "Kapila Group", "Lithology", "Internal detritus bioclass limestone" ], [ "Kapila Group", "Lithology", "Sand chip oasis limestone" ], [ "Kapila Group", "Lithology", "Mesoplasmic volcanic rocks" ] ] }, { "text": "The distribution in the area is limited, with a small block, which is only seen in the area of Tronsegawacheji. The surrounding angle is unconsistent contact is above the 90 teams of the Noribagaribao Group of Kaixinling Group. The Jiapila Group is ligated on it, which has an angle unconsistent contact, local fault contact, with a distribution area of 38m2 and a controlled thickness of 1732.24m. Its lithology is strongly altered from gray-green gray-purple color apricot-like olive basalt to almond-like andesite, and carbonate androsite basalt-based lithotrid tuff fume volcanic breccia interspersed with normal deposited gray-purple medium-thick layered medium-fine feldspar quartz interspers.", "triple_list": [ [ "In the area", "Distribution pattern", "Block" ], [ "In the area", "Exposed", "Tron Saiga Wacheji" ], [ "In the area", "Unconformity contact", "Kaixinling Qun Noriba Garibao Group Ninety-Dada Team" ], [ "In the area", "Unconformity contact", "Ligation group Apira group" ], [ "In the area", "area", "38m2" ], [ "In the area", "thickness", "1732.24m" ], [ "In the area", "Lithology", "Gray-green gray-purple altered almond-like olive basalt" ], [ "In the area", "Lithology", "Almond-shaped andshan rock" ], [ "In the area", "Lithology", "Carbonated Andesite" ], [ "In the area", "Lithology", "Basal rock" ], [ "In the area", "Lithology", "Clextuff" ], [ "In the area", "Lithology", "Fluidic cortical tuff" ], [ "In the area", "Lithology", "Volcanic breccia" ], [ "In the area", "Lithology", "Gray-purple Medium-thick layered medium-fine-grained feldspar quartz interlayer" ] ] }, { "text": "The sandstone formation contains few organisms, and the fossils of the relics on the region reflect the relics combination in deep water environment. They are the relics of Nereites. Members Phycosiphon incertum, Planalites montanus, etc.", "triple_list": [ [ "Sandstone Formation", "Belongs to", "Nereites ruins" ], [ "Sandstone Formation", "Paleontological", "Phycosiphon incertum" ], [ "Sandstone Formation", "Paleontological", "Planalites montanus" ] ] }, { "text": "On the east side, 1:200,000 Yushu has a rich range of cephalopods and bivalves.", "triple_list": [ [ "Yushu", "Paleontological", "Triassic cephalo" ], [ "Yushu", "Paleontological", "Bivalves" ] ] }, { "text": "Gray-green medium-thick layered Yingami glass chip melted tuff, gray-green thin-layered Yingami complex chip melted tuff, 57.36m", "triple_list": [ [ "Gray-green medium-thick layered Yingami glass chip fusion tuff intersected with gray-green thin-layered Yingami complex chip fusion tuff", "thickness", "57.36m" ] ] }, { "text": "The rock formation in Qinghai Province continues to use the Batang group to maintain the distribution range of the original Ba Group, and is temporarily based on the three-part scheme (informal), and is defined as a strata distributed in the Xijin Wulan Lake-Yushu area, composed of clastic volcanic rocks and carbonate rocks. It is difficult to reach the top without bottoming, and there is local unconsolidation contact with the wind volcanic group, including bivalve cephalopods and brachiopods.", "triple_list": [ [ "Batang Group", "Stratigraphical zoning", "Xijin Wulan Lake-Yushu area" ], [ "Batang Group", "Lithology", "Clastite" ], [ "Batang Group", "Lithology", "Volcanic rocks" ], [ "Batang Group", "Lithology", "Carbonate rock" ], [ "Batang Group", "Unconformity contact", "Wind Volcano Group" ], [ "Batang Group", "Paleontological", "Bivalves" ], [ "Batang Group", "Paleontological", "Cephalopod" ], [ "Batang Group", "Paleontological", "Brachiopod" ] ] }, { "text": "Dark gray medium-thick layered fine-grained sandstone with grayish white biological clastic limestone angle unconsolidated Paleogene Quguo Formation (Nq) brick red conglomerate 19.89m", "triple_list": [ [ "Dark gray medium-thick layered fine-grained sandstone with off-white bioclad limestone", "Unconformity contact", "Paleogene Quguo Formation (Nq) brick red gravel" ], [ "Dark gray medium-thick layered fine-grained sandstone with off-white bioclad limestone", "thickness", "19.89m" ] ] }, { "text": "The middle class of the formation Paraceratite sp., and bivalve Hallobia sp., in its appearance, are Ladinian Japonitis yushusnsis. Baltonitis gracilis. B. disparicos tatus. Xizangemsis. Acrochodicera cf.", "triple_list": [ [ "Strata", "Paleontological", "Paraceratite sp." ], [ "Strata", "Paleontological", "bivalve Hallobia sp." ], [ "Strata", "Paleontological", "Ladinian Japonitis yushusnsis." ], [ "Strata", "Paleontological", "Baltonitis gracilis." ], [ "Strata", "Paleontological", "B. disparicos tattoo." ], [ "Strata", "Paleontological", "Xizangemsis." ], [ "Strata", "Paleontological", "Acrochodicera cf." ] ] }, { "text": "Gray medium-layered medium-grained rock-cut feldspar sandstone with gray thin layer fine-grained feldspar sandstone and dark gray silty slate 140.87m", "triple_list": [ [ "Gray medium-layered medium-grained rock-cut feldspar sandstone with gray thin-layer fine-grained feldspar sandstone and dark gray silty slabs", "thickness", "140.87m" ] ] }, { "text": "Purple-red fine-grained feldspar sandstone 179.07m", "triple_list": [ [ "Purple-red fine-grained feldspar sandstone", "thickness", "179.07m" ] ] }, { "text": "In the areas of Batang Poges and Dangjiezhenla, Sichuan Province, a set of limestones with basic volcanic rocks were exposed.", "triple_list": [ [ "Batang Poges and Dangjiezhenla, Sichuan Province", "Lithology", "Basic volcanic rocks" ], [ "Batang Poges and Dangjiezhenla, Sichuan Province", "Lithology", "Limestone" ] ] }, { "text": "Gray-purple thin - Medium-layered medium-grained rock-cut sandstone with gray-green thin - Medium-layered medium-grained rock-cut feldspar sandstone 4.90m", "triple_list": [ [ "Gray-purple thin-medium-layered medium-grained rock-cut sandstone with gray-green thin-medium-layered medium-grained rock-cut feldspar sandstone", "thickness", "4.90m" ] ] }, { "text": "Gray-green medium-thick layered Ying'an compound chip melted tuff 205.89m", "triple_list": [ [ "Gray-green medium-thick layered Ying'an compound chip melted tuff medium-layered Ying'an slurry melted tuff", "thickness", "205.89m" ] ] }, { "text": "1:200 Wanzaduo County District Report divided a set of upper Permian volcanic rock formations with the main lithologies of gray-green-gray-purple basalt andesites and mesobasic volcanic breccia breccia tuffs with a small number of rhyolite formations, but no further work was done.", "triple_list": [ [ "Upper Permian Volcanic Rock Formation", "Lithology", "Gray-green-gray-purple basalt" ], [ "Upper Permian Volcanic Rock Formation", "Lithology", "Andanyan" ], [ "Upper Permian Volcanic Rock Formation", "Lithology", "Mesoplasmic volcanic breccia" ], [ "Upper Permian Volcanic Rock Formation", "Lithology", "breccia tuff" ], [ "Upper Permian Volcanic Rock Formation", "Lithology", "Rhyolite" ] ] }, { "text": "Gray serous quartz schist with dark gray serous green mud schist (tectonic block) 56.40m", "triple_list": [ [ "Gray serous quartz schist with dark gray serous green mud schist", "Distribution pattern", "Tectonic rock blocks" ], [ "Gray serous quartz schist with dark gray serous green mud schist", "thickness", "56.40m" ] ] }, { "text": "Carolinae is commonly found in the Anisian-Ladinian strata in the Alps, Poland, Hungary, Japan, Canada, Yunnan, Guizhou, Sichuan, Tibet and southern Qinghai, my country, but is more common in the Anisian period. Therefore, the era of the Jielong Formation was the Middle Triassic.", "triple_list": [ [ "Carolinae", "Exposed", "Alps" ], [ "Carolinae", "Exposed", "Poland" ], [ "Carolinae", "Exposed", "Hungary" ], [ "Carolinae", "Exposed", "Japan" ], [ "Carolinae", "Exposed", "Canada" ], [ "Carolinae", "Exposed", "Yunnan" ], [ "Carolinae", "Exposed", "Guizhou" ], [ "Carolinae", "Exposed", "Sichuan" ], [ "Carolinae", "Exposed", "Tibet" ], [ "Carolinae", "Exposed", "Southern Qinghai" ], [ "Jilong Group", "Age", "Middle Triassic" ] ] }, { "text": "The ligation group is divided from top to bottom into three rock groups: the purple-red clastic rock formation carbonate rock formation and the coal-containing clastic rock formation.", "triple_list": [ [ "Ligation group", "Outcrop", "Purple-red clastic rock formation" ], [ "Ligation group", "Outcrop", "Carbonate rock formation" ], [ "Ligation group", "Outcrop", "Coal-containing clastic rock formation" ] ] }, { "text": "Gray-dark gray thick layered silty silt marl limestone with gray-green sheets Physical and chemical calcified silt sandstone integration Jielong Formation lower section (2j1) 151.31m", "triple_list": [ [ "Gray-dark gray thick layered silt mud limestone with gray-green sheet physical and chemical calcified silt sandstone", "Integration of contacts", "Jilong Group" ], [ "Jilong Group", "thickness", "151.31m" ] ] }, { "text": "Light gray thin layer of sericite 100-shaped schist 42.63m", "triple_list": [ [ "Light gray thin layer of sericite schist", "thickness", "42.63m" ] ] }, { "text": "Gray purple medium-thick layered medium-grained rock-cut feldspar sandstone with gray purple medium-layered fine-grained feldspar sandstone 1.81m", "triple_list": [ [ "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone with gray-purple medium-layered fine-grained feldspar sandstone", "thickness", "1.81m" ] ] }, { "text": "Gray mud slate 167.8m", "triple_list": [ [ "Gray mud slate", "thickness", "167.8m" ] ] }, { "text": "Dark purple medium-thick layered silt sandstone with gray-green thick layer of mud-containing calcium slate 42.91m", "triple_list": [ [ "Dark purple medium-thick layered silt sandstone with gray-green thick layer of mud-containing calcium slab", "thickness", "42.91m" ] ] }, { "text": "Gray thin layered medium-coarse-grained rock-cut feldspar quartz sandstone 460.84m", "triple_list": [ [ "Gray thin layered medium-coarse-grained feldspar quartz sandstone", "thickness", "460.84m" ] ] }, { "text": "Asymmetrical wave marks are developed in sandstone, with heavy heavy die and groove mold structure on the bottom layer", "triple_list": [ [ "Sandstone", "Develop", "Asymmetric wave marks" ], [ "Sandstone", "Develop", "Dual Heat Module" ], [ "Sandstone", "Develop", "Groove model structure" ] ] }, { "text": "The front curve of the mouth in the measurement area is mainly gray light gray-white mud-crystal shiny biological clastic limestone, and is sandwiched with andesite and mesobasic tuff in the Buqu area.", "triple_list": [ [ "Pre-mouth", "Lithology", "Gray light gray white mud crystal shiny bioclad limestone" ], [ "Butu", "Lithology", "Andanyan" ], [ "Butu", "Lithology", "Mesobasic tuff" ] ] }, { "text": "The east-bound 1:25 Wan Yushu area is equivalent to the paleobiological fossils obtained in this strata, Duplexisporites, Annulispora; Geadigondolella tethydis, Neogondolella mommbergensis combination, commonly found in North America, Europe and my country's Yunnan, Guizhou, Qinghai-Tibet Plateau,", "triple_list": [ [ "Yushu", "Paleontological", "Duplexisporites" ], [ "Yushu", "Paleontological", "Annulispora" ], [ "Yushu", "Paleontological", "Geadigondolella tethydis" ], [ "Yushu", "Paleontological", "Neogondolella mommbergensis" ] ] }, { "text": "The sedimentary era of the Carnate Formation of the Batang Clerotite Formation in the test area was the Carnia-Norian period of the Late Triassic period.", "triple_list": [ [ "Batang Clastomorph", "Age", "Carnia-Norian Period of Late Triassic" ], [ "Carbonate rock formation", "Age", "Carnia-Norian Period of Late Triassic" ] ] }, { "text": "The Bayankala Mountain Group did not see the bottom and was integrated with the slate sandstone section of the above-mentioned slate formation (Figure 2-31). The emergence of a large amount of silty slate overlying is used as the base boundary of the overlying strata.", "triple_list": [ [ "Bayankala Mountain Group", "Integration of contacts", "Slate sandstone section" ], [ "Bayankala Mountain Group", "Integration of contacts", "Silty slab" ], [ "Bayankala Mountain Group", "Integration of contacts", "Mud slate" ] ] }, { "text": "The section of the Zhonggenyong Late Triassic Bagong Formation in Zhaqing Township, Zaduo County, Qinghai Province was revised and tested. This section was 1:200,000 area adjustment data, and the fault at the end of the section was the content of this work review.", "triple_list": [ [ "Zhonggenyong, Zhaqing Township, Zaduo County, Qinghai Province", "Outcrop", "Bagong Group of the Late Triassic" ] ] }, { "text": "Gray sheet physical and chemical fine-grained feldquartz sandstone sandstone clamped dark gray silty slate 123.77m", "triple_list": [ [ "Gray sheet physical and chemical fine-grained feldquartz sandstone sandstone sandstone sandy slab", "thickness", "123.77m" ] ] }, { "text": "The Bolila Formation was introduced in the first rock formation in Qinghai Province. At the same time, the definition of the Tibet strata cleaning form is mainly defined as a set of limestone formations sandwiched between the red clastic rock of the Jiapila Formation of the underside and the coal-containing clastic rock of the Bagong Formation. The upper and lower boundaries are integrated contact, and are rich in bivalve brachiopod ammonites, etc., distributed in the Daandotumengra, Dahandu River, and the Tanggula Mountains of Qinghai Province.", "triple_list": [ [ "Polira group", "Integration of contacts", "Red clastic rock of the Gapila group" ], [ "Polira group", "Integration of contacts", "Bagong Formation Coal Clastola" ], [ "Polira group", "Lithology", "Limestone" ], [ "Polira group", "Paleontological", "Bivalves" ], [ "Polira group", "Paleontological", "Brachiopod" ], [ "Polira group", "Paleontological", "Ammonites" ], [ "Polira group", "Exposed", "Chamdo Uzicha Yajiang Daando Tumengra" ], [ "Polira group", "Exposed", "Tanggula Mountain area of Qinghai Province" ] ] }, { "text": "Gray medium-thick layered crystalline limestone with thickness 65.95m Integration Gapella Formation Dark gray thin layered calcareous silt sandstone with gray thin layered medium-fine grain feldstone", "triple_list": [ [ "Gray medium-thick layered crystalline limestone", "thickness", "65.95m" ], [ "Gray medium-thick layered crystalline limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "Lithology", "Dark gray thin layered calcium silt sandstone" ], [ "Kapila Group", "Lithology", "Gray thin layered medium-fine-grained feldspar sandstone" ] ] }, { "text": "Gray green and thin - Medium-layered Ying-A-based compound chip melted tuff 103.10m", "triple_list": [ [ "Gray-green struggle for thinness - Medium-layered Ying-A-based compound chip melted tuff", "thickness", "103.10m" ] ] }, { "text": "Gray-green pillow-shaped basalt 36.66m", "triple_list": [ [ "Gray-green pillow-shaped basalt", "thickness", "36.66m" ] ] }, { "text": "Gray-green Yangqi petrochemical pillow-shaped basalt 384.80m", "triple_list": [ [ "Gray-green sun-rock petrified pillow-shaped basalt", "thickness", "384.80m" ] ] }, { "text": "Tuotuohe Formation Gray-red Thick Laminated Gray-Matter Congliding Rock with a thickness of 1789.98m", "triple_list": [ [ "Tuotuohe Formation of Gray-red Thick Laminated Gray-Matter Grotto Rock", "thickness", "1789.98m" ] ] }, { "text": "Gray silt-shaped slate with marble, producing bivalve fossils Halobiasp. 239.9m", "triple_list": [ [ "Gray slate with silt sand marble", "Paleontological", "Bivalve fossils Halobiasp." ], [ "Gray slate with silt sand marble", "thickness", "239.9m" ] ] }, { "text": "Volcanic breccia have the same composition as lava, with a size of 5-20mm and a content of 30.", "triple_list": [ [ "Volcanic horns", "thickness", "5-20mm" ] ] }, { "text": "Volcanic breccia rocks are gray-green, with patchy structures and volcanic breccia structures, and the matrix has an interwoven-particle structure.", "triple_list": [ [ "Volcanic breccia", "Distribution pattern", "Spotted structure" ], [ "Volcanic breccia", "Distribution pattern", "Volcanic Breccia Structure" ], [ "Volcanic breccia", "Distribution pattern", "Interleaving-particle structure" ] ] }, { "text": "Gray-purple medium-thick layered medium-grained rock-cut feldspar sandstone 9.70m", "triple_list": [ [ "Gray-purple medium-thick layered medium-grained cuts feldspar sandstone", "thickness", "9.70m" ] ] }, { "text": "Yellow-brown thin-layer fine-grained feldspar quartz sandstone and dark gray silty slate interlayer 104.66m", "triple_list": [ [ "Yellow-brown thin-layered fine-grained feldspar quartz sandstone and dark gray silty slate interlayer", "thickness", "104.66m" ] ] }, { "text": "The volcanic rock formation is distributed in a northwest-south eastward band in the measurement area, and the petrochemical rock geochemistry reflects the characteristics of calcium-alkaline island arc volcanic rocks.", "triple_list": [ [ "Volcanic rocks", "Distribution pattern", "Northwest-southeast-eastern belt distribution" ] ] }, { "text": "Gray medium-layered sand chip limestone 85.09m", "triple_list": [ [ "Gray medium-layered sand chip limestone", "thickness", "85.09m" ] ] }, { "text": "Gray medium-layered lithotrix quartz sandstone with gray-green silty slate thickness 619.57m", "triple_list": [ [ "Gray medium-layered lithotrix quartz sandstone with gray-green silty slab", "thickness", "619.57m" ] ] }, { "text": "Since the fossils collected in the section are concentrated in the middle and lower parts, the upper part is relatively thick, the possibility of middle Permian cannot be ruled out.", "triple_list": [ [ "profile", "Age", "Medium Perm" ] ] }, { "text": "The Permian Gadikao Group (P1-2gd) Qinghai Province Second Region Transfer Team (1982) created the famous Gadikao Group in Gadikao County in Zaduo County.", "triple_list": [ [ "Gadikao Group", "Exposed", "Zaduo County Gadikao" ] ] }, { "text": "The cephalopods east of the test area, Paraceratite sp. and bivalve Hallobia sp., were in the Middle Triassic.", "triple_list": [ [ "Cephalopod Paraceratite sp.", "Age", "Middle Triassic" ], [ "bivalve Hallobia sp.", "Age", "Middle Triassic" ] ] }, { "text": "Light gray-green-gray medium-fine-grain feldspar quartz-to-sandstone feldspar to sandstone and silty slate 82.2m", "triple_list": [ [ "Light gray-green-gray medium-fine-grain feldspar quartz turns into sandstone feldspar sandstone and silty slab", "thickness", "82.2m" ] ] }, { "text": "Dalong Sandstone (chd) thickness 1110.04m", "triple_list": [ [ "Dalong Sandstone", "thickness", "1110.04m" ] ] }, { "text": "Dark gray calcium silty slate 39.88m", "triple_list": [ [ "Dark gray calcium silty slab", "thickness", "39.88m" ] ] }, { "text": "The section VIII003P15 of the late Triassic Batang Group of Niechaqu, Duocai Township, Zhiduo County, Qinghai Province (Figure 2-39), the section position starts at 95°35′54 east longitude, 33°39′21 north latitude, and Elevation is 4313m; the end point is 95°23′49 east longitude, 33°36′52 north latitude, and an elevation is 4583m.", "triple_list": [ [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Contained", "Batang Group of the Late Triassic World" ], [ "Batang Group of the Late Triassic World", "Coordinates", "95°35'54 East longitude" ], [ "Batang Group of the Late Triassic World", "Coordinates", "33°39′21 North latitude" ], [ "Batang Group of the Late Triassic World", "Elevation", "4313m" ], [ "Batang Group of the Late Triassic World", "Coordinates", "95°23'49 East longitude" ], [ "Batang Group of the Late Triassic World", "Coordinates", "33°36′52 North latitude" ], [ "Batang Group of the Late Triassic World", "Elevation", "4583m" ] ] }, { "text": "The thickness of the formation rock layer near the land margin is thick-thick layered, with a single layer of sandstone ranging from 50-200cm, and a silt sandstone mud slate thickness of 20-40cm, and weak deformation (Part 1). Its basic stratigraphic sequence reflects the characteristics of degenerate stratigraphic sequence.", "triple_list": [ [ "Strata", "Lithology", "sandstone" ], [ "Strata", "Lithology", "Silty sandstone mud slate" ], [ "Strata", "Lithology", "Mud slate" ] ] }, { "text": "Gray-green sheet physical and chemical tuff 25.63m", "triple_list": [ [ "Physical and chemical tuff in gray-green sheet", "thickness", "25.63m" ] ] }, { "text": "Granular stratigraphy and bottom brush surfaces are seen in sandstone", "triple_list": [ [ "sandstone", "Develop", "Granular Sequence Laminating" ], [ "sandstone", "Develop", "Cutting face" ] ] }, { "text": "There are trough-type interlaced stratigraphy separated by eroded surfaces in the sandstone, and the interlaced stratigraphy direction indicates the direction of the ancient water flow toward the south.", "triple_list": [ [ "sandstone", "Develop", "Groove interlaced layering" ] ] }, { "text": "The Batang Group strata now refers to a set of gray-purple gray clastic grey carbonate rock formations distributed south of the opalite mixed zone of Tongtian River and north of the Late Triassic ligation group.", "triple_list": [ [ "Batang Group", "Exposed", "South of the ophiolite mixed zone of Tongtian River" ], [ "Batang Group", "Exposed", "North of the Late Triassic Ligation Group" ], [ "Batang Group", "Lithology", "Gray purple grey clastic rock" ], [ "Batang Group", "Lithology", "Grey carbonate rock" ] ] }, { "text": "Parallel layers of particles develop in sandstone and have a flame structure.", "triple_list": [ [ "sandstone", "Develop", "Parallel layer particles" ], [ "sandstone", "Develop", "Flame structure" ] ] }, { "text": "Gray-green green mud schist (andestone) 45.6m", "triple_list": [ [ "Gray-green green mud schist (andestone)", "thickness", "45.6m" ] ] }, { "text": "Ying'anite is grayish white or light gray, with a plodic structure, the matrix has a particle mosaic structure and a cryptocrystalline structure, and the rock consists of two parts: pollastic crystal and matrix.", "triple_list": [ [ "Ying'an Rock", "Distribution pattern", "Spotted structure" ], [ "Ying'an Rock", "Distribution pattern", "Particle mosaic structure" ], [ "Ying'an Rock", "Distribution pattern", "Crystal structure" ], [ "Ying'an Rock", "Contained", "Pyramid" ], [ "Ying'an Rock", "Contained", "Substrate" ] ] }, { "text": "The thickness of the junction group is 1420.4m", "triple_list": [ [ "Jilong Group", "thickness", "1420.4m" ] ] }, { "text": "The Jiapila group is not integrated with the ninety teams of the Noribagaribao group in the early and middle stages of the Permian, and the Polira group containing a large number of brachiopods in the late Triassic period are integrated.", "triple_list": [ [ "Kapila Group", "Unconformity contact", "Early and Middle Permian Noribagaribao Group" ], [ "Kapila Group", "Unconformity contact", "Ninety teams" ], [ "Kapila Group", "Integration of contacts", "Polira group" ], [ "Late Triassic Brachiopod", "Belongs to", "Polira group" ] ] }, { "text": "The ninety-track team contained a large number of fossils, Neoschwangerina craticulifera (Schwager), Neoschwangerina megaspherica Deprat, Verbeeina heimi hompson, Yabeina inouyei Deprat, Parafusulina yunnanica, Pseudofusulina gruperaensis (hompson), Parafusulina vulgaris (Schellwien), Parafusulina upchra Sheng, Yangchinia compressa (Ozawa), Chalaroschwangerina sp. Brachial foot; Dictyoclistus cf. semireticulatus(Mattin), Enteletes sp., Orthotetina sp. Ammonite Epadrites timornsis var. involutus (Haniel) Coral Liangshanophyllum sp.Wentzelella sp.", "triple_list": [ [ "Ninety teams", "Paleontological", "Neoschwangerina craticulifera (Schwager)" ], [ "Ninety teams", "Paleontological", "Neoschwangerina megaspherica Deprat" ], [ "Ninety teams", "Paleontological", "Verbeeina heimi hompson" ], [ "Ninety teams", "Paleontological", "Yabeina inouyei Deprat" ], [ "Ninety teams", "Paleontological", "Parafusulina yunnanica" ], [ "Ninety teams", "Paleontological", "Pseudofusulina gruperaensis (hompson)" ], [ "Ninety teams", "Paleontological", "Parafusulina vulgaris (Schellwien)" ], [ "Ninety teams", "Paleontological", "Parafusulina upchra Sheng" ], [ "Ninety teams", "Paleontological", "Yangchinia compressa (Ozawa)" ], [ "Ninety teams", "Paleontological", "Chalaroschwangerina sp." ], [ "Ninety teams", "Paleontological", "Dictyoclistus cf. semiticulatus(Mattin)" ], [ "Ninety teams", "Paleontological", "Enteletes sp." ], [ "Ninety teams", "Paleontological", "Orthotetina sp. Chrysanthemum" ], [ "Ninety teams", "Paleontological", "Epadrites timornsis var." ], [ "Ninety teams", "Paleontological", "involutus (Haniel) coral" ], [ "Ninety teams", "Paleontological", "Liangshanophyllum sp." ], [ "Ninety teams", "Paleontological", "Wentzelella sp." ] ] }, { "text": "Gray block layered powder glitter containing dolomellitic clastic limestone 283.83m", "triple_list": [ [ "Gray block layered powder glitter containing dolomel clastic limestone", "thickness", "283.83m" ] ] }, { "text": "The cement 22-30 is composed of cryptocrystalline chlorite chlorite silicone and iron.", "triple_list": [ [ "Cement", "Contained", "Crystalline chlorite" ], [ "Cement", "Contained", "chlorite silicon" ], [ "Cement", "Contained", "Iron" ] ] }, { "text": "The Batang group is limited to the south of the Yushu-Xianggu Da Fault.", "triple_list": [ [ "Batang Group", "Exposed", "Yushu-South of Xianggu Da Fault" ] ] }, { "text": "Dark gray quartz sandstone with off-white breccia-like clastic limestone. Fossil-producing brachiops Caucasorhynchia sp., bivalve Placunopsis sp. 494.12m", "triple_list": [ [ "Dark gray quartz sandstone with off-white breccia-like clastic limestone", "Paleontological", "Brachial foot Caucasorhynchia sp." ], [ "Dark gray quartz sandstone with off-white breccia-like clastic limestone", "Paleontological", "bivalve Placunopsis sp." ], [ "Dark gray quartz sandstone with off-white breccia-like clastic limestone", "thickness", "494.12m" ] ] }, { "text": "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone sandstone coal line (not seen in the top), fossil Hoernesia xizangensis Zhang, Cardium (ulongocardium) cf. submartini J. Chen Unionites sp. 18.87m", "triple_list": [ [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone coal line", "Paleontological", "Hoernesia xizangensis Zhang" ], [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone coal line", "Paleontological", "Cardium (ulongocardium) cf." ], [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone coal line", "Paleontological", "submartini J." ], [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone coal line", "Paleontological", "Chen Unionites sp." ], [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone coal line", "thickness", "18.87m" ] ] }, { "text": "Gray-green medium-layered Ying'an complex chip melted tuff, with a small amount of limestone and medium-layered mud crystal limestone, thickness 1033.81m", "triple_list": [ [ "Gray-green medium-layered Ying'an complex chip melted tuff with a small amount of limestone and medium-layered mud crystal limestone", "thickness", "1033.81m" ] ] }, { "text": "The Polila Formation strata and the Bagong Formation in the upper part of the lower Gapila Formation are in integrated contact, with a maximum control thickness of 1789.98m.", "triple_list": [ [ "Polira group", "Integration of contacts", "Kapila Group" ], [ "Polira group", "Integration of contacts", "Bagong Group" ], [ "Polira group", "thickness", "1789.98m" ] ] }, { "text": "Rock consists of two parts: porcine and matrix, where porcine is composed of plagioclase and ordinary pyroxene, with a particle size generally ranging from 0.32-4mm.", "triple_list": [ [ "rock", "Develop", "Pyramid" ], [ "rock", "Develop", "Substrate" ], [ "Pyramid", "Contained", "Plagioclase" ], [ "Pyramid", "Contained", "Ordinary pyrosine" ], [ "Pyramid", "thickness", "0.32-4mm" ] ] }, { "text": "Gray medium-thick layered silty fine-grain feldstone sandstone with light gray thin-layer medium-grained cuts sandstone and silty slate 367.46m", "triple_list": [ [ "Gray medium-thick layered silt fine-grain feldstone sandstone with light gray thin-layered medium-grained cuts sandstone and silt slab", "thickness", "367.46m" ] ] }, { "text": "Gray medium-layered sea surface bone needle mud crystal limestone 222.15m Angle unconsolidation Volcanic rock formation (3Bt2) 233.48m", "triple_list": [ [ "Gray medium-layered sea surface bone needle mud crystal limestone", "thickness", "222.15m" ], [ "Gray medium-layered sea surface bone needle mud crystal limestone", "Unconformity contact", "Volcanic rock formation" ], [ "Volcanic rock formation", "thickness", "233.48m" ] ] }, { "text": "Gray medium-thin layered carbonated wave chip tuff 32.1m", "triple_list": [ [ "Gray medium-thin layered carbonated wave chip tuff", "thickness", "32.1m" ] ] }, { "text": "The Tibetan Geological Brigade (1966-1967) divided the Bagong Group into the lower Adula Group and the upper Dugala Group, which was the late Triassic Era.", "triple_list": [ [ "Bagong Group", "Outcrop", "Adula Group" ], [ "Bagong Group", "Outcrop", "Gala group" ], [ "Bagong Group", "Age", "Late Triassic" ] ] }, { "text": "In the test area, the 1:200,000 area was transferred to the slate formation of the Bayankala Mountain group. Only Montlivaltia sp (Six-Sp Coral) fossils were collected. Duplexisporites Annulispora, Gladagondolella tethydis Neogondolella mommbergensis paleon combination fossils were collected.", "triple_list": [ [ "Bayankala Mountain Slate Formation", "Paleontological", "Montlivaltia sp (Six-Sp Coral) fossil" ], [ "Bayankala Mountain Slate Formation", "Paleontological", "DuplexisporitesAnnulispora" ], [ "Bayankala Mountain Slate Formation", "Paleontological", "Gladagondolella tethydis Neogondolella mommbergensis" ] ] }, { "text": "The analysis believes that the sequence characteristics of other hierarchical groups can be compared with the hierarchical group, and its era is the early and middle triassic period.", "triple_list": [ [ "Jilong Group", "Age", "Early and Middle Triassic" ] ] }, { "text": "Gray thin-medium layered limestone 169.67m", "triple_list": [ [ "Thin gray - medium layered limestone", "thickness", "169.67m" ] ] }, { "text": "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale, fossils of plant Hyrcanopteris sepanensis Kryshtofovich et Prynada, Hyrcanopteris cf. sinensis Li et saoPterophyIIum cf.jaegeri Brongniart, Otozamites sp., Clathropteris meniscioides Brongniart 51.25m", "triple_list": [ [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "Plant fossils Hyrcanopteris sevanensis Kryshtofovich et Prynada" ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "Hyrcanopteris cf." ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "sinensis Li et saoPterophyIIum cf." ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "jaegeri Brongniart" ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "Otozamites sp." ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "Paleontological", "Clathropteris meniscioides Brongniart" ], [ "Dark gray shale silt sandstone sandstone coal seam carbonaceous shale", "thickness", "51.25m" ] ] }, { "text": "From the southwest direction of Xiaocuogema, the base conglomerate increased, and it was a purple-red complex conglomerate, with a thick layered structure.", "triple_list": [ [ "Zocuogema", "Contained", "Polygon" ], [ "Polygon", "Belongs to", "Purple-red complex gravel" ], [ "Polygon", "Distribution pattern", "Thick layered" ] ] }, { "text": "Among these fossils, Neoschwagerina craticulifera (Schwager), is a standard molecule in the middle and late stages of the Middle Permian. It is more appropriate to classify ninety teams as Middle Permian.", "triple_list": [ [ "Neoschwagerina craticulifera(Schwager)", "Age", "Middle Permian" ], [ "Ninety teams", "Age", "Medium Perm" ] ] }, { "text": "The new meaning of the Gadikao Formation is distributed on the northern slope of the Tanggula Mountains, located at the stratiform of the Jiapila Formation. It is composed of gray-green, purple-red and variegated volcanic rocks, volcanic rocks, limestones and clastic rocks, containing fossils of flies and brachiopods, and has not been seen bottomed. The top is sometimes unconformally covered by the Jiapila Formation.", "triple_list": [ [ "Gadikao Group", "Exposed", "The northern slope of Tanggula Mountain" ], [ "Gadikao Group", "Integration of contacts", "Kapila Group" ], [ "Gadikao Group", "Lithology", "Gray green purple and variegated pyroclastic rock" ], [ "Gadikao Group", "Lithology", "Volcanic rocks" ], [ "Gadikao Group", "Lithology", "Limestone" ], [ "Gadikao Group", "Lithology", "Clastite" ], [ "Gadikao Group", "Paleontological", "dragonfly" ], [ "Gadikao Group", "Paleontological", "Brachiopod" ], [ "Gadikao Group", "Unconformity contact", "Kapila Group" ] ] }, { "text": "Sandstone Formation (2-3B) Thickness 2959.61m", "triple_list": [ [ "Sandstone Formation", "thickness", "2959.61m" ] ] }, { "text": "The ligation group area is not integrated on the Gadikao group of the Permian Kaixinling group of the Carboniferous Carboniferous period. It is partially covered by the Tertiary strata and the north side is in contact with the Batang group fault in the late Triassic period.", "triple_list": [ [ "Ligation group", "Unconformity contact", "Carboniferous Miscellaneous Groups" ], [ "Ligation group", "Unconformity contact", "Permian Happy Ridge Group" ], [ "Ligation group", "Unconformity contact", "Gadikao Group" ], [ "Ligation group", "Integration of contacts", "Tertiary strata" ], [ "Ligation group", "Fault contact", "Batang Group in the Late Triassic" ] ] }, { "text": "The Qinghai Provincial Regional Test Team (1970) revised the geological survey report of the 1:1 million Yushu Strip (I-47) and the geological survey report of the 1:1 million hot spring Strip (I-47) area. It proposed that the quartet-like clastic rocks distributed from Kokoxili in the west and ending in the east, almost all of the Triassic system are called the Bayankala Mountain Group. As the local name of the Triassic system in this area, the above middle and chin Bayankala Mountain Group represents the upper middle and lower system respectively.", "triple_list": [ [ "From the west to the west of Kokoxili", "Outcrop", "Bayankala Mountain Group" ], [ "Bayankara Mountain", "Outcrop", "Bayankala Mountain Group" ], [ "marble-like clastic rock", "Belongs to", "Bayankala Mountain Group" ] ] }, { "text": "Triassic period of the ophiogenic rock (ch) The newly discovered tectonic rock formation map unit established in this work, 1:200,000 districts were transferred to the regional geological record of Qinghai Province and included it in the late Triassic Batang Group. The area refers to the Yushu-Zhongdian stratigraphic division north of the Yushu fault of Goulu Mountain Kecuodeng and south of the Yushu line of Wulan Lake in the West Jin Dynasty, and is adjacent to the Bayan Kala Mountains on the north side.", "triple_list": [ [ "Triassic checks on ophiolula mixed rock", "Belongs to", "Batang Group of the Late Triassic World" ], [ "Triassic checks on ophiolula mixed rock", "Located at", "Goulu Shankecuoden north of the Yushu fault of Oyong Qu" ], [ "Triassic checks on ophiolula mixed rock", "Located at", "Yushu, south of the Yuwu line in Wulan Lake in Xijin - Zhongdian" ] ] }, { "text": "Dark gray thin layered medium-coarse-grained rock-cut feldspar sandstone 126.86m", "triple_list": [ [ "Dark gray thin layered medium-coarse-grained feldspar sandstone", "thickness", "126.86m" ] ] }, { "text": "Dalong Sandstone (chd) This rock formation is distributed in the northwest to southeast directions on the line of Dalongdangjiang Township, Riqucha, Riqucha.", "triple_list": [ [ "Dalong Sandstone", "Distribution pattern", "Northwest-Southeast" ], [ "Dalong Sandstone", "Exposed", "Ria Qucha Yongda Longdangjiang Township" ] ] }, { "text": "The southern side of the Jielong Group was in contact with the Bolila Group of the ligation group, and the northwest side was covered by the angle unIntegration of contacts between the late Triassic ligation group, and the Tertiary Yaxicao Group, respectively, with a distribution area of about 2.5m2.", "triple_list": [ [ "Jilong Group", "Fault contact", "Ligation group Polira group" ], [ "Jilong Group", "Unconformity contact", "Late Triassic Ligation Group Kapila Group" ], [ "Jilong Group", "Unconformity contact", "The third century Yashiko group" ], [ "Jilong Group", "area", "2.5m2" ] ] }, { "text": "Chayong ophiolite (chop) thickness 1932.21m", "triple_list": [ [ "Chayong Ophiopolysite", "thickness", "1932.21m" ] ] }, { "text": "Gray medium-thick layer of metamorphic silt clay rock 205.47m", "triple_list": [ [ "Gray medium-thick layer of metamorphic silty clay rock", "thickness", "205.47m" ] ] }, { "text": "Characteristics of basic layer sequences ⑴ Sandstone Formation (2-3B) The basic layer sequence in the upper part of this group is composed of spin-circular sedimentary sequences of medium-grained fine-grained rock sandstone and silty slate", "triple_list": [ [ "Sandstone Formation", "Lithology", "Fine-grained rock" ], [ "Sandstone Formation", "Lithology", "Chop sandstone" ], [ "Sandstone Formation", "Lithology", "Silty slab" ] ] }, { "text": "Gray-green giant thick layered rock-cut tuff 41.74m", "triple_list": [ [ "Gray-green giant thick layered rock-cut chip tuff", "thickness", "41.74m" ] ] }, { "text": "Gray thin layered shiny sand chip limestone with gray thick layered powder crystals containing oximeters and biological clastic limestone produced bryozoosome Stenopora sp.indet", "triple_list": [ [ "Gray thin layered shiny sand chip limestone with gray thick layered powder crystals containing oximeters biological clastic limestone", "Paleontological", "Bryomyces Stenopora sp.indet" ] ] }, { "text": "This strata is in an angle unconsistent contact with the 90 teams of the Kaixinling Group of the lower Permian Permian, and is covered by the angle unconsistent coverage of the Late Triassic Ligation Group of the Jiapila Group. The formation time was between the Late Permian and Early Triassic. Due to the failure of isotope dating to form a line, the specific formation time cannot be determined.", "triple_list": [ [ "Strata", "Unconformity contact", "The Kaixinling Group of the Middle Permian Noribagari Bao Group" ], [ "Strata", "Unconformity contact", "Ninety teams" ], [ "Strata", "Unconformity contact", "Late Triassic Ligation Group Kapila Group" ], [ "Strata", "Age", "Late Permian to Early Triassic" ] ] }, { "text": "Gray medium-thick layered medium-grained quartz sandstone sandstone with dark gray silty slate 9.82m", "triple_list": [ [ "Gray medium-thick layered medium-grained quartz sandstone sandstone with dark gray silty slab", "thickness", "9.82m" ] ] }, { "text": "Gray-purple medium-thick layered medium-coarse-grained rock-cut feldspar sandstone with gray-purple thin-layered fine-grained feldspar sandstone 4.42m", "triple_list": [ [ "Gray-purple medium-thick layered medium-coarse-grained rock-cut feldspar sandstone with gray-purple thin-layered fine-grained feldspar sandstone", "thickness", "4.42m" ] ] }, { "text": "Gray Basal Andestone 78.0m", "triple_list": [ [ "Gray Basal Andshan Rock", "thickness", "78.0m" ] ] }, { "text": "The mud and gravel are developed on the top surface of the sandstone layer, with asymmetrical wave marks; there are heavy load mode structures at the bottom, and groove mode groove mode deposition structures", "triple_list": [ [ "Sandstone layer", "Develop", "Flush mud and gravel" ], [ "Sandstone layer", "Develop", "Asymmetric wave marks" ], [ "Sandstone layer", "Develop", "Heavy load mode structure" ], [ "Sandstone layer", "Develop", "Slot mold" ], [ "Sandstone layer", "Develop", "Grooved mold deposition structure" ] ] }, { "text": "The Gadikao formation was in fault contact with the Carboniferous Zaduo group and the Jiuji team in fault contact with the Noriba Gariba and the Jiuji team in the Kaixinling group in the Early and Middle Permian period, and was not integrated with the Jiapila group in the Late Triassic ligation group.", "triple_list": [ [ "Gadikao Group", "Fault contact", "Carboniferous Miscellaneous Groups" ], [ "Gadikao Group", "Fault contact", "The Permian Kaixinling Qun Noriba Garibao Group" ], [ "Gadikao Group", "Fault contact", "Ninety teams" ], [ "Gadikao Group", "Unconformity contact", "Late Triassic Ligation Group Kapila Group" ] ] }, { "text": "Small staggered lacerations are common in siltstone parallel lacerations bean-shaped interlaced lacerations horizontal lacerations sand pattern interlaced lacerations, etc. The most distinctive laceration structures are vein-shaped wavy and lenticular lacerations, which reflect the lack of hydrodynamic during deposition and only weak bottom flow activities. In terms of the direction of the basic lace sequence, it has good similar shapes, stable lace positions, and good ductility.", "triple_list": [ [ "Siltstone", "Develop", "Interleaved hierarchy" ], [ "Siltstone", "Develop", "Parallel layering" ], [ "Siltstone", "Develop", "Bean-shaped interlaced layering" ], [ "Siltstone", "Develop", "Horizontal stratification" ], [ "Siltstone", "Develop", "Sand pattern interlaced layering" ], [ "Siltstone", "Develop", "Vein-shaped waves and lens-shaped lamellar" ] ] }, { "text": "Gray block layered coarse-grained quartz sandstone 42.44m", "triple_list": [ [ "Gray block layered coarse quartz sandstone", "thickness", "42.44m" ] ] }, { "text": "Among them, the porcine crystal is composed of feldspar (23) and quartz (15). The feldspar has sericated and has a particle size of 0.950.28mm2. An is 17. It is measured that the quartz has a melted appearance.", "triple_list": [ [ "Pyramid", "Contained", "Longer stone" ], [ "Pyramid", "Contained", "quartz" ] ] }, { "text": "Gray medium-layer fine-grained feldspar quartz sandstone with a small amount of gray - dark gray silty slate 198.71m", "triple_list": [ [ "Gray medium-layer fine-grained feldspar quartz sandstone with a small amount of gray - dark gray silty slab", "thickness", "198.71m" ] ] }, { "text": "1:200,000 districts were transferred to Nieka in the northeast corner of this test area and found a six-shot coral fossil Montlivaltia sp.", "triple_list": [ [ "Nieka, northeast corner of the test area", "Paleontological", "Six-Shot Coral Fossil Montlivaltia sp." ] ] }, { "text": "Volcanic rock formation (3Bt2) is exposed in a narrow strip, spreading in Riagu-Zacha and other places, and is in a integrated contact with the upper and lower strata, and is in contact with most faults. The local Xinjiquguo formation is not integrated on it, with a control thickness greater than 1033.81m.", "triple_list": [ [ "Volcanic rock formation", "Distribution pattern", "Narrow stripe" ], [ "Volcanic rock formation", "Exposed", "Sunagu - Zhacha also changed" ], [ "Volcanic rock formation", "Unconformity contact", "New Jiquguo Group" ], [ "Volcanic rock formation", "thickness", "1033.81m" ] ] }, { "text": "Light gray-green sheet physical and chemical tuff 134.14m", "triple_list": [ [ "Light gray-green sheet physical and chemical tuff", "thickness", "134.14m" ] ] }, { "text": "Parallel stratification in siltstone", "triple_list": [ [ "Siltstone", "Develop", "Parallel layering" ] ] }, { "text": "According to the lithological combination method, the strata, ductility and mapability, and referring to the division plan of the Qinghai Province rock formation (1997), the Batang group was divided into clastic rock formation units (3Bt1), volcanic rock formation (3Bt2), carbonate rock formation (3Bt3)-level rock formation units.", "triple_list": [ [ "Batang Group", "Outcrop", "Clastic rock formation" ], [ "Batang Group", "Outcrop", "Volcanic rock formation" ], [ "Batang Group", "Outcrop", "Carbonate rock formation" ] ] }, { "text": "According to the profile analysis, the stratigraphic sequence reflects the characteristics of cyclonic eruption deposits from the bottom to the top. Judging from the changes in the rhythm of volcanic eruption, the lithology is mainly based on the basic lava species of the overflowing phase, followed by the breccia tuff of the erupting phase, with some gray-green normal sedimentary rocks, average stratigraphic nature, clear stratigraphic system, rapid phase change, eye-catching red top and green bottom, and columnar joint Develop (Figure). According to the chemical and geochemical characteristics of volcanic rocks, alkaline volcanic rocks have the characteristics of terrestrial eruption, which is the inland rift tectonic environment (see the volcanic rock part for details).", "triple_list": [ [ "profile", "Lithology", "Basic lava" ], [ "profile", "Lithology", "breccia tuff" ], [ "profile", "Lithology", "Sedimentary rock" ], [ "profile", "Develop", "Column joints" ], [ "profile", "Lithology", "Alkaline volcanic rocks" ], [ "profile", "Belongs to", "Inland rift tectonic environment" ] ] }, { "text": "Gray-green altered coarse basalt 139.63m", "triple_list": [ [ "Gray-green altered coarse basalt", "thickness", "139.63m" ] ] }, { "text": "The measured stratigraphic profile of the upper clastic rock formation in the Batang group of Boche Triassic in Dangjiang Township, Zhiduo County, Qinghai Province (VIII003P10) with a thickness of 206.16m", "triple_list": [ [ "Dangjiang Township, Zhiduo County, Qinghai Province", "Outcrop", "Clastic rock formation on the Batang group in the Boche Triassic period" ], [ "Clastic rock formation on the Batang group in the Boche Triassic period", "thickness", "206.16m" ] ] }, { "text": "Silicone bands or nodules are common in limestone, including a large number of insect fossils and sea lily fragments.", "triple_list": [ [ "Limestone", "Contained", "Silicone strips" ], [ "Limestone", "Contained", "tuberculosis" ], [ "Limestone", "Paleontological", "Insect fossil" ], [ "Limestone", "Paleontological", "Sea lily fragments" ] ] }, { "text": "The section of the sandstone and slate interlayer section (3B) of the Sandstone and slate interlayer section (3B) of the Dangjiang Township, Zhiduo County, Qinghai Province VIII003P14 (Figure 2-30).", "triple_list": [ [ "Dengerqu, Dangjiang Township, Zhiduo County, Qinghai Province", "Outcrop", "Sandstone Formation of Bayan Kala Mountains in the Mid-End Third World" ], [ "Dengerqu, Dangjiang Township, Zhiduo County, Qinghai Province", "Outcrop", "Interlayer section of the slate sandstone and slate" ] ] }, { "text": "The Gadikao composition belt is distributed in the Longmanenarigongma and Ziqu area in the test area, with a distribution area of 330m2 and a maximum control thickness of 1614.37m.", "triple_list": [ [ "Gadikao Group", "Exposed", "Longmanena Rigonma and Ziqu" ], [ "Gadikao Group", "area", "330m2" ], [ "Gadikao Group", "thickness", "1614.37m" ] ] }, { "text": "The name of the ligation group is retained in the rock formation in Qinghai Province, and it extends to the Middle Triassic Period in the era. It is defined as a strata distributed in the Tanggula-Changdu region, super-covered on the Paleozoic strata or the Early Triassic strata, integrated in the Chaya group or not integrated under the new strata such as Yanshiping group, and is composed of clastic rocks and carbonate rocks, with a small amount of volcanic rocks. The upper part is coal-containing and rich in fossils such as bivalve brachiopods and plants.", "triple_list": [ [ "Ligation group", "Age", "Middle Triassic" ], [ "Ligation group", "Exposed", "Tanggula-Chambo area" ], [ "Ligation group", "Integration of contacts", "Chaya Group" ], [ "Ligation group", "Unconformity contact", "Yanshiping Group" ], [ "Ligation group", "Lithology", "Clastite" ], [ "Ligation group", "Lithology", "Carbonate rock" ], [ "Ligation group", "Lithology", "Volcanic rocks" ], [ "Ligation group", "Paleontological", "Bivalves" ], [ "Ligation group", "Paleontological", "Brachiopod" ], [ "Ligation group", "Paleontological", "Cephalopod" ], [ "Ligation group", "Paleontological", "plant" ] ] }, { "text": "The Jiapila group has a wide angular disintegration relationship with the Permian Kaixinling group in the underlying Carboniferous Miscellaneous groups, and is in integrated contact with the overlying Polira group, with a thickness greater than 220.75m.", "triple_list": [ [ "Kapila Group", "Unconformity contact", "Carboniferous Miscellaneous Groups" ], [ "Kapila Group", "Unconformity contact", "The Happy Ridge Group of the Middle Permian" ], [ "Kapila Group", "Integration of contacts", "Polira group" ], [ "Kapila Group", "thickness", "220.75m" ] ] }, { "text": "Gray-green giant thick layered complex volcanic breccia 13.49m", "triple_list": [ [ "Grey-green giant thick layered complex volcanic breccia", "thickness", "13.49m" ] ] }, { "text": "Gray-green fine-grained gabbro (tectonic block) 11.24m", "triple_list": [ [ "Gray-green fine-grained gabbro", "thickness", "11.24m" ] ] }, { "text": "Gray green mud serous schist (tectonic block) 149.01m", "triple_list": [ [ "Gray green mud serous schist", "thickness", "149.01m" ] ] }, { "text": "The late Triassic paleontological fossil area is relatively developed in the test area, mainly distributed in the Batang group and ligation group, and is rare in the Bayankala Mountain group, mainly bivalve brachiopods and some plant fossils.", "triple_list": [ [ "Batang Group", "Paleontological", "Bivalves" ], [ "Batang Group", "Paleontological", "Brachiopod" ], [ "Batang Group", "Paleontological", "Plant fossils" ], [ "Ligation group", "Paleontological", "Bivalves" ], [ "Ligation group", "Paleontological", "Brachiopod" ], [ "Ligation group", "Paleontological", "Plant fossils" ], [ "Bayankala Mountain Group", "Paleontological", "Bivalves" ], [ "Bayankala Mountain Group", "Paleontological", "Brachiopod" ], [ "Bayankala Mountain Group", "Paleontological", "Plant fossils" ] ] }, { "text": "The Jiapila Group is mainly distributed in the area of Zhaqingxiang, Dongjiaoyong-Dongmoyong, south of Narigongma-Ziqu, with a distribution area of 1351.61m2 and a maximum control thickness greater than 1351.61m.", "triple_list": [ [ "Kapila Group", "Exposed", "The area of Dongjiaoyong-Dongmoyong Zhaqingxiang, south of Ziqu" ], [ "Kapila Group", "area", "1351.61m2" ], [ "Kapila Group", "thickness", "1351.61m" ] ] }, { "text": "The early and middle triassic strata of the survey area is only distributed in the Geren Kangba Rhiqu area in the area of Chayong area, and is composed of the early and middle triassic strata of the early and middle triassic strata of the Triassic Chayong opalene mixed rock.", "triple_list": [ [ "Early and Middle Triassic", "Exposed", "Geren Kangba Ryan in Chayong area" ], [ "Early and Middle Triassic", "Outcrop", "Triassic checks on ophiolula mixed rock" ], [ "Early and Middle Triassic", "Outcrop", "The Triassic Triassic Jilong Formation" ] ] }, { "text": "Parahalobia sp (parahalobia clams); Claraia sp (Kercher) brachiopod fossils are found in the area of the Jielong Formation, which are fossil molecules from the Early Triassic and Mid-late Triassic.", "triple_list": [ [ "Jilong Group", "Paleontological", "Parahalobia sp(生生子)." ], [ "Jilong Group", "Paleontological", "Claraia sp (Kerthy clam) brachiopod fossil" ], [ "Jilong Group", "Age", "Early Triassic" ], [ "Jilong Group", "Age", "The Triassic Period" ] ] }, { "text": "The stratigraphic units of the Batang Group Belongs to to the Kanik-Nolik-Strati.", "triple_list": [ [ "Batang Group", "Age", "Kanik-Norik" ] ] }, { "text": "Gray-green thick layered medium-grained rock-cut feldspar sandstone 18.15m", "triple_list": [ [ "Gray-green thick layered medium-grained cuts feldspar sandstone", "thickness", "18.15m" ] ] }, { "text": "The Jielong Formation is not integrated in Changlazondo ligation group, and in the Yuqinsangzhi Akao area, it is also not integrated with the middle and upper devon system and the anterior devon system. The exposed area is 200m2, and it produces a relatively abundant ammonite bivalve coral fossils, which was the Middle Permian period.", "triple_list": [ [ "Jilong Group", "Unconformity contact", "Changlason Duo Ligation Group" ], [ "Jilong Group", "Exposed", "The area of Akao" ], [ "Jilong Group", "Unconformity contact", "Middle and upper ditto" ], [ "Jilong Group", "Unconformity contact", "Front mud pot system" ], [ "Jilong Group", "area", "200m2" ], [ "Jilong Group", "Paleontological", "Chrysanthemum" ], [ "Jilong Group", "Paleontological", "Bivalves" ], [ "Jilong Group", "Paleontological", "Coral fossils" ], [ "Jilong Group", "Age", "Middle Permian" ] ] }, { "text": "Gray limestone fault Bagong Formation with 90 teams in the morning and middle and middle periods, thickness of 2234.26m", "triple_list": [ [ "Gray limestone in the ninety teams of Permian", "Fault contact", "Bagong Group" ], [ "Gray limestone in the ninety teams of Permian", "thickness", "2234.26m" ] ] }, { "text": "Gray-green all-green mud petrochemical Yangqi pyroxene rock (tectonic block) 76.03m", "triple_list": [ [ "Gray green all-green petrochemical Yangqi Petrochemical Pyroxene rock", "Distribution pattern", "Tectonic rock blocks" ], [ "Gray green all-green petrochemical Yangqi Petrochemical Pyroxene rock", "thickness", "76.03m" ] ] }, { "text": "The mud silty silty gravel of 10-20 on the erosion surface in silty silty silty silty silty silty silty silty silty on the erosion surface reflects a relatively turbulent sedimentary environment.", "triple_list": [ [ "Silty slab", "Develop", "Mud silt sandstone mud gravel" ], [ "Mud silt sandstone mud gravel", "thickness", "0.5-4cm" ] ] }, { "text": "To sum up, the Triassic sedimentary environment is an active land margin zone semi-deep sea sedimentary environment.", "triple_list": [ [ "Triassic sedimentary environment", "Belongs to", "Semi-deep oceanic sedimentary environment of active land margin zone" ] ] }, { "text": "The Batang Group and Jielong Group of Bayan Kala Mountain Group Belongs to to the Xijinwulan-Jinshajiang Stratigraphic Zone of the Bayan Kala Mountain Stratigraphic Zone of the Qiangbei-Changdu Stratigraphic Zone.", "triple_list": [ [ "Bayankala Mountain Group", "Stratigraphical zoning", "Bayankala Mountain Stratigraphic Zone" ], [ "Batang Group", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Zone" ], [ "Jielong group ligation group", "Stratigraphical zoning", "Qiangbei-Changdu Stratigraphic Zone" ] ] }, { "text": "This group of turbidite rocks are typical sedimentation of sea and land source clastic turbid currents. The rock structure is mostly mixed with fine medium grains, etc. The composition is complex, mainly quartz plagioclase, and a small amount of potassium feldspar. The rock fragments include slurry, slate, acidic lava, and serosz schist. Occasionally, electrical zircon apatite, opaque minerals, and their source areas show rock combinations in the land margin orogenic belt.", "triple_list": [ [ "Turbidite rock", "Belongs to", "Tumor current sedimentation of sea and land source debris" ], [ "Turbidite rock", "Contained", "Quartz plagioclase" ], [ "Turbidite rock", "Contained", "Potassium feldspar" ], [ "Turbidite rock", "Lithology", "Sandstone" ], [ "Turbidite rock", "Lithology", "Qianmeiyan" ], [ "Turbidite rock", "Lithology", "Slate" ], [ "Turbidite rock", "Lithology", "Medium-basic lava" ], [ "Turbidite rock", "Lithology", "Limestone" ], [ "Turbidite rock", "Lithology", "serous quartz schist" ], [ "Turbidite rock", "Contained", "tourmaline" ], [ "Turbidite rock", "Contained", "Zircon" ], [ "Turbidite rock", "Contained", "apatite" ] ] }, { "text": "According to the profile and route data, the lithologies of the Jiapila Formation do not change much in the region. They are spatially limited by fault circumference. They are produced in the fault zone, and generally have monoclinic outputs from southwest to northeast, with rock formations of 50-60°. In the southeast area of Narigonma, they are generally inclinic outputs from southwest to northeast, with rock formations of 20-40°, and limestone floating on the top of the mountain on the top of the mountain.", "triple_list": [ [ "Kapila Group", "Distribution pattern", "Faulted block" ], [ "Kapila Group", "Distribution pattern", "Mono-climb output from southwest to northeast" ], [ "Kapila Group", "Exposed", "South East of Narigonma" ], [ "Kapila Group", "Distribution pattern", "South-west-northeast-eastern tilt output" ], [ "Kapila Group", "Lithology", "Limestone" ] ] }, { "text": "Dark gray thin - Medium-layered silty slate with gray medium-fine grain feldspar crushed sandstone 85.86m", "triple_list": [ [ "Dark gray thin-medium silty slate with gray medium-fine-grained feldspar crushed sandstone", "thickness", "85.86m" ] ] }, { "text": "Gray medium-thick layer of light metamorphic unequal grain feldspar crushed sandstone sandstone with dark gray thin layer of slate (oblique core) 140.98m", "triple_list": [ [ "Gray medium-thick layer of light metamorphic unequal grain feldspar crushed sandstone sandstone with dark gray thin layer slab", "thickness", "140.98m" ] ] }, { "text": "Purple-red medium-thick layered fine-grained feldspar sandstone sandstone with gray medium-thick layered silt sandstone 120.76m", "triple_list": [ [ "Purple-red medium-thick layered fine-grained feldspar crushed sandstone with gray medium-thick layered siltstone", "thickness", "120.76m" ] ] }, { "text": "Gray medium-thick layered mud crystals containing biological clastic gravel limestone with a small amount of gray medium-layered rhodium mineralized powder glitter sandstone limestone 73.66m", "triple_list": [ [ "Gray medium-thick layered mud crystals containing biological clastic gravel limestone with a small amount of gray medium-layered rhodium-iterate powder glitter sandstone limestone", "thickness", "73.66m" ] ] }, { "text": "Gray silty slate with gray thin layered fine-grained feldspar quartz sandstone 335.03m", "triple_list": [ [ "Gray silty slate with gray thin layered fine-grained feldspar quartz sandstone", "thickness", "335.03m" ] ] }, { "text": "The original definition of the Jielong Formation refers to a set of coastal-shallow marine clastic rock-carbonate rock systems that are mainly grey-based.", "triple_list": [ [ "Jilong Group", "Outcrop", "Coastal-shallow marine clastic rock-carbonate rock system" ] ] }, { "text": "Gray-yellow-light gray-brown flowing Ying'anite 41.57m fault The Carboniferous Miscellaneous Clerotite Formation (C1Z1) has a lithology of sandstone silt sandstone, which produces wrist-foot.", "triple_list": [ [ "Gray-yellow-light gray-brown flowing Ying'an rock", "thickness", "41.57m" ], [ "Gray-yellow-light gray-brown flowing Ying'an rock", "Fault contact", "Carboniferous Clastozoic Rock Formation" ], [ "Carboniferous Clastozoic Rock Formation", "Lithology", "sandstone" ], [ "Carboniferous Clastozoic Rock Formation", "Lithology", "Slate" ], [ "Carboniferous Clastozoic Rock Formation", "Lithology", "Siltstone" ], [ "Carboniferous Clastozoic Rock Formation", "Paleontological", "Wrist foot" ] ] }, { "text": "Gray thin-layer medium-fine-grained feldspar quartz sandstone and gray-green silty slate interlayer 242.67m", "triple_list": [ [ "Gray thin-layer medium-fine-grained feldspar quartz sandstone and gray-green silty slate interlayer", "thickness", "242.67m" ] ] }, { "text": "The matrix is mainly composed of plagioclase, sericamyl chlorite, and chlorite, followed by some carbonate.", "triple_list": [ [ "Substrate", "Contained", "Plagioclase" ], [ "Substrate", "Contained", "sericaceous amphibole chlorite" ], [ "Substrate", "Contained", "Green curtain stone" ], [ "Substrate", "Contained", "Carbonate" ] ] }, { "text": "Parallel slab slabs are developed in silty slabs, with plant clasps, but there are few biological remains fossils, representing the sequence characteristics of different stages of the sedimentation process. Rocks of different particle-level grades are stacked in single layers, which reflects the continuous spatial and temporal changes of sediment in multiple stages. The thickness and basic strata formed are obviously different. In short, the basic strata of this set of clastic rocks is a series of high-level strata sequences composed of coarse and thin spin strata sequences to overlap from bottom to top.", "triple_list": [ [ "Silty slab", "Develop", "Parallel layering" ], [ "Silty slab", "Develop", "Corrugated stratigraphy" ], [ "Silty slab", "Contained", "Plant shavings" ] ] }, { "text": "Early Triassic Paleontology was newly discovered in the Jielong Formation of the test area. According to the division plan of the unit division of the Triassic Paleontology of Qinghai Province, the stratigraphic unit belongs to the peak of Claria aurita, which is the Middle Indian order.", "triple_list": [ [ "Jilong Group", "Paleontological", "Claraia sp (Kerthy clam) brachiopod fossil," ] ] }, { "text": "The Jiapila group is distributed in the area in the upper reaches of the Kouqianqu - Angniyong Qu - Zichequge group - Yako - Zonggen Anitojiyong - Dongjiao Yong Zageyong - Ziqubayanyong Mohai - Baokakhachi Yongchi - Bitangpuba and other places, and is spread in a short belt shape towards northwest-northwest-west-west-west-to-short.", "triple_list": [ [ "Kapila Group", "Exposed", "Upstream of the mouth" ], [ "Kapila Group", "Exposed", "Angun Yongqu" ], [ "Kapila Group", "Exposed", "Ziqiquge group surge" ], [ "Kapila Group", "Exposed", "Yake" ], [ "Kapila Group", "Exposed", "Zongheng Anitoji Chung" ], [ "Kapila Group", "Exposed", "East Corner Chance Zageyong" ], [ "Kapila Group", "Exposed", "Ziqu Bayanyong Mo Hai" ], [ "Kapila Group", "Exposed", "Baokakhachi" ], [ "Kapila Group", "Exposed", "Bitangpuba" ], [ "Kapila Group", "Distribution pattern", "Northwest-Northwest-Northwest-Northwest-Northwest-North" ] ] }, { "text": "The trace element content of clastic rocks in the trace element arthropod group formation is shown in Table 2-7.", "triple_list": [ [ "Jielong Group", "Lithology", "Clastite" ] ] }, { "text": "The thickness of the rock layer in the formation near the subduction zone is medium-thick layer, with a sandstone single layer of 5-50cm, and a silt sandstone argillary slate single layer of 2-100cm, with strong deformation and a tightly closed fold inclined south and west of the Develop axis.", "triple_list": [ [ "Strata", "Lithology", "sandstone" ], [ "Strata", "Lithology", "Siltstone" ], [ "Strata", "Lithology", "Mud slate" ], [ "Strata", "Develop", "Closed folds that tilt south and west of the shaft" ] ] }, { "text": "The exposed width of this layer of bottom conglomerate is about 40m, which is not integrated on different layers of the Permian Kaixin Ridge Group.", "triple_list": [ [ "Polygon", "thickness", "40m" ], [ "Polygon", "Unconformity contact", "Permian Kaixin Ridge Group" ] ] }, { "text": "Gray-purple medium-layered medium-grained feldspar sandstone 1.55m", "triple_list": [ [ "Gray-purple medium-layered medium-grained feldspar sandstone", "thickness", "1.55m" ] ] }, { "text": "The rock has a fine particle size, mainly siltstone mudstone, with an increase in limestone interlayers and occasionally visible conglomerates.", "triple_list": [ [ "rock", "Lithology", "Siltstone" ], [ "rock", "Lithology", "Mudstone" ], [ "rock", "Lithology", "Limestone" ], [ "rock", "Lithology", "Polygon" ] ] }, { "text": "The measured geological profile of Dalong sandstone in Niechaquchayong opalgreen rock in Duocai Township, Zhiduo County, Qinghai Province is Ⅷ003P8 (Figure 2-22), the starting point of the geographical coordinates is 95°22′20 east longitude, 33°56′11 north latitude, and Elevation is 4943m; the end point is 96°20′20 east longitude, 33°53′44 north latitude, and Elevation is 4464m.", "triple_list": [ [ "Nie Chaqu, Duocai Township, Zhiduo County, Qinghai Province", "Lithology", "Chayong ophiogenic mixed rock Dalong sandstone" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Coordinates", "95°22'20 East longitude" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Coordinates", "33°56′11 North latitude" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Elevation", "4943m" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Coordinates", "96°20′20 East longitude" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Coordinates", "33°53′44 North latitude" ], [ "Chayong ophiogenic mixed rock Dalong sandstone", "Elevation", "4464m" ] ] }, { "text": "The lithological combination of the Jiapila Formation is a gray-purple thick layer of medium-fine-grained rock-cut quartz sandstone and feldspar sandstone with huge thick layer complex composition conglomerate gravel coarse sandstone feldspar quartz sandstone amidst silt sandstone and microcrystalline limestone lens, and partially interposed basal volcanic breccia", "triple_list": [ [ "Kapila Group", "Lithology", "Gray purple thick layer of medium-grained rock" ], [ "Kapila Group", "Lithology", "quartz sandstone" ], [ "Kapila Group", "Lithology", "Flyssil sandstone" ], [ "Kapila Group", "Lithology", "Huge thick layer of complex gravel" ], [ "Kapila Group", "Lithology", "Gravel-containing coarse sandstone" ], [ "Kapila Group", "Lithology", "Feldspar quartz sandstone" ], [ "Kapila Group", "Lithology", "Mud siltstone" ], [ "Kapila Group", "Lithology", "Microcrystalline limestone lens" ], [ "Kapila Group", "Lithology", "Mesoplasmic volcanic breccia" ] ] }, { "text": "The limestone is rich in fossils such as flies and a small number of coral bivalves and ammonites. It is in integrated contact with the Upper Permian Wuli Group, and the lithologic biological boundaries of the two are clear.", "triple_list": [ [ "Limestone", "Paleontological", "dragonfly" ], [ "Limestone", "Paleontological", "coral" ], [ "Limestone", "Paleontological", "Bivalves" ], [ "Limestone", "Paleontological", "Chrysanthemum" ], [ "Limestone", "Integration of contacts", "Upper Permian Wuli Group" ] ] }, { "text": "Gray - dark gray medium-thick layered powder glitter containing biological algae sand chip limestone with gray medium-layered biological debris limestone 54.85m", "triple_list": [ [ "Gray - dark gray medium-thick layered powder glitter containing biological algae sand chip limestone intersecting gray medium-layered bioclad limestone", "thickness", "54.85m" ] ] }, { "text": "Gray thin layered medium-fine-grained feldspar quartz sandstone 38.25m", "triple_list": [ [ "Gray thin layered medium-fine-grained feldspar quartz sandstone", "thickness", "38.25m" ] ] }, { "text": "The thickness of this formation varies significantly from north to south, and the rock combination is composed of sandstone siltstone and slate.", "triple_list": [ [ "Strata", "Lithology", "Sandstone silt" ], [ "Strata", "Lithology", "Slate" ] ] }, { "text": "Gray-green medium-layered medium-grained rock-cut sandstone with gray-purple medium-layered rock-cut feldspar sandstone 50.02m", "triple_list": [ [ "Gray-green medium-layered medium-grained rock-cut sandstone with gray-purple medium-layered rock-cut feldstone sandstone", "thickness", "50.02m" ] ] }, { "text": "A large number of turtle back stones have developed in the transformed sandstone, asymmetrical wave marks, and parallel scrubbing mud and gravel, which are cyclic basic stratigraphic sequences (Figure 2-33a). The lower basic stratigraphic sequences are composed of spin-circular sedimentary sequences of medium-fine-grained feldspar quartzite, varied mineral siltstone and silt slate.", "triple_list": [ [ "Sandstone", "Develop", "Turtle back stone" ], [ "Sandstone", "Develop", "Asymmetric wave marks" ], [ "Sandstone", "Develop", "Scrubbing mud and gravel parallel layering" ], [ "Sandstone", "Lithology", "Medium-fine-grained feldspar quartzite" ], [ "Sandstone", "Lithology", "Chop sandstone" ], [ "Sandstone", "Lithology", "Vanju mineral siltstone" ], [ "Sandstone", "Lithology", "Silty slab" ] ] }, { "text": "The lithology of the lower section of the Jielong Formation is purple-red, dark purple, medium-thick layered fine-grained feldspar sandstone sandstone sandstone sandstone sandstone sandstone sandstone sandstone sandstone sandstone sandstone sandstone-dark gray medium-thick layered powder shiny crystal crystal shiny crystal tuff limestone.", "triple_list": [ [ "Jilong Group", "Lithology", "Purple-red dark purple medium-thick layered fine-grained feldspar rock" ], [ "Jilong Group", "Lithology", "Chop sandstone" ], [ "Jilong Group", "Lithology", "Siltstone" ], [ "Jilong Group", "Lithology", "Gray - dark gray medium - thick layered powder glitter containing biological detritus algae sand limestone" ], [ "Jilong Group", "Lithology", "Ying'an Rock" ], [ "Jilong Group", "Lithology", "Crystal Crystal Tuff" ], [ "Jilong Group", "Lithology", "Limestone" ] ] }, { "text": "The Jiapila Formation (J3jp) has a lithologic gray-purple thick layered gravel-containing coarse-grained rock-cut feldstone sandstone with unconsolidated angles Ninety-Dao teams with a thickness of 1351.61m", "triple_list": [ [ "Kapila Group", "Lithology", "Gray purple thick layered gravel coarse grain rock" ], [ "Kapila Group", "Lithology", "Flyssil sandstone" ], [ "Kapila Group", "Unconformity contact", "Ninety teams" ], [ "Kapila Group", "thickness", "1351.61m" ] ] }, { "text": "The conglomerate rock formation is east of Gmaron, with its lithologic purple-red medium-grain feldspar quartz sandstone, and hard sandy quartz sandstone coarse silt sandstone, which are sandstones and limestones containing breccia. The rock has relatively coarse grain size and produces plant fossils and marine petal gill fossils.", "triple_list": [ [ "Polygon", "Located at", "East of Gmaron" ], [ "Polygon", "Lithology", "Purple-red medium-grain feldspar quartz sandstone" ], [ "Polygon", "Lithology", "Hard sandy quartz sandstone" ], [ "Polygon", "Lithology", "Coarse silt sandstone" ], [ "Polygon", "Lithology", "Breccia-containing sandstone" ], [ "Polygon", "Lithology", "Limestone" ], [ "Polygon", "Paleontological", "Plant fossils" ], [ "Polygon", "Paleontological", "Marine petal gill fossil" ] ] }, { "text": "The intersecting sections of the slate sandstone and slate should be the Norian sedimentation of the late Triassic period.", "triple_list": [ [ "Interlayer section of the slate sandstone and slate", "Age", "The Late Triassic Norian Period" ] ] }, { "text": "Gray thick layered medium-fine-grained feldspar sandstone with gray medium-layered medium-grained feldspar sandstone and a small amount of dark gray thin-layered silt sandstone 116.02m", "triple_list": [ [ "Gray thick layered medium-fine-grained feldspar sandstone with gray medium-layered medium-grained feldspar sandstone and a small amount of dark gray thin-layer silt sandstone", "thickness", "116.02m" ] ] }, { "text": "Light gray-green sheet physical and chemical tuffs with gray-green sheet physical and chemical basaltite faults Early and middle Permian Obada limestone (P1-2ca)", "triple_list": [ [ "Light gray-green sheet physical and chemical tuff sandwiched gray-green sheet physical and chemical basalt andshan rock", "Fault contact", "Obada limestone in the early and middle Permian" ] ] }, { "text": "Brown gray medium-thick layered medium-grain feldspar quartz sandstone, petal gill fossils and plant fossil fragments Posidonia sp. 158.31m", "triple_list": [ [ "Brown gray medium-thick layered medium-grain feldspar quartz sandstone", "Paleontological", "Petal gill fossil" ], [ "Brown gray medium-thick layered medium-grain feldspar quartz sandstone", "Paleontological", "Plant fossil fragments" ], [ "Brown gray medium-thick layered medium-grain feldspar quartz sandstone", "Paleontological", "Posidonia sp." ], [ "Brown gray medium-thick layered medium-grain feldspar quartz sandstone", "thickness", "158.31m" ] ] }, { "text": "Gray medium-thick layered fine-grained rock-cut feldspar sandstone with gray thin layer of calcareous silt sandstone and silt silt silt 231.03m", "triple_list": [ [ "Gray medium-thick layered fine-grained rock fragment feldspar sandstone with gray thin layer of calcium silty sandstone and silty silty silty silty silty", "thickness", "231.03m" ] ] }, { "text": "Gray-green medium-layered medium-grained rock-cut feldspar sandstone 2.33m", "triple_list": [ [ "Gray-green medium-layered medium-grained feldspar sandstone", "Lithology", "2.33m" ] ] }, { "text": "Gray limestone and silty slate (incomplete exposure of the lower strata due to faults) 46.7m", "triple_list": [ [ "Gray limestone with silty slab", "thickness", "46.7m" ] ] }, { "text": "Gray medium-thick layered shiny crystal containing biological clastic gravel limestone with gray medium-layered fine crystal dolomite 95.00m", "triple_list": [ [ "Gray medium-thick layered shiny crystal containing biological debris gravel limestone with gray medium-layered fine crystal dolomite", "thickness", "95.00m" ] ] }, { "text": "This work recourses to the obvious fault contact relationship between the formation and the Nuoribagaribao group of the Kaixinling Jiushen Team. The local strong deformation zone in the Zhonggenyong area is in contact with the tough shear zone, developing mylopsided surface treatment and rotating scattered spots.", "triple_list": [ [ "Strata", "Fault contact", "Kaixinling Ninety Train Team" ], [ "Strata", "Fault contact", "Nuoribagari protection group" ], [ "Strata", "Develop", "Myrgonal facial" ], [ "Strata", "Develop", "Rotating smudges" ] ] }, { "text": "The volcanic rocks of this rock formation are mainly mesoplasmic lava, and clastic rocks are characterized by feldspar and have fewer fossils. The corals are only collected in the lower strata in the region, including Pinacophyllum sp., Margaosmilia sp.; Cyclocyclicus sp.; Epigondolella Postera (oxur et Mostles)E.abneptis spatultus (Hayashi).", "triple_list": [ [ "Volcanic rocks", "Lithology", "Medium-basic lava" ], [ "Volcanic rocks", "Lithology", "Clastite" ], [ "Volcanic rocks", "Paleontological", "Coral Pinacophyllum sp." ], [ "Volcanic rocks", "Paleontological", "Margaosmilia sp." ], [ "Volcanic rocks", "Paleontological", "Sea Lily Cyclocyclicus sp." ], [ "Volcanic rocks", "Paleontological", "Epigondolella Postera (oxur et Mostles)" ], [ "Volcanic rocks", "Paleontological", "E.abneptis spatultus (Hayashi)" ] ] }, { "text": "Polila Group (3b) was created by Sichuan Province's Third Regional Test Team (1974) based on the Polila section of Chaya County, Tibet.", "triple_list": [ [ "Polira group", "Exposed", "Chaya County, Tibet" ] ] }, { "text": "Gray limestone and slate interlayer, producing head-fossils. Balatonites sp. Cuccoceras sp. Lonooborditoides sp. Actocordiceras sp. 248.6m", "triple_list": [ [ "Gray limestone and slate interlayer", "Paleontological", "fossils of cephalost Balatonites sp." ], [ "Gray limestone and slate interlayer", "Paleontological", "Cuccoceras sp." ], [ "Gray limestone and slate interlayer", "Paleontological", "Lonooborditoides sp." ], [ "Gray limestone and slate interlayer", "Paleontological", "Actocordiceras sp." ], [ "Gray limestone and slate interlayer", "thickness", "248.6m" ] ] }, { "text": "The stratigraphic units of the Kapila Group Belongs to to the Kanik order.", "triple_list": [ [ "Kapila Group", "Age", "Kanik-level" ] ] }, { "text": "Gray Yingan Fluid Glassic Tuff 8.0m", "triple_list": [ [ "Gray Ying'an Fluid Glassic Tuff", "thickness", "8.0m" ] ] }, { "text": "The formation contains pyrite grains with a particle size of 22mm.", "triple_list": [ [ "Pyrite crystal grains", "thickness", "22mm" ] ] }, { "text": "Among the limestone layers are the brachiopod Liosotella cylinrica (Ustrisi), Orthoticia morganina (Derby) and Misellina claudiae (Deprat), Pseudofusulina sp., which are important molecules in the early Permian.", "triple_list": [ [ "Limestone", "Paleontological", "Liosotella cylinrica (Ustrisi)" ], [ "Limestone", "Paleontological", "Orthoticia morganina(Derby)" ], [ "Limestone", "Paleontological", "Misellina claudiae (Deprat)" ], [ "Limestone", "Paleontological", "Pseudofusulina sp." ], [ "Limestone", "Age", "Early Permian" ] ] }, { "text": "The newly determined Jielong Group was transferred to the Batang Group in the late Triassic period. 1:50 million Qinghai Province digital geological maps are classified into the Triassic Jielong Formation, but they all lack the basis for the times.", "triple_list": [ [ "Jilong Group", "Belongs to", "Batang Group of the Late Triassic Period" ], [ "Jilong Group", "Belongs to", "Triassic Yukiro Formation" ] ] }, { "text": "Gray-green thin-medium tuff intersected gray-green mesolayer flow-like complex-chiss melted tuff 83.67m", "triple_list": [ [ "Gray-green thin-medium tuff intersected with gray-green medium tuff complex chip fusion tuff", "thickness", "83.67m" ] ] }, { "text": "In the stratigraphic sequence, the sedimentary rhythm of sandstone-siltstone-slate is obvious.", "triple_list": [ [ "Sandstone-siltstone-slate", "Develop", "Sedimentary rhythm" ] ] }, { "text": "The measured profiles of the Xiaocuogema Late Triassic Jiapila Group and Polila Group in Jiezha Township, Zaduo County, Qinghai Province (Figure 2-48), the starting point of the geographical coordinates is 95°50′12 east longitude, 33°11′08 north latitude, and 4637m above sea level; the end point is 95°51′54 east longitude, 33°12′07 north latitude, and 4843m above sea level.", "triple_list": [ [ "Xiaocuogema, Jiezha Township, Zaduo County, Qinghai Province", "Contained", "Late Triassic Apira Group" ], [ "Xiaocuogema, Jiezha Township, Zaduo County, Qinghai Province", "Contained", "Polira group" ], [ "profile", "Coordinates", "95°50'12 East longitude" ], [ "profile", "Coordinates", "33°11′08 North latitude" ], [ "profile", "Elevation", "4637m" ], [ "profile", "Coordinates", "95°51'54 East longitude" ], [ "profile", "Coordinates", "33°12′07 North latitude" ], [ "profile", "Elevation", "4843m" ] ] }, { "text": "Light gray thick layered limestone 18.44m", "triple_list": [ [ "Light gray thick layered limestone", "thickness", "18.44m" ] ] }, { "text": "Dark gray thin-layer fine-grained feldspar quartz sandstone and dark gray silty slate interlayer 101.60m", "triple_list": [ [ "Dark gray thin-layer fine-grained feldspar quartz sandstone and dark gray silty slate interlayer", "thickness", "101.60m" ] ] }, { "text": "Gray thick layered fluidic slurry crustal tuff 14.04m", "triple_list": [ [ "Gray thick layered fluidic slurry tuff", "thickness", "14.04m" ] ] }, { "text": "The spin-circular sedimentary sequence is mainly composed of gravel-containing sandstone and rock-cut sandstone silt sandstone in the basic strata sequence.", "triple_list": [ [ "Basic hierarchy", "Lithology", "Gravel-containing sandstone" ], [ "Basic hierarchy", "Lithology", "Rock cuttings sandstone" ], [ "Basic hierarchy", "Lithology", "Siltstone" ] ] }, { "text": "Dark gray thin-medium-layered medium-fine-grained feldspar quartz sandstone and dark gray silty slate interlayer 448.97m", "triple_list": [ [ "Dark gray thin-medium-layered medium-fine-grained feldspar quartz sandstone and dark gray silty slate interlayer", "thickness", "448.97m" ] ] }, { "text": "Gray-green medium-layered tuff intersected with gray thin-layered dolomel-containing radioworm siliceous rock 29.45m", "triple_list": [ [ "Gray-green medium-layered tuff intersected with gray thin-layered dolomel-containing siliceous rocks", "thickness", "29.45m" ] ] }, { "text": "The Jiapila Group (3jp) was created by the Sichuan Province Third Regional Test Team (1974) in the section of Jiapila Mountain in Changdu, Tibet.", "triple_list": [ [ "Kapila Group", "Exposed", "Kapila Mountain, Changdu, Tibet" ] ] }, { "text": "The Polila Formation is rich in fossils, reflected in the sedimentary environment of shallow ocean phases.", "triple_list": [ [ "Polira group", "Belongs to", "The sedimentary environment of shallow ocean phase" ] ] }, { "text": "Dark gray thin layer of chlorite petrochemical schist mica quartz schist 12.21m", "triple_list": [ [ "Dark gray thin layer of chlorite petrochemical schist mica quartz schist", "thickness", "12.21m" ] ] }, { "text": "In the area of Longmanen-Narigonma-Zhonggenyong-Ri Ajika, lava is mainly composed of volcanic breccia, clastic rock and limestone. The lithogly gray-green Andesite Andesite Andesite The basalt basalt medium-basic acid volcanic clastic rock is mixed with limestone and sandstone silt sandstone, with a thickness of about 2000m.", "triple_list": [ [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Lava" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Volcanic breccia" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Clastite" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Limestone" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Gray green Andesan rock" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Anshan basalt" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Basalt" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Medium-basic medium acidic pyroclastic rock" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Limestone" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "sandstone" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "Lithology", "Siltstone" ], [ "Longmanen-Narigonma-Zhonggenyong-Ri Ajika", "thickness", "2000m" ] ] }, { "text": "Almond-shaped andesite gray-green, spotty structure, matrix with interwoven structure, almond structure", "triple_list": [ [ "Almond-shaped Andesanite", "Distribution pattern", "Spotted structure" ], [ "Almond-shaped Andesanite", "Distribution pattern", "Interwoven structure" ], [ "Almond-shaped Andesanite", "Develop", "Almond structure" ] ] }, { "text": "The measured profiles of the Gma Late Triassic Jiapila Group and Polila Group in Jiezha Township, Zaduo County, Qinghai Province (Figure 2-45), the starting point of the geographical coordinates is 95°52′40 east longitude, 33°07′58 north latitude, and 4750m above sea level; the end point is 95°52′58 east longitude, 33°08′02 north latitude, and 4955m above sea level.", "triple_list": [ [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Late Triassic Apira Group" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Outcrop", "Polira group" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Coordinates", "95°52′40 East longitude" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Coordinates", "33°07'58 North latitude" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Elevation", "4750m" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Coordinates", "95°52'58 East longitude" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Coordinates", "33°08'02 North latitude" ], [ "Gema, Jiezha Township, Zaduo County, Qinghai Province", "Elevation", "4955m" ] ] }, { "text": "The crystalline tuff is gray-green or light purple, with a tuff structure. The rock consists of three parts: pollastic tuff and cement.", "triple_list": [ [ "Crystal rock", "Distribution pattern", "Tuff structure" ], [ "Crystal rock", "Develop", "Polgocele" ], [ "Crystal rock", "Develop", "Cement" ], [ "Clextuff", "Distribution pattern", "Tuff structure" ], [ "Clextuff", "Develop", "Polgocele" ], [ "Clextuff", "Develop", "Cement" ] ] }, { "text": "The rocks of the Bayankala Mountain Sandstone Formation are generally gray-gray-green, with fine rock particle size, and have a complete Bauma sequence, a erosion-imprint structure, parallel stratigraphic structure, and obvious sedimentary characteristics of oceanic turbidite rocks reflect the semi-deep-sea sedimentary environment. At the same time, during the sedimentation process, there are weak medium acid volcanic eruptions.", "triple_list": [ [ "Bayankala Mountain Sandstone Formation", "Contained", "Bauma Sequence" ], [ "Bayankala Mountain Sandstone Formation", "Develop", "Flushing impression structure" ], [ "Bayankala Mountain Sandstone Formation", "Develop", "Parallel layering" ], [ "Bayankala Mountain Sandstone Formation", "Lithology", "Oceanic turbid rock" ], [ "Bayankala Mountain Sandstone Formation", "Belongs to", "Semi-deep sea-deep sea sedimentary environment" ], [ "Bayankala Mountain Sandstone Formation", "Contained", "Medium acidic volcanic eruption" ] ] }, { "text": "The Triassic strata in the measurement area can be divided into the late Triassic Batang group and ligation group of the Bayankala Mountain group in the early and middle Triassic (Borila group and Bagong group in the Jiapila group).", "triple_list": [ [ "Triassic", "Outcrop", "The Triassic Triassic Jilong Formation" ], [ "Triassic", "Outcrop", "The Triassic Bayankara Mountains" ], [ "Triassic", "Outcrop", "Batang Group of the Late Triassic World" ], [ "Triassic", "Outcrop", "Ligation group" ], [ "Ligation group", "Outcrop", "Kapila Group" ], [ "Ligation group", "Outcrop", "Polira group" ], [ "Ligation group", "Outcrop", "Bagong Group" ] ] }, { "text": "Bival fossils (VIII003ZDH15-1) Posidonia gemmellaroi (Lorenzo) gemmellaroi clams; (VIII003ZDH201-1) Minetrigonia qinghaiensis Ching et Lu Qinghai Mei triangular clam Placunopsis sp. Pleuromya clams sp. Fierce sea edum clams.", "triple_list": [ [ "Dalong Sandstone", "Paleontological", "Posidonia gemmellaroi (Lorenzo) Gummar sea cob" ], [ "Dalong Sandstone", "Paleontological", "Minetrigonia qinghaiensis Ching et Lu Qinghai Mei Triangle Clam" ], [ "Dalong Sandstone", "Paleontological", "Placunopsis sp." ], [ "Dalong Sandstone", "Paleontological", "Pleuromya sp.海海海海海海海海海海海" ] ] }, { "text": "Regional geological surveys in the West Kunlun area 1:250,000 regional geological surveys found that the angle of the late Permian strata is not integrated above the Middle Permian strata at least indicates that the angle of the early and middle Permian Kaixinling group and the Late Permian-Early Triassic volcanic rock formation in the test area is still distributed in the region and has not seen large-scale exposure.", "triple_list": [ [ "Late Permian strata", "Unconformity contact", "Middle Permian strata" ], [ "Happy Ridge Group in the Permian", "Unconformity contact", "Late Permian-early Triassic Volcanic Formation" ] ] }, { "text": "The fossils collected mainly include brachiopod and petal gills.", "triple_list": [ [ "fossil", "Paleontological", "Wrist foot" ], [ "fossil", "Paleontological", "Valve gills" ] ] }, { "text": "The measured profile of the Volcanic Rock Formation in the late Triassic Batang Group of Songsai Lane, Duocai Township, Zhiduo County, Qinghai Province (Figure 2-40), the section position starts at 95°09′33 east longitude, 33°50′01 north latitude, and Elevation is 4567m; the end point is 95°06′52 east longitude, 33°48′44 north latitude, and an elevation is 4872m.", "triple_list": [ [ "Songsai Lane, Duocai Township, Zhiduo County, Qinghai Province", "Contained", "Volcanic rock formation in Batang Group in the late Triassic" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Coordinates", "95°09'33 East longitude" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Coordinates", "33°50'01 North latitude" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Elevation", "4567m" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Coordinates", "95°06'52 East longitude" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Coordinates", "33°48′44 North latitude" ], [ "Volcanic rock formation in Batang Group in the late Triassic", "Elevation", "4872m" ] ] }, { "text": "Gray-green medium-thick layered Ying'an compound chip melted tuff, gray-green medium-layered flow-gray crystal chips glass chip melted tuff, 57.74m", "triple_list": [ [ "Gray-green medium-thick layered Ying'an compound chip melted tuff, gray-green medium-layered flow-gray crystal chips glass chip melted tuff,", "thickness", "57.74m" ] ] }, { "text": "It can be divided into three rock formations with a thickness of 1330-3305m; the central volcanic carbonate formation with a thickness of 1777-1846m; the upper clastic rock formation with a thickness of 645-3038m.", "triple_list": [ [ "Clastic rock formation", "thickness", "1330-3305m" ], [ "Volcanic Carbonate Formation", "thickness", "1777-1846m" ], [ "Clastic rock formation", "thickness", "645-3038m" ] ] }, { "text": "Gray medium-thick layered fine-grained feldspar quartz sandstone and dark gray silty slate interlayer (towards the oblique core) did not reach the top 47.09m", "triple_list": [ [ "Gray medium-thick layered fine-grained feldspar quartz sandstone and dark gray silty slate interlayer", "thickness", "47.09m" ] ] }, { "text": "The Qixia Formation was integrated and contacted with the Low Fu Liangshan Formation, and the emergence of carbonyl tumor-like limestone was used as the boundary marker.", "triple_list": [ [ "Qixia Group", "Integration of contacts", "Liangshan Group" ], [ "Qixia Group", "Lithology", "Carbonomatous limestone" ] ] }, { "text": "Anshan volcanic breccia, 79.12 meters thick.", "triple_list": [ [ "Andesan volcanic breccia", "thickness", "79.12 meters" ] ] }, { "text": "The Maoshan Group and the second section of the Xiafu Tombtou Group are in integrated contact.", "triple_list": [ [ "Maoshan Group", "Integration of contacts", "Grave Group Second Section" ] ] }, { "text": "The second section of the gravet group is horizontally laminated and parallel laminated, with a single layer thickness of 1-5cm.", "triple_list": [ [ "Grave Group Second Section", "Develop", "Horizontal stratification" ], [ "Grave Group Second Section", "Develop", "Parallel layering" ] ] }, { "text": "The devon system has steep ridges on its landform, which is parallel and unconsistent with the underlying strata.", "triple_list": [ [ "Mud pot system", "Integration of contacts", "The underlying strata" ] ] }, { "text": "The angles of silt sandstone and shale are not in conjunction with the andesite.", "triple_list": [ [ "Silty sandstone with shale", "Unconformity contact", "Andanyan" ] ] }, { "text": "The flesh-red thick layer of breccia-like dolomite has a breccia-like structure, a block-like structure, and a sparsely developed knife-cutting pattern. The local crystal hole structure is suture structure, with parallel layering, a single layer thickness >50cm, and a thickness of 18.18 meters.", "triple_list": [ [ "Thick layer of flesh-red breccia dolomite", "Develop", "Breccia-like structure" ], [ "Thick layer of flesh-red breccia dolomite", "Develop", "Blocky structure" ], [ "Thick layer of flesh-red breccia dolomite", "Develop", "Knife cut pattern" ], [ "Thick layer of flesh-red breccia dolomite", "Develop", "Crystal cave structure" ], [ "Thick layer of flesh-red breccia dolomite", "Develop", "Suture construction" ], [ "Thick layer of flesh-red breccia dolomite", "Develop", "Parallel layering" ], [ "Thick layer of flesh-red breccia dolomite", "thickness", "18.18 meters" ] ] }, { "text": "Gray-green, gray-purple gravel-containing mud iron siltstone containing mud quartz siltstone on the top of the first section of Dasi Formation.", "triple_list": [ [ "A section of the big temple group", "Lithology", "Gray green gray purple gravel silt sandstone" ], [ "A section of the big temple group", "Lithology", "Amy quartz siltstone" ] ] }, { "text": "The Puqi group returned to the Middle Triassic Era.", "triple_list": [ [ "Puqi Group", "Age", "Middle Triassic" ] ] }, { "text": "The Yuntaiguan group and the Maoshan group in the lower Fu Fu Shiliu system were inconsistent contact, with a thickness of 0-3.61 meters, and the thickness in the area varies greatly.", "triple_list": [ [ "Yuntai View Group", "Integration of contacts", "Silurian Maoshan Group" ], [ "Yuntai View Group", "thickness", "0-3.61 meters" ] ] }, { "text": "Light gray gray thick layer of blocky fragmented bioclass limestone, 23.31 meters thick.", "triple_list": [ [ "Light gray gray thick layer of blocky fragmented bioclast limestone", "thickness", "23.31 meters" ] ] }, { "text": "Off-white clay is occasionally seen on the top of the Yuntaiguan group.", "triple_list": [ [ "Yuntai View Group", "Contained", "Off-white clay" ] ] }, { "text": "Jurassic off-white medium-thick layered medium-coarse-grained feldspar quartz sandstone in the overlying formation.", "triple_list": [ [ "Central Jurassic", "Lithology", "Off-white medium-thick layered medium-coarse-grained feldspar quartz sandstone" ] ] }, { "text": "Light purple gray-purple Ying'anite, 16.07 meters thick.", "triple_list": [ [ "Light purple gray purple Ying'an rock", "thickness", "16.07 meters" ] ] }, { "text": "Gray-green gray-yellow quartz sandstone, medium-fine-grained sand-like structure, horizontal lamination parallel lamination, single layer thickness 1-5cm, and a small amount of yellow-green shale, with a thickness of 7.00 meters.", "triple_list": [ [ "Gray green gray yellow quartz sandstone", "Distribution pattern", "Medium fine grain sandy structure" ], [ "Gray green gray yellow quartz sandstone", "Develop", "Horizontal stratification" ], [ "Gray green gray yellow quartz sandstone", "Develop", "Parallel layering" ], [ "Gray green gray yellow quartz sandstone", "thickness", "7.00 meters" ] ] }, { "text": "Gray yellow gray-green silty shale with iron-containing sandy quartz silty sandstone, sandy silty structure, sheet-like structure, and layer Develop, 4.31 meters thick.", "triple_list": [ [ "Gray yellow gray-green silty shale with iron-containing sand quartz silty", "Distribution pattern", "Sandy silty structure" ], [ "Gray yellow gray-green silty shale with iron-containing sand quartz silty", "Develop", "Sheet structure" ], [ "Gray yellow gray-green silty shale with iron-containing sand quartz silty", "Develop", "Layer" ], [ "Gray yellow gray-green silty shale with iron-containing sand quartz silty", "thickness", "4.31 meters" ] ] }, { "text": "Brown-yellow thick layered iron-containing calcium fine-grained quartz sandstone, 1.16 meters thick.", "triple_list": [ [ "Brown-yellow thick layered iron-containing calcium fine-grained quartz sandstone", "thickness", "1.16 meters" ] ] }, { "text": "The B-layer shale thickens, showing an extrinsic sequence.", "triple_list": [ [ "B-layer", "Lithology", "shale" ] ] }, { "text": "Purple-red, gray-yellow, gray-green, silty water mica shale, silty mud structure, 10.77 meters thick", "triple_list": [ [ "purple-red gray-yellow gray-green silt water mica shale", "Distribution pattern", "Silty-containing mud structure" ], [ "purple-red gray-yellow gray-green silt water mica shale", "Develop", "Page structure" ], [ "purple-red gray-yellow gray-green silt water mica shale", "thickness", "10.77 meters" ] ] }, { "text": "Gray-green, gray-yellow fine-grained rock-cut quartz sandstone, fine-grained sand-like structure, horizontal lamination parallel lamination, single layer thickness 10-35cm. Clip a small amount of yellow-green shale. 10.69 meters thick, integrating the second section of the grave group.", "triple_list": [ [ "Gray green gray yellow fine-grained quartz sandstone", "Distribution pattern", "Fine-grained sandy structure" ], [ "Gray green gray yellow fine-grained quartz sandstone", "Develop", "Horizontal stratification" ], [ "Gray green gray yellow fine-grained quartz sandstone", "Develop", "Parallel layering" ], [ "Gray green gray yellow fine-grained quartz sandstone", "thickness", "10.69 meters" ], [ "Gray green gray yellow fine-grained quartz sandstone", "Integration of contacts", "Grave Group Second Section" ] ] }, { "text": "The Yuntaiguan Formation and the Dapu Formation are in parallel and unconformed contact, and Contained iron quartz sandstone.", "triple_list": [ [ "Yuntai View Group", "Integration of contacts", "Dapu Group" ], [ "Yuntai View Group", "Lithology", "Iron-containing quartz sandstone" ] ] }, { "text": "The gray-black siltstone contains Podozamites IancoIntus (Let H) Braun (batch cycad), 18.02m thick.", "triple_list": [ [ "Gray black siltstone", "Paleontological", "Podozamites IancoIntus (Let H) Braun (Batch Cycad)" ], [ "Gray black siltstone", "thickness", "18.02m" ] ] }, { "text": "Light yellow medium-thick layered calcareous feldspar quartz sandstone, 6.56 meters thick.", "triple_list": [ [ "Light yellow medium-thick layered calcareous feldspar quartz sandstone", "thickness", "6.56 meters" ] ] }, { "text": "Only the upper devon system is seen in the test area, which is divided into Shetianqiao tin mine stairs.", "triple_list": [ [ "Upper ditto", "Contained", "Shetian Bridge Steps" ], [ "Upper ditto", "Contained", "Tin mine stairs" ] ] }, { "text": "The Maoshan Formation is produced in the interlayer of gray-yellow fine-grained quartz sandstone and yellow-green gray-yellow argillite quartz silt sandstone in Cai Huasheng area, which is rich in iron minerals, including limonite hematite magnetite platinum, etc.", "triple_list": [ [ "Maoshan Group", "Exposed", "Cai Huasheng" ], [ "Maoshan Group", "Lithology", "Gray yellow fine-grained quartz sandstone" ], [ "Maoshan Group", "Lithology", "Yellow-green gray-yellow mud quartz siltstone" ], [ "Maoshan Group", "Contained", "Iron minerals" ], [ "Maoshan Group", "Contained", "Limonite" ], [ "Maoshan Group", "Contained", "Hematite mine" ], [ "Maoshan Group", "Contained", "magnetite" ], [ "Maoshan Group", "Contained", "Titanium ore" ] ] }, { "text": "Maoshan Group and Yuntaiguan Group are in parallel and unconsistent contact", "triple_list": [ [ "Maoshan Group", "Integration of contacts", "Yuntai View Group" ] ] }, { "text": "The lower basic stratigraphic sequence of Qixia Formation A carbonomatous limestone B carbonaceous shale", "triple_list": [ [ "Qixia Group", "Lithology", "Carbonomatous limestone" ], [ "Qixia Group", "Lithology", "Carbon shale" ] ] }, { "text": "The trace amount of biocracks is distributed in sparse distribution, including chevrons and echinoderms, with a thickness of 18.24 meters.", "triple_list": [ [ "Biochips", "Paleontological", "Petal gills" ], [ "Biochips", "Paleontological", "Acanthus" ], [ "Biochips", "thickness", "18.24 meters" ] ] }, { "text": "Purple-red thin layer of stuccostone, stucco (microcrystalline) structure, thin layer structure, knife-cutting pattern Develop, local oblique lamellar structure, crystal hole structure, horizontal lamellar, single layer thickness 1-5cm, and 4.58 meters thick.", "triple_list": [ [ "Purple-red thin layer of stucco", "Distribution pattern", "Stucco (microcrystalline) structure" ], [ "Purple-red thin layer of stucco", "Develop", "Thin layered structure" ], [ "Purple-red thin layer of stucco", "Develop", "Knife cut pattern" ], [ "Purple-red thin layer of stucco", "Develop", "Inclined layering structure" ], [ "Purple-red thin layer of stucco", "Develop", "Crystal cave structure" ], [ "Purple-red thin layer of stucco", "Develop", "Horizontal stratification" ], [ "Purple-red thin layer of stucco", "thickness", "4.58 meters" ] ] }, { "text": "Gray yellow gray-green mud-sand quartz siltstone, mud-sand silt-like structure, sheet-like structure, stratum Develop, iron minerals (magnetite, tetrateite), 55.76 meters thick", "triple_list": [ [ "Gray yellow gray-green mud-containing sandy quartz silt sandstone", "Distribution pattern", "Silty sand-containing structure" ], [ "Gray yellow gray-green mud-containing sandy quartz silt sandstone", "Develop", "Sheet structure" ], [ "Gray yellow gray-green mud-containing sandy quartz silt sandstone", "Develop", "Layer" ], [ "Gray yellow gray-green mud-containing sandy quartz silt sandstone", "thickness", "55.76 meters" ] ] }, { "text": "Yellow-green aquatic shale is accompanied by gray thin-layer aquatic microcrystalline limestone. The rock contains aquatic bands, 19.23 meters thick, containing Opiceras cf. demissum (Oppel), O.cf.sinense ien, O.sp., Lytophiceras sp., L.cf.sauntala (Diener), Claraia sp. C. griesbachi (Bittner).", "triple_list": [ [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Contained", "Mud strips" ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "thickness", "19.23 meters" ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "Opiceras cf. demissum (Oppel)" ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "O.cf.sinense ien" ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "O.sp." ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "Lytophiceras sp." ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "L.cf.sauntala (Diener)" ], [ "Yellow-green muddy shale with gray thin-layered muddy microcrystalline limestone", "Paleontological", "Claraia sp. C. griesbachi (Bittner)" ] ] }, { "text": "Gray yellow gray-green pattern layered mud-containing quartz silt sandstone, mud-containing silt sand structure, sheet-like structure, layer Develop, 21.75 meters thick.", "triple_list": [ [ "Gray yellow gray-green layered mud-containing quartz silt sandstone", "Distribution pattern", "Silty sand-containing structure" ], [ "Gray yellow gray-green layered mud-containing quartz silt sandstone", "Develop", "Sheet structure" ], [ "Gray yellow gray-green layered mud-containing quartz silt sandstone", "Develop", "Layer" ], [ "Gray yellow gray-green layered mud-containing quartz silt sandstone", "thickness", "21.75 meters" ] ] }, { "text": "The Chalaceous-Paleogenesis is exposed around Liangzihu District in the western part of the test area, and appears sporadically isolated outcrops, with a distribution area of 5.38Km2, accounting for 0.6% of the test area.", "triple_list": [ [ "Chalk - Paleogene", "Exposed", "Surrounding Liangzi Lake District in the western part of the test area" ], [ "Chalk - Paleogene", "area", "5.38Km2" ] ] }, { "text": "The second section of Daye Formation is light gray medium-thick layered mortar, with horizontal layering and rock Develop suture structure, and is integrated and in contact with the first section of the Underworld Daye Formation. The appearance of medium-thick layered mortar is used as a boundary marker, with stable lithology and a thickness of 35.67-65 meters.", "triple_list": [ [ "Daye Group Second Section", "Lithology", "Light gray medium-thick layered stucco" ], [ "Daye Group Second Section", "Develop", "Horizontal stratification" ], [ "Daye Group Second Section", "Develop", "Suture construction" ], [ "Daye Group Second Section", "Integration of contacts", "Daye Group One" ], [ "Daye Group Second Section", "Lithology", "Medium-thick layered mortar" ], [ "Daye Group Second Section", "thickness", "35.67-65 meters" ] ] }, { "text": "The volcanic rocks of the Dasi Formation are widely distributed in the eastern half of the Taurus landform in the measurement area, and are crescent-shaped curved to the west, with an exposed area of about 113.93Km2, with strong activity and large scale. The relationship between volcanic institutions is complex, and the mineralization relationship is relatively close to mineralization of minerals such as CuAuPbZn, which is the focus of this work research.", "triple_list": [ [ "Dasi Formation Volcanic Rock", "Exposed", "Taurus eastern half" ], [ "Dasi Formation Volcanic Rock", "Distribution pattern", "Crescent curved westward" ], [ "Dasi Formation Volcanic Rock", "area", "113.93Km2" ] ] }, { "text": "Light gray thick layered gravel-containing oxibe limestone, with breccia-like structure, block-like structure, sparsely developed knife-cutting patterns, locally visible crystal hole structure suture structure, parallel layering, single layer thickness >45cm, and thickness 8.03 meters.", "triple_list": [ [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Breccia-like structure" ], [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Blocky structure" ], [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Knife cut pattern" ], [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Crystal cave structure" ], [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Suture construction" ], [ "Light gray thick layered gravel-containing oximeter limestone", "Develop", "Parallel layering" ], [ "Light gray thick layered gravel-containing oximeter limestone", "thickness", "8.03 meters" ] ] }, { "text": "Dark gray thick layer of osaminite sand chip limestone, osaminite sand chip structure, block structure, local visible crystal hole structure, horizontal layer thickness 25-35cm, containing osaminite, sand chips and a small amount of gravel clumps, 87.09 meters thick.", "triple_list": [ [ "Dark gray thick layer of osagrail limestone", "Distribution pattern", "Oxygen sand chip structure" ], [ "Dark gray thick layer of osagrail limestone", "Develop", "Blocky structure" ], [ "Dark gray thick layer of osagrail limestone", "Develop", "Crystal cave structure" ], [ "Dark gray thick layer of osagrail limestone", "Develop", "Horizontal stratification" ], [ "Dark gray thick layer of osagrail limestone", "Lithology", "Oxygen" ], [ "Dark gray thick layer of osagrail limestone", "Lithology", "Sand chips" ], [ "Dark gray thick layer of osagrail limestone", "Lithology", "Gravel clumps" ], [ "Dark gray thick layer of osagrail limestone", "thickness", "87.09 meters" ] ] }, { "text": "Pterophyllum decurrens Sze is contained in mud siltstone.", "triple_list": [ [ "Mud siltstone", "Contained", "Pterophyllum decurrens Sze" ] ] }, { "text": "Yellow-green gray-green argill quartz siltstone, a muddy silt structure, a block-like structure, 16.78 meters thick, integrating a section of the gravet group.", "triple_list": [ [ "Yellow-green gray-green amy quartz siltstone", "Distribution pattern", "Mud-containing silty sandy structure" ], [ "Yellow-green gray-green amy quartz siltstone", "Develop", "Blocky structure" ], [ "Yellow-green gray-green amy quartz siltstone", "thickness", "16.78 meters" ], [ "Yellow-green gray-green amy quartz siltstone", "Integration of contacts", "A grave group" ] ] }, { "text": "There are many types of biodies in the Maokou group, including cyanobacteria, mesophobia, acropenesis, brachiopods, foraminifera, gastropods, bryozoosomes, and sponge bone needles.", "triple_list": [ [ "Maokou Group", "Paleontological", "Petal gills" ], [ "Maokou Group", "Paleontological", "Cyanobacteria" ], [ "Maokou Group", "Paleontological", "Aphrodisiac" ], [ "Maokou Group", "Paleontological", "Acanthus" ], [ "Maokou Group", "Paleontological", "Brachiopod" ], [ "Maokou Group", "Paleontological", "Foraminifera" ], [ "Maokou Group", "Paleontological", "Gastropod" ], [ "Maokou Group", "Paleontological", "Fly" ], [ "Maokou Group", "Paleontological", "Belimidia" ], [ "Maokou Group", "Paleontological", "Sponge bone needle" ] ] }, { "text": "Gray-purple thick layered dolomite breccia, with breccia-like structure, blocky structure, sparsely developed knife-cutting patterns, locally visible crystal hole structure suture structure, parallel layering, single layer thickness >45cm, and 12.72 meters thick.", "triple_list": [ [ "Gray-purple thick layered dolomite breccia", "Develop", "Breccia-like structure" ], [ "Gray-purple thick layered dolomite breccia", "Develop", "Blocky structure" ], [ "Gray-purple thick layered dolomite breccia", "Develop", "Knife cut pattern" ], [ "Gray-purple thick layered dolomite breccia", "Develop", "Crystal cave structure" ], [ "Gray-purple thick layered dolomite breccia", "Develop", "Suture construction" ], [ "Gray-purple thick layered dolomite breccia", "Develop", "Parallel layering" ], [ "Gray-purple thick layered dolomite breccia", "thickness", "12.72 meters" ] ] }, { "text": "The basic stratigraphic sequence of the Maokou Formation consists of A medium-thick layer of stucco bioclass limestone; B thick layer of carbonaceous bioclass limestone.", "triple_list": [ [ "Maokou Group", "Lithology", "Medium-thick layer of stucco bioclass limestone" ], [ "Maokou Group", "Lithology", "Thick layered carbonaceous bioclass limestone" ] ] }, { "text": "The tectonic position of the survey area belongs to the Wuhan-Daye platform fold belt under the Yangtze River Float, which is located in the contact area between the Xianning Stand and the Jiayu Platform fold, and the tectonic activity is strong.", "triple_list": [ [ "Test area", "Earth tectonic location", "Yangzitaiping, Wuhan-Dayetai pleated belt under the platform" ], [ "Test area", "Located at", "Daye platform fold Xianning platform fold" ], [ "Test area", "Located at", "Jiayutai Pleated Buckle" ] ] }, { "text": "The Majiashan Formation was inconsistent contact with the Lingxiang rock mass erupted, 1 tuff breccia; 2 angular glittery elliptic elliptic, accounting for 14.86% of the total area of the measured area.", "triple_list": [ [ "Majiashan Group", "Unconformity contact", "Lingxiang rock body" ], [ "Majiashan Group", "Lithology", "tuff breccia" ], [ "Majiashan Group", "Lithology", "Glittering horns" ] ] }, { "text": "Light purple gray-purple andestone, 11.92 meters thick.", "triple_list": [ [ "Light purple gray purple Andesan rock", "thickness", "11.92 meters" ] ] }, { "text": "Off-white, gray-red medium-thin layered dolomite, horizontal laminated, developed suture structure, 1.10 meters thick.", "triple_list": [ [ "Off-white, gray-red, medium-thin layered dolomite", "Develop", "Horizontal stratification" ], [ "Off-white, gray-red, medium-thin layered dolomite", "Develop", "Suture construction" ], [ "Off-white, gray-red, medium-thin layered dolomite", "thickness", "1.10 meters" ] ] }, { "text": "Gray yellow yellow-green containing silty mica shale, containing silty mud structure, silty structure, and stratum Develop.", "triple_list": [ [ "Gray yellow yellow green silty mica shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray yellow yellow green silty mica shale", "Develop", "Page structure" ], [ "Gray yellow yellow green silty mica shale", "Develop", "Layer" ] ] }, { "text": "Light gray thick layered algae-containing sand chips algae oxibe limestone, 11.48 meters thick", "triple_list": [ [ "Light gray thick layered algae-containing sand chips algae oasis limestone", "thickness", "11.48 meters" ] ] }, { "text": "Green gray-yellow fine-grained quartz sandstone, fine-grained sand-like structure, horizontal lamination parallel lamination, single layer thickness 1-8cm, iron species include limonite and hematite, with a content of 4%. 2.67 meters thick", "triple_list": [ [ "Green gray yellow fine-grained quartz sandstone", "Distribution pattern", "Fine-grained sandy structure" ], [ "Green gray yellow fine-grained quartz sandstone", "Develop", "Horizontal stratification" ], [ "Green gray yellow fine-grained quartz sandstone", "Develop", "Parallel layering" ], [ "Green gray yellow fine-grained quartz sandstone", "Contained", "Limonite" ], [ "Green gray yellow fine-grained quartz sandstone", "Contained", "Hematite mine" ], [ "Green gray yellow fine-grained quartz sandstone", "thickness", "2.67 meters" ] ] }, { "text": "The Qixia Formation and the Huanglong Formation are parallel and unconformed in contact 1. Carbon shale 2. Carbon limestone 3. Biological clastic oolitic limestone", "triple_list": [ [ "Qixia Group", "Integration of contacts", "Huanglong Group" ], [ "Qixia Group", "Lithology", "Carbon shale" ], [ "Qixia Group", "Lithology", "Carbonite limestone" ], [ "Qixia Group", "Lithology", "Bioclastic ovalite limestone" ] ] }, { "text": "Meat-red grey pelleted rhyolite, 66.51 meters thick.", "triple_list": [ [ "Meat red grey rhizome", "thickness", "66.51 meters" ] ] }, { "text": "Fine sandstone strips are sandwiched in the rock, with a thickness of about 1-2cm.", "triple_list": [ [ "rock", "Contained", "Fine sandstone strips" ], [ "rock", "thickness", "1-2cm" ] ] }, { "text": "The Longtan Formation is a shore marsh phase deposit.", "triple_list": [ [ "Longtan Group", "Belongs to", "Coastal swamp sedimentation" ] ] }, { "text": "Off-white andesite, a patchy matrix with interwoven structure and apricot body structure.", "triple_list": [ [ "Off-white Andesanite", "Distribution pattern", "Less spot-like structure" ], [ "Off-white Andesanite", "Distribution pattern", "Interwoven structure" ], [ "Off-white Andesanite", "Develop", "Apricot body structure" ] ] }, { "text": "Cai Huasheng's thickness in the southern part of the test area is 58.18m, Maopu Reservoir in the central part is 116.93m, and Lihou's thickness in the Xifan's thickness is 98.48m.", "triple_list": [ [ "Cai Huasheng, southern part of the test area", "thickness", "58.18m" ], [ "Maopu Reservoir", "thickness", "116.93m" ], [ "Xifan Li", "thickness", "98.48m" ] ] }, { "text": "This work tentatively sets the Majiashan Group's era as the late Jurassic period.", "triple_list": [ [ "Majiashan Group", "Age", "Late Jurassic" ] ] }, { "text": "Strispirifer cf. hsiehi was found in the south; Cornocephalus orientalis, and the times Belongs to to the world.", "triple_list": [ [ "The south borders Tongshan", "Paleontological", "Strispirifer cf. hsiehi" ], [ "The south borders Tongshan", "Paleontological", "Cornocephalus orientalis" ], [ "The south borders Tongshan", "Age", "Zhongshiliushi" ] ] }, { "text": "Gray medium-thin layered stucco stucco smudges sandwiched gray dark gray thin-layered amidst limestone, with horizontal stratigraphic, locally visible suture structure, 45.00 meters thick.", "triple_list": [ [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray thin-layered amidst limestone", "Develop", "Horizontal stratification" ], [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray thin-layered amidst limestone", "Develop", "Suture construction" ], [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray thin-layered amidst limestone", "thickness", "45.00 meters" ] ] }, { "text": "The rock contains a very small amount of sandy strips, with the strips being 0.5cm thick and 120.96 meters thick.", "triple_list": [ [ "rock", "Contained", "Sand strips" ], [ "rock", "thickness", "120.96 meters" ] ] }, { "text": "The rocks in Xintan Formation have mud structures containing silt mud structures. The horizontal silt structure is developed in parallel silt layers, and the stratum Develop is developed, and there are local wavy marks.", "triple_list": [ [ "Xintan Group Rocks", "Distribution pattern", "Mud structure" ], [ "Xintan Group Rocks", "Distribution pattern", "Silty-containing mud structure" ], [ "Xintan Group Rocks", "Distribution pattern", "Mud silt structure" ], [ "Xintan Group Rocks", "Develop", "Horizontal stratification" ], [ "Xintan Group Rocks", "Develop", "Parallel layering" ], [ "Xintan Group Rocks", "Develop", "Layer" ], [ "Xintan Group Rocks", "Contained", "Wave trace" ] ] }, { "text": "Light gray thick layer of dolomel oval limestone, oval structure, block structure, local bird's eye tectonic oblique stratigraphic structure, horizontal stratigraphic, single layer thickness >45cm, and thickness 21.62 meters.", "triple_list": [ [ "Light gray thick layer of dolomite oasis limestone", "Distribution pattern", "Ocillary structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Blocky structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Bird's eye structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Inclined layering structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Horizontal stratification" ], [ "Light gray thick layer of dolomite oasis limestone", "thickness", "21.62 meters" ] ] }, { "text": "The muddy siltstone contains a large number of petals and plant fossils, Utschamiella SP (Chamm), Unio sp (Beaded mussels), Ciathropteris sp (lattice fern), PtilophyIIum Pecten (Phillips) Morris (cnoid hairy leaves), etc., with a thickness of 26.18m.", "triple_list": [ [ "Mud siltstone", "Paleontological", "Petal gills" ], [ "Mud siltstone", "Paleontological", "Plant fossil Utschamiella SP (Camm)" ], [ "Mud siltstone", "Paleontological", "Unio sp (bead mussel)" ], [ "Mud siltstone", "Paleontological", "Ciathropteris sp (lattice fern)" ], [ "Mud siltstone", "Paleontological", "PtilophyIIum Pecten (Phillips) Morris (Cron-shaped feather leaf)" ], [ "Mud siltstone", "thickness", "26.18m" ] ] }, { "text": "The upper basic sequence of the second section of the Tomb Tou Formation is composed of thin layers of quartz sandstone A and B squarelle. It is thick and thinned to the upper layer, showing an infiltration and accumulation-type sequence, which is shallow sea-shore-shore phase sedimentation.", "triple_list": [ [ "Grave Group Second Section", "Lithology", "Thin layer of quartz sandstone" ], [ "Grave Group Second Section", "Lithology", "shale" ], [ "Grave Group Second Section", "Belongs to", "Shallow sea-shore coastal phase sedimentation" ] ] }, { "text": "Silu Xintan Formation-Carboniferous Huanglong Formation-Carboniferous Huanglong Formation, Tongshan County, Hubei Province", "triple_list": [ [ "Cai Huasheng, Tongshan County, Hubei Province", "Outcrop", "Shiliu Xintan Group-Carboniferous Huanglong Group" ] ] }, { "text": "The gravehead group is sandwiched with thin layers or pod-like gravel-like silty phosphorus blocks.", "triple_list": [ [ "Grave group", "Lithology", "Thin layer or pod-like gravel-like silty phosphate block" ] ] }, { "text": "Light gray blocky ovalite limestone with parallel stratigraphics, which can be seen as a bird's eye tectonic suture structure, 36.72 meters thick.", "triple_list": [ [ "Light gray blocky oasis limestone", "Develop", "Parallel layering" ], [ "Light gray blocky oasis limestone", "Develop", "Bird's eye structure" ], [ "Light gray blocky oasis limestone", "Develop", "Crystal cave structure" ], [ "Light gray blocky oasis limestone", "Develop", "Suture construction" ], [ "Light gray blocky oasis limestone", "thickness", "36.72 meters" ] ] }, { "text": "The B-layer shale thickens, showing an extrinsic sequence.", "triple_list": [ [ "B-layer", "Lithology", "shale" ] ] }, { "text": "The angle of the gray-yellow clingy sandy soil does not integrate into the underlying strata.", "triple_list": [ [ "Gray yellow clingy sandy soil", "Unconformity contact", "Dasi Group" ] ] }, { "text": "Dark gray medium-thick layered flint tuber (band) contains algae sand chips and biocrystalline fine-microcrystalline limestone, curved along the layer, laterally sharply destruction, algae traces are common in biocrystalline species, and rare in chevron species and foraminifera. 13.04 meters thick.", "triple_list": [ [ "Dark gray medium-thick layered chert-containing nodules (bands) containing algae sand chips and bioclass fine-microcrystal limestone", "Paleontological", "Algae traces" ], [ "Dark gray medium-thick layered chert-containing nodules (bands) containing algae sand chips and bioclass fine-microcrystal limestone", "Paleontological", "Petal gills" ], [ "Dark gray medium-thick layered chert-containing nodules (bands) containing algae sand chips and bioclass fine-microcrystal limestone", "Paleontological", "Aphrodisiac" ], [ "Dark gray medium-thick layered chert-containing nodules (bands) containing algae sand chips and bioclass fine-microcrystal limestone", "Paleontological", "Foraminifera" ], [ "Dark gray medium-thick layered chert-containing nodules (bands) containing algae sand chips and bioclass fine-microcrystal limestone", "thickness", "13.04 meters" ] ] }, { "text": "Dark gray medium-thick layered bioclastic stuccosm with black charcoal shale, 12.43 meters thick, containing Misellina claudiae (Deprat), Orthoticia cheiangensis Chao, Schuchertella semiplana (Waagen), Ogbinia Sp., Cystomichelinia sp.", "triple_list": [ [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "thickness", "12.43 meters" ], [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "Paleontological", "Misellina claudiae (Deprat)" ], [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "Paleontological", "Orthoticia cheiangensis Chao" ], [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "Paleontological", "Schuchertella semiplana (Waagen)" ], [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "Paleontological", "Ogbinia Sp." ], [ "Dark gray medium-thick layered tumor-like biocrystal stuccostone with black charcoal shale", "Paleontological", "Cystomichelinia sp." ] ] }, { "text": "Gray yellow gray-green contains muddy sandy quartz siltstone, containing muddy sandy silt structure, sheet-like structure, and layer Develop. Insert thin layer - fine-grained quartz sandstone, layer thickness of 1-8cm. 6.68 meters thick", "triple_list": [ [ "Gray yellow gray-green muddy sandy quartz silt sandstone", "Distribution pattern", "Silty sandy sandy structure" ], [ "Gray yellow gray-green muddy sandy quartz silt sandstone", "Develop", "Sheet structure" ], [ "Gray yellow gray-green muddy sandy quartz silt sandstone", "Develop", "Layer" ], [ "Gray yellow gray-green muddy sandy quartz silt sandstone", "thickness", "6.68 meters" ] ] }, { "text": "Anshan volcanic breccia, 29.66 meters thick.", "triple_list": [ [ "Andesan volcanic breccia", "thickness", "29.66 meters" ] ] }, { "text": "The basic stratigraphic sequence of Maokou Formation A limestone B carbonaceous limestone, with light gray blocky flint-containing strips (clutches) fragmented and bioclastic dolomite mortarstone.", "triple_list": [ [ "Maokou Group", "Lithology", "Limestone" ], [ "Maokou Group", "Lithology", "Carbonite limestone" ], [ "Maokou Group", "Lithology", "Light gray blocky flint strips containing grey matter (clusters) fragmented bioclastic dolomite stucco" ] ] }, { "text": "The third and second sections of the Dasi Group are in an eruption unconsistent relationship.", "triple_list": [ [ "The third section of the Dasi Group", "Unconformity contact", "Second paragraph" ] ] }, { "text": "The dark gray medium-thick layered flint strips Contained flint tuberculosis bioclass limestone, mainly flint tuberculosis, secondarily, Contained Polythecalis sp., with a thickness of 9.99 meters.", "triple_list": [ [ "Dark gray medium-thick layered flint strips flint tuberculosis bioclass limestone", "Paleontological", "Polythecalis sp." ], [ "Dark gray medium-thick layered flint strips flint tuberculosis bioclass limestone", "thickness", "9.99 meters" ] ] }, { "text": "An basalt is 46.43 meters thick.", "triple_list": [ [ "An Xuanyan", "thickness", "46.43 meters" ] ] }, { "text": "The Daye Group and the first section of the Lower Jialingjiang Group were in integrated contact.", "triple_list": [ [ "Daye Group", "Integration of contacts", "Jialingjiang Group One Section" ] ] }, { "text": "The dark gray medium-thin layered flint-containing strips (tuberculosis) in the middle of the Qixia Formation has fine algae traces-microcrystalline limestone.", "triple_list": [ [ "Qixia Group", "Lithology", "The dark gray medium-thin layered flint-containing strips (tuberculosis) in the middle is fine algae traces - microcrystalline limestone" ] ] }, { "text": "The lake accumulation in Wujiadun area on the east side of Liangzi Hubei was formed in the middle-late Holocene.", "triple_list": [ [ "The lake accumulation in Wujiadun area on the east side of Liangzi Hubei", "Age", "Middle-late Holocene" ] ] }, { "text": "Light gray-green Andesan volcanic breccia, volcanic breccia structure, blocky structure, 6.46 meters thick.", "triple_list": [ [ "Light gray-green Andesan volcanic breccia", "Distribution pattern", "Volcanic Breccia Structure" ], [ "Light gray-green Andesan volcanic breccia", "Develop", "Blocky structure" ], [ "Light gray-green Andesan volcanic breccia", "thickness", "6.46 meters" ] ] }, { "text": "Light gray block-containing dolomite micro-fine crystal limestone, with parallel stratigraphics, common cave structure suture structure, and local oblique stratigraphic structure, 27.33 meters thick.", "triple_list": [ [ "Light gray blocky dolomite-fine crystalline limestone", "Develop", "Parallel layering" ], [ "Light gray blocky dolomite-fine crystalline limestone", "Develop", "Cave structure" ], [ "Light gray blocky dolomite-fine crystalline limestone", "Develop", "Suture construction" ], [ "Light gray blocky dolomite-fine crystalline limestone", "Develop", "Inclined layering structure" ], [ "Light gray blocky dolomite-fine crystalline limestone", "thickness", "27.33 meters" ] ] }, { "text": "The biochips components of Longtan Formation are calcium, with a huge difference in size, roughly parallel microstructured surfaces, and there are brachiopod mesophobia chevrons.", "triple_list": [ [ "Longtan Group", "Paleontological", "Brachiopod" ], [ "Longtan Group", "Paleontological", "Aphrodisiac" ], [ "Longtan Group", "Paleontological", "Petal gills" ] ] }, { "text": "The third section of Jialingjiang Formation is in integrated contact with the second section of the lower Jialingjiang Formation.", "triple_list": [ [ "Section 3 of Jialingjiang Formation", "Integration of contacts", "Section 2 of Jialingjiang Formation" ] ] }, { "text": "Overall analysis shows that the upper devon system in the measurement area is a marine clastic rock sedimentation.", "triple_list": [ [ "Upper ditto", "Belongs to", "Maritime clastic rock sedimentation" ] ] }, { "text": "Gray dark gray thick-huge layered flint-containing clumps containing stucco bioclass limestone, 11.65 meters thick, containing Chusenella sp., Ch. Cf. tingi Chen, Glomospira sp., Pseudoliolina pulchra Sheng, P. chinghaiensis sheng, P. pseudolepida (Deprat), P. ozawai Yabe et Hanzawa, schwagerina sp., Fenestella sp., Pseudobatostomella cf. delinghensis Yang et Loo.", "triple_list": [ [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "thickness", "11.65 meters thick" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Chusenella sp." ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Ch. Cf. tingi Chen" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Glomospira sp." ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Pseudoliolina pulchra Sheng" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "P. chinghaiensis sheng" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "P.pseudolepida (Deprat)" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "P. ozawai Yabe et Hanzawa" ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "schwagerina sp." ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Fenestella sp." ], [ "Gray dark gray thick-huge layered flint clumps containing stucco bioclastic limestone", "Paleontological", "Pseudobatostomella cf. delinghensis Yang et Loo" ] ] }, { "text": "The Cretaceous system is mainly distributed in the northeast of the test area, with an exposed area of about 132.43Km2.", "triple_list": [ [ "Cretaceous", "Exposed", "Northeast of the test area" ], [ "Cretaceous", "area", "132.43Km2" ] ] }, { "text": "The Liangshan Group is parallel and does not integrate the Huanglong Group.", "triple_list": [ [ "Liangshan Group", "Integration of contacts", "Huanglong Group" ] ] }, { "text": "The dark gray medium-thin layered bioclass stuccostone contains interlayers with black carbonaceous shale, 3.73 meters thick, with different bioclastic morphology, calcium, and a species of foraminifera.", "triple_list": [ [ "Dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale interlayer", "thickness", "3.73 meters" ], [ "Dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale interlayer", "Paleontological", "Foraminifera" ], [ "Dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale interlayer", "Paleontological", "Petal gills" ], [ "Dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale interlayer", "Paleontological", "Aphrodisiac" ] ] }, { "text": "The basic sequence of the lower Dalong Formation consists of thin layers of aleite limestone A and aleite B.", "triple_list": [ [ "Dalong Group", "Lithology", "Thin layer of argillite" ], [ "Dalong Group", "Lithology", "Mud shale" ] ] }, { "text": "Parallel unconsolidation of the Dapu Formation in the overlying strata", "triple_list": [ [ "Dapu Group", "Integration of contacts", "Yuntai View Group" ] ] }, { "text": "Light gray blocky flint strips containing grey matter (clusters) fragmented biocrystal dolomite mortarstone, 3.66 meters thick", "triple_list": [ [ "Light gray blocky flint strips containing grey matter (clusters) fragmented bioclastic dolomite stucco", "thickness", "3.66 meters" ] ] }, { "text": "Gray-yellow silty clay rock, silty mud structure, thin-layer structure, single layer thickness 1-5cm. Horizontal laminar Develop. Globally weathered. 9.27 meters thick", "triple_list": [ [ "Gray yellow silty clay rock", "Distribution pattern", "Silty sandy structure" ], [ "Gray yellow silty clay rock", "Develop", "Thin layered structure" ], [ "Gray yellow silty clay rock", "Develop", "Horizontal stratification" ], [ "Gray yellow silty clay rock", "thickness", "9.27 meters" ] ] }, { "text": "Gray-purple Ying'anite-Anshanite volcanic breccia, volcanic breccia structure, blocky structure.", "triple_list": [ [ "Gray-purple Ying'an-Anshan volcanic breccia", "Distribution pattern", "Volcanic Breccia Structure" ], [ "Gray-purple Ying'an-Anshan volcanic breccia", "Develop", "Blocky structure" ] ] }, { "text": "Liangshan Group Integrates the Dapu Group", "triple_list": [ [ "Liangshan Group", "Integration of contacts", "Tai Po Group" ] ] }, { "text": "Actual stratigraphic profile diagram of the Li Permian Liangshan Formation-Dalong Formation in Xifan Daye City, Hubei Province", "triple_list": [ [ "Li in Xifan, Daye City, Hubei Province", "Outcrop", "Permian Liangshan Group-Dalong Group" ] ] }, { "text": "Codonofusiella schubertelloides sheng, Schubertella sp., Nodosaria sp., Palaeospecularia sp., Linoproductus sp., coral achylasma sp., Notothyris sp., etc., this combination belongs to the early stage of the late Permian period.", "triple_list": [ [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "schubertelloides sheng" ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "Schubertella sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "Nodosaria sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "Palaeotextularia sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "Linoproductus sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "coral achylasma sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Paleontological", "Notothyris sp." ], [ "Longtan Formation-Xiayao Formation limestone", "Age", "Early Late Permian" ] ] }, { "text": "Gray thick layered bioclass limestone with black thin layered lens-like carbonaceous shale, 13.05 meters thick.", "triple_list": [ [ "Gray thick layered biocliclass limestone with black thin layered lens-like carbon shale", "thickness", "13.05 meters" ] ] }, { "text": "The basic stratigraphic sequence of the three sections of Daye Formation consists of A-thin-thin layered limestone; B-middle layered limestone.", "triple_list": [ [ "Daye Group Three Section", "Lithology", "Thin-thin layered limestone" ], [ "Daye Group Three Section", "Lithology", "Medium layered limestone" ] ] }, { "text": "Liangshan Formation and Huanglong Formation have parallel and unconformity contact, and the emergence of gray-black charcoal shale is used as a demarcation mark.", "triple_list": [ [ "Liangshan Group", "Integration of contacts", "Huanglong Group" ], [ "Liangshan Group", "Lithology", "Gray-black charcoal" ] ] }, { "text": "The upper basic layer sequence of Qixia Formation consists of A dark gray thin-medium-thick layer of tumor-like biocliclass limestone and B thin layer of mudite limestone. Layer A becomes thinner in the upper single layer, layer B contains carbonaceous locally, and the upward mudite content increases, which is the degenerate basic layer sequence.", "triple_list": [ [ "Qixia Group", "Lithology", "Dark gray thin-medium-thick layer of tumor-like bioclast limestone" ], [ "Qixia Group", "Lithology", "Thin layer of argillite" ] ] }, { "text": "Gray-brown stomatal almond-like andesite, with a splotchy structure, 82.95 meters thick.", "triple_list": [ [ "Gray-brown stomata almond-shaped Andesite", "Distribution pattern", "Spotted structure" ], [ "Gray-brown stomata almond-shaped Andesite", "thickness", "82.95 meters" ] ] }, { "text": "The lower system of the test area is divided into Longmaxi steps, Dazhongba steps, Ziyang steps; the middle system is Ankang steps.", "triple_list": [ [ "Shiliu Department", "Contained", "Longma Creek Steps" ], [ "Shiliu Department", "Contained", "Dazhongba stairs" ], [ "Shiliu Department", "Contained", "Ziyang stairs" ], [ "Shiliu Department", "Contained", "Ankang rank" ] ] }, { "text": "Only the Shangtong Majiashan Formation is a set of volcanic eruption phase products, which are divided into upper and lower sections according to lithological characteristics.", "triple_list": [ [ "Majiashan Group", "Belongs to", "Volcanic eruption phase" ] ] }, { "text": "The Dapu Formation gray gray-white thick layer - blocky fine crystal dolomite containing algae powder clot algae sand-clad fine crystal dolomite, with light gray blocky breccia dolomite at the bottom. Some rocks are flint nodules or bands, and the knife-cutting pattern is developed and has blocky stratigraphic structure. The bird's eye tectonic crystal hole tectonic suture structure can be seen locally, with horizontal stratigraphic parallel stratigraphic, and a single layer thickness of 50cm.", "triple_list": [ [ "Tai Po Group", "Lithology", "Gray off-white thick layer - blocky fine crystal dolomite" ], [ "Tai Po Group", "Lithology", "Algae powder containing algae sand chips fine crystal dolomite" ], [ "Tai Po Group", "Lithology", "Light grey blocky breccia dolomite" ], [ "Tai Po Group", "Develop", "Flint tuberculosis" ], [ "Tai Po Group", "Develop", "Strips" ], [ "Tai Po Group", "Develop", "Knife cut pattern" ], [ "Tai Po Group", "Develop", "Block lamina" ], [ "Tai Po Group", "Develop", "Bird's eye structure" ], [ "Tai Po Group", "Develop", "Crystal cave structure" ], [ "Tai Po Group", "Develop", "Suture construction" ], [ "Tai Po Group", "Develop", "Horizontal stratification" ], [ "Tai Po Group", "Develop", "Parallel layering" ] ] }, { "text": "Xifan Lihou 3.73m.", "triple_list": [ [ "Xifan Li", "thickness", "3.73m" ] ] }, { "text": "Yellow-green-gray-black thin-layer silty sandstone with silty shale and coal line, 31.33m thick.", "triple_list": [ [ "Yellow-green-gray black thin layered silty sandstone with silty shale and coal line", "thickness", "31.33m" ] ] }, { "text": "The Dala stairs and the Xiaoyao stairs correspond to the Huanglong group.", "triple_list": [ [ "Dala Tier", "Belongs to", "Huanglong Group" ], [ "Freedom", "Belongs to", "Huanglong Group" ] ] }, { "text": "The bottom of the Yuntaiguan Formation is purple-red light flesh-red medium-layered dolomite sandy conglomerate.", "triple_list": [ [ "Yuntai View Group", "Lithology", "purple-red light flesh-red medium-layered dolomite sandy gravel" ] ] }, { "text": "The Maokou Formation is adjacent to Tianjiashan area of Dayebing. It has a single lithology and is a light gray-gray thick layered crystalline biolimestone containing flint nodule limestone, with flint strip limestone in the middle, and a dolomite limestone and dolomite lens body in the upper.", "triple_list": [ [ "Maokou Group", "Exposed", "Daye Bing Tianjiashan" ], [ "Maokou Group", "Lithology", "Light gray - gray thick layered chert-containing tuberculosis limestone" ], [ "Maokou Group", "Lithology", "Crystalline biolimestone" ], [ "Maokou Group", "Lithology", "Flint strip limestone" ], [ "Maokou Group", "Lithology", "Dolomite limestone containing flint" ], [ "Maokou Group", "Lithology", "Dolomites lens body" ] ] }, { "text": "Gray-purple Andesan volcanic breccia, volcanic breccia structure, blocky structure, 10.92 meters thick.", "triple_list": [ [ "Gray-purple Andesan volcanic breccia", "Distribution pattern", "Volcanic Breccia Structure" ], [ "Gray-purple Andesan volcanic breccia", "Develop", "Blocky structure" ], [ "Gray-purple Andesan volcanic breccia", "thickness", "10.92 meters" ] ] }, { "text": "The third section of Jialingjiang Formation, the lower part has a thick layer of dolomite breccia, and the upper part is light gray, thick layer of blocky striatum-microcrystal dolomite intersects with purple-red thin layer of plasters.", "triple_list": [ [ "Section 3 of Jialingjiang Formation", "Lithology", "Thick layer of dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Breccia" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Light gray thick layer of blocky striatum thin-microcrystalline dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Purple-red thin layer of stucco" ] ] }, { "text": "Gray yellow gray-green containing silty mica shale, silty mud structure, 102.31 meters thick.", "triple_list": [ [ "Gray yellow gray-green silty mica shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray yellow gray-green silty mica shale", "Develop", "Page structure" ], [ "Gray yellow gray-green silty mica shale", "thickness", "102.31 meters" ] ] }, { "text": "Integration of contacts between the Fontou Formation and Xintan Formation 1. Shale 2. Silty shale", "triple_list": [ [ "Grave group", "Integration of contacts", "Xintan Group" ], [ "Grave group", "Lithology", "shale" ], [ "Grave group", "Lithology", "Silty shale" ] ] }, { "text": "The Yinzuwing Qingshan Reservoir is adjacent to the east of the survey area, which is 268m thick.", "triple_list": [ [ "The east of the test area is Yinzufeng Qingshan Reservoir", "thickness", "268m" ] ] }, { "text": "The upper basic layer sequence: Layer A is a muddy siltstone, which is thicker and thinner to the upper layer, showing the proliferation layer sequence.", "triple_list": [ [ "Layer A", "Lithology", "Mud siltstone" ] ] }, { "text": "The survey area is located in the southeastern Hubei region and is under the jurisdiction of four regions including Daye, Ezhou, Xianning, Wuhan, Daye, Ezhou, and other regions. It has an area of 891.34 square kilometers. The geographical coordinates are 114°30′-114°45′ east longitude and 29°50′-30°10′ north latitude.", "triple_list": [ [ "Test area", "Located at", "Southeast Hubei region" ], [ "Test area", "Belongs to", "Wuhan" ], [ "Test area", "Belongs to", "Daye" ], [ "Test area", "Belongs to", "Ezhou" ], [ "Test area", "Belongs to", "Xianning" ], [ "Test area", "area", "891.34 square kilometers" ], [ "Test area", "Coordinates", "114°30′-114°45′" ], [ "Test area", "Coordinates", "29°50′-30°10′" ] ] }, { "text": "Gray medium-thin layered stucco stucco smudges sandwiched gray dark gray micro-layered amidst limestone, with horizontal stratigraphic structure, visible suture structure, 114.97 meters thick.", "triple_list": [ [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray micro-layered amidst limestone", "Develop", "Horizontal stratification" ], [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray micro-layered amidst limestone", "Develop", "Suture construction" ], [ "Gray medium-thin layered stucco stucco smear sandstone with gray dark gray micro-layered amidst limestone", "thickness", "114.97 meters" ] ] }, { "text": "According to the comparison of lithological characteristics, it is designated as the Gong'anzhai Group, which is a set of purple-red inland lake basin phase debris deposits, and the contact relationship with the underlying formation is an angle unconformal contact.", "triple_list": [ [ "Public Security Village Group", "Belongs to", "Purple-red inland lake basin phase debris sedimentation" ] ] }, { "text": "The B layer is phosphorus-containing feldspar quartz sandstone, which is deposited by shallow sea sheds.", "triple_list": [ [ "B-layer", "Lithology", "Phosphate-containing quartz sandstone" ], [ "B-layer", "Belongs to", "Shallow sea shed sediment" ] ] }, { "text": "1:50,000 Daye Band set the Majiashan Formation era as the early Cretaceous period.", "triple_list": [ [ "Majiashan Group", "Age", "Early Cretaceous" ] ] }, { "text": "The parallel unconsolidation of the substructure of the Yuntaiguan Formation", "triple_list": [ [ "Yuntai View Group", "Integration of contacts", "Maoshan Group" ] ] }, { "text": "Purple gray, green, yellow, thin-medium-thick layer of silt sandstone is mixed with green yellow feldspar quartz fine sandstone, and the upper part contains a small amount of siderite nodules of 2.56cm in size.", "triple_list": [ [ "Purple gray green yellow thin-medium thick layer of silt sandstone with green yellow feldspar quartz fine sandstone", "Contained", "siderite nodule" ] ] }, { "text": "The first section of Daye Formation was integrated with the Dalong Formation of the Lower Permian period, and the appearance of yellow-green mud shale was used as the boundary marker, with a thickness of 28.51-55 meters.", "triple_list": [ [ "Daye Group One", "Integration of contacts", "Permian Dalong Formation" ], [ "Daye Group One", "Lithology", "Yellow-green mud shale" ], [ "Daye Group One", "thickness", "28.51-55 meters" ] ] }, { "text": "Light purple off-white rhyolite, with a splotchy structure, 110.00 meters thick.", "triple_list": [ [ "Light purple off-white rhizome", "Distribution pattern", "Spotted structure" ], [ "Light purple off-white rhizome", "thickness", "110.00 meters" ] ] }, { "text": "Xiayao Group Integrates Longtan Group", "triple_list": [ [ "Xia Kiln Group", "Integration of contacts", "Longtan Group" ] ] }, { "text": "The Yuntaiguan Formation purple-red medium-thin layered iron-containing calcium fine-grained quartz sandstone brown-yellow thick-layered iron-containing calcium fine-grained quartz sandstone sandstone yellow-brown purple-red muddy silty sandstone silty clay shale gray-white bauxite shale.", "triple_list": [ [ "Yuntai View Group", "Lithology", "Purple-red medium-thin layered iron-containing calcium fine-grained quartz sandstone" ], [ "Yuntai View Group", "Lithology", "Brown-yellow thick layered iron-containing calcium fine-grained quartz sandstone" ], [ "Yuntai View Group", "Lithology", "Yellow-brown purple-red mud siltstone" ], [ "Yuntai View Group", "Lithology", "Silty clay shale" ], [ "Yuntai View Group", "Lithology", "Off-white bauxite shale" ] ] }, { "text": "Purple-red, gray-yellow silty shale, silty mud structure, flake-like structure, lamellar Develop, 0.54 meters thick.", "triple_list": [ [ "Purple-red, gray-yellow silty shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Purple-red, gray-yellow silty shale", "Develop", "Sheet structure" ], [ "Purple-red, gray-yellow silty shale", "Develop", "Layer" ], [ "Purple-red, gray-yellow silty shale", "thickness", "0.54 meters" ] ] }, { "text": "The middle part of the Maokou Formation is a black medium-thin layer of carbon-containing biocliclass stuccostone gray medium-thin layered biocliclass dolomite stuccostone and gray medium-thin layered lenticular biocliclass stuccostone. The thickness of the single layer varies greatly in the transverse direction and is often lenticular.", "triple_list": [ [ "Maokou Group", "Lithology", "Black medium-thin layer of charcoal-containing bioclass stucco" ], [ "Maokou Group", "Lithology", "Gray medium-thin layered bioclastic dolomite mortar" ], [ "Maokou Group", "Lithology", "Gray medium-thin layered lens-like biocrystal stucco" ] ] }, { "text": "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone, algae trace microcrystalline structure, medium-thick layered structure, single layer thickness 10-25cm, and 11.28 meters thick.", "triple_list": [ [ "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone", "Distribution pattern", "Algae trace microcrystalline structure" ], [ "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone", "Develop", "Medium-thick layered structure" ], [ "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone", "thickness", "11.28 meters" ] ] }, { "text": "The sandstone Develop of Gong'anzhai Formation is interlaced with strata, A sandstone; B gravel-containing fine sandstone; C silt sandstone forms multiple cyclic layers.", "triple_list": [ [ "Public Security Village Group", "Lithology", "sandstone" ], [ "Public Security Village Group", "Develop", "Interleaved hierarchy" ], [ "Public Security Village Group", "Lithology", "Sandstone" ], [ "Public Security Village Group", "Lithology", "Gravel-containing fine sandstone" ], [ "Public Security Village Group", "Lithology", "Siltstone" ] ] }, { "text": "The Jialingjiang Group integrates contact relationship with the Daye Group.", "triple_list": [ [ "Jialingjiang Group", "Integration of contacts", "Daye Group" ] ] }, { "text": "Jiuligang Group and the Lower Fu Puqi Group have parallel and unconformed contact, and the thickness is unknown.", "triple_list": [ [ "Jiuligang Group", "Integration of contacts", "Puqi Group" ] ] }, { "text": "The exposed strata in the measurement area are well preserved. According to comprehensive analysis and research on the strata comparison of rock combination characteristics and isotope age neighboring areas, the Jurassic-Cretaceous strata and the Neozoic strata are divided from old to new to the Paleozoic Silurian-Triassic strata, and the Jurassic-Cretaceous strata and the Neozoic strata are divided into 25 formal strata units and 15 informal strata units.", "triple_list": [ [ "Test area", "Outcrop", "Silurian-Triassic strata in the Paleozoic" ], [ "Test area", "Outcrop", "Jurassic-Cretaceous strata in the Mesozoic" ], [ "Test area", "Outcrop", "New World" ] ] }, { "text": "Gray medium-thin layered bioclastic dolomite stuccos, mixed with black thin layered carbon-containing bioclastic stuccos, 3.07 meters thick, containing Hinganotrypa sichuanensis (Yang et Hsia).", "triple_list": [ [ "Gray medium-thin layered bioclastic dolomite stuccos and black thin layered carbon-containing bioclastic stuccos", "thickness", "3.07 meters" ], [ "Gray medium-thin layered bioclastic dolomite stuccos and black thin layered carbon-containing bioclastic stuccos", "Paleontological", "Hinganotrypa sichuanensis (Yang et Hsia)" ] ] }, { "text": "Light yellow-light purple feldspar fine sandstone, fine stratigraphic Develop, single layer thickness 0.7-1mm, 9.61 meters thick.", "triple_list": [ [ "Light yellow-light purple feldspar fine sandstone", "Develop", "Micro-layering" ], [ "Light yellow-light purple feldspar fine sandstone", "thickness", "9.61 meters" ] ] }, { "text": "The third section of Daye Formation is gray medium-thin layered mortarstone, dark gray thin-layered - micro-layered aleic limestone.", "triple_list": [ [ "Daye Group Three Section", "Lithology", "Gray medium-thin layered stucco" ], [ "Daye Group Three Section", "Lithology", "Dark gray thin layered-microlayered argillite" ] ] }, { "text": "Light gray-purple andestone, with a sparse structure, 21.41 meters thick.", "triple_list": [ [ "Light gray purple Andesan rock", "Distribution pattern", "Spotted structure" ], [ "Light gray purple Andesan rock", "thickness", "21.41 meters" ] ] }, { "text": "The first section of the gravetou group is in integrated contact with the Lower Fu Xintan Group.", "triple_list": [ [ "A grave group", "Integration of contacts", "Xintan Group" ] ] }, { "text": "The rock contains very many sandy strips, 0.5-1cm thick and 30.12 meters thick.", "triple_list": [ [ "rock", "Contained", "Sand strips" ], [ "rock", "thickness", "30.12 meters" ], [ "Sand strips", "thickness", "0.5-1cm" ] ] }, { "text": "The Andanyan eruption does not integrate into the second section of Dasi Formation.", "triple_list": [ [ "Andanyan", "Unconformity contact", "Dasi Group Second Section" ] ] }, { "text": "Yellow-green, gray-yellow mud-containing quartz siltstone, mud-containing silt-like structure, horizontal silt-type layer Develop, single layer thickness 1-3cm, local gray-yellow thick layer of siltstone, with a layer thickness of about 35cm. 24.43 meters thick", "triple_list": [ [ "Yellow-green gray-yellow mud-containing sandy quartz silt sandstone", "Distribution pattern", "Silty sand-containing structure" ], [ "Yellow-green gray-yellow mud-containing sandy quartz silt sandstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud-containing sandy quartz silt sandstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud-containing sandy quartz silt sandstone", "thickness", "24.43 meters" ] ] }, { "text": "The richer fossils were obtained in Xifanli in this area, including trilobite Coronocephalus changningensis, C.ovatus, and Nalivinia capillata.", "triple_list": [ [ "Xifan Li", "Paleontological", "Trilobite Coronocephalus changningensis" ], [ "Xifan Li", "Paleontological", "C.ovatus" ], [ "Xifan Li", "Paleontological", "Nalivinia capillata" ] ] }, { "text": "This area has the Bistone Pseudoclimacographus sp., Pristiographus sp., and the times were early and the world were left behind.", "triple_list": [ [ "This area", "Paleontological", "Bistone Pseudoclimacographus sp." ], [ "This area", "Paleontological", "Pristiographus sp." ], [ "This area", "Age", "Early Shili" ] ] }, { "text": "The Liangshan Group is parallel and does not integrate the Huanglong Group.", "triple_list": [ [ "Liangshan Group", "Integration of contacts", "Huanglong Group" ] ] }, { "text": "Light gray blocky sand-fine-crystal limestone with parallel stratigraphics, can be seen with inclined stratigraphic structure cave tectonic suture structure, 14.28 meters thick.", "triple_list": [ [ "Light gray blocky sand chips-fine crystal limestone", "Develop", "Parallel layering" ], [ "Light gray blocky sand chips-fine crystal limestone", "Develop", "Inclined layering structure" ], [ "Light gray blocky sand chips-fine crystal limestone", "Develop", "Cave structure" ], [ "Light gray blocky sand chips-fine crystal limestone", "Develop", "Suture construction" ], [ "Light gray blocky sand chips-fine crystal limestone", "thickness", "14.28 meters" ] ] }, { "text": "The basic sequence of the second section of Daye Formation consists of thin layer of mortars A and medium-thick layer of mortars B.", "triple_list": [ [ "Daye Group Second Section", "Lithology", "Thin layer of stucco" ], [ "Daye Group Second Section", "Lithology", "Medium-thick layer of stucco" ] ] }, { "text": "The Huanglong Formation has light gray thick layer - block bioclass limestone, the upper part is light gray thick layered algae (sand chip) limestone, with different crystal structures containing algae sand chips, blocky structures, and local bird's eye tectonic crystal hole tectonic suture structure, with horizontal stratigraphic parallel stratigraphic, and a single layer thickness of 35cm. Thickness is 58.18-116.93 meters.", "triple_list": [ [ "Huanglong Group", "Lithology", "Light gray thick layer-block bioclast limestone" ], [ "Huanglong Group", "Lithology", "Light gray thick layered algae traces (sand chips) limestone" ], [ "Huanglong Group", "Distribution pattern", "Algae sand chips are not equal crystal structure" ], [ "Huanglong Group", "Develop", "Blocky structure" ], [ "Huanglong Group", "Develop", "Bird's eye structure" ], [ "Huanglong Group", "Develop", "Crystal cave structure" ], [ "Huanglong Group", "Develop", "Suture construction" ], [ "Huanglong Group", "Develop", "Horizontal stratification" ], [ "Huanglong Group", "Develop", "Parallel layering" ], [ "Huanglong Group", "thickness", "58.18-116.93 meters" ] ] }, { "text": "The Yinzuwing Qingshan Reservoir is adjacent to the east of the survey area and is 600m thick.", "triple_list": [ [ "The east of the test area is Yinzufeng Qingshan Reservoir", "thickness", "600m" ] ] }, { "text": "The thickness of the second section of Dasi Group is 119.72-178.46 meters.", "triple_list": [ [ "Dasi Group Second Section", "thickness", "119.72-178.46 meters" ] ] }, { "text": "Yellow-green, gray-yellow muddy quartz siltstone, muddy silt structure, horizontal silt Develop, single layer thickness 1-5cm, and thickness 23.89 meters.", "triple_list": [ [ "Yellow-green gray-yellow mud quartz siltstone", "Distribution pattern", "Mud silty sandy structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud quartz siltstone", "thickness", "23.89 meters" ] ] }, { "text": "Level A Develop level stratigraphy orthoparticle sequence stratigraphy; rock layer Develop wave mark structure.", "triple_list": [ [ "Layer A", "Develop", "Horizontal stratification" ], [ "Layer A", "Develop", "Orthoparticle sequence stratigraphy" ], [ "Layer A", "Develop", "Wave mark structure" ] ] }, { "text": "Light gray-green-gray-purple rhizostriaceous breccia, block structure, block structure, 14.97 meters thick.", "triple_list": [ [ "Light gray-green-gray purple blepharocephala", "Distribution pattern", "Block structure" ], [ "Light gray-green-gray purple blepharocephala", "Develop", "Blocky structure" ], [ "Light gray-green-gray purple blepharocephala", "thickness", "14.97 meters" ] ] }, { "text": "Yellow-green, gray-yellow argic quartz siltstone, a mud-silt structure, horizontal silt-like layering, parallel silt-Develop, single layer thickness 1-5cm, and thickness 9.19 meters.", "triple_list": [ [ "Yellow-green gray-yellow mud quartz siltstone", "Distribution pattern", "Mud silty sandy structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud quartz siltstone", "thickness", "9.19 meters" ] ] }, { "text": "The Ankang stage corresponds to a section of the grave group.", "triple_list": [ [ "Ankang rank", "Belongs to", "A grave group" ] ] }, { "text": "Light gray medium-thick layered stucco, with horizontal stratigraphic, rock Develop suture structure, 35.67 meters thick.", "triple_list": [ [ "Light gray medium-thick layered stucco", "Develop", "Horizontal stratification" ], [ "Light gray medium-thick layered stucco", "Develop", "Suture construction" ], [ "Light gray medium-thick layered stucco", "thickness", "35.67 meters" ] ] }, { "text": "Maoshan Group parallel unconsolidation of Dapu Group", "triple_list": [ [ "Maoshan Group", "Integration of contacts", "Tai Po Group" ] ] }, { "text": "Gray yellow yellow-green muddy shale, flaky structure, lamellar Develop, 12.88 meters thick.", "triple_list": [ [ "Gray yellow yellow green mud shale", "Develop", "Sheet structure" ], [ "Gray yellow yellow green mud shale", "Develop", "Layer" ], [ "Gray yellow yellow green mud shale", "thickness", "12.88 meters" ] ] }, { "text": "The Shiliu system in the survey area is mainly distributed in the Maojiapu area of Sunjianpu in the south - Tuanlinwan, with an exposed area of about 141.28m2, accounting for 15.85% of the total area of the map. The strata moves northwest and west, forming an anticline core strata, with a relatively large thickness.", "triple_list": [ [ "Shiliu Department", "Exposed", "Southern Sun Jianshu-Tuanlinwan Maojiashu" ], [ "Shiliu Department", "area", "141.28m2" ], [ "Shiliu Department", "Distribution pattern", "North West toward" ] ] }, { "text": "The C-layer siltstone develops parallel stratigraphics, which are deposited in the intermountain basins.", "triple_list": [ [ "C-layer siltstone", "Develop", "Parallel layering" ], [ "C-layer siltstone", "Belongs to", "Sedimentation of the Luxiang Mountain Basin" ] ] }, { "text": "The geological era of Daye Formation belongs to the early Triassic period.", "triple_list": [ [ "Daye Group", "Age", "Early Triassic" ] ] }, { "text": "The Permian system is divided from bottom to top into the Liangshan Group of the Lower Tong, Maokou Group of the Qixia Group of the Zhongtong, and Dalong Group of the Xiayao Group of the Shangtong Longtan Group.", "triple_list": [ [ "Permian", "Outcrop", "Liangshan Group" ], [ "Permian", "Outcrop", "Qixia Group" ], [ "Permian", "Outcrop", "Maokou Group" ], [ "Permian", "Outcrop", "Longtan Group" ], [ "Permian", "Outcrop", "Xia Kiln Group" ], [ "Permian", "Outcrop", "Dalong Group" ] ] }, { "text": "Due to the strong concealment of the Fourth System, the contact relationship with the underlying formation in the picture is unknown, and the region shows integrated contact with the Jialingjiang Formation strata, with a thickness greater than 765.93 meters.", "triple_list": [ [ "The fourth series", "Integration of contacts", "Jialingjiang Group" ], [ "The fourth series", "thickness", "765.93 meters" ] ] }, { "text": "Light purple fragmented Andestone almond-shaped Andestone with Anshanite and basalt and Andestone with Anshanite and Breccia-containing volcanic breccia-containing tuff, etc., reflecting volcanic overflow activities", "triple_list": [ [ "Dasi Group Second Section", "Lithology", "Light purple shattered Andesan rock" ], [ "Dasi Group Second Section", "Lithology", "Almond-shaped Andesanite" ], [ "Dasi Group Second Section", "Lithology", "An Xuanyan" ], [ "Dasi Group Second Section", "Lithology", "Basalt" ], [ "Dasi Group Second Section", "Lithology", "Anshan volcanic breccia crystalline rock" ], [ "Dasi Group Second Section", "Lithology", "Clextuff" ] ] }, { "text": "Jiuligang Formation develops sedimentary structures such as oblique stratigraphic interlaced stratigraphic, producing abundant fossils of petal gill plant, which are deposited by river phases.", "triple_list": [ [ "Jiuligang Group", "Develop", "Inclined layering" ], [ "Jiuligang Group", "Develop", "Interleaved hierarchy" ], [ "Jiuligang Group", "Paleontological", "Fossils of petal gills" ], [ "Jiuligang Group", "Belongs to", "River phase sedimentation" ] ] }, { "text": "The purple-red shale layer is 2-5m thick, reflecting the hot and arid climatic conditions at that time.", "triple_list": [ [ "Purple-red shale", "thickness", "2-5m" ] ] }, { "text": "The lower system of the Triassic System in the measurement area is divided into the Yinkeng step Chaohu step; the middle system is the Qingyan step; and the upper system is divided into the Asian Zhiliang step Tulong step.", "triple_list": [ [ "Triassic system", "Contained", "Yinkeng Step" ], [ "Triassic system", "Contained", "Chaohu steps" ], [ "Triassic system", "Contained", "Blue Rock Step" ], [ "Triassic system", "Contained", "Yazhiliang stairs" ], [ "Triassic system", "Contained", "Tulong rank" ] ] }, { "text": "The second section of the grave group is in integrated contact with the first section of the lower tomb group, with a thickness of 44.04-209.72 meters.", "triple_list": [ [ "Grave Group Second Section", "Integration of contacts", "A grave group" ], [ "Grave Group Second Section", "thickness", "44.04-209.72 meters" ] ] }, { "text": "The triassic system is distributed in the southern part of the measurement area, the inclined Maobaishi, the inclined core of Zhufengling, and the northeast side of the Tonggushan rock mass.", "triple_list": [ [ "Triassic system", "Exposed", "Caijia's brain tilt in the southern part of the test area" ], [ "Triassic system", "Exposed", "Maobaishi's slant" ], [ "Triassic system", "Exposed", "Zhufengling ridge oblique core" ], [ "Triassic system", "Exposed", "Northeast side of Tonggushan rock mass" ] ] }, { "text": "Cai Huasheng's thickness in the southern part of the test area is 52.74m, Maopu Reservoir in the central part is 26.59m, and Lisheng's thickness in the Xifan is 40.52m.", "triple_list": [ [ "Cai Huasheng, southern part of the test area", "thickness", "52.74m" ], [ "Maopu Reservoir", "thickness", "26.59m" ], [ "Xifan Li", "thickness", "40.52m" ] ] }, { "text": "In the yellow-brown purple-red muddy siltstone in the upper part of the Yuntaiguan Formation, there is a lens-like iron clay rock in the gray-white bauxite shale interlayer, with a low content of about 5%, which is not of industrial significance.", "triple_list": [ [ "Yuntai View Group", "Lithology", "Yellow-brown purple-red mud siltstone" ], [ "Yuntai View Group", "Lithology", "Silty clay shale" ], [ "Yuntai View Group", "Lithology", "Off-white bauxite shale" ], [ "Yuntai View Group", "Lithology", "Lens-like iron clay rock" ], [ "Yuntai View Group", "Contained", "Fe" ] ] }, { "text": "The basic strata sequence of the lower part of the Tomb Tou Formation A silty shale intersected with thin silty silty B shale", "triple_list": [ [ "A grave group", "Lithology", "Silty shale" ], [ "A grave group", "Lithology", "Thin layer of siltstone" ], [ "A grave group", "Lithology", "shale" ] ] }, { "text": "Lingxiang Formation contains 1. Shale 2. Amy siltstone 3. Siltstone 4. Calcium siltstone 5. Fine sandstone 6. Feldspar quartz sandstone 7. Gross tuff coarse sandstone 8. Gross sandstone 9. Conglomerate 10. Limestone 11. Amy 12. Silt silt limestone 13. Marlstone 14. Layered breccia tuff 15. Layered volcanic breccia 16. Andestone 17. Anite basal 18. Basal 19. Rhyolite 20. Ying'anite 21. Diorite 22. Lens-shaped gravel 23. Stomatal 24. Plant fossil 25. Anite fossil, with a thickness of 409.99-947.03 meters, and is in an eruptive and unconsistent contact with the section of the Low Fu Dasi Formation.", "triple_list": [ [ "Lingxiang Group", "Lithology", "shale" ], [ "Lingxiang Group", "Lithology", "Mud siltstone" ], [ "Lingxiang Group", "Lithology", "Siltstone" ], [ "Lingxiang Group", "Lithology", "Calcium siltstone" ], [ "Lingxiang Group", "Lithology", "Fine sandstone" ], [ "Lingxiang Group", "Lithology", "Feldspar quartz sandstone" ], [ "Lingxiang Group", "Lithology", "Gross tuff coarse sandstone" ], [ "Lingxiang Group", "Lithology", "Gravel-containing sandstone" ], [ "Lingxiang Group", "Lithology", "Polygon" ], [ "Lingxiang Group", "Lithology", "Limestone" ], [ "Lingxiang Group", "Lithology", "Mixed limestone" ], [ "Lingxiang Group", "Lithology", "Silty limestone" ], [ "Lingxiang Group", "Lithology", "Marlite" ], [ "Lingxiang Group", "Lithology", "Laminated breccia tuff" ], [ "Lingxiang Group", "Lithology", "Layered volcanic breccia" ], [ "Lingxiang Group", "Lithology", "Andanyan" ], [ "Lingxiang Group", "Lithology", "An Xuanyan" ], [ "Lingxiang Group", "Lithology", "Basalt" ], [ "Lingxiang Group", "Lithology", "Rhyolite" ], [ "Lingxiang Group", "Lithology", "Ying'an Rock" ], [ "Lingxiang Group", "Lithology", "Diorite" ], [ "Lingxiang Group", "Lithology", "Lens-like gravel" ], [ "Lingxiang Group", "Lithology", "Air hole" ], [ "Lingxiang Group", "Paleontological", "Plant fossils" ], [ "Lingxiang Group", "Paleontological", "Animal fossils" ], [ "Lingxiang Group", "thickness", "409.99-947.03 meters" ], [ "Lingxiang Group", "Unconformity contact", "A section of the big temple group" ] ] }, { "text": "The gray thick layered bioclass limestone contains sand-class, with different bioclass forms, containing Caninia sp., and is 13.12 meters thick.", "triple_list": [ [ "Gray thick layered sand-containing bioclass limestone", "Paleontological", "Caninia sp." ], [ "Gray thick layered sand-containing bioclass limestone", "thickness", "13.12 meters" ] ] }, { "text": "Gray-green gray-purple Anshan tuff breccia, 12.07 meters thick, erupting does not integrate the Lingxiang Formation of the underlying strata.", "triple_list": [ [ "Gray green gray purple Anshan tuff breccia", "thickness", "12.07 meters" ], [ "Gray green gray purple Anshan tuff breccia", "Unconformity contact", "Lingxiang Group" ] ] }, { "text": "The upper basic stratigraphic sequence A thin layer limestone B in the first section of Daye Formation.", "triple_list": [ [ "Daye Group One", "Lithology", "Thin layered limestone" ], [ "Daye Group One", "Lithology", "Medium layered limestone" ] ] }, { "text": "Dalong Formation gray-black hydromica clay rock intersects gray siliceous shale.", "triple_list": [ [ "Dalong Group", "Lithology", "gray-black water mica clay rock" ], [ "Dalong Group", "Lithology", "Gray siliceous shale" ] ] }, { "text": "Anshanite melted tuff erupts do not integrate Anshanite.", "triple_list": [ [ "Andanite melted tuff", "Unconformity contact", "An Xuanyan" ] ] }, { "text": "Luosu talc stairs correspond to Dapu Group", "triple_list": [ [ "Luo Sujie", "Belongs to", "Tai Po Group" ], [ "Talc stairs", "Belongs to", "Tai Po Group" ] ] }, { "text": "The basic sequence of the third section of the Jialingjiang Formation is composed of A thin-medium-thick layered crystalline dolomite; B gray matter dolomite; and C dissolved disintegration breccia.", "triple_list": [ [ "Section 3 of Jialingjiang Formation", "Lithology", "Thin-medium-thick layered crystalline dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Grey matter dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Breccia" ] ] }, { "text": "Medium-thin layered bioclass stuccostone-containing carbonaceous shale, 11.18 meters thick.", "triple_list": [ [ "Medium-thin layered bioclastic stuccosmic stuccosmic shale", "thickness", "11.18 meters" ] ] }, { "text": "A light gray medium-thin layered microcrystalline limestone in Daye Formation is equipped with horizontal stratigraphic structure and locally visible suture structure; the lower part is yellow-green muddy shale mixed with gray thin-layered muddy limestone, and the rock contains muddy strips, with a thickness of 1-3mm.", "triple_list": [ [ "Daye Group One", "Lithology", "Light gray medium-thin layered microcrystalline limestone" ], [ "Daye Group One", "Develop", "Horizontal stratification" ], [ "Daye Group One", "Develop", "Suture construction" ], [ "Daye Group One", "Lithology", "Yellow-green mud shale" ], [ "Daye Group One", "Lithology", "Gray thin-layered argillary microcrystalline limestone" ], [ "Daye Group One", "Contained", "Mud strips" ] ] }, { "text": "Gray yellow gray-green silty shale, silty mud structure, flake-like structure, lamellar Develop, thickness of 4.86 meters.", "triple_list": [ [ "Gray yellow gray-green silty shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray yellow gray-green silty shale", "Develop", "Sheet structure" ], [ "Gray yellow gray-green silty shale", "Develop", "Layer" ], [ "Gray yellow gray-green silty shale", "thickness", "4.86 meters" ] ] }, { "text": "The Qixia group has a wide variety of biofilm species and different shapes, including apriculi (sea lily stem), foraminifera, brachiopod, cyanobacteria, gastropod, etc.", "triple_list": [ [ "Qixia Group", "Paleontological", "Acanthus" ], [ "Qixia Group", "Paleontological", "Sea lily stem" ], [ "Qixia Group", "Paleontological", "Foraminifera" ], [ "Qixia Group", "Paleontological", "Brachiopod" ], [ "Qixia Group", "Paleontological", "Petal gills" ], [ "Qixia Group", "Paleontological", "Cyanobacteria" ], [ "Qixia Group", "Paleontological", "Gastropod" ], [ "Qixia Group", "Paleontological", "Aphrodisiac" ] ] }, { "text": "Bamboo leaf-like limestone about 3m thick appeared in Maobai City, the area of the test area, reflecting the characteristics of water turmoil and in integrated contact with the third section of the Underground Daye Formation.", "triple_list": [ [ "Test area Maobai City", "Contained", "Bamboo leaf limestone" ], [ "Bamboo leaf limestone", "Integration of contacts", "Daye Group Three Section" ] ] }, { "text": "In addition to cyanobacteria, foraminifera, brachiopod, aphrodisiac, and bryozoos can also be seen.", "triple_list": [ [ "Biochips", "Paleontological", "Cyanobacteria" ], [ "Biochips", "Paleontological", "Foraminifera" ], [ "Biochips", "Paleontological", "Brachiopod" ], [ "Biochips", "Paleontological", "Acanthus" ], [ "Biochips", "Paleontological", "Aphrodisiac" ], [ "Biochips", "Paleontological", "Fly" ], [ "Biochips", "Paleontological", "Belimidia" ] ] }, { "text": "Purple-gray thick layer of dolomelized particle microcrystalline limestone, particle microcrystalline structure, blocky structure, and sparsely developed knife-cutting patterns. The bird's eye tectonic crystal hole structure can be seen locally. The single layer has a thickness of 25-35cm, containing oximeters, debris and biochips, and a thickness of 15.75 meters.", "triple_list": [ [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Distribution pattern", "Particle crystalline structure" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Develop", "Blocky structure" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Develop", "Knife cut pattern" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Develop", "Bird's eye structure" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Develop", "Crystal cave structure" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Contained", "Oxygen" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Contained", "Broken" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "Contained", "Biochips" ], [ "Purple-gray thick layer of dolomelized particle crystalline limestone", "thickness", "15.75 meters" ] ] }, { "text": "Light gray medium-thin layered sand-containing stucco stucco, horizontally layered, 15.94 meters thick.", "triple_list": [ [ "Light gray medium-thin layered sand-containing stucco", "Develop", "Horizontal stratification" ], [ "Light gray medium-thin layered sand-containing stucco", "thickness", "15.94 meters" ] ] }, { "text": "Among them, Permophorus Sp. is common in the Xujiahe Formation of the Upper Triassic Period in Sichuan, and is mainly prosperous in the Middle Triassic Period.", "triple_list": [ [ "Permophorus Sp.", "Located at", "Xujiahe Formation of the Shangsansanded dynasty in Sichuan" ], [ "Permophorus Sp.", "Age", "Middle Triassic" ] ] }, { "text": "The Triassic system is divided into the Daye Group of the Lower Order, the Jialingjiang Group of the Middle and Lower Order, the Puqi Group of the Middle and Upper Order, and is in an integrated contact with the Permian System.", "triple_list": [ [ "Triassic system", "Outcrop", "Daye Group" ], [ "Triassic system", "Outcrop", "Jialingjiang Group" ], [ "Triassic system", "Outcrop", "Puqi Group" ], [ "Triassic system", "Outcrop", "Jiuligang Group" ], [ "Triassic system", "Integration of contacts", "Permian" ] ] }, { "text": "The Dalong Formation is integrated and contacted with the Lower Lower Kiln Formation.", "triple_list": [ [ "Dalong Group", "Integration of contacts", "Xia Kiln Group" ] ] }, { "text": "Longtan Group parallel unconsolidation Maokou Group", "triple_list": [ [ "Longtan Group", "Integration of contacts", "Maokou Group" ] ] }, { "text": "The marl contains Darwinula yongfuensis Guan (Yongfu Darwin), Cypridea (Cypridea) gunsulinensis Su (Prince Ridge), Cypridea (Cypridea) dongfangensis Ding (Oriental actress), Cypridea (Cypridea) SP.1 (Female star 1), Naamnranaia Cf. Chingshanense (Similar species of Qingshan Nakamura), Cladophlebis heterophylla (Fontaine) (Sex-leaved vein fern), Cladophlebis Pachyphylla (Fontaine) (Thick-leaved vein fern), Gleichenites SP.2 (Libai star 2).", "triple_list": [ [ "Marlite", "Paleontological", "Darwinula yongfuensis Guan (Introduction to Yongfuensis)" ], [ "Marlite", "Paleontological", "Cypridea (Cypridea) gunsulinensis Su (Princess Princess Ridge actress)" ], [ "Marlite", "Paleontological", "Cypridea (Cypridea) dongfangensis Ding (Oriental actress introduction)" ], [ "Marlite", "Paleontological", "Cypridea (Cypridea) SP.1 (Actors Introduction to Undecided 1)" ], [ "Marlite", "Paleontological", "Naamnranaia Cf. Chingshanense (similar species of clams in Qingshan Nakamura)" ], [ "Marlite", "Paleontological", "Cladophlebis heterophylla (Fontaine)" ], [ "Marlite", "Paleontological", "Cladophlebis Pachyphylla (Fontaine) (Thick Leaf-branched Vein Fern)" ], [ "Marlite", "Paleontological", "Gleichenites SP.2 (Libai Undetermined Type 2)" ] ] }, { "text": "Gray yellow gray-green silty shale, silty mud structure, flake-like structure, and stratigraphic Develop.", "triple_list": [ [ "Gray yellow gray-green silty shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray yellow gray-green silty shale", "Develop", "Sheet structure" ], [ "Gray yellow gray-green silty shale", "Develop", "Layer" ] ] }, { "text": "The rhyolite eruption does not integrate into the Dashi Formation.", "triple_list": [ [ "Rhyolite", "Unconformity contact", "A section of the big temple group" ] ] }, { "text": "The devon system only has the exposed Upper Devon Tong Yuntaiguan Group, with an exposed area of about 2.15m2, accounting for 0.24% of the total area of the figure.", "triple_list": [ [ "Mud pot system", "Outcrop", "Upper Devon Tong Yuntai Temple Group" ], [ "Mud pot system", "area", "2.15m2" ] ] }, { "text": "Actual measured stratigraphic profile of Liangshan Formation-Dalong Formation in Xifan Lipermation, Daye City, Hubei Province", "triple_list": [ [ "Li in Xifan, Daye City, Hubei Province", "Contained", "Permian Liangshan Group-Dalong Group" ] ] }, { "text": "Qixia group integrates Liangshan group.", "triple_list": [ [ "Qixia Group", "Integration of contacts", "Liangshan Group" ] ] }, { "text": "Purple-red clay rock (shale) appeared at the bottom of the gravetou group and showed stable exposure in the area.", "triple_list": [ [ "A grave group", "Lithology", "Purple-red clay rock" ], [ "A grave group", "Lithology", "shale" ] ] }, { "text": "Purple-red, gray-yellow, gray-green silty shale, silty mud structure, flake-like structure, stratum Develop, 3.76m thick.", "triple_list": [ [ "purple-red gray-yellow gray-green silty shale", "Distribution pattern", "Silty-containing mud structure" ], [ "purple-red gray-yellow gray-green silty shale", "Develop", "Sheet structure" ], [ "purple-red gray-yellow gray-green silty shale", "Develop", "Layer" ], [ "purple-red gray-yellow gray-green silty shale", "thickness", "3.76m" ] ] }, { "text": "The middle basic layer sequence A medium-thick quartz sandstone B shale in the second section of the Tombtou Formation", "triple_list": [ [ "Grave Group Second Section", "Lithology", "Medium-thick quartz sandstone" ], [ "Grave Group Second Section", "Lithology", "shale" ] ] }, { "text": "Gray-green silty shale, silty mud structure, flake-like structure, lamellar Develop, 14.97 meters thick.", "triple_list": [ [ "Gray-green silty shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray-green silty shale", "Develop", "Sheet structure" ], [ "Gray-green silty shale", "Develop", "Layer" ], [ "Gray-green silty shale", "thickness", "14.97 meters" ] ] }, { "text": "The Permian system is relatively fully exposed in the southern eastern part, and has parallel and unconformal contact with the Huanglong Group of the underlying Carboniferous System.", "triple_list": [ [ "Permian", "Exposed", "South East" ], [ "Permian", "Integration of contacts", "Carbonite Huanglong Group" ] ] }, { "text": "The era of the Majiashan Formation is more objective to the late Jurassic period.", "triple_list": [ [ "Majiashan Group", "Age", "Late Jurassic" ] ] }, { "text": "Dalong Group Integrates Xiayao Group", "triple_list": [ [ "Dalong Group", "Integration of contacts", "Xia Kiln Group" ] ] }, { "text": "The lower part of the Maokou Formation is gray dark gray thick layered bioclass limestone containing flint tuberculosis, and locally dolomite limestone irregular clusters.", "triple_list": [ [ "Maokou Group", "Lithology", "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone" ], [ "Maokou Group", "Lithology", "Dolomites limestone" ] ] }, { "text": "The Permian system is also distributed in the southern part of the measurement area, the Caijianaoang, Maobaishi, Zhufengling, and the northeast side of the Tonggushan rock mass, with an exposed area of about 56.65m2, accounting for 6.36% of the total area of the map.", "triple_list": [ [ "Permian", "Exposed", "Caijia's brain tilt in the southern part of the test area" ], [ "Permian", "Exposed", "Maobaishi's slant" ], [ "Permian", "Exposed", "Zhufengling tilts" ], [ "Permian", "Exposed", "Northeast side of Tonggushan rock mass" ], [ "Permian", "area", "56.65m2" ] ] }, { "text": "Dark gray medium-thin layered flint strip flint tuber limestone, 21.94 meters thick", "triple_list": [ [ "Dark gray medium-thin layered flint strip flint limestone", "thickness", "21.94 meters" ] ] }, { "text": "The middle and lower part of the yellow-green muddy siltstone contains siderite nodules of 610 cm in size and 8.10 m in thickness.", "triple_list": [ [ "Yellow-green mud siltstone", "Contained", "siderite nodule" ], [ "Yellow-green mud siltstone", "thickness", "8.10m" ] ] }, { "text": "A section A-thickness-giant thick layer of stuccostone B-thickness-giant thick layer of fine crystal dolomite", "triple_list": [ [ "Jialingjiang Group One Section", "Lithology", "Thick-giant thick layer of stucco" ], [ "Jialingjiang Group One Section", "Lithology", "Thick-giant thick layer of fine crystal dolomite" ] ] }, { "text": "Mica rhyolite, erupting and unconforming to Lingxiang Formation.", "triple_list": [ [ "Mica rhizome", "Unconformity contact", "Lingxiang Group" ] ] }, { "text": "The second section of Majiashan Formation is purple-brown gray-purple slight rock with stomata almond-shaped slight rock, with a top of the tuff breccia, which is 215.34 meters thick.", "triple_list": [ [ "Majiashan Group Section 2", "Lithology", "Purple brown gray purple slim rock" ], [ "Majiashan Group Section 2", "Lithology", "Stomatal almond-shaped slight rock" ], [ "Majiashan Group Section 2", "Lithology", "Fluid tuff breccia" ], [ "Majiashan Group Section 2", "thickness", "215.34 meters" ] ] }, { "text": "Gray yellow yellow-green pattern layered arable quartz silt sandstone intersected with iron sandy quartz silt sandstone, the interlayer thickness ranges from 2-10cm, the rock contains a small amount of pyrite, the iron mineral content is 8%, and the thickness is 8.77 meters.", "triple_list": [ [ "Gray yellow yellow-green pattern layered arable quartz silt sandstone with iron-containing sand quartz silt sandstone", "Contained", "Pyrite" ], [ "Gray yellow yellow-green pattern layered arable quartz silt sandstone with iron-containing sand quartz silt sandstone", "Contained", "Iron minerals" ], [ "Gray yellow yellow-green pattern layered arable quartz silt sandstone with iron-containing sand quartz silt sandstone", "thickness", "8.77 meters" ] ] }, { "text": "Andesan rock is 68.48 meters thick.", "triple_list": [ [ "Andanyan", "thickness", "68.48 meters" ] ] }, { "text": "A set of acidic lava domes appeared in the Casar Tree-Trigao Mountain area in the southern volcanic rock basin, which are rhyolite spherical rhyolites.", "triple_list": [ [ "Cana trees in the southern volcanic rock basin - Triangle Mountain", "Contained", "Acid lava dome" ], [ "Acid lava dome", "Lithology", "Rhyolite" ], [ "Acid lava dome", "Lithology", "Spherical rhizome" ] ] }, { "text": "The angle of the new unified residual slope deposit does not integrate the new unified lake deposit.", "triple_list": [ [ "Brand new system residual slope accumulation", "Unconformity contact", "Brand new Tonghu accumulation" ] ] }, { "text": "The basic sequence of the Maoshan Formation A thick layer of block feldspar quartz sandstone B silt sandy shale", "triple_list": [ [ "Maoshan Group", "Lithology", "Thick layer of blocky feldspar quartz sandstone" ], [ "Maoshan Group", "Lithology", "Silty shale" ] ] }, { "text": "Gray-purple gray-yellow silt sandstone with Ying'anite, 17.69 meters thick.", "triple_list": [ [ "Gray purple gray yellow silt sandstone with Ying'an rock", "thickness", "17.69 meters" ] ] }, { "text": "Light gray-purple light gray-green basalt, with a speckled structure, 9.29 meters thick.", "triple_list": [ [ "Light gray purple light gray green basalt", "Distribution pattern", "Spotted structure" ], [ "Light gray purple light gray green basalt", "thickness", "9.29 meters" ] ] }, { "text": "Yellow-green, gray-yellow argic quartz siltstone, argic silt structure, block-like structure, horizontal silt parallel silt Develop, single layer thickness 3-6cm, 3.99 meters thick.", "triple_list": [ [ "Yellow-green gray-yellow mud quartz siltstone", "Distribution pattern", "Mud silty sandy structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Blocky structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud quartz siltstone", "thickness", "3.99 meters" ] ] }, { "text": "Yellow-green, gray-yellow argic quartz siltstone, argic silt structure, block-like structure, horizontal silt parallel silt Develop, single layer thickness 1-5cm, and thickness 7.18 meters.", "triple_list": [ [ "Yellow-green gray-yellow mud quartz siltstone", "Distribution pattern", "Mud silty sandy structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Blocky structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud quartz siltstone", "thickness", "7.18 meters" ] ] }, { "text": "The upper part of the first section of the Tomb Tou Formation is yellow-green, gray-yellow mud quartz silt sandstone, with horizontal stratigraphic Develop, and the single layer is 1-12cm thick.", "triple_list": [ [ "A grave group", "Lithology", "Mixed quartz siltstone" ], [ "A grave group", "Lithology", "Silty shale" ], [ "A grave group", "Develop", "Horizontal stratification" ], [ "A grave group", "Develop", "Parallel layering" ], [ "A grave group", "Develop", "Layer" ] ] }, { "text": "Xiayao Group is integrated and contacted with Xiafu Longtan Group.", "triple_list": [ [ "Xia Kiln Group", "Integration of contacts", "Longtan Group" ] ] }, { "text": "The flesh-red thick layer of dolomite breccia has breccia-like structure, blocky structure, sparsely developed knife-cutting patterns, locally visible crystal hole structure suture structure, and parallel stratigraphic.", "triple_list": [ [ "Thick layer of dolomite breccia", "Develop", "Breccia-like structure" ], [ "Thick layer of dolomite breccia", "Develop", "Blocky structure" ], [ "Thick layer of dolomite breccia", "Develop", "Knife cut pattern" ], [ "Thick layer of dolomite breccia", "Develop", "Crystal cave structure" ], [ "Thick layer of dolomite breccia", "Develop", "Suture construction" ], [ "Thick layer of dolomite breccia", "Develop", "Parallel layering" ] ] }, { "text": "The Jiuligang Formation has interlayered with earth-yellow quartz fine sandstone, earth-yellow thin-layer silty sandstone argillic silty sandstone and gray-black silty shale.", "triple_list": [ [ "Jiuligang Group", "Lithology", "Ocillary quartz fine sandstone" ], [ "Jiuligang Group", "Lithology", "Soil yellow thin layered siltstone" ], [ "Jiuligang Group", "Lithology", "Mud siltstone" ], [ "Jiuligang Group", "Lithology", "Gray-black silty shale" ] ] }, { "text": "Off-white, light purple-red almond-shaped angamite, 35.53 meters thick.", "triple_list": [ [ "Off-white light purple-red almond-shaped Ying'anite", "thickness", "35.53 meters" ] ] }, { "text": "Siltstone is rich in plant fossil fragments and is 23.45m thick.", "triple_list": [ [ "Siltstone", "Paleontological", "Plant fossil fragments" ], [ "Siltstone", "thickness", "23.45m" ] ] }, { "text": "Dark gray medium-layer micro-fine crystal limestone is mixed with gray medium-thin layer of stucco bioclass limestone, 3.75 meters thick, with large lateral thickness changes, and the stratigraphic surface is curved, making the rock layer look like a tumor.", "triple_list": [ [ "Dark gray medium-layer micro-fine crystal limestone with gray medium-thin layer of stucco bioclass limestone", "thickness", "3.75 meters" ], [ "Dark gray medium-layer micro-fine crystal limestone with gray medium-thin layer of stucco bioclass limestone", "Distribution pattern", "Tumor" ] ] }, { "text": "Light purple-purple-red basalt, with a splotchy structure, 15.21 meters thick.", "triple_list": [ [ "Light purple-red Anite", "Distribution pattern", "Spotted structure" ], [ "Light purple-red Anite", "thickness", "15.21 meters" ] ] }, { "text": "The Dalong Formation Gray-black Medium-layered carbon clay rocks in the Dalong Formation were mixed with gray light gray dolomite-containing clay rocks.", "triple_list": [ [ "Dalong Group", "Lithology", "Gray-black medium-layer carbon clay rock with gray light gray dolomite clay rock" ] ] }, { "text": "Purple-red brown silty limestone is mixed with purple-red gravel-containing silty sandstone, 20.06 meters thick.", "triple_list": [ [ "Purple-red brown silty limestone intersected with purple-red gravel-containing silty sandstone", "thickness", "20.06 meters" ] ] }, { "text": "The purple-red thin layer of microcrystalline dolomite, microcrystalline structure, thin layer structure, knife-cutting pattern Develop, local oblique lamellar structure, crystal hole structure, horizontal lamellar, single layer thickness 1-5cm, and 11.13 meters thick.", "triple_list": [ [ "Purple-red thin layer of microcrystalline dolomite", "Distribution pattern", "Microcrystalline structure" ], [ "Purple-red thin layer of microcrystalline dolomite", "Develop", "Thin layered structure" ], [ "Purple-red thin layer of microcrystalline dolomite", "Develop", "Knife cut pattern" ], [ "Purple-red thin layer of microcrystalline dolomite", "Develop", "Inclined layering structure" ], [ "Purple-red thin layer of microcrystalline dolomite", "Develop", "Crystal cave structure" ], [ "Purple-red thin layer of microcrystalline dolomite", "Develop", "Horizontal stratification" ], [ "Purple-red thin layer of microcrystalline dolomite", "thickness", "11.13 meters" ] ] }, { "text": "The Maoshan Formation has interlaced silt sandstone. The lower lithology of this group is simple, and it is sandy argill quartz silt sandstone and fine-grained quartz sandstone, which constitutes an accretion-type basic stratigraphic sequence, and the lithology changes little laterally. It is a basin with a shed margin.", "triple_list": [ [ "Maoshan Group", "Lithology", "Siltstone" ], [ "Maoshan Group", "Lithology", "Sand-containing mud quartz silt sandstone" ], [ "Maoshan Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Maoshan Group", "Belongs to", "Facilities of basins at the edge of sheds" ], [ "Siltstone", "Develop", "Interleaved hierarchy" ] ] }, { "text": "Light gray thick layered dolomite microcrystalline limestone with parallel stratigraphics, can be seen with suture structure of cave structure, 45.06 meters thick.", "triple_list": [ [ "Light gray thick layered dolomite microcrystalline limestone", "Develop", "Parallel layering" ], [ "Light gray thick layered dolomite microcrystalline limestone", "Develop", "Cave structure" ], [ "Light gray thick layered dolomite microcrystalline limestone", "Develop", "Suture construction" ], [ "Light gray thick layered dolomite microcrystalline limestone", "thickness", "45.06 meters" ] ] }, { "text": "Gray microlayer-thin layered stucco plasterstone, horizontally layered, 1.71 meters thick.", "triple_list": [ [ "Gray microlayer-thin layered stucco", "Develop", "Horizontal stratification" ], [ "Gray microlayer-thin layered stucco", "thickness", "1.71 meters" ] ] }, { "text": "The dark gray medium-thin layered algae-containing sand chips and bioclass limestone with calcified shale, 27.11 meters thick", "triple_list": [ [ "Dark gray medium-thin layered algae-containing sand chips and bioclass limestone with calcified shale", "thickness", "27.11 meters" ] ] }, { "text": "The era of Lingxiang Formation was classified as early Cretaceous.", "triple_list": [ [ "Lingxiang Group", "Age", "Early Cretaceous" ] ] }, { "text": "The thickness of Daye Bing Zouma Mountain is greater than 456m.", "triple_list": [ [ "Daye Bing Zouma Mountain", "thickness", "456m" ] ] }, { "text": "The first section of Dasi Group had no integration contact with the Lingxiang Group.", "triple_list": [ [ "A section of the big temple group", "Unconformity contact", "Lingxiang Group" ] ] }, { "text": "The lower part of the first section of Majiashan Formation is gray-green gray-purple flow-grain breccia cluster rock", "triple_list": [ [ "Majiashan Group", "Lithology", "Gray green gray purple trellis breccia" ] ] }, { "text": "Light purple purple-red briccial-containing rhyolite, 11.82 meters thick.", "triple_list": [ [ "Light purple purple red briccus buckle buckle rock", "thickness", "11.82 meters" ] ] }, { "text": "The Puqi Formation in the underlying formation is yellow-green purple-red calcareous silt sandstone with gray silt microcrystalline limestone.", "triple_list": [ [ "Puqi Group", "Lithology", "Yellow-green purple-red calcium silt sandstone" ], [ "Puqi Group", "Lithology", "Gray silt microcrystalline limestone" ] ] }, { "text": "Yellow-green purple-red thin-medium-thick layered siltstone sandstone intersected with mud siltstone and silt shale, containing fossil fragments of fossils, 39.57m thick.", "triple_list": [ [ "Yellow-green purple-red thin-medium-thick layered silt sandstone with mud silt sandstone and silt shale", "Paleontological", "Fossil fragments of flap" ], [ "Yellow-green purple-red thin-medium-thick layered silt sandstone with mud silt sandstone and silt shale", "thickness", "39.57m" ] ] }, { "text": "Ash-dark gray thin-layer silt sandstone sandstone lenticular fine sandstone gray-black silt shale and coal line, 19.25m thick.", "triple_list": [ [ "Ash-dark gray thin layered silt sandstone sandstone lenticular fine sandstone gray black silt shale and coal line", "thickness", "19.25m" ] ] }, { "text": "Gray-green, gray-purple Anshan volcanic breccia, 10.03 meters thick.", "triple_list": [ [ "Gray green gray purple Andesan volcanic breccia", "thickness", "10.03 meters" ] ] }, { "text": "Gray yellow yellow-green water mica shale, mud structure, 87.05 meters thick.", "triple_list": [ [ "Gray yellow yellow green water mica shale", "Distribution pattern", "Mud structure" ], [ "Gray yellow yellow green water mica shale", "Develop", "Page structure" ], [ "Gray yellow yellow green water mica shale", "thickness", "87.05 meters" ] ] }, { "text": "Maopu Reservoir is 202.48m thick.", "triple_list": [ [ "Maopu Reservoir", "thickness", "202.48m" ] ] }, { "text": "The lower basic strata sequence A, amily shale B, amily limestone.", "triple_list": [ [ "Daye Group One", "Lithology", "Mud shale" ], [ "Daye Group One", "Lithology", "Mixed limestone" ] ] }, { "text": "Gray-yellow mica shale, muddy structure, flake-like structure, lamellar Develop, 15.07 meters thick.", "triple_list": [ [ "Gray yellow water mica shale", "Distribution pattern", "Mud structure" ], [ "Gray yellow water mica shale", "Develop", "Sheet structure" ], [ "Gray yellow water mica shale", "Develop", "Layer" ], [ "Gray yellow water mica shale", "thickness", "15.07 meters" ] ] }, { "text": "The renewal system is widely distributed in the longgang area west of Liangzihu-Jinniu Town in the test area, with an area of 185.725Km2, accounting for 20.84% of the total area of the test area.", "triple_list": [ [ "Update system", "Exposed", "Liangzihu, the test area - the west of Jinniu Town" ], [ "Update system", "area", "185.725Km2" ] ] }, { "text": "The Carbonite system is distributed in the southeast of the measurement area, with an exposed area of about 13.5m2, accounting for 1.51% of the total area of the map. Only the Huanglong Formation of the Dapu Formation of the Shangtong Taipu Formation is missing. It is a set of carbonate rock sedimentation, which is in parallel and unconformal contact with the Devonian Yuntaiguan Formation or the Silurian Maoshan Formation.", "triple_list": [ [ "Carbonite", "Exposed", "South East of the test area" ], [ "Carbonite", "area", "13.5m2" ], [ "Carbonite", "Outcrop", "Tai Po Group" ], [ "Carbonite", "Outcrop", "Huanglong Group" ], [ "Carbonite", "Belongs to", "Carbonate sedimentation" ], [ "Carbonite", "Integration of contacts", "Devonian Yuntai Temple Group" ], [ "Carbonite", "Integration of contacts", "Siluri Maoshan Group" ] ] }, { "text": "Daye Group and Dalong Group were integrated and contacted.", "triple_list": [ [ "Daye Group", "Integration of contacts", "Dalong Group" ] ] }, { "text": "The upper part of the second section of Daye Formation is composed of thin-medium-thick layer of algae agglomerated mortars and medium-thick layered mortars. The horizontal stratigraphy and blocky stratigraphy are developed, and the sutures are relatively developed. The stratigraphy sequence generally thickens upwards, and the particles become coarser, which is a weak accumulation-agglomerated basic stratigraphy sequence, which is a shallow sea shed phase sedimentation.", "triple_list": [ [ "Daye Group Second Section", "Lithology", "Thin-medium-thick layer of algae agglomerated stucco" ], [ "Daye Group Second Section", "Lithology", "Medium-thick layered stucco" ], [ "Daye Group Second Section", "Develop", "Horizontal stratification" ], [ "Daye Group Second Section", "Develop", "Block lamina" ], [ "Daye Group Second Section", "Develop", "Suture" ], [ "Daye Group Second Section", "Belongs to", "Shallow sea sheds sedimentation" ] ] }, { "text": "Dark gray-black almond-shaped basalt, with intergranular structure, 32.62 meters thick.", "triple_list": [ [ "Dark gray-black almond-shaped basil", "Distribution pattern", "Intergranular intergranular structure" ], [ "Dark gray-black almond-shaped basil", "thickness", "32.62 meters" ] ] }, { "text": "The high water level system area is a strip-shaped silty shale and fine sandstone in the upper part of the Xintan Formation. Due to the rapid advance and retreat of seawater, no obvious starvation segment sedimentation was formed.", "triple_list": [ [ "Xintan Group", "Lithology", "Striped silty shale" ], [ "Xintan Group", "Lithology", "Fine sandstone" ] ] }, { "text": "The sorting and roundness of the A-layer gravel are poor, and the block-like layering is developed, and the exposed thickness is irregular.", "triple_list": [ [ "A-layer gravel", "Develop", "Block lamina" ] ] }, { "text": "The eruption of the Majiashan Formation is not integrated on the rock mass of Jurassic Lingxiang.", "triple_list": [ [ "Majiashan Group", "Unconformity contact", "Jurassic Lingxiang Rock Body" ] ] }, { "text": "The Qixia Formation belongs to shallow sea sheds.", "triple_list": [ [ "Qixia Group", "Belongs to", "Shallow sea sheds sedimentation" ] ] }, { "text": "The light gray thick layered microcrystalline limestone is parallel layered, and the cave structure is suture structure, 12.09 meters thick.", "triple_list": [ [ "Light gray thick layered microcrystalline limestone", "Develop", "Parallel layering" ], [ "Light gray thick layered microcrystalline limestone", "Develop", "Cave structure" ], [ "Light gray thick layered microcrystalline limestone", "Develop", "Suture construction" ], [ "Light gray thick layered microcrystalline limestone", "thickness", "12.09 meters" ] ] }, { "text": "Yellow-green, gray-yellow mud-containing quartz silt sandstone, mud-containing silt sand-like structure, horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-shaped horizontal silt-", "triple_list": [ [ "Yellow-green gray-yellow mud-containing sand-containing quartz silt sandstone", "Distribution pattern", "Mud-containing sand-containing silt structure" ], [ "Yellow-green gray-yellow mud-containing sand-containing quartz silt sandstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud-containing sand-containing quartz silt sandstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud-containing sand-containing quartz silt sandstone", "thickness", "22.35 meters" ] ] }, { "text": "Gray-purple Yinganite volcanic breccia, 2.17 meters thick.", "triple_list": [ [ "Gray-purple yinganite volcanic breccia", "thickness", "2.17 meters" ] ] }, { "text": "Off-white medium-thick layered feldspar quartz sandstone, 21.75m thick.", "triple_list": [ [ "Off-white medium-thick layered feldspar quartz sandstone", "thickness", "21.75m" ] ] }, { "text": "The Carbonite Dapu Group parallelly does not integrate the Maoshan Group.", "triple_list": [ [ "Carbonite Dapu Group", "Integration of contacts", "Maoshan Group" ] ] }, { "text": "Gray medium-thick layered dolomite microcrystalline limestone, microcrystalline structure, block-like structure, knife-cutting pattern Develop, and extreme layer Develop.", "triple_list": [ [ "Gray medium-thick layered dolomite microcrystalline limestone", "Distribution pattern", "Microcrystalline structure" ], [ "Gray medium-thick layered dolomite microcrystalline limestone", "Develop", "Blocky structure" ], [ "Gray medium-thick layered dolomite microcrystalline limestone", "Develop", "Knife cut pattern" ], [ "Gray medium-thick layered dolomite microcrystalline limestone", "Develop", "Layer" ] ] }, { "text": "Off-white, gray-red thick layer - blocky sand-containing dolomite with light gray medium-thick layer - blocky dolomite, with parallel layering, 34.89 meters thick.", "triple_list": [ [ "Off-white, gray-red thick layer - blocky sand-containing dolomite with light gray medium-thick layer - blocky dolomite", "Develop", "Parallel layering" ], [ "Off-white, gray-red thick layer - blocky sand-containing dolomite with light gray medium-thick layer - blocky dolomite", "thickness", "34.89 meters" ] ] }, { "text": "Light gray thick layer of dolomel oval limestone, oval structure, block structure, local bird's eye tectonic oblique stratigraphic structure, horizontal stratigraphic, single layer thickness >45cm, and thickness 14.14 meters.", "triple_list": [ [ "Light gray thick layer of dolomite oasis limestone", "Distribution pattern", "Ocillary structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Blocky structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Bird's eye structure" ], [ "Light gray thick layer of dolomite oasis limestone", "Develop", "Horizontal stratification" ], [ "Light gray thick layer of dolomite oasis limestone", "thickness", "14.14 meters" ] ] }, { "text": "Gray-black thin-layer siltstone sandstone intersects purple-red siltstone, 2.92m thick.", "triple_list": [ [ "Gray-black thin-layer siltstone intersected with purple-red siltstone", "thickness", "2.92m" ] ] }, { "text": "The second section of Jialingjiang Formation changes to the dark gray thick oval sand-clad limestone.", "triple_list": [ [ "Section 2 of Jialingjiang Formation", "Lithology", "Purple-gray thick layer of dolomelized particle crystalline limestone" ], [ "Section 2 of Jialingjiang Formation", "Lithology", "Dark gray thick layer of osagrail limestone" ] ] }, { "text": "Layered limestone B thick layered limestone in the basic strata A of the second section of Daye Formation.", "triple_list": [ [ "Daye Group Second Section", "Lithology", "Medium layered limestone" ], [ "Daye Group Second Section", "Lithology", "Thick layered limestone" ] ] }, { "text": "Black carbon shale is mixed with gray-black medium-thin layered biosalis carbon mortars. The biosalis components are calcium, with a huge difference in size, roughly parallel micro-layered surfaces, and there are brachiopod mesophobia chestica. 7.70 meters thick", "triple_list": [ [ "Black carbon shale with gray-black medium-thin layered biosandra carbonaceous mortar", "Paleontological", "Brachiopod" ], [ "Black carbon shale with gray-black medium-thin layered biosandra carbonaceous mortar", "Paleontological", "Aphrodisiac" ], [ "Black carbon shale with gray-black medium-thin layered biosandra carbonaceous mortar", "Paleontological", "Petal gills" ], [ "Black carbon shale with gray-black medium-thin layered biosandra carbonaceous mortar", "thickness", "7.70 meters" ] ] }, { "text": "Interlaced stratigraphic stratigraphic and strata Develop can be seen in sandstone.", "triple_list": [ [ "sandstone", "Develop", "Interleaved hierarchy" ], [ "sandstone", "Develop", "Inclined layering" ], [ "sandstone", "Develop", "Wave mark structure" ] ] }, { "text": "The microcrystalline limestone is sandwiched in the charcoal limestone in the form of a lens, with a thickness of 8.43 meters.", "triple_list": [ [ "Microcrystalline limestone is sandwiched with carbonaceous limestone in a lens-like shape", "thickness", "8.43 meters" ] ] }, { "text": "The neighboring area of Echeng Chengchao Da Wang Chong obtained Permophorus Sp., Entolium Discites, Pteria sp., Mytilus ex.gr. deuliformis, etc.", "triple_list": [ [ "Echeng Chengchao King Chong", "Paleontological", "Permophorus Sp." ], [ "Echeng Chengchao King Chong", "Paleontological", "Entolium discites" ], [ "Echeng Chengchao King Chong", "Paleontological", "Pteria sp." ], [ "Echeng Chengchao King Chong", "Paleontological", "Mytilus ex.gr.deuliformis" ] ] }, { "text": "The basic stratigraphic sequence of Qixia Formation A carbonaceous shale B carbonaceous limestone C amylin limestone.", "triple_list": [ [ "Qixia Group", "Lithology", "Carbon shale" ], [ "Qixia Group", "Lithology", "Carbonite limestone" ], [ "Qixia Group", "Lithology", "Mixed limestone" ] ] }, { "text": "Ash-light gray medium-thick layered feldspar quartz sandstone fine sandstone silt sandstone sandstone intersects gray-black silt shale and coal line, 37.73m thick.", "triple_list": [ [ "Ash-light gray medium-thick layered feldspar quartz sandstone fine sandstone silt sandstone sandstone intersected with gray-black silt shale and coal line", "thickness", "37.73m" ] ] }, { "text": "Gray-yellow Yingan volcanic breccia, 50.95 meters thick.", "triple_list": [ [ "Gray yellow volcanic breccia", "thickness", "50.95 meters" ] ] }, { "text": "Section 2 of the Tomb Tou Formation: Gray yellow yellow-green layered arable quartz silt sandstone intersected with yellow-green shale gray-green silt shale, and thin layer of quartz sandstone appeared in the upper part.", "triple_list": [ [ "Grave Group Second Section", "Lithology", "Gray yellow yellow-green layered mud quartz silt sandstone" ], [ "Grave Group Second Section", "Lithology", "Yellow-green shale" ], [ "Grave Group Second Section", "Lithology", "Gray-green silty shale" ], [ "Grave Group Second Section", "Lithology", "Thin layer of quartz sandstone" ] ] }, { "text": "Light purple yellow-white Ying'an rock and Andesite eruption does not integrate into the second section of Dasi Formation", "triple_list": [ [ "Light purple yellow-white Ying'an rocks and Andesan rocks", "Unconformity contact", "Dasi Group Second Section" ] ] }, { "text": "The thickness of Daye Bing Zouma Mountain is 81m.", "triple_list": [ [ "Daye Bing Zouma Mountain", "thickness", "81m" ] ] }, { "text": "Light purple purple-red Ying'an rock with rhyolite, 4.23 meters thick.", "triple_list": [ [ "Light purple purple-red Ying'an rock with rhyme", "thickness", "4.23 meters" ] ] }, { "text": "The basic layer sequence of the lower third section of Daye Formation consists of A-thick-thick layer of mortars; B-thick-thick layer of fine crystal dolomite.", "triple_list": [ [ "Daye Group Three Section", "Lithology", "Thick - huge thick layer of stucco" ], [ "Daye Group Three Section", "Lithology", "Thick-giant thick layer of fine crystal dolomite" ] ] }, { "text": "Purple-red clay rock, muddy structure, sheet-like structure, horizontal strata Develop, single layer thickness 1-2mm and 6.17 meters thick, integrating Xintan Formation.", "triple_list": [ [ "Purple-red clay rock", "Distribution pattern", "Mud structure" ], [ "Purple-red clay rock", "Develop", "Sheet structure" ], [ "Purple-red clay rock", "Develop", "Horizontal stratification" ], [ "Purple-red clay rock", "thickness", "6.17 meters" ], [ "Purple-red clay rock", "Integration of contacts", "Xintan Group" ] ] }, { "text": "Maoshan Formation is 54.23-214.11 meters thick.", "triple_list": [ [ "Maoshan Group", "thickness", "54.23-214.11 meters" ] ] }, { "text": "The Silurian system is a set of terrestrial debris deposition of shallow-sea-surrounding phases, and the upper and lower Ordovician systems are in integrated contact.", "triple_list": [ [ "Shiliu Department", "Belongs to", "Shallow sea-shore terrestrial debris sedimentation" ], [ "Shiliu Department", "Integration of contacts", "Ordovician" ] ] }, { "text": "The upper system of the carbolithic system is divided into Luosu talc slab stairs Dala stairs Xiaoyao stairs.", "triple_list": [ [ "Carbonite system", "Contained", "Luo Sujie" ], [ "Carbonite system", "Contained", "Talc stairs" ], [ "Carbonite system", "Contained", "Dala Tier" ], [ "Carbonite system", "Contained", "Freedom" ] ] }, { "text": "The Carboniferous System Dapu Formation (C2d) is covered with overlying strata, with gray-white light gray algae powder containing algae sand chips fine crystal dolomite, algae powder containing algae sand chip structure, block structure, knife-cutting pattern Develop, bird's eye tectonic crystal hole structure suture structure can be seen locally, with horizontal strata parallel strata, and a single layer thickness of 50cm. 14.99 meters thick", "triple_list": [ [ "Carbonite Dapu Group", "Lithology", "Off-white light gray algae powder algae sand chips fine crystal dolomite" ], [ "Carbonite Dapu Group", "Distribution pattern", "Algae powder crumbs algae sand crumbs structure" ], [ "Carbonite Dapu Group", "Develop", "Blocky structure" ], [ "Carbonite Dapu Group", "Develop", "Knife cut pattern" ], [ "Carbonite Dapu Group", "Develop", "Bird's eye structure" ], [ "Carbonite Dapu Group", "Develop", "Crystal cave structure" ], [ "Carbonite Dapu Group", "Develop", "Suture construction" ], [ "Carbonite Dapu Group", "Develop", "Horizontal stratification" ], [ "Carbonite Dapu Group", "Develop", "Parallel layering" ], [ "Carbonite Dapu Group", "thickness", "14.99 meters" ] ] }, { "text": "Integration of contacts between Liangshan Formation and Qixia Formation 1. Carbon shale 2. Carbon lemite 3. Carbon tumour limestone", "triple_list": [ [ "Liangshan Group", "Integration of contacts", "Qixia Group" ], [ "Liangshan Group", "Lithology", "Carbon shale" ], [ "Liangshan Group", "Lithology", "Carbonite limestone" ], [ "Liangshan Group", "Lithology", "Carbonomatous limestone" ] ] }, { "text": "Maokou group and the Lower Qixia group were in contact with each other.", "triple_list": [ [ "Maokou Group", "Integration of contacts", "Qixia Group" ] ] }, { "text": "Yellow-green, gray-yellow argic quartz siltstone, a mud-silt structure, horizontal silt-like lamination, parallel silt-Develop, single layer thickness 1-5cm, and thickness 23.22 meters.", "triple_list": [ [ "Yellow-green gray-yellow mud quartz siltstone", "Distribution pattern", "Mud silty sandy structure" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green gray-yellow mud quartz siltstone", "Develop", "23.22 meters" ] ] }, { "text": "The biochips in the Longtan Formation are very different in size, mixed distribution, and the components are calcium. They are of various species, including bryozoos, chesticopods, foraminifera, brachiopods, and brachiopods.", "triple_list": [ [ "Longtan Group", "Paleontological", "Belimidia" ], [ "Longtan Group", "Paleontological", "Petal gills" ], [ "Longtan Group", "Paleontological", "Gastropod" ], [ "Longtan Group", "Paleontological", "Foraminifera" ], [ "Longtan Group", "Paleontological", "Brachiopod" ], [ "Longtan Group", "Paleontological", "Michizao" ] ] }, { "text": "The rock surface has developed cutting patterns, block-like stratigraphy, single layer thickness >45cm, and other structures with exposed characteristics such as crystal cave paste and salt.", "triple_list": [ [ "rock", "Develop", "Knife cut pattern" ], [ "rock", "Develop", "Block lamina" ], [ "rock", "Develop", "Crystal Cave" ], [ "rock", "Develop", "Paste salt" ], [ "rock", "Develop", "False crystal" ] ] }, { "text": "The Huanglong Formation has acquired many fossils of the Flyaceae family in Xifan.", "triple_list": [ [ "Huanglong Group", "Exposed", "Xifan Li" ], [ "Huanglong Group", "Paleontological", "fossils of fernaceae" ] ] }, { "text": "The adjacent Yin Zubing Dishuiyan area is 19-21m thick.", "triple_list": [ [ "Yin Zubing Drops Rock", "thickness", "19-21m" ] ] }, { "text": "Purple-red medium-thin layered iron-containing calcium fine-grained quartz sandstone, 2.16 meters thick", "triple_list": [ [ "Purple-red medium-thin layered iron-containing calcium fine-grained quartz sandstone", "thickness", "2.16 meters" ] ] }, { "text": "The upper basic strata A thick layer of feldspar quartz sandstone B silt shale shale", "triple_list": [ [ "Maoshan Group", "Lithology", "Thick feldspar quartz sandstone" ], [ "Maoshan Group", "Lithology", "Silty shale" ] ] }, { "text": "Biocrack species include acneoplastics and mesophylla.", "triple_list": [ [ "Biochips", "Paleontological", "Acanthus" ], [ "Biochips", "Paleontological", "Aphrodisiac" ] ] }, { "text": "The lower part of the first section of the Tomb Tomb Formation is purple-red, gray-yellow gray-green silty shale containing silty water mica shale intersected with thin layers of fine sandstone argillic quartz silty sandstone, horizontal stratigraphic Develop, single layer thickness 1-6cm.", "triple_list": [ [ "A grave group", "Lithology", "Silty shale" ], [ "A grave group", "Lithology", "silt water mica shale" ], [ "A grave group", "Lithology", "Thin layer of fine sandstone" ], [ "A grave group", "Lithology", "Mixed quartz siltstone" ], [ "A grave group", "Develop", "Horizontal stratification" ], [ "A grave group", "Develop", "Parallel layering" ] ] }, { "text": "Light gray-green-gray-purple Andesan volcanic breccia, volcanic breccia structure, blocky structure.", "triple_list": [ [ "Light gray-green-gray purple Anshan volcanic breccia", "Distribution pattern", "Volcanic Breccia Structure" ], [ "Light gray-green-gray purple Anshan volcanic breccia", "Develop", "Blocky structure" ] ] }, { "text": "Psendosageceras, Nordophiceras and fish fossils were harvested in the third- and fourth sections of the Daye Formation in the adjacent 1:50,000 Tieshanbing.", "triple_list": [ [ "Daye Group Third-4 Sections", "Paleontological", "Psendosageceras" ], [ "Daye Group Third-4 Sections", "Paleontological", "Nordophiceras" ], [ "Daye Group Third-4 Sections", "Paleontological", "Fish fossil" ] ] }, { "text": "Light gray thick layered layered with grey matter medium-fine crystal dolomite, medium-fine crystal structure, block-like structure, sparsely developed knife-cutting patterns, horizontal layered, single layer thickness 30-40cm, and 13.25 meters thick.", "triple_list": [ [ "Light gray thick layered layered grey matter-fine crystal dolomite", "Distribution pattern", "Medium-fine crystal structure" ], [ "Light gray thick layered layered grey matter-fine crystal dolomite", "Develop", "Blocky structure" ], [ "Light gray thick layered layered grey matter-fine crystal dolomite", "Develop", "Knife cut pattern" ], [ "Light gray thick layered layered grey matter-fine crystal dolomite", "Develop", "Horizontal stratification" ], [ "Light gray thick layered layered grey matter-fine crystal dolomite", "thickness", "13.25 meters" ] ] }, { "text": "The basic stratigraphy sequence of the lower part is shown in the figure, where the A layer develops horizontal stratigraphy, the rock layer develops wave mark structure, and the upward thin layer of quartz sandstone clamps have been thinned.", "triple_list": [ [ "Layer A", "Develop", "Horizontal stratification" ], [ "Layer A", "Develop", "Wave mark structure" ], [ "Layer A", "Lithology", "Thin layer of quartz sandstone" ] ] }, { "text": "The upper basic layer sequence of the first section of the Tomb Tou Formation A, amule siltstone B, phosphorus-containing feldspar quartz sandstone", "triple_list": [ [ "A grave group", "Lithology", "Mud siltstone" ], [ "A grave group", "Lithology", "Phosphate-containing quartz sandstone" ] ] }, { "text": "Gray-purple basalt, with a splotchy structure, 38.62 meters thick.", "triple_list": [ [ "Gray purple basalt", "Distribution pattern", "Spotted structure" ], [ "Gray purple basalt", "thickness", "38.62 meters" ] ] }, { "text": "The basic stratigraphic sequence of the third section of the Jialingjiang Formation A. Thin-medium crystalline dolomite B. Grafted gray matter dolomite C. Dissolved breccia", "triple_list": [ [ "Section 3 of Jialingjiang Formation", "Lithology", "Thin-middle crystalline dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Laminated gray matter dolomite" ], [ "Section 3 of Jialingjiang Formation", "Lithology", "Breccia" ] ] }, { "text": "The Gong'anzhai Formation's purple-red gravel-containing sandstone gravel-containing muddy silt sandstone sandstone silt sandstone amid silt sandstone, forming multiple rhythmic layers.", "triple_list": [ [ "Public Security Village Group", "Lithology", "Purple-red gravel sandstone" ], [ "Public Security Village Group", "Lithology", "Gravel-containing mud siltstone" ], [ "Public Security Village Group", "Lithology", "Polygon" ], [ "Public Security Village Group", "Lithology", "Siltstone" ], [ "Public Security Village Group", "Lithology", "Mud siltstone" ] ] }, { "text": "Daye Formation belongs to the platform-the shallow phase deposits on the edge of the platform.", "triple_list": [ [ "Daye Group", "Belongs to", "Platform-Shade phase sedimentation on the edge of the platform" ] ] }, { "text": "The first section of Daye Formation was found in the yellow-green shale in Xifanli area, fossils such as Claraia griesbachi, Cl. Wangi, Opiceras cf. demissum, O.cf.sinense, Lytophiceras cf.sauntala, etc. in yellow-green shale in Xifanli area.", "triple_list": [ [ "Daye Group One", "Exposed", "Xifan Li" ], [ "Daye Group One", "Lithology", "Yellow-green shale" ], [ "Daye Group One", "Paleontological", "Claraia griesbachi" ], [ "Daye Group One", "Paleontological", "Cl.Wangi" ], [ "Daye Group One", "Paleontological", "Opiceras cf. demissum" ], [ "Daye Group One", "Paleontological", "O.cf.sinense" ], [ "Daye Group One", "Paleontological", "Lytophiceras cf.sauntala" ] ] }, { "text": "The basic strata sequence A thin layer quartz sandstone B shale in the middle of the second section of the Tombtou Formation", "triple_list": [ [ "Grave Group Second Section", "Lithology", "Thin layer of quartz sandstone" ], [ "Grave Group Second Section", "Lithology", "shale" ] ] }, { "text": "The upper and lower triassic strata of the northern Wangsheng area was exposed sporadically, with an exposed area of about 34.5m2, accounting for 3.87% of the total area of the map.", "triple_list": [ [ "The area around the king of northern", "Outcrop", "Middle-up Triassic" ], [ "Middle-up Triassic", "area", "34.5m2" ] ] }, { "text": "Off-white brown-yellow feldspar quartz sandstone, 14.37 meters thick.", "triple_list": [ [ "Off-white brown yellow feldspar quartz sandstone", "thickness", "14.37 meters" ] ] }, { "text": "Maoshan Formation (S3m) gray-yellow fine-grained quartz sandstone, fine-grained sand-like structure, block-like structure, parallel layering, single layer thickness 30cm. The iron mineral content is 4%, and the thickness is 45.52 meters.", "triple_list": [ [ "Maoshan Group", "Lithology", "Gray yellow fine-grained quartz sandstone" ], [ "Maoshan Group", "Distribution pattern", "Fine-grained sandy structure" ], [ "Maoshan Group", "Develop", "Blocky structure" ], [ "Maoshan Group", "Develop", "Parallel layering" ], [ "Maoshan Group", "thickness", "45.52 meters thick" ] ] }, { "text": "Medium gravel layer, 0.5 meters thick.", "triple_list": [ [ "Medium gravel layer", "thickness", "0.5 meters" ] ] }, { "text": "Biodies are mainly petals, containing a small amount of foraminifera and cyanobacteria.", "triple_list": [ [ "Biochips", "Paleontological", "Petal gills" ], [ "Biochips", "Paleontological", "Foraminifera" ], [ "Biochips", "Paleontological", "Aphrodisiac" ], [ "Biochips", "Paleontological", "Cyanobacteria" ] ] }, { "text": "Cai Huasheng's thickness in the southern part of the test area is 105.65m.", "triple_list": [ [ "Cai Huasheng, southern part of the test area", "thickness", "105.65m" ] ] }, { "text": "Dark gray medium-thin layered flint-containing strips (tuberculosis) fine algae traces-microcrystalline limestone, 18.74 meters thick", "triple_list": [ [ "Dark gray medium-thin layered flint-containing strips (tuberculosis) fine algae traces-microcrystalline limestone", "thickness", "18.74 meters" ] ] }, { "text": "The Xintan Formation gray-yellow-yellow-green water mica shale is produced in the interlayer of gray-yellow-green silty water mica shale and iron-containing arable quartz siltstone, and the local gray-yellow silty clay rock.", "triple_list": [ [ "Xintan Group", "Lithology", "Gray yellow-yellow-green water mica shale" ], [ "Xintan Group", "Lithology", "Gray yellow gray-green silty mica shale" ], [ "Xintan Group", "Lithology", "Iron-containing mud quartz silt" ], [ "Xintan Group", "Lithology", "Gray yellow silty clay rock" ] ] }, { "text": "The Longtan Formation and the Low Fu Maokou Formation are in parallel and unconformed contact, and the emergence of gray-black carbon shale is used as the boundary mark.", "triple_list": [ [ "Longtan Group", "Unconformity contact", "Maokou Group" ], [ "Longtan Group", "Lithology", "Gray-black charcoal" ] ] }, { "text": "The Maoshan Formation is gray-green medium-thick layered fine-grained rock-cut quartz sandstone with yellow-green medium-thin layered arable quartz siltstone, and the upper part is purple-red medium-thin layered fine-grained feldspar quartz sandstone with silt shale. The feldspar quartz sandstone with gray-yellow sandy strips are intermittently distributed.", "triple_list": [ [ "Maoshan Group", "Exposed", "Hairy shop" ], [ "Maoshan Group", "Lithology", "Gray green medium-thick layered fine-grained quartz sandstone" ], [ "Maoshan Group", "Lithology", "Yellow-green medium-thin layered arable quartz siltstone" ], [ "Maoshan Group", "Lithology", "Purple-red medium-thin layer of fine-grained feldspar quartz sandstone" ], [ "Maoshan Group", "Lithology", "Silty shale" ], [ "Maoshan Group", "Lithology", "Feldspar quartz sandstone" ], [ "Maoshan Group", "Contained", "Gray yellow sandy strips" ] ] }, { "text": "Daye Bing Zoumashan is composed of a basic layer sequence of accumulation-degradation-degradation type composed of shale silty shale and a small amount of silty sandstone.", "triple_list": [ [ "Daye Bing Zouma Mountain", "Lithology", "shale" ], [ "Daye Bing Zouma Mountain", "Lithology", "Silty shale" ], [ "Daye Bing Zouma Mountain", "Lithology", "Siltstone" ] ] }, { "text": "Xifan Lihou 135m.", "triple_list": [ [ "Xifan Li", "thickness", "135m" ] ] }, { "text": "The fourth section of Daye Formation, the middle-upper basic strata A thick layer ooclase limestone B stratum dolomite C thick layer dolomite", "triple_list": [ [ "Daye Group Four Section", "Lithology", "Thick layer of oasis limestone" ], [ "Daye Group Four Section", "Lithology", "Dolomite" ], [ "Daye Group Four Section", "Lithology", "Thick layer of dolomite" ] ] }, { "text": "Overly covered strata Dapu Formation, grayish-white bulk microcrystalline dolomite.", "triple_list": [ [ "Dapu Group", "Lithology", "Off-white blocky microcrystalline dolomite" ] ] }, { "text": "The A layer becomes thinner in the upper single layer, and the content of biodebris decreases from bottom to top. The biodebris is brachiopod anthracene and flap gills, etc.", "triple_list": [ [ "Layer A", "Paleontological", "Brachiopod" ], [ "Layer A", "Paleontological", "Acanthus" ], [ "Layer A", "Paleontological", "Petal gills" ] ] }, { "text": "The Dapu Formation captured fossils in Li Cai in Xifan Li. Climacammina sp., Pseudoglandulina sp.", "triple_list": [ [ "Tai Po Group", "Exposed", "Xifan Li" ], [ "Tai Po Group", "Paleontological", "Climacammina sp." ], [ "Tai Po Group", "Paleontological", "Pseudoglandulina sp." ] ] }, { "text": "The biocracking component is calcium, and its species are mainly echinoderm (sea lily stem) and mesophylla, and secondly are algae traces, containing a small amount of brachiopods and foraminiferous fragments.", "triple_list": [ [ "Biochips", "Paleontological", "Acanthus" ], [ "Biochips", "Paleontological", "Sea lily stem" ], [ "Biochips", "Paleontological", "Aphrodisiac" ], [ "Biochips", "Paleontological", "Algae traces" ], [ "Biochips", "Paleontological", "Brachiopod" ], [ "Biochips", "Paleontological", "Foraminiferous fragments" ] ] }, { "text": "The basic sequence of the lower Qixia Formation is composed of A gray-black medium-thick layer of tumor-containing carbonaceous bioclass limestone; B carbonaceous shale.", "triple_list": [ [ "Qixia Group", "Lithology", "Gray-black medium-thick layer of tumor-containing carbonaceous bioclass limestone" ], [ "Qixia Group", "Lithology", "Carbonaceous shale" ] ] }, { "text": "Light gray thick layer of blocky algae traces are fine-microcrystalline dolomite containing Climacammina sp., Pseudoglandulina sp.", "triple_list": [ [ "Light gray thick layer of blocky algae traces - microcrystalline dolomite", "Paleontological", "Climacammina sp." ], [ "Light gray thick layer of blocky algae traces - microcrystalline dolomite", "Paleontological", "Pseudoglandulina sp." ] ] }, { "text": "Gray-green marlstone with calcified shale, 9.97 meters thick, containing Cladophlebis heterophylla (Fontaine) (a heterophylla vein fern), Gleichenites lingxianggensis (SP.nov) (a new species of Silibai in Lingxiang), Gleichenites SP. (SP.nov) (a new species of Libai in Libai).", "triple_list": [ [ "Gray-green marl stone with calcified shale", "thickness", "9.97 meters" ], [ "Gray-green marl stone with calcified shale", "Paleontological", "Cladophlebis heterophylla (Fontaine)" ], [ "Gray-green marl stone with calcified shale", "Paleontological", "Gleichenites lingxianggensis (SP.nov) (Lingxiang Sili Bai New Seed)" ], [ "Gray-green marl stone with calcified shale", "Paleontological", "Gleichenites SP. (SP.nov) (Libai not determined species)" ] ] }, { "text": "The thickness of Xintan Group is 105.65-232 meters.", "triple_list": [ [ "Xintan Group", "thickness", "105.65-232 meters" ] ] }, { "text": "The rocks of Xintan Formation generally Contained thin layers of fine sandstone or sandy strips, with a thickness of 0.5-1cm. The spacing is generally 5-15cm, relatively sparse, no bottoming, and the thickness is greater than 654.71 meters.", "triple_list": [ [ "Xintan Group", "Lithology", "Thin layer of fine sandstone" ], [ "Xintan Group", "Contained", "Sand strips" ], [ "Xintan Group", "thickness", "654.71 meters" ], [ "Sand strips", "thickness", "0.5-1cm" ] ] }, { "text": "Xifan Lihou is 24.12 meters.", "triple_list": [ [ "Xifan Li", "thickness", "24.12 meters" ] ] }, { "text": "The basic stratigraphy sequence of the Yuntaiguan Formation is composed of medium-layer dolomite sandy conglomerate thick-layered iron-containing calcium fine-grained quartz sandstone. It has finer upward particle size, thinner single-layer thickness, and has degenerate structural characteristics.", "triple_list": [ [ "Yuntai View Group", "Lithology", "Medium-layer dolomite sandy gravel" ], [ "Yuntai View Group", "Lithology", "Thick layered iron-containing calcium fine-grained quartz sandstone" ], [ "Yuntai View Group", "Lithology", "Medium-thin layered iron-containing calcium fine-grained quartz sandstone" ] ] }, { "text": "The Maoshan Formation develops horizontal strata and parallel strata and strata, and locally visible interlaced strata structure, indicating that the direction of the ancient water flow is a rhythmic strata pair with changes in thickness and thickness from south to north, and locally visible.", "triple_list": [ [ "Maoshan Group", "Develop", "Horizontal stratification" ], [ "Maoshan Group", "Develop", "Parallel layering" ], [ "Maoshan Group", "Develop", "Layer" ], [ "Maoshan Group", "Develop", "Interleaved hierarchy" ], [ "Maoshan Group", "Develop", "Inclined layering structure" ] ] }, { "text": "Andesan rock is 148.24 meters thick.", "triple_list": [ [ "Andanyan", "thickness", "148.24 meters" ] ] }, { "text": "The third section of Daye Formation is integrated and in contact with the second section of Daye Formation, and the emergence of thin strip-shaped mortars or the disappearance of medium-thick layered mortars are used as the boundary mark.", "triple_list": [ [ "Daye Group Three Section", "Integration of contacts", "Daye Group Second Section" ], [ "Daye Group Three Section", "Lithology", "Thin layers of striped stucco" ], [ "Daye Group Three Section", "Lithology", "Medium-thick layered mortar" ] ] }, { "text": "1:200,000 Wuhan area designated Majiashan Group as the late Middle Jurassic period.", "triple_list": [ [ "Majiashan Group", "Belongs to", "Late Middle Jurassic" ] ] }, { "text": "The lower part of the main lithologic part of the fourth section of Daye Formation is light gray blocky dolomite-containing micro-fine crystalline limestone in the middle, the light gray thick layered micro-ceramic limestone in the upper part, the light gray blocky sand-ceramic limestone in the upper part, and the light gray blocky oagra limestone in the top. Common dissolving tectonic suture structures, oblique lamellar structures can be seen locally, and bird's eye tectonic crystal hole structures are developed at the top.", "triple_list": [ [ "Daye Group Four Section", "Lithology", "Light gray blocky dolomite-fine crystalline limestone" ], [ "Daye Group Four Section", "Lithology", "Light gray thick layered microcrystalline limestone" ], [ "Daye Group Four Section", "Lithology", "Light gray blocky sand chips-fine crystal limestone" ], [ "Daye Group Four Section", "Lithology", "Light gray blocky oasis limestone" ], [ "Daye Group Four Section", "Develop", "Dissolution structure" ], [ "Daye Group Four Section", "Develop", "Suture construction" ], [ "Daye Group Four Section", "Develop", "Inclined layering structure" ], [ "Daye Group Four Section", "Develop", "Bird's eye structure" ], [ "Daye Group Four Section", "Develop", "Crystal cave structure" ] ] }, { "text": "Andesan rock is 125.49 meters thick.", "triple_list": [ [ "Andanyan", "thickness", "125.49 meters" ] ] }, { "text": "The Dapu Formation is 26.59-52.74 meters thick, and is deposited in shallow sea plaids, and has parallel and unconformal contact with the underlying Yuntaiguan Formation.", "triple_list": [ [ "Tai Po Group", "thickness", "26.59-52.74 meters" ], [ "Tai Po Group", "Belongs to", "Shallow sea terrace phase sedimentation" ], [ "Tai Po Group", "Integration of contacts", "Yuntai View Group" ] ] }, { "text": "The third basic strata sequence of Daye Formation A thin layer limestone B middle layer limestone.", "triple_list": [ [ "Daye Group Three Section", "Lithology", "Thin layered limestone" ], [ "Daye Group Three Section", "Lithology", "Medium layered limestone" ] ] }, { "text": "The upper basic stratigraphic sequence A limestone B argate limestone", "triple_list": [ [ "Qixia Group", "Lithology", "Limestone" ], [ "Qixia Group", "Lithology", "Mixed limestone" ] ] }, { "text": "The Yuntaiguan Formation is a coastal phase deposition.", "triple_list": [ [ "Yuntai View Group", "Belongs to", "Maritime sedimentation" ] ] }, { "text": "Gray dark grey thick layered frack-containing chondrite-containing cleavage bioclass limestone, 42.16 meters thick, Hefengnautilus sp., Neochonetes nantanensis (Grabau), Martinia sp., Verbeeina grabaui hompson et Foster, Cribrogenerina sp., Schwagerina cf. pactiruga Chen, S.cf. subobobsoletus var. ouboensis (Ozawa), Multidiscus cf. viriosa Wang, Eogoniolina sp., Hinganotrypa sichuanensis (Yang et Hsia).", "triple_list": [ [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "thickness", "42.16 meters" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Hefengnautilus sp." ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Neochonetes nantanensis (Grabau)" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Martinia sp." ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Verbeeina grabaui hompson et Foster" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Cribrogenena sp." ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Schwagerina cf. pactiruga Chen" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "S.cf. subobsoletus var. ouboensis (Ozawa)" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Multidiscus cf.viriosa Wang" ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Eogoniolina sp." ], [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "Paleontological", "Hinganotrypa sichuanensis (Yang et Hsia)" ] ] }, { "text": "The basic stratigraphic sequence of the Huanglong Formation consists of A carbonaceous shale and B carbonaceous limestone, with a degenerate basic stratigraphic sequence, forming a stratigraphic sequence of the maritime invasion system.", "triple_list": [ [ "Huanglong Group", "Lithology", "Carbon shale" ], [ "Huanglong Group", "Lithology", "Carbonite limestone" ] ] }, { "text": "Light yellow-gray-yellow basalt, glass-based interwoven structure, almond structure, 20.29 meters thick.", "triple_list": [ [ "Light yellow-gray yellow basalt", "Distribution pattern", "Glass interwoven structure" ], [ "Light yellow-gray yellow basalt", "Develop", "Almond structure" ], [ "Light yellow-gray yellow basalt", "thickness", "20.29 meters" ] ] }, { "text": "Light gray medium-thin layered microcrystalline limestone, horizontal stratigraphic, locally visible suture structure, 9.28 meters thick.", "triple_list": [ [ "Light gray medium-thin layered microcrystalline limestone", "Develop", "Horizontal stratification" ], [ "Light gray medium-thin layered microcrystalline limestone", "Develop", "Suture construction" ], [ "Light gray medium-thin layered microcrystalline limestone", "thickness", "9.28 meters" ] ] }, { "text": "Gray thin-layered fine-microcrystalline limestone, horizontally layered, locally visible suture structure, 59.58 meters thick.", "triple_list": [ [ "Gray thin layered fine-microcrystalline limestone", "Develop", "Horizontal stratification" ], [ "Gray thin layered fine-microcrystalline limestone", "Develop", "Suture construction" ], [ "Gray thin layered fine-microcrystalline limestone", "thickness", "59.58 meters" ] ] }, { "text": "Meat-red grey ball granular rhyolite, 53.81 meters thick.", "triple_list": [ [ "Meat red grey ball granular rhizome", "thickness", "53.81 meters" ] ] }, { "text": "Light purple grayish white rhyolite, with a speckled structure and a flowing structure, 156.62 meters thick.", "triple_list": [ [ "Light purple off-white rhizome", "Distribution pattern", "Spotted structure" ], [ "Light purple off-white rhizome", "Develop", "Flow-like structure" ], [ "Light purple off-white rhizome", "thickness", "156.62 meters" ] ] }, { "text": "The Puqi Formation was exposed near Wangsheng, the northeast corner of the test area. The lithology was purple-red muddy silty silty mudstone and yellow-green calcified silty silty sandstone containing iron nodules silty mudstone. It has interlaced slaking and corrugated structures, produced flap gills and plant fossil fragments, and was deposited in inland lake facies.", "triple_list": [ [ "Puqi Group", "Lithology", "Purple-red mud siltstone" ], [ "Puqi Group", "Lithology", "Silty mudstone" ], [ "Puqi Group", "Lithology", "Yellow-green calcium-containing siltstone" ], [ "Puqi Group", "Lithology", "Iron-containing nodule silt mudstone" ], [ "Puqi Group", "Develop", "Interleaved hierarchy" ], [ "Puqi Group", "Develop", "Wave mark structure" ], [ "Puqi Group", "Develop", "Valve gills" ], [ "Puqi Group", "Develop", "Plant fossil fragments" ], [ "Puqi Group", "Belongs to", "Inland lake sedimentation" ] ] }, { "text": "The top is dark green mica clay shale, 1.2m thick, containing utueIIa SP (Tushi clam).", "triple_list": [ [ "Dark green water mica clay shale", "thickness", "1.2m" ], [ "Dark green water mica clay shale", "Paleontological", "utueIIa SP (Tushi clam)" ] ] }, { "text": "The Dalong Formation gray-black thin-layer carbon-containing silica rock siliceous rock siliceous shale carbon-like shale mixed with carbon-like clay rock, produces biological fossils such as amaryllite petals and brachiopods, with a thickness of 3-15m.", "triple_list": [ [ "Dalong Group", "Lithology", "Grey-black thin layered carbon-containing silica rock" ], [ "Dalong Group", "Lithology", "Silicone shale" ], [ "Dalong Group", "Lithology", "Carbon shale" ], [ "Dalong Group", "Lithology", "Carbon clay rock" ], [ "Dalong Group", "Paleontological", "Ammonites" ], [ "Dalong Group", "Paleontological", "Valve gills" ], [ "Dalong Group", "Paleontological", "Brachiopod" ], [ "Dalong Group", "thickness", "3-15m" ] ] }, { "text": "The third section of Daye Formation is 156.09-251 meters thick.", "triple_list": [ [ "Daye Group Three Section", "thickness", "156.09-251 meters" ] ] }, { "text": "Silty shale contains Pseuqocrdinia sp (fake hinged clam), with a thickness of 25.51m.", "triple_list": [ [ "Silty shale", "Paleontological", "Pseuqocrdinia sp (fake hinged clam)" ], [ "Silty shale", "thickness", "25.51m" ] ] }, { "text": "The dark gray medium-thick layer of Xiayao Formation contains flint-tuberculosis bioclass limestone, and the upper part is sometimes sandwiched with carbon-containing stucco bioclass limestone.", "triple_list": [ [ "Xia Kiln Group", "Lithology", "Dark gray medium-thick layer of chert-tuberculosis limestone" ], [ "Xia Kiln Group", "Lithology", "Carbon-containing stucco bioclass limestone" ] ] }, { "text": "The dark gray medium-thin layered bioclastic stuccostone and black carbonaceous shale are interlayered in the Liangshan Formation.", "triple_list": [ [ "Liangshan Group", "Lithology", "Dark gray medium-thin layered bioclast-containing stuccos" ], [ "Liangshan Group", "Lithology", "Black charcoal shale" ] ] }, { "text": "The basic sequence of the lower part of the fourth section of Daye Formation, gray-white, gray-red thick layer-blocked sand-clathrate dolomite with light gray medium-thick layer-blocked dolomite; local thick layered dolomite breccia, etc.", "triple_list": [ [ "Daye Group Four Section", "Lithology", "Grey white gray-red thick layer - blocky sand-filled dolomite" ], [ "Daye Group Four Section", "Lithology", "Light gray medium-thick layer-block dolomite" ], [ "Daye Group Four Section", "Lithology", "Thick layered dolomite" ], [ "Daye Group Four Section", "Lithology", "Breccia" ] ] }, { "text": "The basic stratigraphic sequence of the Jialingjiang Formation consists of A thick layer of dolomelized particle microcrystalline limestone and B thick layer of oad sand-clad limestone, with high biological debris content, indicating a high-energy turbulent environment with strong hydrodynamic conditions (shallow facies environment on the edge of the platform).", "triple_list": [ [ "Jialingjiang Group", "Lithology", "Thick layer of dolomelized particle crystallite limestone" ], [ "Jialingjiang Group", "Lithology", "Thick layer of oaxanthin limestone" ], [ "Jialingjiang Group", "Belongs to", "Shoals on the edge of the platform" ] ] }, { "text": "The coal line contains Podozamites Iance olatusf Iatier Sze (broad type of hemlock).", "triple_list": [ [ "Coal line", "Paleontological", "Podozamites Iance olatusf Iatier Sze (Batch needle cycad wide-shaped)" ] ] }, { "text": "The Huanglong Formation is in integrated contact with the Lower Dapu Formation, and the emergence of thick-layered bioclass limestone or mortarstone is used as the boundary mark.", "triple_list": [ [ "Huanglong Group", "Integration of contacts", "Tai Po Group" ], [ "Huanglong Group", "Lithology", "Thick layered bioclast limestone" ], [ "Huanglong Group", "Lithology", "Stucco" ] ] }, { "text": "The Maoshan Formation's purple-red medium-thin layer of fine-grained feldspar quartz sandstone is interspersed with purple-red silty shale, with a thickness of 47.03 meters.", "triple_list": [ [ "The purple-red medium-thin layer of fine-grained feldspar quartz sandstone intersected with purple-red silty shale in Maoshan Formation", "thickness", "47.03 meters" ] ] }, { "text": "Yellow-green, gray-yellow iron-containing muddy quartz siltstone, with muddy silt structure, horizontal silt Develop in parallel, single layer thickness 2-12cm and 0.60 meters thick.", "triple_list": [ [ "Yellow-green, gray-yellow iron-containing mud-containing quartz siltstone", "Distribution pattern", "Mud-containing silty sandy structure" ], [ "Yellow-green, gray-yellow iron-containing mud-containing quartz siltstone", "Develop", "Horizontal stratification" ], [ "Yellow-green, gray-yellow iron-containing mud-containing quartz siltstone", "Develop", "Parallel layering" ], [ "Yellow-green, gray-yellow iron-containing mud-containing quartz siltstone", "thickness", "0.60 meters" ] ] }, { "text": "Light gray thick layer of blocky stratum layered fine-microcrystal dolomite, fine-microcrystal structure, blocky structure, knife-cutting pattern Develop, locally visible crystal hole structure suture structure, horizontal stratigraphic structure.", "triple_list": [ [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Distribution pattern", "Fine-microcrystal structure" ], [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Develop", "Blocky structure" ], [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Develop", "Knife cut pattern" ], [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Develop", "Crystal cave structure" ], [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Develop", "Suture construction" ], [ "Light gray thick layer of blocky striatum-microcrystalline dolomite", "Develop", "Horizontal stratification" ] ] }, { "text": "The Dalong Formation is generally sedimented in semi-deep sea basin-shallow sea shedding.", "triple_list": [ [ "Dalong Group", "Belongs to", "Semi-deep sea basin-shallow sea shed sedimentation" ] ] }, { "text": "Due to the unconformity area of the Maoshan Group and the Devonian Yuntaiguan Group, compared with the neighboring areas, the era is tentatively determined to be the late Shiliushi.", "triple_list": [ [ "Maoshan Group", "Unconformity contact", "Devon-type gimbal group" ], [ "Maoshan Group", "Age", "Evening Silent" ] ] }, { "text": "The lower part of Qixia Formation is gray-dark gray medium-thick layered bioclimb limestone medium-thick layered bioclimb limestone with gray-black medium-thin layered carbon shale", "triple_list": [ [ "Qixia Group", "Lithology", "Gray dark gray medium-thick layered tumor-like bioclast limestone" ], [ "Qixia Group", "Lithology", "Medium-thick layered bioclast limestone" ], [ "Qixia Group", "Lithology", "Gray-black medium-thin layered carbon shale" ] ] }, { "text": "Dark gray thick layer-blocked flax-containing limestone clumps containing stucco bioclass limestone, 84.76 meters thick.", "triple_list": [ [ "Dark gray thick layer-blocked flax-containing limestone clumps containing stucco bioclastic limestone", "thickness", "84.76 meters" ] ] }, { "text": "The dark gray medium-thin layered bioclastic stuccostone and black carbonaceous shale are interlayered in the Liangshan Formation. The biocracks have different morphology, calcium, and the species include foraminifera, flap, mesophobia.", "triple_list": [ [ "The dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale in Liangshan Formation", "Paleontological", "Foraminifera" ], [ "The dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale in Liangshan Formation", "Paleontological", "Petal gills" ], [ "The dark gray medium-thin layered bioclast-containing stuccosmic stuccostone and black carbonaceous shale in Liangshan Formation", "Paleontological", "Aphrodisiac" ] ] }, { "text": "Dark gray-black basalt, with a speckled structure, 21.47 meters thick.", "triple_list": [ [ "Dark gray black basalt", "Distribution pattern", "Spotted structure" ], [ "Dark gray black basalt", "thickness", "21.47 meters" ] ] }, { "text": "No fossils were found in this area. The eastern small crown worm Kaili worm Xie's striped stone Engulfed (similar species) was found in the upper part of the Tomb Tomb Group near Tongshan Bing. The above fossils are all common molecules in the Middle Silurian world.", "triple_list": [ [ "Grave group", "Paleontological", "Oriental Little Crown Worm" ], [ "Grave group", "Paleontological", "Kailibu" ], [ "Grave group", "Paleontological", "Xie's striped stone Engulfed" ], [ "Grave group", "Age", "Zhongshiliushi" ] ] }, { "text": "A thin layer of fine sandstone is interspersed in the rock, 1-3cm thick.", "triple_list": [ [ "rock", "Contained", "Thin layer of fine sandstone" ], [ "Thin layer of fine sandstone", "thickness", "1-3cm" ] ] }, { "text": "The new system is mainly distributed in the Liangzihu-Jinniu Town area in the western part of the test area, as well as the gully area in the hilly ridge terrain, with an area of 307.53Km2, accounting for 34.5% of the total area of the test area.", "triple_list": [ [ "Brand new system", "Exposed", "Liangzi Lake in the western part of the test area - Jinniu Town" ], [ "Brand new system", "area", "307.53Km2" ] ] }, { "text": "Dark gray-yellow stomatal andesite, with a splotchy structure, 45.83 meters thick.", "triple_list": [ [ "Dark gray-yellow stomatal Andesite", "Distribution pattern", "Spotted structure" ], [ "Dark gray-yellow stomatal Andesite", "thickness", "45.83 meters" ] ] }, { "text": "Basic Sequence of Xintan Formation A Silty Shale B Fine Sandstone", "triple_list": [ [ "Xintan Group", "Lithology", "Silty shale" ], [ "Xintan Group", "Lithology", "Fine sandstone" ] ] }, { "text": "Andesite eruption does not integrate the underlying strata Lingxiang Formation", "triple_list": [ [ "Andanyan", "Unconformity contact", "Lingxiang Group" ] ] }, { "text": "Gray yellow yellow-green containing silty mica shale, containing silty mud structure, 38.38 meters thick.", "triple_list": [ [ "Gray yellow yellow green silty mica shale", "Distribution pattern", "Silty-containing mud structure" ], [ "Gray yellow yellow green silty mica shale", "Develop", "Page structure" ], [ "Gray yellow yellow green silty mica shale", "thickness", "38.38 meters" ] ] }, { "text": "Purple-red light flesh-red medium-layered dolomite sandy conglomerate, 0.29 meters thick", "triple_list": [ [ "purple-red light flesh-red medium-layered dolomite sandy gravel", "thickness", "0.29 meters" ] ] }, { "text": "Off-white rhyolite 4.5m", "triple_list": [ [ "Off-white rhizome", "thickness", "4.5m" ] ] }, { "text": "Tested profile of the Manktou Ebo Formation (J3m) of Tgeyinhanwula upper Jurassics, Zalut Banner, Inner Mongolia Autonomous Region (P-8)", "triple_list": [ [ "Tegeyinhanwula, Zarut Banner, Inner Mongolia Autonomous Region", "Contained", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "Gray-green flow-grained crystalline tuff 22.7m", "triple_list": [ [ "Gray-green flow-grained crystalline tuff", "thickness", "22.7m" ] ] }, { "text": "The work area is located in the central and southern section of Daxinganling and its northwest slope near the main peak. It belongs to Zhongshan District. The Elevation of the mountain is above 1,000m.", "triple_list": [ [ "Workspace", "Located at", "Central and southern section of Daxinganling" ], [ "Workspace", "Located at", "Northwest slope of the main peak" ], [ "Workspace", "Belongs to", "Zhongshan District" ], [ "Workspace", "Elevation", "1000m" ] ] }, { "text": "The fourth system of the new system slope flood accumulation material (Qhspl): mainly distributed in smaller valleys, with an area of about 50m2 and a thickness of more than 10m. Its lithology is gray-yellow gray-brown clay soil, and variegated gray-yellow sand gravel sand and gravel layer.", "triple_list": [ [ "The fourth system of the new system of the slope flood accumulation", "area", "50m2" ], [ "The fourth system of the new system of the slope flood accumulation", "thickness", "10m" ], [ "The fourth system of the new system of the slope flood accumulation", "Lithology", "Gray yellow gray-brown clay soil" ], [ "The fourth system of the new system of the slope flood accumulation", "Lithology", "Variegated gray-yellow gravel sand and gravel layer" ] ] }, { "text": "The measured profile of the Manktou Ebo Group (J3m), Manitu Group (J3mn), Baiyingao Group (J3b) in Ulanhada Shangjurassic Banner, Zarut Banner, Inner Mongolia Autonomous Region (P-2)", "triple_list": [ [ "Ulanhada, Zhalut Banner, Inner Mongolia Autonomous Region", "Contained", "Upper Jurassic Manktou Ebo Group" ], [ "Ulanhada, Zhalut Banner, Inner Mongolia Autonomous Region", "Contained", "Mani Tu Group" ], [ "Ulanhada, Zhalut Banner, Inner Mongolia Autonomous Region", "Contained", "Baiyingao old group" ] ] }, { "text": "Dark gray sericite slate 81.0m", "triple_list": [ [ "Dark gray sericite slate", "thickness", "81.0m" ] ] }, { "text": "Gray-purple rhyolite 7.4m", "triple_list": [ [ "Gray-purple rhizome", "thickness", "7.4m" ] ] }, { "text": "Chaganchulu coarse-grained mica granite (J3β5) is mainly distributed on the north side of Hanshan Luchang in the Hanshan Luchang in the Hanshan Luchang and the south side of Chaganchulu in the Alatandabadao band. It produces lithobe beads, with an exposed area of about 20m2. The rock is grayish-white, gray-yellow and flesh-red, and has a coarse-grained structure. The rock mass invades the Mankitou Ebo Formation of the Upper Jurassic Mankitou Ebo Formation (J3m). It has quartz veins distribution.", "triple_list": [ [ "Chagan Chulu coarse grained mica granite", "Exposed", "The north side of Hanshan Deer Farm in Hanshan Deer Farm" ], [ "Chagan Chulu coarse grained mica granite", "Exposed", "The southern side of Chaganchulu in Altandabadao" ], [ "Chagan Chulu coarse grained mica granite", "Distribution pattern", "Lithic beads" ], [ "Chagan Chulu coarse grained mica granite", "area", "20m2" ], [ "Chagan Chulu coarse grained mica granite", "Develop", "Coarse-grained structure" ] ] }, { "text": "Subvolcanic rocks are mainly gray-yellow rhyolites, exposed in the southern eastern part of the mining area, mostly exposed in the form of veins, and are the main carriers of metal minerals.", "triple_list": [ [ "Sub-volcanic rock", "Lithology", "Gray-yellow rhizome" ], [ "Sub-volcanic rock", "Exposed", "The southeast of the mine" ], [ "Sub-volcanic rock", "Distribution pattern", "Fertilizer form" ] ] }, { "text": "Tested profile of Linxi Formation (P3l) of Chaganhan Motoula Upper Permian in Zhalut Banner, Inner Mongolia Autonomous Region", "triple_list": [ [ "Chaganhan Motewula, Zhalut Banner, Inner Mongolia Autonomous Region", "Contained", "The Linxi Group of the Upper Permian" ] ] }, { "text": "Tenigerzarag anticline, which is located on the south side of the inclination of Hartugle, with a central Coordinates of x:4990.5, y:20734, and the inclined axis is about 5m long. The direction is northeast and eastward. The eastern end converges rapidly. The inclined formation is the Manktou Ebo Formation.", "triple_list": [ [ "Tenigerzarag anticline", "Located at", "Hartugrad's oblique south side" ], [ "Tenigerzarag anticline", "Coordinates", "x:4990.5" ], [ "Tenigerzarag anticline", "Coordinates", "y:20734" ], [ "Tenigerzarag anticline", "length", "5m" ], [ "Tenigerzarag anticline", "Distribution pattern", "North-East and East-East" ], [ "Tenigerzarag anticline", "Belongs to", "Manktou Ebo Group" ] ] }, { "text": "The actual cross-sectional diagram of the old Jurassic white pitch old group in the 299th class of Zarut Banner", "triple_list": [ [ "Zarut Banner 299th Road Class", "Contained", "Old Jurassic White Pitch" ] ] }, { "text": "Overlapping white pitch old group (J3b) off-white flow-like breccia-containing crystal-clad tuff", "triple_list": [ [ "Baiyingao old group", "Lithology", "Off-white breccia" ], [ "Baiyingao old group", "Lithology", "Crystal Crystal Tuff" ] ] }, { "text": "Fossils were found in the Manktou Obo group of the North Salad Brigade, and the fossils were composed of Ferganococha cyrta chern. Lycopoditis sp. Gingotes sp. Baiera grvilis.", "triple_list": [ [ "The North Salad Team's busy and Tuaobao", "Contained", "Manktou Ebo Group" ], [ "Manktou Ebo Group", "Paleontological", "Ferganococha cyrta chern." ], [ "Manktou Ebo Group", "Paleontological", "Lycopoditis sp." ], [ "Manktou Ebo Group", "Paleontological", "Gingotes sp." ], [ "Manktou Ebo Group", "Paleontological", "Baiera grvilis." ] ] }, { "text": "Gray-green silty slate in the Lower Fulinxi Formation (P3l)", "triple_list": [ [ "Linxi Group", "Lithology", "Gray green silty slab" ] ] }, { "text": "Dark gray metamorphic fine sandstone with silty slate 461.5m", "triple_list": [ [ "Dark gray metamorphic fine sandstone with silty slab", "thickness", "461.5m" ] ] }, { "text": "The Yanshan period folds develop in the wide and gentle folds in the upper Jurassic formation, which moves 40° northeast, mainly due to the northwest squeeze of the late Jurassic Pacific plate and the Eurasian plate, forming a series of wide and gentle folds towards the northeast, accompanied by the northwest translational normal fault and the northeast counter fault, and formed the Mesozoic volcanic eruption basin spreading to the northeast.", "triple_list": [ [ "Yanshan period fold", "Belongs to", "Upper Jurassic" ] ] }, { "text": "The geological background is the exposed area of Jurassic Mica granite, which is invasive contact with the volcanic clastic rock formation.", "triple_list": [ [ "Jurassic Mica granite", "Invade", "Pyroclastic rock formations" ] ] }, { "text": "Gray flow-like breccia-containing crystal-clad tuff 42.1m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "42.1m" ] ] }, { "text": "The Linxi Formation strata should be classified as the upper Permian Linxi Formation (P3l), which is a set of clastic rock sedimentary combinations in inland lake sedimentary environments. The colors are mostly gray-black and gray, including slate metamorphic sandstone metamorphic fine sandstone metamorphic siltstone, etc.", "triple_list": [ [ "Linxi Group", "Belongs to", "The Linxi Group of the Upper Permian" ], [ "Linxi Group", "Belongs to", "Clastic rock sedimentation in inland lake sedimentary environment" ], [ "Linxi Group", "Lithology", "Slate" ], [ "Linxi Group", "Lithology", "Metamorphic Sandstone" ], [ "Linxi Group", "Lithology", "Metamorphic fine sandstone" ], [ "Linxi Group", "Lithology", "Metamorphic siltstone" ] ] }, { "text": "The volcanic eruption of the Baiyingao old group does not integrate gray andshan rocks", "triple_list": [ [ "Baiyingao old group", "Unconformity contact", "Gray Andesan rock" ] ] }, { "text": "Dark gray metamorphic fine sandstone 480m", "triple_list": [ [ "Dark gray metamorphic fine sandstone", "thickness", "480m" ] ] }, { "text": "Off-white fluid-like breccia crystal tuff 177.3m", "triple_list": [ [ "Off-white flow-grained breccia crystal tuff", "thickness", "177.3m" ] ] }, { "text": "Gray-yellow flow-grained breccia crystal tuff 35.4m", "triple_list": [ [ "Gray-yellow flow-grained breccia crystal tuff", "thickness", "35.4m" ] ] }, { "text": "Light green and gray andestone 735m", "triple_list": [ [ "Light green and grey andshan rock", "thickness", "735m" ] ] }, { "text": "Gray Fluid Crystal Crush Tuff 25.0m", "triple_list": [ [ "Gray Fluid Crystal Tuff", "thickness", "25.0m" ] ] }, { "text": "Gray flow-like breccia-containing crystal-cles tuff 54.3m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "54.3m" ] ] }, { "text": "The northwest-west fault structure in the measurement area is relatively developed, mainly F1, F2, F3, F5, F8, which are mainly distributed in the Delestai fire prevention station Hanshan Lu Field. The representative of this type of fault is the Uhanda Bayinzarag fault (F2). This type of fault is 320-330°, with an extension length of about 8m and a width of about 10-20m.", "triple_list": [ [ "North-west-failure structure", "Located at", "DelesTaiwan fire prevention station Hanshan Deer Farm" ], [ "North-west-failure structure", "Contained", "Uhanda Bayinzarag fracture" ] ] }, { "text": "Invasive rocks in the mining area are relatively developed, mainly invasive bodies in the late Jurassic period, gray-white fine medium-grained mica granite (J3β1), and gray fine-grained diorite.", "triple_list": [ [ "Invasion of the rock", "Belongs to", "Late Jurassic invasion" ], [ "Invasion of the rock", "Lithology", "Off-white fine medium-grained mica granite" ], [ "Invasion of the rock", "Lithology", "Gray fine grain diorite" ] ] }, { "text": "The vein rocks mostly spread northeast and northwest.", "triple_list": [ [ "Maiyan", "Distribution pattern", "North-East" ], [ "Maiyan", "Distribution pattern", "North-west-facing cloth" ] ] }, { "text": "Gray-gray-green flow-gray breccia-containing crystal chips melted tuff 1.6m", "triple_list": [ [ "Gray-gray-green flow-gray breccia-containing crystal chips melted tuff", "thickness", "1.6m" ] ] }, { "text": "The sediments in the cyclone in the area mainly include the fourth-order flood accumulation deposit and the fourth-order slope flood accumulation deposit, which are mainly caused by the rise of the earth's crust.", "triple_list": [ [ "Sediments", "Contained", "The fourth system flood accumulation" ], [ "Sediments", "Contained", "The fourth system of slope flood accumulation" ] ] }, { "text": "The tuff contains breccia crystal chips with weak melting tuff, weak melting tuff structure, locally resembles the tuff structure, and the rocks are composed of crystal chip slurry chips and plastic transformed glass chips.", "triple_list": [ [ "Fluid tuff containing breccia crystal chips", "Distribution pattern", "Weak fusion tuff structure" ], [ "Fluid tuff containing breccia crystal chips", "Develop", "Flow pattern structure" ], [ "Fluid tuff containing breccia crystal chips", "Contained", "Crystal chips" ], [ "Fluid tuff containing breccia crystal chips", "Contained", "Slurry" ], [ "Fluid tuff containing breccia crystal chips", "Contained", "Plastic glass chips" ], [ "Fluid tuff containing breccia crystal chips", "Contained", "Glass chips" ] ] }, { "text": "Gray flow-like breccia-containing crystal-cles tuff 27.3m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "27.3m" ] ] }, { "text": "The rock combination is green, gray, andshanite, purple, gray, andshanite, and breccia-containing crystal crystal fusion tuff, etc.", "triple_list": [ [ "rock", "Lithology", "Green gray andshan rock" ], [ "rock", "Lithology", "Purple-gray Andesan breccia" ], [ "rock", "Lithology", "Crystal chip melt tuff" ] ] }, { "text": "Off-white rhyolite 1.8m", "triple_list": [ [ "Off-white rhizome", "thickness", "1.8m" ] ] }, { "text": "Subvolcanic rocks have less exposed in the survey area, simple rock types, rhyolites, and mostly exposed near craters or occupy volcanic channels.", "triple_list": [ [ "Subvolcanic rocks", "Lithology", "Rhyolite" ], [ "Subvolcanic rocks", "Exposed", "Near the crater" ], [ "Subvolcanic rocks", "Exposed", "Volcanic passage" ] ] }, { "text": "Andesanite 62.3m", "triple_list": [ [ "Andanyan", "thickness", "62.3m" ] ] }, { "text": "Andesite integration of purple-gray flow-grain crystal chip fusion tuff in the undervolved Manktou Ebo Formation", "triple_list": [ [ "Andanyan", "Integration of contacts", "Manktou Ebo Group" ], [ "Manktou Ebo Group", "Lithology", "Purple-gray flow-grain crystal chip melted tuff" ] ] }, { "text": "The main lithologies of the Manketou Obo Formation (J3m) in the Upper Jurassics are gray-white rhizome containing breccia crystal smelted tuff grey-white rhizome containing breccia crystal smelted tuff and rhyolite.", "triple_list": [ [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Off-white breccia" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Crystal chip melt tuff" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Off-white breccia" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Crystal chip melt tuff" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Rhyolite" ] ] }, { "text": "Gray-purple flow-formed breccia crystal tuff 68.3m", "triple_list": [ [ "Gray-purple flow-formed breccia crystal tuff", "thickness", "68.3m" ] ] }, { "text": "Overlapping Manito Formation (J3mn) dark grey andesite - Integration - Gray fluidic breccia-containing crystal chip melted tuff 328.4m", "triple_list": [ [ "Mani Tu Group", "Lithology", "Dark grey Andesan rock" ], [ "Mani Tu Group", "Integration of contacts", "Gray flow-grained breccia-containing crystal chips melted tuff" ], [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "328.4m" ] ] }, { "text": "The Late Jurassic volcanic activity in the Mesozoic measurement area is very strong, forming a volcanic rock system with a large thickness, with a distribution area of about 1,000m2, accounting for 67% of the total area of the measurement area.", "triple_list": [ [ "Volcanic rock system", "area", "1000m2" ] ] }, { "text": "Gray tuff sand conglomerate 9.9m", "triple_list": [ [ "Gray tuff sandstone", "thickness", "9.9m" ] ] }, { "text": "Gray-gray-green flow-gray breccia-containing crystal chips melted tuff 32.5m", "triple_list": [ [ "Gray-gray-green flow-gray breccia-containing crystal chips melted tuff", "thickness", "32.5m" ] ] }, { "text": "Petological characteristics: rocks have coarse-grained structure and blocky structure. The mineral particle size changes in the rocks are between 1-5mm and greater than 5mm. Potassium feldspar (43) is irregular and has a feldspar composition with a sodium feldspar profile, and the surface is strongly soiled.", "triple_list": [ [ "rock", "Distribution pattern", "Coarse-grained structure" ], [ "rock", "Develop", "Blocky structure" ] ] }, { "text": "The upper Jurassic Manito Formation (J3mn) This strata is mainly distributed in a large area on the west side of the north salad brigade of Ganzhuer Aobao on the north west side of the Luchang Bend in Hanshan. The exposed area is 120m2 and the thickness is >1600m. The rock formation is relatively gentle, generally between 10-25°.", "triple_list": [ [ "Upper Jurassic Mani Tender Group", "Exposed", "The northwest side of Gerchulu, Hanshan Luchang" ], [ "Upper Jurassic Mani Tender Group", "Exposed", "The south east side of Ganzhuer Aobao" ], [ "Upper Jurassic Mani Tender Group", "Exposed", "The west side of the North Salad Brigade" ], [ "Upper Jurassic Mani Tender Group", "area", "120m2" ], [ "Upper Jurassic Mani Tender Group", "thickness", "1600m" ] ] }, { "text": "The quaternary new system flood accumulation deposits (Qhapl) are mainly distributed in the valleys of the Holingaole River, Arhun Delun Gordale Lingaole, with an area of about 150m2 and a thickness greater than 30m. Their lithology is mainly gray-brown clay sand and soil variegated sand and gravel.", "triple_list": [ [ "The fourth-Series New System Flood Accumulation", "Exposed", "Holin Gaole River Alhun Delun Goldale Lin Gaole" ], [ "The fourth-Series New System Flood Accumulation", "area", "150m2" ], [ "The fourth-Series New System Flood Accumulation", "thickness", "30m" ], [ "The fourth-Series New System Flood Accumulation", "Lithology", "Gray-brown clay soil variegated gravel stone" ] ] }, { "text": "The fault zone of the North Salad Brigade is located in the north of the North Salad Brigade, starting from the North Salad Brigade (X5023, Y20734) in the east and ending at the west end of the Daibugayinwula Mountain (X5024, Y20727). It is distributed east-west and east, and is displayed by a jumping abnormal zone with higher intensity. It has good continuity, intensity 400-700n, and negative values appear between (-600--800n).", "triple_list": [ [ "North Salad Brigade Fracture Zone", "Located at", "North salad brigade north" ], [ "North Salad Brigade Fracture Zone", "Located at", "North Salad Team" ], [ "North Salad Brigade Fracture Zone", "Located at", "Daibugayin Wula Mountain" ], [ "North Salad Brigade Fracture Zone", "Distribution pattern", "East-west distribution" ] ] }, { "text": "The volcanic uplift belt of Bayinchulu-Hanshan Forest Farm. The uplift belt is located in the area of Beishala Brigade-Hanshan Forest Farm-Hanshan Luchang, and is spread in the northeast direction. The upper Permian Linxi Formation strata are intermittently exposed on the uplift belt, and there are sporadic Late Jurassic invasion rocks along the belt.", "triple_list": [ [ "Bayinchulu-Hanshan Forest Farm Volcanic Uplift Belt", "Exposed", "North Salad Brigade-Hanshan Forest Farm-Hanshan Deer Farm" ], [ "Bayinchulu-Hanshan Forest Farm Volcanic Uplift Belt", "Distribution pattern", "Northeast direction of the layout" ], [ "Bayinchulu-Hanshan Forest Farm Volcanic Uplift Belt", "Outcrop", "The Linxi Group of the Upper Permian" ], [ "Bayinchulu-Hanshan Forest Farm Volcanic Uplift Belt", "Lithology", "Late Jurassic Invasion Rock" ] ] }, { "text": "Off-white blepharose breccia tuff 35.4m", "triple_list": [ [ "Off-white breccia tuff", "thickness", "35.4m" ] ] }, { "text": "Gray-green Ying'anite containing breccia crystal tuff, with a thickness of 58.4m.", "triple_list": [ [ "Gray-green Ying'an Breccia-containing Crystal Crush tuff", "thickness", "58.4m" ] ] }, { "text": "The work area is a high-Elevation mountainous area and has a subtropical continental climate. It has long winters and short summers, and has severe changes in cold and heat. The temperature difference between day and night is large, and the annual temperature difference is large.", "triple_list": [ [ "Workspace", "Belongs to", "High-Elevation mountainous areas" ], [ "Workspace", "Belongs to", "Subtropical continental climate" ] ] }, { "text": "The invasive rocks in the mining area are not developed, mainly Late Jurassic volcanic rocks (λJ3b), with a light fleshy rhyolite, and are produced in a rock-like shape.", "triple_list": [ [ "Invasion of the rock", "Lithology", "Late Jurassic Volcanic Rock" ], [ "Invasion of the rock", "Lithology", "Light fleshy red rhizome" ], [ "Invasion of the rock", "Distribution pattern", "Rock plant-like output" ] ] }, { "text": "The Mellut group is not integrated on the old white song group (J3b), and is controlled by the P-4 profile in the measurement area.", "triple_list": [ [ "Melletou Group", "Unconformity contact", "Baiyingao old group" ] ] }, { "text": "Gray-purple flow-formed breccia-containing crystal-clad tuff 17.6m", "triple_list": [ [ "Gray-purple flow-formed breccia-containing crystal-clad tuff", "thickness", "17.6m" ] ] }, { "text": "Purple gray black mica andestone 21.6m", "triple_list": [ [ "Purple gray black mica andshan rock", "thickness", "21.6m" ] ] }, { "text": "Micro-grained porphyry potassium granite is mainly exposed south of Tunter Mountain, producing lithobead-like output with an area of about 15m2.", "triple_list": [ [ "Microgranular pimple-like potassium granite", "Exposed", "South of Mount Tuntel" ], [ "Microgranular pimple-like potassium granite", "Distribution pattern", "Lithic beads" ], [ "Microgranular pimple-like potassium granite", "area", "15m2" ] ] }, { "text": "Gray tuff sand conglomerate 23.8m", "triple_list": [ [ "Gray tuff sandstone", "thickness", "23.8m" ] ] }, { "text": "Gray flow-like breccia-containing crystal-cles tuff 19.5m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "19.5m" ] ] }, { "text": "The invasive rocks in the mining area do not develop, mainly Late Jurassic volcanic rocks, with light fleshy red rhyolites, and are produced in rock-like shapes.", "triple_list": [ [ "Invasion of the rock", "Lithology", "Late Jurassic Volcanic Rock" ], [ "Invasion of the rock", "Lithology", "Light fleshy red rhizome" ], [ "Invasion of the rock", "Distribution pattern", "Rock plant-like output" ] ] }, { "text": "The construction angle of the neutral volcanic rock of the Upper Jurassic White Pingo and the Meletu Formation of the Lower Cretaceous in the area is the product of this orogenic movement, forming a northeast-east-oriented magma belt dominated by granite, and producing minerals such as copper, lead, zinc, and silver.", "triple_list": [ [ "Old Jurassic White Pitch", "Unconformity contact", "Neutral volcanic rocks of the Meletu Formation in the Lower Cretaceous" ] ] }, { "text": "Only the lower Cretaceous Meletu Formation (K1ml) green-gray black mica andesite was exposed in the test area.", "triple_list": [ [ "Lower Cretaceous Meletu Formation", "Lithology", "Green gray black mica andesan rock" ] ] }, { "text": "Gray flow-grained crystalline tuff 121.8m", "triple_list": [ [ "Gray Fluid Crystal Tuff", "thickness", "121.8m" ] ] }, { "text": "Gray tuff coarse sandstone 17.8m", "triple_list": [ [ "Gray tuff coarse sandstone", "thickness", "17.8m" ] ] }, { "text": "The upper Jurassic Manketou Ebo Formation (J3m) formation is widely distributed in the measurement area, with a large thickness, and the overall distribution direction is northeastward, with an exposed area of about 700m2, and the rock formation is relatively slow, generally 10-20°. The lithological combination is rheology containing breccia crystalline tuff Fluctuate Breccia crystalline tuff Fluctuate Breccia crystalline tuff Fluctuate Rheolite Rheolite Rheolite containing volcanic breccia.", "triple_list": [ [ "Upper Jurassic Manktou Ebo Group", "Distribution pattern", "North-East" ], [ "Upper Jurassic Manktou Ebo Group", "area", "700m2" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Breccia" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Crystal Crystal Tuff" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Breccia" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Crystal chip melt tuff" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Rhyolite" ], [ "Upper Jurassic Manktou Ebo Group", "Lithology", "Rheagra contains volcanic breccia" ] ] }, { "text": "The granite rock mass invaded the Manktou Obo Formation of the Upper Jurassics, invaded the fine-grained mica dichotomy rock (J3ηβ1) in Sabal Prague, and was invaded by the coarse-grained mica granite (J3β5).", "triple_list": [ [ "granite", "Invade", "Upper Jurassic Manktou Ebo Group" ], [ "granite", "Invade", "Medium-grained black mica diacea rock in Sabal Prague" ], [ "granite", "Lithology", "Chagan Chulu coarse grained mica granite" ] ] }, { "text": "There was no mineralization alteration in the fault zone, and the fault era was inferred as the Late Jurassic-Early Cretaceous.", "triple_list": [ [ "Fracture zone", "Age", "Late Jurassic-Early Cretaceous" ] ] }, { "text": "The actual measurement profile of the upper Jurassic Manktou Ebo Formation (J3m) Manitu Formation (J3mn) on the east side of Hun Obote, Arikundulen Sumu, Zharut Banner", "triple_list": [ [ "East side of Hun Aobaote, Arikundulensumu, Zarut Banner", "Contained", "Upper Jurassic Manktou Ebo Group" ], [ "East side of Hun Aobaote, Arikundulensumu, Zarut Banner", "Contained", "Mani Tu Group" ] ] }, { "text": "Gray fluidic breccia-containing crystal chips melted tuff 51.4m", "triple_list": [ [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "51.4m" ] ] }, { "text": "Gray tuff sand conglomerate 51.1m", "triple_list": [ [ "Gray tuff sandstone", "thickness", "51.1m" ] ] }, { "text": "The stratigraphic angle of the Ebo Formation is not integrated on the upper Permian Linxi Formation (P3l), and is in integrated contact with the upper Jurassic Manitu Formation.", "triple_list": [ [ "Ebo Group", "Unconformity contact", "The Linxi Group of the Upper Permian" ], [ "Ebo Group", "Integration of contacts", "Upper Jurassic Mani Tender Group" ] ] }, { "text": "The strata in the volcanic basin of the Delestai Fire Prevention Station on the north side are relatively fully developed, mainly including the Manitu group of the Manktou Orbo Formation of the Upper Jurassic Manktou Orbo Formation of the White Pingao Group and the Lower Cretaceous Meletu Group, and are relatively well developed.", "triple_list": [ [ "Delestai Fire Protection Station volcanic basin", "Outcrop", "Upper Jurassic Manktou Ebo Group" ], [ "Delestai Fire Protection Station volcanic basin", "Outcrop", "Mani Tu Group" ], [ "Delestai Fire Protection Station volcanic basin", "Outcrop", "Baiyingao old group" ], [ "Delestai Fire Protection Station volcanic basin", "Outcrop", "Lower Cretaceous Meletu Formation" ] ] }, { "text": "The actual measurement profile of the upper Jurassic Manktou Ebo Formation (J3m) Manitu Formation (J3mn) on the east side of Hun Obote, Arikundulen Sumu, Zarut Banner, Inner Mongolia (P-5)", "triple_list": [ [ "East side of Hun Aobaote, Arikundulensumu, Zarut Banner, Mongolia", "Contained", "Upper Jurassic Manktou Ebo Group" ], [ "East side of Hun Aobaote, Arikundulensumu, Zarut Banner, Mongolia", "Contained", "Mani Tu Group" ] ] }, { "text": "Blue-gray black mica andestone>58.6m", "triple_list": [ [ "Blue-gray black mica Andesan rock", "thickness", "58.6m" ] ] }, { "text": "Purple-gray flow-grained breccia crystal tuff 23.4m", "triple_list": [ [ "Purple-gray flow-grained breccia crystal tuff", "thickness", "23.4m" ] ] }, { "text": "Overlaid with Ketou Ebo Formation (J3mn) gray-yellow breccia-containing crystal-clad tuff", "triple_list": [ [ "Manktou Ebo Group", "Lithology", "Gray-yellow flow-like breccia-containing crystal-clad tuff" ] ] }, { "text": "Gray-yellow rhyolite 6.5m", "triple_list": [ [ "Gray-yellow rhizome", "thickness", "6.5m" ] ] }, { "text": "The Sengrendaba Fault Zone (F1) is located in the Hanshanluchang area in the western part of the measurement area, within the Delestai fire prevention station area, and is distributed in the northeast 40° direction.", "triple_list": [ [ "Sengrendaba fault zone", "Located at", "The size of Hanshan deer farm in the western part of the test area" ], [ "Sengrendaba fault zone", "Located at", "DelesTaiwan fire prevention station area" ], [ "Sengrendaba fault zone", "Distribution pattern", "Distribution in the direction of 40° northeast" ] ] }, { "text": "The Manktou Ebo Formation (J3m) of the Tgeyinhanwula upper Jurassic system of Zhalut Banner has scattered strata of pyroclastic sedimentary rocks on the northwestern side.", "triple_list": [ [ "Tgeyinhanwula, Zarut Banner", "Contained", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "Subrhyolite (λJ3b) is mainly distributed in the northern part of Tegyinhanwula Mountain, with sporadic output in the shape of lithobeads, with an area of about 8m2.", "triple_list": [ [ "Secondary rhyolite", "Exposed", "Tegeyinhanwula Mountain North Super Hoertu Mountain North" ], [ "Secondary rhyolite", "Distribution pattern", "Sporadic output of rock beads" ], [ "Secondary rhyolite", "area", "8m2" ] ] }, { "text": "Light yellow green black mica andestone>14.6m", "triple_list": [ [ "Light yellow green black mica Andesan rock", "thickness", "14.6m" ] ] }, { "text": "Dark gray silty slate 15.6m", "triple_list": [ [ "Dark gray silty slab", "thickness", "15.6m" ] ] }, { "text": "Off-white rhyolite 34.4m", "triple_list": [ [ "Off-white rhizome", "thickness", "34.4m" ] ] }, { "text": "Metamorphic siltstone in the Lower Fulinxi Formation (P3l)", "triple_list": [ [ "Linxi Group", "Lithology", "Metamorphic siltstone" ] ] }, { "text": "The new central slope flood (Qhspl) is mainly distributed in the slopes of the valleys in the mining area, and the main lithology is composed of loose gravel soil, sand and soil.", "triple_list": [ [ "Brand new Tongpo Hongji", "Exposed", "The slopes of the valleys in the mine area" ], [ "Brand new Tongpo Hongji", "Lithology", "Gravel soil" ], [ "Brand new Tongpo Hongji", "Lithology", "sand" ] ] }, { "text": "Gray tuff fine sandstone 10.8m", "triple_list": [ [ "Gray tuff fine sandstone", "thickness", "10.8m" ] ] }, { "text": "The medium-fine-grained mica dicyclone (J3ηβ1) in Sabal Prague has a gray-yellow rock with a medium-fine-grained structure. It is distributed in the area of Sabal Prague in the east of Ganzhur Obaubao in the Hanshan Deer Farm. There is a small amount of exposure on the north side of Hundi in the Hanshan Deer Farm Farm, with an exposed area of 7.5m2.", "triple_list": [ [ "Medium-grained black mica diacea rock in Sabal Prague", "Distribution pattern", "Medium fine-grained structure" ], [ "Medium-grained black mica diacea rock in Sabal Prague", "Exposed", "Sabal Prague, Ganjul Obao East Testing in Hanshan Luchang" ], [ "Medium-grained black mica diacea rock in Sabal Prague", "Exposed", "Hanshan Luchang Prague Hundi North Side" ], [ "Medium-grained black mica diacea rock in Sabal Prague", "area", "7.5m2" ] ] }, { "text": "Gray-green flow-grained breccia crystal chip fusion tuff 34.9m", "triple_list": [ [ "Gray-green flow-grained breccia-containing crystal chips melted tuff", "thickness", "34.9m" ] ] }, { "text": "The upper Jurassic White Pitch Old Group (J3b) This strata is mainly distributed in the large area on the west side of the 299 Daoban in the North Sala Brigade, the large area on the north side of the Obau, and the large area on the west side of the Holingaole River. The exposed area is about 110m2 and the thickness is >700m.", "triple_list": [ [ "Old Jurassic White Pitch", "Exposed", "A large area on the west side of the 299th Daoban in the North Salad Brigade" ], [ "Old Jurassic White Pitch", "Exposed", "Large areas on the north side of the Obo in Alprague" ], [ "Old Jurassic White Pitch", "Exposed", "Large area on the west side of the Holingaole River" ], [ "Old Jurassic White Pitch", "area", "110m2" ], [ "Old Jurassic White Pitch", "thickness", "700m" ] ] }, { "text": "Gray fluidic breccia-containing crystal chips melted tuff 233.1m", "triple_list": [ [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "233.1m" ] ] }, { "text": "Zhalut Banner Ulanhada Urarassy Manktou Ebo Group (J3m) Manitu Group (J3mn) Baiyingao Old Group (J3b)", "triple_list": [ [ "Ulanhada, Zarut Banner", "Contained", "Upper Jurassic Manktou Ebo Group" ], [ "Ulanhada, Zarut Banner", "Contained", "Mani Tu Group" ], [ "Ulanhada, Zarut Banner", "Contained", "Baiyingao old group" ] ] }, { "text": "Off-white tuff fine sandstone 13.2m", "triple_list": [ [ "Off-white tuff fine sandstone", "thickness", "13.2m" ] ] }, { "text": "The late Jurassic invasive rocks in the area are not very developed, with an area of 96m2, accounting for 6.5% of the area of the measured area. They are mainly distributed in the area of Hanshan Forest Farm-Banichulu, and are spread to the eastward direction in the north.", "triple_list": [ [ "Late Jurassic Invasion Rock", "area", "96m2," ], [ "Late Jurassic Invasion Rock", "Exposed", "Hanshan Forest Farm-Bayinchulu" ], [ "Late Jurassic Invasion Rock", "Distribution pattern", "North-east-oriented cloth" ] ] }, { "text": "Gray fluidic breccia-containing crystal chips melted tuff 478.9m", "triple_list": [ [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "478.9m" ] ] }, { "text": "Arukorqin Banner Badaiai Ubo Group (J3m) measured profile", "triple_list": [ [ "Badaiailai, Arukorqin Banner", "Contained", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "The Administrative areas of the work area Belongs to to Zhalut Banner, Tongliao City, Inner Mongolia Autonomous Region and Alukorqin Banner, Chifeng City, with geographical coordinates 119°30′00′00′00′00′00′ east longitude; 45°00′00′n north latitude 45°00′00′n-45°20′00′n.", "triple_list": [ [ "Workspace", "Administrative area", "Zhalute Banner, Tongliao City, Inner Mongolia Autonomous Region" ], [ "Workspace", "Administrative area", "Chifeng City Alukorqin Banner" ], [ "Workspace", "Coordinates", "119°30′00″—120°00′00′00″" ], [ "Workspace", "Coordinates", "North latitude 45°00′00″—45°20′00″" ] ] }, { "text": "Gray black mica andestone 43.2m", "triple_list": [ [ "Gray black mica andesan rock", "thickness", "43.2m" ] ] }, { "text": "Tested sectional view of the lower Cretaceous Meletu Formation (K1 ml) in the Meleheitu Mountain, Zharut Banner, Inner Mongolia Autonomous Region (P-4)", "triple_list": [ [ "Meleheitu Mountain, Zhalut Banner, Inner Mongolia Autonomous Region", "Contained", "Lower Cretaceous Meletu Formation" ] ] }, { "text": "The tectonic units of the measurement area are divided into 1. The volcanic uplift belt of Bayingchulu-Hanshan Forest Farm, 2. The Mesozoic volcanic eruption basin of the Delestai Fire Protection Station, and 3. The Mesozoic volcanic eruption basin of the Alatandabadaoban.", "triple_list": [ [ "Test area construction unit", "Contained", "Bayinchulu-Hanshan Forest Farm Volcanic Uplift Belt" ], [ "Test area construction unit", "Contained", "Mesozoic volcanic eruption basin in Delestai Fire Prevention Station" ], [ "Test area construction unit", "Contained", "Alatandabadabadang Mesozoic Volcano Eruption Basin" ] ] }, { "text": "Gray fluidic breccia-containing crystalline tuff 20.2m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "20.2m" ] ] }, { "text": "The polymetallic zone of Badeailai-Hanshan Forest Farm is located in the area of Tegeyinhanwula, spreading in the northeast direction. The exposed strata include the Upper Permian Linxi Formation (P3l) and the Upper Jurassic Manktou Ebo Formation (J3m).", "triple_list": [ [ "Badeailai-Hanshan Forest Farm Multi-Metal Area", "Located at", "Tegeyinhanula" ], [ "Badeailai-Hanshan Forest Farm Multi-Metal Area", "Distribution pattern", "North-east-oriented cloth" ], [ "Badeailai-Hanshan Forest Farm Multi-Metal Area", "Outcrop", "The Linxi Group of the Upper Permian" ], [ "Badeailai-Hanshan Forest Farm Multi-Metal Area", "Outcrop", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "Volcanic-sealing clastic rock types include tuff fine sand siltstone, fine-grained feldspar sandstone in tuff and unequal feldspar sandstone in tuff.", "triple_list": [ [ "Volcano-seeding clastic rocks", "Lithology", "tuff fine sand siltstone" ], [ "Volcano-seeding clastic rocks", "Lithology", "Fine-grained feldsparite in tuff matter" ], [ "Volcano-seeding clastic rocks", "Lithology", "Chop sandstone" ], [ "Volcano-seeding clastic rocks", "Lithology", "tuffy unequal feldsparite" ], [ "Volcano-seeding clastic rocks", "Lithology", "Chop sandstone" ] ] }, { "text": "Dark gray silty slate with gray metamorphic silty 179.2m", "triple_list": [ [ "Dark gray silty silty silty silty silty silty", "thickness", "179.2m" ] ] }, { "text": "The mesozoic strata in the measurement area are very developed, mainly developing include the Baiyingao group of Manktou Ebo Formation and the Meletu Formation. The lithologic combination and Develop are different in the eruptions of the north and south.", "triple_list": [ [ "Test area", "Outcrop", "Manktou Ebo Group" ], [ "Test area", "Outcrop", "Mani Tu Group" ], [ "Test area", "Outcrop", "Baiyingao old group" ], [ "Test area", "Outcrop", "Melletou Group" ] ] }, { "text": "Gray-yellow rhyolite 5.1m", "triple_list": [ [ "Gray-yellow rhizome", "thickness", "5.1m" ] ] }, { "text": "Off-white rhyolite 7.1m", "triple_list": [ [ "Off-white rhizome", "thickness", "7.1m" ] ] }, { "text": "Green gray black mica andestone 16.6m", "triple_list": [ [ "Green gray black mica andesan rock", "thickness", "16.6m" ] ] }, { "text": "Overlapping Manitu Formation (J3mn) purple-gray Andesanite", "triple_list": [ [ "Mani Tu Group", "Lithology", "Purple-gray Andesan rock" ] ] }, { "text": "Gray flow-like rock-clad crystal tuff 36.4m", "triple_list": [ [ "Gray rhizome-like crystalline tuff", "thickness", "36.4m" ] ] }, { "text": "The lithogonal rock (αJ3m), the lithogonal section is relatively star-distributed in the measurement area, the exposed area is not large, and most of them are produced in the form of lithogonal beads.", "triple_list": [ [ "Andyama", "Distribution pattern", "Lithic beads" ] ] }, { "text": "The Sricolem Fault Zone (F2) is located in the southeast corner of the measurement area, within the Altandaba Road area, with a total length of about 20m.", "triple_list": [ [ "Siri collapse fault zone", "Located at", "Southeast corner of the test area" ], [ "Siri collapse fault zone", "Located at", "Altandabadao" ], [ "Siri collapse fault zone", "length", "20m" ] ] }, { "text": "Gray flow-grained crystalline tuff angle unconformity Lower Fulinxi Formation", "triple_list": [ [ "Gray Fluid Crystal Tuff", "thickness", "Linxi Group" ] ] }, { "text": "The rock composition contains slurry-containing slurry-containing glass chips and slurry-containing slurry-containing rocks have slurry-containing structures, and the rock composition is mainly plastic glass chips, and there are a small amount of crystal chip slurry-containing slurry-containing slurry-containing rocks.", "triple_list": [ [ "Fluidized tuff containing slurry and glass chips", "Distribution pattern", "Fused tuff structure" ], [ "Fluidized tuff containing slurry and glass chips", "Develop", "Fake flow pattern structure" ], [ "Fluidized tuff containing slurry and glass chips", "Contained", "Plastic glass chips" ], [ "Fluidized tuff containing slurry and glass chips", "Contained", "Crystal chips" ], [ "Fluidized tuff containing slurry and glass chips", "Contained", "Slurry" ] ] }, { "text": "The old formation of the Upper Jurassic White Pingao (J3b), the rock combination of this group is light gray rhizome-containing breccia-containing crystal clastic tuff light gray rhizome-containing breccia-containing crystal clastic tuff rhizome-containing rhizome-containing tuff rhizome-containing tuff and tuff sand conglomerate.", "triple_list": [ [ "Old Jurassic White Pitch", "Lithology", "Light gray breccia" ], [ "Old Jurassic White Pitch", "Lithology", "Crystal Crystal Tuff" ], [ "Old Jurassic White Pitch", "Lithology", "Light gray breccia" ], [ "Old Jurassic White Pitch", "Lithology", "Crystal chip melt tuff" ], [ "Old Jurassic White Pitch", "Lithology", "Rhyolite" ], [ "Old Jurassic White Pitch", "Lithology", "Tuff" ], [ "Old Jurassic White Pitch", "Lithology", "tuff sand gravel" ] ] }, { "text": "Gray metamorphic fine sandstone 585m", "triple_list": [ [ "Gray metamorphic fine sandstone", "thickness", "585m" ] ] }, { "text": "Gray-white fluid-grained breccia-containing crystal-cles tuff 93.9m", "triple_list": [ [ "Gray-white fluid-grained breccia-containing crystal-clad tuff", "thickness", "93.9m" ] ] }, { "text": "Dark gray black mica andestone 35.6m", "triple_list": [ [ "Dark gray black mica andesan rock", "thickness", "35.6m" ] ] }, { "text": "Fluorite containing breccia tuff 160.4m", "triple_list": [ [ "Fluorite containing breccia tuff", "thickness", "160.4m" ] ] }, { "text": "Gray metamorphic siltstone 104.2m", "triple_list": [ [ "Gray metamorphic siltstone", "thickness", "104.2m" ] ] }, { "text": "Gray-yellow flow-like breccia-containing crystal-cles tuff 5.3m", "triple_list": [ [ "Gray-yellow flow-like breccia-containing crystal-clad tuff", "thickness", "5.3m" ] ] }, { "text": "Yijida Bazarag short-axis anticline. The anticline is located in the area of Yijida Bazarag in the southeast of Hanshan Forest Farm. The central Coordinates is: x:5002, y:20726.5. The anticline axis is about 3m long, and the anticline direction is north-north and westward.", "triple_list": [ [ "Ideda Bazarag short axis anticline", "Located at", "Hanshan Forest Farm, Nandong Yijida Bazarag" ], [ "Ideda Bazarag short axis anticline", "Coordinates", "x:5002" ], [ "Ideda Bazarag short axis anticline", "Coordinates", "y:20726.5" ], [ "Ideda Bazarag short axis anticline", "length", "3m" ], [ "Ideda Bazarag short axis anticline", "Distribution pattern", "North-north-west" ] ] }, { "text": "Light gray tuff fine sandstone 91.2m", "triple_list": [ [ "Light gray tuff fine sandstone", "thickness", "91.2m" ] ] }, { "text": "Gray rhizome-containing breccia-containing crystal-clad tuff 43.3m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "43.3m" ] ] }, { "text": "The actual test profile of the Badaiai Shangjurassic Manktou Ebo Formation (J3m) in Arukorqin Banner, Inner Mongolia Autonomous Region (P-7)", "triple_list": [ [ "Badaiailai, Arukorqin Banner, Inner Mongolia Autonomous Region", "Contained", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "The subvolcanic rocks include the subrhyolite of the Manktou Obo Formation in the Late Jurassic Manktou Obo Formation (λJ3m) and the subrhyolite of the Baiyingao Formation (λJ3b).", "triple_list": [ [ "Sub-volcanic rock", "Contained", "Rhyemite in the Manktou Ebo Formation in the Late Jurassic" ], [ "Sub-volcanic rock", "Contained", "White Pingao Old Group Rhyme Rock" ] ] }, { "text": "Gray flow-grained crystalline tuff 50.5m", "triple_list": [ [ "Gray Fluid Crystal Tuff", "thickness", "50.5m" ] ] }, { "text": "Purple-gray flow-grained breccia crystal chips melted tuff 34.6m", "triple_list": [ [ "Purple-gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "34.6m" ] ] }, { "text": "Hanshan Luchang-Bainchulu Uplift Belt This uplift Belt is located in the area of Hanshan Luchang-Bishala Brigade, extending intermittently in the northeast direction, mainly composed of the Linxi Formation of the Upper Permian (P3l).", "triple_list": [ [ "Hanshan Deer Field-Bainchulu Uplift Belt", "Exposed", "Hanshan Deer Farm-North Sala Team" ], [ "Hanshan Deer Field-Bainchulu Uplift Belt", "Distribution pattern", "Intermittently extending to the northeast" ], [ "Hanshan Deer Field-Bainchulu Uplift Belt", "Outcrop", "The Linxi Group of the Upper Permian" ] ] }, { "text": "Gray-yellow rhyolite 110.4m", "triple_list": [ [ "Gray-yellow rhizome", "thickness", "110.4m" ] ] }, { "text": "The rock combination is light gray rhizome-containing breccia-containing crystal clastic tuff light gray rhizome-containing breccia-containing crystal clastic tuff rhizome-containing rhizome-containing tuff rhizome-sedged tuff and tuff sand conglomerate, etc. This strata is covered by the micro-angle discontinuity of the lower Cretaceous Melletto Formation.", "triple_list": [ [ "rock", "Lithology", "Light gray breccia" ], [ "rock", "Lithology", "Crystal Crystal Tuff" ], [ "rock", "Lithology", "Light gray breccia" ], [ "rock", "Lithology", "Crystal chip melt tuff" ], [ "rock", "Lithology", "Rhyolite" ], [ "rock", "Lithology", "Tuff" ], [ "rock", "Lithology", "tuff sand gravel" ], [ "rock", "Unconformity contact", "Lower Cretaceous Meletu Formation" ] ] }, { "text": "Gray-yellow rhyolite 21.5m", "triple_list": [ [ "Gray-yellow rhizome", "thickness", "21.5m" ] ] }, { "text": "The Manitu Formation was integrated on the Manktou Ebo Formation and was covered by the unconsolidation of the volcanic eruption of the Baiyingao Old Formation of the Upper Jurassic.", "triple_list": [ [ "Mani Tu Group", "Integration of contacts", "Manktou Ebo Group" ], [ "Mani Tu Group", "Unconformity contact", "Old Jurassic White Pitch" ] ] }, { "text": "Gray-purple flow-formed breccia-containing crystal-clad tuff 16.2m", "triple_list": [ [ "Gray-purple flow-formed breccia-containing crystal-clad tuff", "thickness", "16.2m" ] ] }, { "text": "Linxi Formation (P3l) is distributed on the southern side of the mining area, and its lithology is mainly yellow-green-gray slate metamorphic siltstone and dark gray metamorphic fine sandstone.", "triple_list": [ [ "Linxi Group", "Exposed", "The south side of the mine" ], [ "Linxi Group", "Lithology", "Yellow-green-gray slate" ], [ "Linxi Group", "Lithology", "Metamorphic siltstone" ], [ "Linxi Group", "Lithology", "Dark gray metamorphic fine sandstone" ] ] }, { "text": "The tectonic location of the survey area belongs to the Tianshan-Inner Mongolia-Xing'an trench fold area, the trench fold system in central Inner Mongolia, the late Huali West Groove fold belt of Xiwuzhumuqin Banner, and the tectonic location of the plate belongs to the northern edge of North China.", "triple_list": [ [ "Test area", "Earth tectonic location", "Tianshan-Inner Mongolia-Xing'an Ditch Folding Area" ], [ "Test area", "Earth tectonic location", "Folding system of ground troughs in central Inner Mongolia" ], [ "Test area", "Earth tectonic location", "Xiwuzhumuqin Banner Late Huali Xidi Grooving Belt" ], [ "Test area", "Earth tectonic location", "Taipei Fringe, North China" ] ] }, { "text": "Dark gray metamorphic silt sandstone 510m", "triple_list": [ [ "Dark gray metamorphic siltstone", "thickness", "510m" ] ] }, { "text": "Gray flow-grained crystal chips melted tuff 53.2m", "triple_list": [ [ "Gray Fluid Crystal Fracturing Tuff", "thickness", "53.2m" ] ] }, { "text": "The stratigraphic tendency of the Linxi Formation is 120-150°, with an inclination angle of 40-70°, and there are sporadic Late Jurassic invasion rocks along this zone.", "triple_list": [ [ "Linxi Group", "Lithology", "Late Jurassic Invasion Rock" ] ] }, { "text": "Gray flow-like breccia-containing crystal-cles tuff 41.2m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "41.2m" ] ] }, { "text": "Gray-yellow rhyolite 5.3m", "triple_list": [ [ "Gray-yellow rhizome", "thickness", "5.3m" ] ] }, { "text": "The measured profile of Linxi Formation (P3l) of the Chaganhan Motoula Upper Permian in Zharut Banner (P-3), the basic layer sequence has an upwardly thinning basic layer sequence composed of siltstone (single layer thickness 50-80cm) → slate (single layer thickness 30-40cm) → fine sandstone (single layer thickness 20-30cm) → sericca slate (single layer thickness 10-20cm) from bottom to top. The interface is straight and smooth, and there is no erosion surface, indicating that the water flow rate is lower and relatively calm.", "triple_list": [ [ "Chaganhan Motoula, Zarut Banner", "Contained", "The Linxi Group of the Upper Permian" ], [ "Chaganhan Motoula, Zarut Banner", "Lithology", "Siltstone" ], [ "Chaganhan Motoula, Zarut Banner", "Lithology", "Slate" ], [ "Chaganhan Motoula, Zarut Banner", "Lithology", "Fine sandstone" ], [ "Chaganhan Motoula, Zarut Banner", "Lithology", "sericite slate" ] ] }, { "text": "Gray fluidic breccia-containing crystal chips melted tuff 18.2m", "triple_list": [ [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "18.2m" ] ] }, { "text": "Gray tuff 13.2m", "triple_list": [ [ "Gray tuff", "thickness", "13.2m" ] ] }, { "text": "Gray-purple flow-formed breccia-containing crystal-clad tuff 51.7m", "triple_list": [ [ "Gray-purple flow-formed breccia-containing crystal-clad tuff", "thickness", "51.7m" ] ] }, { "text": "Blue-gray submerged tuff 2.8m", "triple_list": [ [ "Blue-gray tuff", "thickness", "2.8m" ] ] }, { "text": "Off-white tuff fine sandstone 32.3m", "triple_list": [ [ "Off-white tuff fine sandstone", "thickness", "32.3m" ] ] }, { "text": "Gray tuff sand conglomerate 6.9m", "triple_list": [ [ "Gray tuff sandstone", "thickness", "6.9m" ] ] }, { "text": "The lithological combination of the Linxi Formation in the Upper Permian is a dark gray gray sericaceous slate metamorphic siltstone metamorphic fine sandstone, which is produced monoclinically and has a thickness greater than 2908.7m. No fossils have been found in this strata.", "triple_list": [ [ "The Linxi Group of the Upper Permian", "Lithology", "Dark gray sericite slate" ], [ "The Linxi Group of the Upper Permian", "Lithology", "Metamorphic siltstone" ], [ "The Linxi Group of the Upper Permian", "Lithology", "Metamorphic fine sandstone" ], [ "The Linxi Group of the Upper Permian", "thickness", "2908.7m" ] ] }, { "text": "Off-white fluid-like breccia-containing crystal chips melted tuff 70.5m", "triple_list": [ [ "Off-white fluid-like breccia-containing crystal chip melt tuff", "thickness", "70.5m" ] ] }, { "text": "The basin of Altandabadaoban Volcano Eruption Basin is located on the southeast side of the line of the North Sala Brigade-Hanshan Luchang. The basin area is about 400m2 and the basin is spread in the northeast direction.", "triple_list": [ [ "Altandabadauban Volcano Eruption Basin", "Located at", "North Salad Brigade-South East Side of Hanshan Luchang Line" ], [ "Altandabadauban Volcano Eruption Basin", "area", "400m2" ], [ "Altandabadauban Volcano Eruption Basin", "Distribution pattern", "North-east-oriented cloth" ] ] }, { "text": "Medium-fine-grained mica dicyclone (J3ηβ1) This lithology is mainly exposed on the north side of Hanshan Luchang, producing in a lithobead-like shape, with an exposed area of about 4m2.", "triple_list": [ [ "Medium fine-grained black mica dicyclone", "Exposed", "North side of Hanshan Luchang" ], [ "Medium fine-grained black mica dicyclone", "Distribution pattern", "Lithic beads" ], [ "Medium fine-grained black mica dicyclone", "area", "4m2" ] ] }, { "text": "Gray-gray-green flow-gray breccia-containing crystal-cles tuff 41.3m", "triple_list": [ [ "Gray-gray-green flow-gray breccia-containing crystal-clad tuff", "thickness", "41.3m" ] ] }, { "text": "Gray fluidic breccia-containing crystal chips melted tuff 418.6m", "triple_list": [ [ "Gray flow-grained breccia-containing crystal chips melted tuff", "thickness", "418.6m" ] ] }, { "text": "The lithogenic section is only exposed near the North Sala Brigade North Forest Fire Protection Station and is produced in a vein-like manner.", "triple_list": [ [ "Andyama", "Exposed", "Near the North Sala Brigade Band Near the North Forest Fire Protection Station" ], [ "Andyama", "Distribution pattern", "Vein-like output" ] ] }, { "text": "The Linxi Formation of the Upper Permian regime is mainly distributed in the area of the North Sala Brigade in the North Sala Brigade and the Chaganhan Motewula in the Hanshan Luchang. The Altandabadao fleet and the Delestai fire prevention station surface appear sporadically, and are generally spread to the northeast, with an exposed area of about 60m2.", "triple_list": [ [ "The Linxi Group of the Upper Permian", "Exposed", "North Salad Team" ], [ "The Linxi Group of the Upper Permian", "Exposed", "Chaganhan Motewula of Hanshan Deer Farm" ], [ "The Linxi Group of the Upper Permian", "Exposed", "Altandabadao" ], [ "The Linxi Group of the Upper Permian", "Exposed", "DelesTaiwan fire protection station" ], [ "The Linxi Group of the Upper Permian", "Distribution pattern", "North-east-oriented cloth" ], [ "The Linxi Group of the Upper Permian", "area", "60m2" ] ] }, { "text": "The inclination of the Haltugrad is located on the southeast side of the Altandabadao line. The central coordinates are: x:4996.6, y:20734.5. The nuclear part is the Manktou Ebo Formation. The nuclear part develops the Andesite veins and Ying'anite veins in the northeast direction.", "triple_list": [ [ "Haltugrad tilt", "Located at", "The southeast side of the Alatandabadao" ], [ "Haltugrad tilt", "Coordinates", "x:4996.6" ], [ "Haltugrad tilt", "Coordinates", "y:20734.5" ], [ "Haltugrad tilt", "Belongs to", "Manktou Ebo Group" ], [ "Haltugrad tilt", "Develop", "Andesan rock vein" ], [ "Haltugrad tilt", "Develop", "Ying'an rock vein" ] ] }, { "text": "Dark gray Ying'an breccia-containing crystal-cles tuff 164.6m", "triple_list": [ [ "Dark gray Ying'an breccia-containing crystalline tuff", "thickness", "164.6m" ] ] }, { "text": "Dark gray sericite slate 406m", "triple_list": [ [ "Dark gray sericite slate", "thickness", "406m" ] ] }, { "text": "The diochangite rocks are gray-green-gray, with fine-grained crystal structure and blocky structure. The main minerals are plagiarite potassium feldspar and a small amount of quartz.", "triple_list": [ [ "Erchangyan", "Distribution pattern", "Fine-grained crystal structure" ], [ "Erchangyan", "Develop", "Blocky structure" ], [ "Erchangyan", "Contained", "Plagioclase" ], [ "Erchangyan", "Contained", "Potassium feldspar" ], [ "Erchangyan", "Contained", "Black Mouse" ], [ "Erchangyan", "Contained", "quartz" ] ] }, { "text": "Fine-grained mica granite (J3β4) in the Wulan Mountains is mainly distributed in the Wulan Mountain area measured in Ganzhuer Aobao east of the Luchang, Hanshan Mountain. It produces in a lithobead-like shape with an exposed area of 6m2.", "triple_list": [ [ "Fine-grained mica granite in Ulan Mountains", "Exposed", "Wulan Mountain in Ganzhuer Aobao East Testing in Hanshan Luchang" ], [ "Fine-grained mica granite in Ulan Mountains", "Distribution pattern", "Lithic beads" ], [ "Fine-grained mica granite in Ulan Mountains", "area", "6m2" ] ] }, { "text": "Gray metamorphic fine sandstone 17.4m", "triple_list": [ [ "Gray metamorphic fine sandstone", "thickness", "17.4m" ] ] }, { "text": "Dark gray metamorphic silt sandstone with gray metamorphic fine sandstone 84.4m", "triple_list": [ [ "Dark gray metamorphic silt sandstone with gray metamorphic fine sandstone", "thickness", "84.4m" ] ] }, { "text": "The north-west west-west fault (F4) of Ulanhada is located in the middle of Hanshan Luchang, on the north-west side of Ulanhada Mountain, distributed in the north-west direction, about 9m long.", "triple_list": [ [ "Ulanhada broke north, west and west", "Located at", "The middle part of Hanshan deer farm" ], [ "Ulanhada broke north, west and west", "Located at", "North West Side of Ulanhada Mountain" ], [ "Ulanhada broke north, west and west", "Distribution pattern", "Distribution to the north and west" ], [ "Ulanhada broke north, west and west", "length", "9m" ] ] }, { "text": "Gray-green flow-grained breccia-containing crystal-cles tuff 36.3m", "triple_list": [ [ "Gray-green flow-grained breccia-containing crystal-clad tuff", "thickness", "36.3m" ] ] }, { "text": "Gray rhizome-containing breccia-containing crystal-cles tuff 4.5m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "4.5m" ] ] }, { "text": "The Ganzhuer Aobau anomaly is located in the north-west corner of the Hanshan Luchang, 2m south-east of the Zhuer Aobau. The central location geographical Coordinates (X:5004 Y:20703) local anomaly occurring in the high background area.", "triple_list": [ [ "Garzur Abbo abnormality", "Located at", "Hanshan Deer Farm is north-west corner" ], [ "Garzur Abbo abnormality", "Located at", "2m southeast of Zhuer Aobao" ], [ "Garzur Abbo abnormality", "Coordinates", "X:5004" ], [ "Garzur Abbo abnormality", "Coordinates", "Y:20703" ] ] }, { "text": "Gray flow-like breccia-containing crystal-cles tuff 617.9m", "triple_list": [ [ "Gray rhizome-containing breccia-containing crystal-clad tuff", "thickness", "617.9m" ] ] }, { "text": "Gray flow-grained crystal chips melted tuff 34.6m", "triple_list": [ [ "Gray Fluid Crystal Fracturing Tuff", "thickness", "34.6m" ] ] }, { "text": "The lithology of the Mankitou Ebo Formation (J3m) is mainly composed of gray-gray-yellow rhizome-containing breccia-containing crystalline crystal (fusion) tuff sedimentary tuff tuff as the grey tuff sand conglomerate and gray-yellow rhyolite.", "triple_list": [ [ "Manktou Ebo Group", "Lithology", "Gray gray-yellow flowing breccia" ], [ "Manktou Ebo Group", "Lithology", "Clast crystal chips (smelted) tuff" ], [ "Manktou Ebo Group", "Lithology", "Tuff" ], [ "Manktou Ebo Group", "Lithology", "Gray tuff sandstone" ], [ "Manktou Ebo Group", "Lithology", "Gray-yellow rhizome" ] ] }, { "text": "Gray-gray yellow fuzzy breccia crystal tuff 79.9m", "triple_list": [ [ "Gray-gray yellow fuzzy breccia crystal tuff", "thickness", "79.9m" ] ] }, { "text": "Gray tuff fine sandstone 31.4m", "triple_list": [ [ "Gray tuff fine sandstone", "thickness", "31.4m" ] ] }, { "text": "Test profile diagram of the lower Cretaceous Meletu Formation (K1ml) in the Meletu Mountains of Zhalut Banner", "triple_list": [ [ "Meleheitu Mountain in Zarut Banner", "Contained", "Lower Cretaceous Meletu Formation" ] ] }, { "text": "Super Holtou North Silver Polymetallic Mine Spot (Newly Discovered Mine Spot) is located in the north of Zhalut Banner, Tongliao City, Inner Mongolia Autonomous Region. It is under the jurisdiction of Hanshan Forest Farm. The geographical coordinates are east longitude: 119°39′30″ and north latitude 45°16′30″.", "triple_list": [ [ "Super Holtou North Silver Polymetallic Mining Site", "Located at", "North Zhalut Banner, Tongliao City, Inner Mongolia Autonomous Region" ], [ "Super Holtou North Silver Polymetallic Mining Site", "Administrative area", "Hanshan Forest Farm" ], [ "Super Holtou North Silver Polymetallic Mining Site", "Coordinates", "119°39′30″" ], [ "Super Holtou North Silver Polymetallic Mining Site", "Coordinates", "45°16′30″ North latitude" ] ] }, { "text": "The actual measured profile of the invasion of the invasion of Tunter North West Late Jurassic fine-grained porphyry potassium long granite in Hanshan Forest Farm (P-5) is mainly exposed in the area of Tunter in Hanshan Deer Farm, spreading in an near east-west direction. The rock is gray-yellow, with a fine-grained patchy structure, and an exposed area of 10m2.", "triple_list": [ [ "Hanshan Forest Farm Tuntel North West", "Lithology", "Late Jurassic fine particle papillary potassium granite" ], [ "Late Jurassic fine particle papillary potassium granite", "Exposed", "Hanshan Luchang Tuntel" ], [ "Late Jurassic fine particle papillary potassium granite", "Distribution pattern", "Near east-west spread" ], [ "Late Jurassic fine particle papillary potassium granite", "Distribution pattern", "Micro-grained spot-like structure" ], [ "Late Jurassic fine particle papillary potassium granite", "area", "10m2" ] ] }, { "text": "Light gray-green flow-grain crystal chips melted tuff 33.1m", "triple_list": [ [ "Light gray-green flow-grain crystal chip fusion tuff", "thickness", "33.1m" ] ] }, { "text": "Off-white submerged tuff 9.4m", "triple_list": [ [ "Off-white tuff", "thickness", "9.4m" ] ] }, { "text": "Gray flow-grained texture contains 28.1m of tuff", "triple_list": [ [ "Gray flow-grained tuff containing bricci tuff", "thickness", "28.1m" ] ] }, { "text": "Gray-yellow flow-grained crystal chips melted tuff 123.7m", "triple_list": [ [ "Gray-yellow flow-grained crystal chips melted tuff", "thickness", "123.7m" ] ] }, { "text": "The volcanic eruption basin of the Delestai Fire Prevention Station is located on the northwest side of the line of the North Sala Brigade-Hanshan Forest Farm-Hanshan Lu Farm. The basin area is about 500m2. The basin extends in the northeast, mainly composed of the SuperHoltu volcanic mechanism and the Tegeyin Hanwula volcanic mechanism.", "triple_list": [ [ "Delestai Fire Protection Station Volcanic Eruption Basin", "Located at", "North Salad Brigade-Hanshan Forest Farm-Northwest Side of the North West of Hanshan Lu Farm" ], [ "Delestai Fire Protection Station Volcanic Eruption Basin", "area", "500m2" ], [ "Delestai Fire Protection Station Volcanic Eruption Basin", "Distribution pattern", "Extend northeast" ], [ "Delestai Fire Protection Station Volcanic Eruption Basin", "Contained", "Super Holt volcanic mechanism" ], [ "Delestai Fire Protection Station Volcanic Eruption Basin", "Contained", "Tegeyinhanula Volcano Institution" ] ] }, { "text": "The base of the volcanic eruption is composed of the Linxi Formation of the Upper Permian system. The main part is volcanic rocks from the Manktou Obo Formation. The center of the volcanic eruption is a rhizome-collapsed block rock, which changes to the outer lithology into rhizome-containing breccia-containing crystalline tuff, and the outermost layer is rhizome-containing breccia-containing crystalline tuff.", "triple_list": [ [ "Volcanic eruption base", "Contained", "The Linxi Group of the Upper Permian" ], [ "Volcanic eruption base", "Lithology", "Volcanic rocks in the Mankitou Ebo Formation" ], [ "Volcanic eruption base", "Lithology", "Flow-grained rock" ], [ "Volcanic eruption base", "Lithology", "Breccia" ], [ "Volcanic eruption base", "Lithology", "Crystal chip melt tuff" ], [ "Volcanic eruption base", "Lithology", "Breccia" ], [ "Volcanic eruption base", "Lithology", "Crystal Crystal Tuff" ] ] }, { "text": "The fourth system of the new system flood alluvial slopes has the lithology of gray-brown clay sand-sand gravel and gray-brown clay sand-sand gravel.", "triple_list": [ [ "The fourth system of all-round flood alluvial slopes", "Lithology", "Gray-brown clay soil" ], [ "The fourth system of all-round flood alluvial slopes", "Lithology", "Gravel" ], [ "The fourth system of all-round flood alluvial slopes", "Lithology", "Gray-brown clay soil" ], [ "The fourth system of all-round flood alluvial slopes", "Lithology", "gravel" ] ] }, { "text": "Gray-yellow flow-grained breccia crystal tuff 138.7m", "triple_list": [ [ "Gray-yellow flow-grained breccia crystal tuff", "thickness", "138.7m" ] ] }, { "text": "Light gray flow tuff 23.8m", "triple_list": [ [ "Light gray flow tuff", "thickness", "23.8m" ] ] }, { "text": "The rock has a gray-yellow color and is medium-fine-grained structure.", "triple_list": [ [ "rock", "Distribution pattern", "Medium fine-grained structure" ] ] }, { "text": "Gray-purple flow-formed breccia-containing crystal-clad tuff 6.4m", "triple_list": [ [ "Gray-purple flow-formed breccia-containing crystal-clad tuff", "thickness", "6.4m" ] ] }, { "text": "The exposed strata in the mining area are mainly gray-white rhizome-containing breccia-containing crystal-clad tuff, gray-white rhizome-containing breccia-containing crystal-clad tuff, rhyolite, etc.", "triple_list": [ [ "Mining area", "Lithology", "The off-white breccia-containing breccia in the Manktou Ebo Formation of Upper Jurassic" ], [ "Mining area", "Lithology", "Crystal chip melt tuff" ], [ "Mining area", "Lithology", "Off-white breccia" ], [ "Mining area", "Lithology", "Crystal chip melt tuff" ], [ "Mining area", "Lithology", "Rhyolite" ] ] }, { "text": "The exposed strata in the mining area are mainly gray rhizome-containing breccia-containing crystalline tuff rhizome-clad crystalline tuff rhizome-clad crystalline tuff rhizome-clad tuff rhizome-clad tuff rhizome-clad tuff rhizome-clad tuff rhizome-clad tuff rhizome-clad tuff in the Upper Jurassics Manketto Obo Formation.", "triple_list": [ [ "Mining area", "Outcrop", "Gray breccia-containing crystal tuff of Manktou Ebo Formation in Upper Jurassic" ], [ "Mining area", "Outcrop", "Fluid crystal chip fusion tuff" ], [ "Mining area", "Outcrop", "Rhyolite" ] ] }, { "text": "Green-gray Anshan-containing breccia-containing crystal-clad tuff 13.9m", "triple_list": [ [ "Green-gray Anshan-like breccia-containing crystal-clad tuff", "thickness", "13.9m" ] ] }, { "text": "The angle of blue-gray black mica andestone is not integrated under the underworld white pitch old group gray-white flow-like breccia-containing crystal-clad tuff", "triple_list": [ [ "Blue-gray black mica Andesan rock", "Unconformity contact", "Baiyingao old group" ], [ "Baiyingao old group", "Lithology", "Off-white breccia" ], [ "Baiyingao old group", "Lithology", "Crystal Crystal Tuff" ] ] }, { "text": "Gray-green tuff fine sandstone 39m", "triple_list": [ [ "Gray-green tuff fine sandstone", "thickness", "39m" ] ] }, { "text": "Gray-green tuff siltstone 19m", "triple_list": [ [ "Gray-green tuff siltstone", "thickness", "19m" ] ] }, { "text": "Gray dark gray thick layered chert-containing cleavage bioclass limestone, 9m thick", "triple_list": [ [ "Gray dark gray thick layered chert-containing tuberculosis fragmented bioclass limestone", "thickness", "9m" ] ] }, { "text": "Gray-green-light gray-green flowing Anite, 57m thick", "triple_list": [ [ "Gray-green-light gray-green flowing Ying'an rock", "thickness", "57m" ] ] }, { "text": "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone, 17m thick", "triple_list": [ [ "Light gray-dark gray medium-thick layered algae trace microcrystalline limestone", "thickness", "17m" ] ] }, { "text": "Dark gray medium-thick layered fine-grained quartz sandstone with gray-black slate, 7m thick", "triple_list": [ [ "Dark gray medium-thick layered fine-grained quartz sandstone with gray black slate", "thickness", "7m" ] ] }, { "text": "Silty sandstone with shale, 46m thick", "triple_list": [ [ "Silty sandstone with shale", "thickness", "46m" ] ] }, { "text": "Slate sandstone, 25m thick", "triple_list": [ [ "Slate sandstone", "thickness", "25m" ] ] }, { "text": "Linxi Formation Gray Dark Gray Silty Slate with Metamorphic Silty Silty Silty Silty Silty", "triple_list": [ [ "Linxi Group", "Lithology", "Gray dark grey silty slab" ], [ "Linxi Group", "Lithology", "Metamorphic siltstone" ] ] }, { "text": "The lower Cretaceous Meletu Formation (K1ml) has less exposed in this set of strata, and it only produces in the cap-shaped shape of Melehetto Mountain. The rock formation is gentle and has an exposed area of about 4m2 and a thickness of >210m. The rock combination is dark gray basalt and green gray androsite, etc.", "triple_list": [ [ "Lower Cretaceous Meletu Formation", "Exposed", "Melehei Tushan" ], [ "Lower Cretaceous Meletu Formation", "Distribution pattern", "Cap-like output" ], [ "Lower Cretaceous Meletu Formation", "area", "4m2" ], [ "Lower Cretaceous Meletu Formation", "thickness", "210m" ], [ "Lower Cretaceous Meletu Formation", "Lithology", "Dark gray basalt Andesan rock" ], [ "Lower Cretaceous Meletu Formation", "Lithology", "Green Gray Andesan Rock" ] ] }, { "text": "Flow-like crystal chip tuff has a crystal chip tuff structure. The debris composition in the rock is mainly crystal chips, followed by glass chips, and occasionally rock chips are distributed.", "triple_list": [ [ "Fluidic crystal tuff", "Distribution pattern", "Crystal chip tuff structure" ], [ "Fluidic crystal tuff", "Contained", "Crystal chips" ], [ "Fluidic crystal tuff", "Contained", "Glass chips" ], [ "Fluidic crystal tuff", "Contained", "Rock chips" ] ] }, { "text": "The fault structure in the measurement area is mainly manifested in the northeastern fault structure and the northwest fault structure.", "triple_list": [ [ "Test area", "Develop", "Northeast-oriented fault structure" ], [ "Test area", "Develop", "North-west-failure structure" ] ] }, { "text": "The medium-grained black mica 2-long granite (J3η2) in Hanshan Deer Farm, the rocks are flesh-red and have a medium-grained structure. They are distributed on the eastern ridges of the Hanshan Deer Farm, spreading in the northeast, with an exposed area of about 10m2. The rock mass invades the Mankitou Ebo Formation of the Upper Jurassic (J3m) (see Figure 2-22).", "triple_list": [ [ "Fine-grained black mica 2 Chang granite in Hanshan Deer Farm", "Distribution pattern", "Medium fine-grained structure" ], [ "Fine-grained black mica 2 Chang granite in Hanshan Deer Farm", "Exposed", "The eastern mountain beams of Hanshan Luchang" ], [ "Fine-grained black mica 2 Chang granite in Hanshan Deer Farm", "Distribution pattern", "North-east-oriented cloth" ], [ "Fine-grained black mica 2 Chang granite in Hanshan Deer Farm", "area", "10m2" ] ] }, { "text": "Gray-gray yellow fuzzy breccia fusion tuff 11.7m", "triple_list": [ [ "Gray-gray yellow fuzzy breccia fusion tuff", "thickness", "11.7m" ] ] }, { "text": "Gray flow-grained crystal chips melted tuff 162.6m", "triple_list": [ [ "Gray Fluid Crystal Fracturing Tuff", "thickness", "162.6m" ] ] }, { "text": "A large-thick late Jurassic volcanic rock combination was developed in the Mesozoic volcanic eruption basin, from old to new, the Manktou Obo Formation and the Baiyingao Old Formation.", "triple_list": [ [ "Mesozoic volcanic eruption basin", "Develop", "Late Jurassic Volcanic Rocks" ], [ "Mesozoic volcanic eruption basin", "Outcrop", "Manktou Ebo Group" ], [ "Mesozoic volcanic eruption basin", "Outcrop", "Mani Tu Group" ], [ "Mesozoic volcanic eruption basin", "Outcrop", "Baiyingao old group" ] ] }, { "text": "Maoxigadabazarag is inclined. This direction is located in Maoxigadabazarag in the south of the vegetable garden of Hanshan Forest Farm. The central Coordinates is x:4998.5, y:2072.2. The oblique axis is 4m long, and it goes north to north and west. The oblique core is the Upper Jurassic Manitu Formation, and its two wing lithologies are the Upper Jurassic Manktou Ebo Formation.", "triple_list": [ [ "Mao Xigada Bazarag tilts", "Located at", "Maoxigada Bazarag in Zinan, Hanshan Forest Farm Vegetable Garden" ], [ "Mao Xigada Bazarag tilts", "Coordinates", "x:4998.5" ], [ "Mao Xigada Bazarag tilts", "Coordinates", "y:2072.2" ], [ "Mao Xigada Bazarag tilts", "length", "4m" ], [ "Mao Xigada Bazarag tilts", "Distribution pattern", "North-north-west" ], [ "Mao Xigada Bazarag tilts", "Belongs to", "Upper Jurassic Mani Tender Group" ], [ "Mao Xigada Bazarag tilts", "Belongs to", "Upper Jurassic Manktou Ebo Group" ] ] }, { "text": "Gray grayish-white black cloud granite gneiss with dark gray oblique elongated schist and grayish-white pomegranate black cloud granite gneiss 287m", "triple_list": [ [ "Gray grayish-white black cloud granite gneiss with dark gray oblique elongated schist and grayish-white pomegranate black cloud granite gneiss", "thickness", "287m" ] ] }, { "text": "Gray black cloud granite gneiss 2 cloud granite gneiss 50m", "triple_list": [ [ "Gray black clouds granite gneiss two clouds granite gneiss", "thickness", "50m" ] ] }, { "text": "Off-white thick layer of marble 87.50m", "triple_list": [ [ "Off-white thick layer of marble", "thickness", "87.50m" ] ] }, { "text": "Light gray middle layer sericite-black mica quartz thousand rock 287.44m", "triple_list": [ [ "Light gray middle layer sericite-black mica quartz thousand rocks", "thickness", "287.44m" ] ] }, { "text": "Light gray blocky oblique length grey rock dark gray blocky black cloud grey rock sandwich black cloud two long length gneiss 62.0m", "triple_list": [ [ "Light gray blocky oblique length grey rock dark gray blocky black cloud grainy rock sandwich black cloud two long gneis", "thickness", "62.0m" ] ] }, { "text": "Gray blocky black cloud oblique elongated gneiss diclosed potassium gneiss intersecting gray gray black clouds diclosed grey rock oblique elongated amphibol 597m", "triple_list": [ [ "Gray blocky black clouds oblique elongated gneiss diclosed potassium gneiss intersecting grey black clouds diclosed grey grey black clouds oblique elongated amphibolite", "thickness", "597m" ] ] }, { "text": "To sum up, the Qingnidong Formation in this area transitions from bottom to top, and the sedimentary environment from shallow sea shed to outward sheds, which is a passive continental marginal sedimentation.", "triple_list": [ [ "Qingni Cave Group", "Belongs to", "Passive continental marginal sedimentation" ] ] }, { "text": "Light gray striped dolomite schist 61.67m", "triple_list": [ [ "Light gray striped dolomite schist", "thickness", "61.67m" ] ] }, { "text": "Gray medium-thick layer of limestone intersects biolimestone, coral Pseudozaphrentis minor; brachiopod Atrypa richthofeni, A. interruptta; tooth-shaped spines Polygnathus xylus, Icriodus aff. brevis; foramini Amphpora sp., 19.5m", "triple_list": [ [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "Coral Pseudozaphrentis minor" ], [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "Brachiopod Atrypa richthofeni" ], [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "A. interrupta" ], [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "tooth thorn Polygnathus xylus" ], [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "Icriodus aff. brevis" ], [ "Gray medium-thick layer of limestone intersects biolimestone", "Paleontological", "Foraminifera Amphipora sp." ], [ "Gray medium-thick layer of limestone intersects biolimestone", "thickness", "19.5m" ] ] }, { "text": "Gray thick limestone intersected with thin layers of limestone biolimestone and amylin limestone, producing foraminifera Amphipora sp., 8.6m ───────────────────────────── Ding Zonglong Formation (D2d), thickness 267.6m", "triple_list": [ [ "Thin layers of limestone biolimestone and amylin limestone in the grey thick layer of limestone", "Paleontological", "Foraminifera Amphipora sp." ], [ "Thin layers of limestone biolimestone and amylin limestone in the grey thick layer of limestone", "thickness", "8.6m" ], [ "Thin layers of limestone biolimestone and amylin limestone in the grey thick layer of limestone", "Integration of contacts", "Ding Zonglong Group" ], [ "Thin layers of limestone biolimestone and amylin limestone in the grey thick layer of limestone", "thickness", "267.6m" ] ] }, { "text": "The survey area is located on the eastern edge of the Tanggula Mountains and belongs to the northern part of the Hengduan Mountains. The mountain ranges are mostly in the northwest to the east, with an overall high in the north and low in the south, with a minimum Elevation of 2,800 meters, a maximum Elevation of 5,752 meters, and an average Elevation of 4,250 meters. The terrain is dangerous, with deep cutting and large fluctuations, and is generally manifested as a plateau, alpine and narrow valley landform.", "triple_list": [ [ "Test area", "Located at", "Tanggula Shandong Edge" ], [ "Test area", "Located at", "North Hengduan Mountains" ], [ "Test area", "Distribution pattern", "Northwest-South East" ], [ "Test area", "Elevation", "2800 meters" ], [ "Test area", "Elevation", "5752 meters" ], [ "Test area", "Elevation", "4250 meters" ] ] }, { "text": "In the slate in Bagalan area, there are individual small shells decorated with simple bivalves.", "triple_list": [ [ "Baga Nong", "Contained", "Slate" ], [ "Slate", "Paleontological", "Bivalves" ] ] }, { "text": "The Wuqingna Formation is relatively stable in the area. It is a set of gray-gray-black middle-block limestone with a muddy limestone, with flint strips on the upper part and a large number of coral brachiopod bivalve ammonite gastropods, etc. It is integrated and covered on the Late Devons Drogo Cave Formation with a thickness of 790,981m.", "triple_list": [ [ "Wuqingna Group", "Lithology", "Gray-gray-black middle layer—blocky limestone" ], [ "Wuqingna Group", "Lithology", "Mixed limestone" ], [ "Wuqingna Group", "Contained", "Flint strip" ], [ "Wuqingna Group", "Paleontological", "coral" ], [ "Wuqingna Group", "Paleontological", "Brachiopod" ], [ "Wuqingna Group", "Paleontological", "Bivalves" ], [ "Wuqingna Group", "Paleontological", "Chrysanthemum" ], [ "Wuqingna Group", "Paleontological", "Gastropod" ], [ "Wuqingna Group", "Integration of contacts", "Late Devon Drogo Cave Group" ], [ "Wuqingna Group", "thickness", "790981m" ] ] }, { "text": "Light gray-green altered clastic neutral volcanic rock 53.98m.", "triple_list": [ [ "Light gray-green altered clastic neutral volcanic rock", "thickness", "53.98m" ] ] }, { "text": "The lithology of the Dongla Formation is light gray-gray-black sticky slate in the lower part of the Gucai Village-Eila Township, Jiangda County. It has a light gray-gray black sticky slate, and the metamorphic silt sandstone is mixed with light gray light gray green medium acidic volcanic rocks. It has clear sedimentary rhythm and is granular stratigraphic horizontal stratigraphic sand patterns intertwined.", "triple_list": [ [ "Donla Group", "Exposed", "Gucai Village, Jiangda County - Ella Township" ], [ "Donla Group", "Lithology", "Light gray-gray black sticky slate" ], [ "Donla Group", "Lithology", "Qianmeiyan" ], [ "Donla Group", "Lithology", "Metamorphic siltstone" ], [ "Donla Group", "Lithology", "Light gray light gray green medium acidic volcanic rock" ], [ "Donla Group", "Develop", "Granular Sequence Laminating" ], [ "Donla Group", "Develop", "Horizontal stratification" ], [ "Donla Group", "Develop", "Sand pattern interlaced layering" ] ] }, { "text": "The Youxi group has very little distribution range in this area, exposed to the Jiangdengka area in the southern part of Changdu County at 1:25,000, and the profile has not been measured.", "triple_list": [ [ "Youxi Group", "Exposed", "The southern part of Changdu County will be light card" ] ] }, { "text": "Gray blocky appearance scattered black cloud plagiaria granite alternating flake pyroxene black cloud plagiaria granite 220.0m", "triple_list": [ [ "Gray blocky appearance flakes of lemon-shaped black clouds plagiaria granite alternating flakes of pyroxene black clouds plagiaria granite", "thickness", "220.0m" ] ] }, { "text": "Gray thick layer of blocky microcrystalline limestone with sutures and horizontal stratigraphic 10.0m", "triple_list": [ [ "Gray thick layer of blocky microcrystalline limestone", "Develop", "Suture" ], [ "Gray thick layer of blocky microcrystalline limestone", "Develop", "Horizontal stratification" ], [ "Gray thick layer of blocky microcrystalline limestone", "thickness", "10.0m" ] ] }, { "text": "In 1997, the rock formations of the Tibet Autonomous Region continued to use the Dzonlong Formation (D2d) Drogo Cave Formation (D3zˆ) in Haitong Formation (D1h).", "triple_list": [ [ "Rocky strata in Tibet Autonomous Region", "Outcrop", "Haitong Group" ], [ "Rocky strata in Tibet Autonomous Region", "Outcrop", "Ding Zonglong Group" ], [ "Rocky strata in Tibet Autonomous Region", "Outcrop", "Drogo Cave Group" ] ] }, { "text": "1:25 million Nanqian County, Bingjiangda County, Binglian Test Area (hereinafter referred to as this area) stratigraphic divisions Belongs to to the Gangdes-Himalayan tectonic stratigraphic area, Pangong Lake-Nujiang stratigraphic area (1) Jiayuqiao-Chawalong stratigraphic area (1-1) and Qiangtang-Sanjiang stratigraphic area, Nanqiangtang-Zuogong stratigraphic area (1) Lewuqi-Zuogong stratigraphic area (1-1), Lancang River stratigraphic area ( 2) Beilancang River Stratigraphic Zone (2-1), Changdu-Simao Stratigraphic Zone (3) Yu-Rang-Zhuka Stratigraphic Zone (3-1) Changdu-Mangkang Stratigraphic Zone (3-2) Jiangda-Deqin Stratigraphic Zone (3-3), Xijin Wulan-Jinsha River Stratigraphic Zone (4) Gangtu-Xiqu River Stratigraphic Zone (4-1), Dege-Zhongdian Stratigraphic Zone (5) Dege-Baiyu Stratigraphic Zone (5-1).", "triple_list": [ [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Gangdise-Himalayan tectonic formation area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Pangong Lake-Nujiang Formation Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Jiayu Bridge-Chawalong Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Qiangtang-Sanjiang Tectonics-Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Nanqiangtang-Zuogong Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Lewuqi-Zuogong Stratigraphic Division" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Lancang River Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "North Lancang River Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Chamdo-Simao Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Russia-Zhuka Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Chamdo-Mangkang Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Jiangda-Deqin Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Xijin Wulan-Jinshajiang Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Gangtuo-Xiquhe Stratigraphic Zone" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Dege-Zhongdian Stratigraphic Area" ], [ "Nangqian County Changdu County Bianjiangda County Bian Joint Test Area", "Stratigraphical zoning", "Dege-White Jade Stratigraphic Zone" ] ] }, { "text": "In 125 million, a small amount of Dongla Group (D3d) was exposed in the area of Sangzhi Akao in Bailiangniang Township, Yushu County, Nangqian County, with a total exposed area of about 47.5m2.", "triple_list": [ [ "Sangzhi Akao, Bailiangniang Township, Yushu County, Nangqian County", "Outcrop", "Donla Group" ], [ "Donla Group", "area", "47.5m2" ] ] }, { "text": "Qingni Cave Group (O1q), thickness 1430m", "triple_list": [ [ "Qingni Cave Group", "thickness", "1430m" ] ] }, { "text": "The gray-white thin-middle cross black cloud quartz schist and the light gray-gray thick-block layered cross pomegranate dolomite quartz schist are interlayered with gray-green medium-thick layer of oblique elongated flash schist 189m", "triple_list": [ [ "Gray-white thin-middle cross black cloud quartz schist and light gray-gray-thick-block layered cross pomegranate dolomite quartz schist interlayered with gray-green medium-thick layer of oblique elongated radiuschist", "thickness", "189m" ] ] }, { "text": "Gray light gray middle layer shiny biosandra limestone thin layer striatically limestone with gray yellow gray-green biosandra clay rock, containing bryozoa Fenestella sp. and coral brachiopod fragments, 124.56m", "triple_list": [ [ "Gray light gray middle layer shiny biosandra limestone thin layer striatically limestone with gray yellow gray-green biosandra clay rock", "Paleontological", "Bryomyces Fenestella sp." ], [ "Gray light gray middle layer shiny biosandra limestone thin layer striatically limestone with gray yellow gray-green biosandra clay rock", "Paleontological", "coral" ], [ "Gray light gray middle layer shiny biosandra limestone thin layer striatically limestone with gray yellow gray-green biosandra clay rock", "Paleontological", "Brachiopod" ], [ "Gray light gray middle layer shiny biosandra limestone thin layer striatically limestone with gray yellow gray-green biosandra clay rock", "thickness", "124.56m" ] ] }, { "text": "Gray-black thin-medium-thick layered argillite limestone, containing coral Cystophrentis sp. Zaphriphriphyllum stereoseptatum Paralithostrotion sp. Diphyphyllum tuobaense Bifossulara sp. Syningopora sp.; Brachiopora elicospirif sp.; Bivalves Plerinapecten cf.rigidus Permophorus sp., 94.8m.", "triple_list": [ [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "Coral Cystophrentis sp." ], [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "Zaphriphriphyllum stereoseptatum Paralithostrotion sp." ], [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "Diphyphyllum tuobaense Bifossulara sp." ], [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "Syringopora sp." ], [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "Brachiopod elicospirif sp." ], [ "Gray-black thin-medium-thick layered argillite", "Paleontological", "bivalves Plerinapecten cf. rigidus Permophorus sp." ], [ "Gray-black thin-medium-thick layered argillite", "thickness", "94.8m" ] ] }, { "text": "The Devonian strata of the Chamdo-Mangkang strata are well developed, from old to new, there are early Devon Shi Haitong Formation (D1h), middle Devon Shi Ding Zonglong Formation (D2d), late Devon Shi Drogo Cave Formation (D3z∧), and Haitong Formation (D1h), Ding Zonglong Formation (D2d) Drogo Cave Formation (D3z∧).", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Contained", "Devonian strata" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Devon Shihaitong Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Ding Zonglong Group of Zhongdian" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Late Devon Drogo Cave Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Haitong Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Ding Zonglong Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Drogo Cave Group" ] ] }, { "text": "Brachiopod Atrypa richthofeni appears from bottom to top in the Ding Zonglong Group throughout the region.", "triple_list": [ [ "Brachiopod Atrypa richthofeni", "Belongs to", "Ding Zonglong Group" ] ] }, { "text": "Gray fine-grained block biolimestone with medium-thick limestone, coral Disphyllum sp. and brachiopod foramen, 5.0m", "triple_list": [ [ "Gray fine-grained block biolimestone with medium-thick limestone", "Paleontological", "Coral Disphyllum sp." ], [ "Gray fine-grained block biolimestone with medium-thick limestone", "Paleontological", "Brachiopod" ], [ "Gray fine-grained block biolimestone with medium-thick limestone", "Paleontological", "Laminar worm" ], [ "Gray fine-grained block biolimestone with medium-thick limestone", "thickness", "5.0m" ] ] }, { "text": "The Drogo Cave Formation is widely distributed, and it is exposed in the Qingnidong area in Jiangda County, Tuoba, Changdu. The lithology is gray, light gray, thin-block layered dolomite limestone marl limestone dolomite, the bottom shale and limestone interlayer, and contains rich brachiopod coral bivalve foramen fang-shaped spines, especially the Develop of flute corals, which are integrated with the Early Carboniferous Wuqingna Formation, and the lower part is integrated with the Ding Zonglong Formation.", "triple_list": [ [ "Drogo Cave Group", "Exposed", "Qingni Cave, Jiangda County, Toba, Changdu" ], [ "Drogo Cave Group", "Lithology", "Gray light gray thin-block layered dolomite limestone" ], [ "Drogo Cave Group", "Lithology", "Marlite" ], [ "Drogo Cave Group", "Lithology", "Dolomite" ], [ "Drogo Cave Group", "Lithology", "shale" ], [ "Drogo Cave Group", "Lithology", "Limestone" ], [ "Drogo Cave Group", "Paleontological", "Brachiopod" ], [ "Drogo Cave Group", "Paleontological", "Coral bivalves" ], [ "Drogo Cave Group", "Paleontological", "Laminar worm" ], [ "Drogo Cave Group", "Paleontological", "Teeth thorn" ], [ "Drogo Cave Group", "Paleontological", "Flute tube coral" ], [ "Drogo Cave Group", "Integration of contacts", "Early Carboniferous World Wuqingna Formation" ], [ "Drogo Cave Group", "Integration of contacts", "Ding Zonglong Group" ] ] }, { "text": "Light gray calcium slate with dark gray thin layer of limestone 75m", "triple_list": [ [ "Light gray calcium slate with dark gray thin layer of limestone", "thickness", "75m" ] ] }, { "text": "Brachiopod Zdimir is a fossil of the Yangmaba Formation in the early stages of the Devonian period in Jiangyou, Sichuan Province. It appears at the bottom of the Ding Zonglong Formation in the Nizadian period.", "triple_list": [ [ "Brachiopod Zdimir", "Belongs to", "Yangmaba Formation in the Early Devons of Jiangyou, Sichuan" ], [ "Brachiopod Zdimir", "Exposed", "Niza Ding Zonglong Group" ] ] }, { "text": "The quartz schist fault contacts the overlying strata, the late Triassic Kung Yelan Formation of limestone.", "triple_list": [ [ "Quartz schist", "Fault contact", "The Late Triassic Gong also formed limestone" ] ] }, { "text": "Brachiopods Emanuella tawanensis, Schizophoria cf. excellens, Desquamatia (Desquamatia) peshiensis, Independatrypa interruptta, Pseudoatrypa guanwushanensis, P. cf. baiguopingensis, P. maramensis, Atrypa richthofeni, Schizophoria ütsingensis, S. striatula, Zdimir sp.", "triple_list": [ [ "Enjoy the profile", "Paleontological", "Brachiopod Emanuella tawanensis" ], [ "Enjoy the profile", "Paleontological", "Schizophoria cf. excellens" ], [ "Enjoy the profile", "Paleontological", "Desquamatia (Desquamatia) peshiensis" ], [ "Enjoy the profile", "Paleontological", "Independatrypa interrupta" ], [ "Enjoy the profile", "Paleontological", "Pseudoatrypa guanwushanensis" ], [ "Enjoy the profile", "Paleontological", "P. cf. baiguopingensis" ], [ "Enjoy the profile", "Paleontological", "P. maramensis" ], [ "Enjoy the profile", "Paleontological", "Atrypa richthofeni" ], [ "Enjoy the profile", "Paleontological", "Schizophoria ütsingensis" ], [ "Enjoy the profile", "Paleontological", "S. striatula" ], [ "Enjoy the profile", "Paleontological", "Zdimir sp." ] ] }, { "text": "Accompanied by them are coral abulophyllum sp., Penecialla sp., Placocoenites sp., hamnopora sp., Brachiopod Spinatrypa sp., Undispirifer sp., algae Devoncalculus sp., Katavella sp., Leiospheridia sp., and other early-late Devonian molecules.", "triple_list": [ [ "coral abulophyllum sp.", "Age", "Early Divon World - Late Divon World" ], [ "Penecialla sp.", "Age", "Early Divon World - Late Divon World" ], [ "Placocoenites sp.", "Age", "Early Divon World - Late Divon World" ], [ "hamnopora sp.", "Age", "Early Divon World - Late Divon World" ], [ "Brachiopod Spinatrypa sp.", "Age", "Early Divon World - Late Divon World" ], [ "Undispirifer sp.", "Age", "Early Divon World - Late Divon World" ], [ "algae Devoncalculus sp.", "Age", "Early Divon World - Late Divon World" ], [ "Katavella sp.", "Age", "Early Divon World - Late Divon World" ], [ "Leiospheridia sp.", "Age", "Early Divon World - Late Divon World" ] ] }, { "text": "The lithology of the Senza Formation is gray-green alteration, basalt alteration, basalt green curtain sunrise, green mud schist green mud sodium perchist, and gray-dark gray serous quartz schist quartz thousand rock crystal limestone biolimestone, etc.", "triple_list": [ [ "Senza Group", "Lithology", "Gray-green alteration medium-basic tuff" ], [ "Senza Group", "Lithology", "Alteration basalt" ], [ "Senza Group", "Lithology", "Green curtain sun schist" ], [ "Senza Group", "Lithology", "Yangqi green mud schist" ], [ "Senza Group", "Lithology", "Green mud sodium perchillus" ], [ "Senza Group", "Lithology", "Grey-dark gray serous quartz schist" ], [ "Senza Group", "Lithology", "Quartz thousand rocks" ], [ "Senza Group", "Lithology", "Crystalline limestone" ], [ "Senza Group", "Lithology", "Biolimestone" ] ] }, { "text": "The Ningduoyan Group era was placed in the ancient-midoproterozoic period.", "triple_list": [ [ "Ningduoyan Group", "Age", "Ancient - Middle Proterozoic" ] ] }, { "text": "The era of Youxi Group was placed in the Neoproterozoic period.", "triple_list": [ [ "Youxi Group", "Age", "Neoproterozoic" ] ] }, { "text": "Light gray green clay slate 124.33m", "triple_list": [ [ "Light gray green clay slate", "thickness", "124.33m" ] ] }, { "text": "The Machara Formation (C1m) is distributed in the southwest of Nangqian County and the Baqu-Jingyu area in the central and western part of Changdu County. The Machara-Gondayong area is generally distributed in the northwest-south east direction, with a total exposed area of about 1064.6m2.", "triple_list": [ [ "Machara Group", "Exposed", "Southwest of Nangqian County" ], [ "Machara Group", "Exposed", "Baqu-Jiangsu, Central and Western Band of Changdu County" ], [ "Machara Group", "Exposed", "Machara-Gonda Chung" ], [ "Machara Group", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Machara Group", "area", "1064.6m2" ] ] }, { "text": "Gray-green green mud sericin thousand rock silt sandy green mud sericin thousand rock interlayer, 56.91m", "triple_list": [ [ "Gray green green mud sericin thousand rocks silt sandy green mud sericin thousand rocks interlayer", "thickness", "56.91m" ] ] }, { "text": "Light gray calcium slate 40m", "triple_list": [ [ "Light gray calcium slab", "thickness", "40m" ] ] }, { "text": "The Nujiangyan Formation in the Late Paleozoic Period (Pz2n.) in this area is part of the Jiayuqiao Rock Group (Pz2J.), distributed in the southwest corner of Changdu County with an area of 34.6m2.", "triple_list": [ [ "Nujiangyan Formation in Late Paleozoic", "Belongs to", "Jiayuqiao Rock Group" ], [ "Nujiangyan Formation in Late Paleozoic", "Exposed", "The southwest corner of Changdu County" ], [ "Nujiangyan Formation in Late Paleozoic", "area", "34.6m2" ] ] }, { "text": "Dark gray thick block layered black cloud oblique length gneiss silicified black cloud oblique length gneiss quartz granular rock 250.0m", "triple_list": [ [ "Dark gray thick-block layered black clouds oblique elongated gneiss silicified black clouds oblique elongated gneiss quartz granular rock", "thickness", "250.0m" ] ] }, { "text": "Jitang rock group (Pt1-2J.) is distributed in this area at 1:25 Wanchangdu County. It is distributed in the same area as the pyrolysis ring-Nahuo-Muda-Niza-Wa, and is spread in the northwest-south eastward direction. It is a medium-deep metamorphic rock system composed of gneiss metamorphic rock schist (flake) marble, etc., with an exposed area of about 533.87m2.", "triple_list": [ [ "Jitang Rock Group", "Exposed", "Changdu County pyrolysis lane - that guy - Muda - Niza - Watong" ], [ "Jitang Rock Group", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Jitang Rock Group", "Lithology", "Gneis" ], [ "Jitang Rock Group", "Lithology", "Granular rock" ], [ "Jitang Rock Group", "Lithology", "Inclined long angle flash (flake) rock" ], [ "Jitang Rock Group", "Lithology", "Rock Schist" ], [ "Jitang Rock Group", "Lithology", "Dali Rock" ], [ "Jitang Rock Group", "area", "533.87m2" ] ] }, { "text": "Early Devonshi Dorje Edition Group (D1dj) Middle Devonshi Senza Group (D2s) Late Devonshi Donla Group (D3d) was exposed in 1:25 Wanjiangda County Bengguo-Gucai Village-Senza-Eila Township.", "triple_list": [ [ "Early Devonshi Doji Edition Group", "Exposed", "Jiangda County Bengzhuangguo-Gucai Village-Senza-Eila Township" ], [ "Zhongdevon Shisenza Group", "Exposed", "Jiangda County Bengzhuangguo-Gucai Village-Senza-Eila Township" ], [ "Late Devons Donra Group", "Exposed", "Jiangda County Bengzhuangguo-Gucai Village-Senza-Eila Township" ] ] }, { "text": "Light gray-white thin-medium-layered marble 2m", "triple_list": [ [ "Light gray-white thin-medium-layered marble", "thickness", "2m" ] ] }, { "text": "Ningduoyan Group (Pt1-2Nd.) in the Chamdo-Mangkang Stratigraphic Zone and the Jiangda-Deqin Stratigraphic Zone.", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Ningduoyan Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Ningduoyan Group" ] ] }, { "text": "Gray white medium to thick layered calcified mussel quartz schist quartz schist quartz schist schist 227.6m", "triple_list": [ [ "Off-white medium to thick layered calcified mussel quartz schist quartz schist quartz schist schist schist schist schist schist schist metamorphic quartz silts sandstone green mussel schist", "thickness", "227.6m" ] ] }, { "text": "Dark gray thick-block layered black cloud oblique elongated gneiss with two cloud oblique elongated gneiss 225.0m", "triple_list": [ [ "Dark gray thick-block layered black cloud oblique elongated gneiss with two cloud oblique elongated gneiss", "thickness", "225.0m" ] ] }, { "text": "Dark gray thick layered mica quartz sandstone with black slate, not seen, 376m thick", "triple_list": [ [ "Dark gray thick layered mica quartz sandstone with black slate", "thickness", "376m" ] ] }, { "text": "Light gray dolomite sodium longschist with the same color medium metamorphic feldspar quartz coarse sandstone 185.28m", "triple_list": [ [ "Light gray dolomite sodium longschist with the same color medium metamorphic feldspar quartz coarse sandstone", "thickness", "185.28m" ] ] }, { "text": "Ria Zenong Group (C1r.) fake thickness 1625m", "triple_list": [ [ "Ria Zenong Group", "thickness", "1625m" ] ] }, { "text": "The Ding Zonglong Formation (D2d) and the Late Drogo Cave Formation (D3z∧) in the Early Devon Shi Haitong Formation (D1h) in the Chamdo-Mangkang Formation (D1h).", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Early Devon Shihaitong Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Ding Zonglong Group of Zhongdian" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Late Devon Drogo Cave Group" ] ] }, { "text": "Purple-red, gray-green slate interlayer 55m", "triple_list": [ [ "Purple-red, gray-green slate interlayer", "thickness", "55m" ] ] }, { "text": "Early Carboniferous Wuqingna Formation══════ Fault Contact ═══════ Limestone of Early Carboniferous Wuqingna Formation", "triple_list": [ [ "Early Carboniferous World Wuqingna Formation", "Fault contact", "Limestone of Wuqingna Formation in the Early Carboniferous" ] ] }, { "text": "Purple-red mudstone, 5.8m", "triple_list": [ [ "Purple-red mudstone", "thickness", "5.8m" ] ] }, { "text": "Light gray gray medium-thick layered black cloud translucent grey rock Golden cloud translucent marble and light gray white silicidic quartz shallow grey-grained rock interlayer 232.0m", "triple_list": [ [ "Light gray gray medium-thick layered black cloud translucent grey rock Golden cloud translucent marble and light gray-white silicidic quartz shallow grey-grained rock interlayer", "thickness", "232.0m" ] ] }, { "text": "The Early Devonshi Doji Band Formation (D1dj) Middle Devonshi Senza Formation (D2s) Late Devonshi Donra Formation (D3d) in Jiangda-Deqin stratigraphic zone.", "triple_list": [ [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Early Devonshi Doji Edition Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Zhongdevon Shisenza Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Late Devons Donra Group" ] ] }, { "text": "Dark gray black clouds oblique length gneiss black clouds granite gneiss clamps dark gray oblique length gneiss 143m", "triple_list": [ [ "Dark gray black clouds oblique elongated gneiss black clouds granite gneiss clamps dark gray oblique elongated radics", "thickness", "143m" ] ] }, { "text": "Light gray light green green mud green curtain sodium longschill dolomite sodium longschill sandwiched dark gray medium layer fine-grained crystalline limestone and amylin crystalline limestone 114.00m", "triple_list": [ [ "Light gray light green green mud green curtain sodium longschill dolom sodium longschill sandwiched dark gray medium-layer medium-grained crystalline limestone and amylin crystalline limestone", "thickness", "114.00m" ] ] }, { "text": "In the Mupu Wangge area, there is mainly a set of oblique length gneiss schist marble, etc., which produces residual bodies.", "triple_list": [ [ "Mupu Wangge", "Lithology", "Gneiss" ], [ "Mupu Wangge", "Lithology", "Rock Schist" ], [ "Mupu Wangge", "Lithology", "Dali Rock" ] ] }, { "text": "Gray-green serous green mud schist 100m", "triple_list": [ [ "Gray-green serous green mud schist", "thickness", "100m" ] ] }, { "text": "Gray black clouds potassium long granite gneiss black clouds granite gneiss two long clouds two long long gneiss black clouds oblique long gneiss two long granite shallow grain rocks; late Triassic second granite (η3) invasion and damage, 165m", "triple_list": [ [ "Gray black clouds Potassium long granite gneiss black clouds Granite gneiss two long clouds two long long long granite gneiss black clouds oblique gneiss two long granite rock shallow grain rock", "Invade", "Late Triassic Granite" ], [ "Gray black clouds Potassium long granite gneiss black clouds Granite gneiss two long clouds two long long long granite gneiss black clouds oblique gneiss two long granite rock shallow grain rock", "thickness", "165m" ] ] }, { "text": "Gray thick layered metamorphic ferrous quartz sandstone 43.8m", "triple_list": [ [ "Gray thick layered metamorphic ferrous quartz sandstone", "thickness", "43.8m" ] ] }, { "text": "Ningduoyan Group is mainly a set of black clouds, slant elongated gneiss two clouds, slant elongated gneiss quartz granite rocks slant elongated granite rocks black clouds two long gneiss black clouds slant elongated granite rocks slant elongated granite rocks golden clouds translucent marble black clouds translucent granite rocks, etc., among which new invasion bodies invade.", "triple_list": [ [ "Ningduoyan Group", "Exposed", "Lado Township has more summer days" ], [ "Ningduoyan Group", "Lithology", "Black clouds oblique gneis" ], [ "Ningduoyan Group", "Lithology", "Eryun oblique length gneis" ], [ "Ningduoyan Group", "Lithology", "Black cloud quartz granular rock" ], [ "Ningduoyan Group", "Lithology", "slant-length grain rock" ], [ "Ningduoyan Group", "Lithology", "Black clouds and grain rock" ], [ "Ningduoyan Group", "Lithology", "Black Cloud Two Long Ginsels" ], [ "Ningduoyan Group", "Lithology", "Black cloud slant quartz schist" ], [ "Ningduoyan Group", "Lithology", "Black clouds slanted long grain rock" ], [ "Ningduoyan Group", "Lithology", "Jinyun Transparent Marble Rock" ], [ "Ningduoyan Group", "Lithology", "Black cloud translucent grain rock" ], [ "Ningduoyan Group", "Invade", "Invasive body" ] ] }, { "text": "The Devonian strata of the Jiangda-Deqin strata are well developed, from old to new, there are early Devon Shidoji Bang Formation (D1dj), middle Devon Shisenza Formation (D2s), late Devon Shidolla Formation (D3d).", "triple_list": [ [ "Jiangda-Deqin Stratigraphic Zone", "Contained", "Devonian" ], [ "Devonian", "Outcrop", "Early Devonshi Doji Edition Group" ], [ "Devonian", "Outcrop", "Zhongdevon Shisenza Group" ], [ "Devonian", "Outcrop", "Late Devons Donra Group" ] ] }, { "text": "Light gray - grayish white blocky stripes eyeball vein-shaped black cloud granite gneiss clamped oblique elongated schist grey black block oblique elongated amphibian gneiss angle schist grey black block oblique elongated amphibian gneiss angle schist greystone, 661m", "triple_list": [ [ "Light gray-white blocky stripes eyeball vein-shaped black cloud granite gneiss clamped oblique elongated schist grey black block oblique elongated amphibian oblique elongated schist gneiss angle dichotomy grey", "thickness", "661m" ] ] }, { "text": "Gray dark gray medium-thick layer to block layered black clouds oblique length gneiss mixed with black clouds oblique feld quartz schist black cloud oblique length granular rock 511.6m", "triple_list": [ [ "Gray dark gray medium-thick layer to block layered black clouds oblique length gneiss intersecting black clouds oblique feld quartz schist black cloud oblique length granular rock", "thickness", "511.6m" ] ] }, { "text": "Light gray striped dolomite sodium schist 188.66m", "triple_list": [ [ "Light gray striped dolomite sodium perchlid", "thickness", "188.66m" ] ] }, { "text": "Off-white mica sodium feldquartz schist with mica green mud sodium feldschist 211m", "triple_list": [ [ "Off-white mica sodium feldquartz schist with mica green mud sodium feldschist", "thickness", "211m" ] ] }, { "text": "The Youxi group in this area is a set of low-green schist facies-high-green schist facies metamorphic rock systems. The rock combinations include dimoschist sodium long-gemoschist greemoschist greemoschist greemoschist greemoschist greemoschist greemoschist greemoschist greemoschist greemoschist , etc. The construction of the original rock may be a set of sedimentary rocks with acidic volcanic rocks and tuffs.", "triple_list": [ [ "Youxi Group", "Belongs to", "Low-green schist facies-high-green schist facies metamorphic rock system" ], [ "Youxi Group", "Lithology", "quartz schist" ], [ "Youxi Group", "Lithology", "Sodium 2-millichrys" ], [ "Youxi Group", "Lithology", "Green mud sodium perchillus" ], [ "Youxi Group", "Lithology", "Green mud sodium feld quartz schist" ], [ "Youxi Group", "Lithology", "Eryunschist" ], [ "Youxi Group", "Lithology", "Sedimentary rock" ], [ "Youxi Group", "Lithology", "Medium acidic volcanic rocks" ], [ "Youxi Group", "Lithology", "Basic volcanic rocks" ], [ "Youxi Group", "Lithology", "Tuff" ] ] }, { "text": "Black purple-red gray-green slate 31m", "triple_list": [ [ "Black purple gray green slate", "thickness", "31m" ] ] }, { "text": "The algae in the limestone in the central region, Lophosphaeridium cf. citrinum, Renalcis papilla, was in the early Ordovician period.", "triple_list": [ [ "Limestone", "Paleontological", "algae Lophosphaeridium cf. citrinum" ], [ "Limestone", "Paleontological", "Renalcis papilla" ], [ "Limestone", "Age", "Early Ordovician Shining State" ] ] }, { "text": "Gray clay slate 84.69m", "triple_list": [ [ "Gray clay slab", "thickness", "84.69m" ] ] }, { "text": "The Donla Formation contains plant fragments, brachiopod bivalve sea lily and other fossils; the upper part is the acidic layer of tuff breccia tuff and light gray altered acidic volcanic rock rhyolite.", "triple_list": [ [ "Donla Group", "Paleontological", "Brachiopod" ], [ "Donla Group", "Paleontological", "Bivalves" ], [ "Donla Group", "Paleontological", "sea lily" ], [ "Donla Group", "Paleontological", "Gray thick layer of acidic tuff" ], [ "Donla Group", "Paleontological", "breccia tuff" ], [ "Donla Group", "Paleontological", "Light gray altered acidic volcanic rock" ], [ "Donla Group", "Paleontological", "Rhyolite" ] ] }, { "text": "Gray-white black cloud granite granite granite, 510m invaded by late Triassic 2-chang granite", "triple_list": [ [ "Gray white black cloud granite granite mylonite", "Invade", "Late Triassic Granite" ], [ "Gray white black cloud granite granite mylonite", "thickness", "510m" ] ] }, { "text": "In the Ningdu area of Xiaosumang Township, it is mainly a set of mica quartz flakes gneiss plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria pyroxene granite rock containing garnet plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria plagiaria", "triple_list": [ [ "Xiao Sumang Xiangningduo", "Lithology", "Mica Quartz Ginsel" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Mica diagonal gneis" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Chlorite quartz schist" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Eryun oblique length gneis" ], [ "Xiao Sumang Xiangningduo", "Lithology", "quartz schist" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Black cloud quartz gneiss" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Black clouds oblique gneis" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Pyroxene Granular Rock" ], [ "Xiao Sumang Xiangningduo", "Lithology", "Garnet black cloud oblique length gneiss" ] ] }, { "text": "Light gray thin to medium-layer green mud mud mud mud mud mud mud sericin mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud", "triple_list": [ [ "Light gray thin to medium-layer green mud mud mud mud mud mud mud mud sericin mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud", "thickness", "323.5m" ] ] }, { "text": "Gray gray-white angle flashing oblique gneiss puppet with black cloud oblique gneiss 204m", "triple_list": [ [ "Gray gray-white angled slant gneiss juxtapose black cloud slant gneiss", "thickness", "204m" ] ] }, { "text": "In 1982, Fu Gongqin and others were renamed Jiayuqiao Group, which were divided into Nujiang Formation (Nujiang Schister Formation) and Xiarongqu Formation from top to bottom. Only the Nujiang Rock Formation part was exposed in this area.", "triple_list": [ [ "Jiayu Bridge Group", "Outcrop", "Nujiang Group" ], [ "Jiayu Bridge Group", "Outcrop", "Nujiang Schist Formation" ], [ "Jiayu Bridge Group", "Outcrop", "Blind robe group" ], [ "Jiayu Bridge Group", "Outcrop", "Nujiangyan Formation" ] ] }, { "text": "Gray thick layer of blocky limestone with thin layer of limestone and marl 13.7m", "triple_list": [ [ "Gray thick layer of blocky limestone with thin layer of limestone and marl", "thickness", "13.7m" ] ] }, { "text": "Gray-black mud-sandy limestone and quartz sandstone mud-sandy shale, containing brachiopod Gigantoproductus sp. Echinoco nchuselengans Antiquatonia antiquatonis A. serenensis; coral Lithostrotion petalaxoideaSyringopora sp.; sea lily stem Cyclocyclicus suni, 447.4m", "triple_list": [ [ "Gray-black mud sandy limestone and quartz sandstone mud sandy shale shale", "Paleontological", "Brachiopod Gigantoproductus sp. Echinoco nchuselengans Antiquatonia antiquatonis A. serenensis" ], [ "Gray-black mud sandy limestone and quartz sandstone mud sandy shale shale", "Paleontological", "Coral Lithostrotion petalaxoideaSyringopora sp." ], [ "Gray-black mud sandy limestone and quartz sandstone mud sandy shale shale", "Paleontological", "Sea lily stem Cyclocyclicus suni" ], [ "Gray-black mud sandy limestone and quartz sandstone mud sandy shale shale", "thickness", "447.4m" ] ] }, { "text": "Light gray striped dolomite schist 212.37m", "triple_list": [ [ "Light gray striped dolomite schist", "thickness", "212.37m" ] ] }, { "text": "The actual test profile of the Early Ordovician World Qingnidong Group (O1q) in Qingnidong Township, Jiangda County, Tibet was measured and tested by the Sichuan Provincial Geological and Mineral Engineering Bureau District Transmission Team in 1986 at 1:200,000 Luolong Changdu area area.", "triple_list": [ [ "Qingnidong Township, Jiangda County, Tibet", "Contained", "Early Ordovician Qingni Cave Group" ] ] }, { "text": "Light green gray gray gray white thick-block layer metamorphic quartz mixed sandstone-light gray serous thousand rock silty sand serous thousand rock, 251.31m", "triple_list": [ [ "Light green gray gray gray white thick-block layer metamorphic quartz mixed sandstone-light gray sericin thousand rock silty sand sericin thousand rock", "thickness", "251.31m" ] ] }, { "text": "Gray dark gray middle layer bioclass limestone and black gray thin plate-like carbon-containing calcium shale rhythm interlayer, producing brachiopod Gigantopoductus sp. Neospirifer cf. orientalis and sea lily stems, 70.52m", "triple_list": [ [ "Gray dark gray middle layer biological clastic limestone and black gray thin plate-shaped carbon-containing calcium shale rhythm interlayer", "Paleontological", "Brachiopod Gigantopoductus sp. Neospirifer cf. orientalis" ], [ "Gray dark gray middle layer biological clastic limestone and black gray thin plate-shaped carbon-containing calcium shale rhythm interlayer", "Paleontological", "Sea lily stem" ], [ "Gray dark gray middle layer biological clastic limestone and black gray thin plate-shaped carbon-containing calcium shale rhythm interlayer", "thickness", "70.52m" ] ] }, { "text": "Gray thin to medium-layered medium-coarse crystal marble 164.8m", "triple_list": [ [ "Gray thin to medium-layered medium-coarse crystal marble", "thickness", "164.8m" ] ] }, { "text": "Ningduoyan Group (Pt1-2Nd.) is distributed in the area of 1:25,000 Nangqian County, the Dongfangda-Ningduo area; 1:25,000 Changdu County, the Goukuanda-Summer Duo area; 1:25,000 Jiangda County, the exposed area is about 483m2, and it consists of a set of medium-deep metamorphic gneiss schist and marble.", "triple_list": [ [ "Ningduoyan Group", "Exposed", "Nangqian County Winter House-Ningduo" ], [ "Ningduoyan Group", "Exposed", "Changdu County has a lot of money - many summers" ], [ "Ningduoyan Group", "Exposed", "Jiangda County Bingmupu-Wang Ge" ], [ "Ningduoyan Group", "area", "483m2" ], [ "Ningduoyan Group", "Lithology", "Gneis" ], [ "Ningduoyan Group", "Lithology", "Granular rock" ], [ "Ningduoyan Group", "Lithology", "Rock Schist" ], [ "Ningduoyan Group", "Lithology", "Dali Rock" ] ] }, { "text": "Light gray gray layered black cloud oblique gneiss 211.0m", "triple_list": [ [ "Light gray grey layered black cloud oblique gneis", "thickness", "211.0m" ] ] }, { "text": "Gray dark gray medium-thick layered block black cloud oblique length gneiss mixed with black cloud oblique length granular rock 162.0m", "triple_list": [ [ "Gray dark gray medium-thick layered block black cloud oblique length gneiss mixed with black cloud oblique length granular rock", "thickness", "162.0m" ] ] }, { "text": "Light green and gray sericinous thousand rock silty sericinous thousand rock and medium-thick layer of metamorphic quartz sandstone are not equally thick interlayered, 105.01m", "triple_list": [ [ "Light green and gray sericite thousand rock silty sericite thousand rock and medium-thick layer of metamorphic quartz sandstone are interlayered with different thicknesses", "thickness", "105.01m" ] ] }, { "text": "The upper dark gray blocky limestone, produced coral Argutastrea jiwozhaiensisSociophyllum sp.", "triple_list": [ [ "Dark gray blocky limestone", "Paleontological", "Coral Argutastrea jiwozhaiensisSociophyllum sp." ] ] }, { "text": "Gray thick layer of blocky limestone 21.2m", "triple_list": [ [ "Gray thick layer of blocky limestone", "thickness", "21.2m" ] ] }, { "text": "The purple-red conglomerate sandstone of the late Triassic Jiapila Formation of the overlying formation is unconsistent. Ningduoyan Group (Pt1-2Nd.), with a false thickness of 2602.6m", "triple_list": [ [ "Late Triassic Jiapila Formation Purple-red Conglomerate Sandstone", "Unconformity contact", "Ningduoyan Group" ], [ "Ningduoyan Group", "thickness", "2602.6m" ] ] }, { "text": "Gray white flesh-red gravel quartz sandstone gravel and quartz sandstone, 2.9m", "triple_list": [ [ "Gray white flesh-red gravel quartz sandstone gravel and quartz sandstone", "thickness", "2.9m" ] ] }, { "text": "Gray-green thick layer metamorphic feldspar quartz sandstone metamorphic gravel-containing quartz sandstone 83.55m", "triple_list": [ [ "Gray-green thick layer metamorphic feldspar quartz sandstone metamorphic gravel-containing quartz sandstone", "thickness", "83.55m" ] ] }, { "text": "The early Carboniferous Dongque Formation (C1d) and the late Carboniferous Wangguo Formation (C1w) in the Jiangda-Deqin strata area have a total exposed area of 1612.3m2.", "triple_list": [ [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "The Dongque Group of the Early Carboniferous World" ], [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Late Carboniferous World Wangguo Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "area", "1612.3m2" ] ] }, { "text": "The independatrypa interruptta and coral emnophyllum sp. that were accompanied by it appeared in the Ding Zonglong group.", "triple_list": [ [ "Independatrypa interrupta", "Exposed", "Ding Zonglong Group" ], [ "coral emnophyllum sp.", "Exposed", "Ding Zonglong Group" ] ] }, { "text": "The Riazenang Rock Formation is distributed in the Riazenang area of Gangzi Township, Leiwuqi County, this district. It is a tectonic rock formation mainly composed of basic volcanic rocks, and is distributed in the North Lancang River junction belt in tectonic blocks.", "triple_list": [ [ "Riazenongyan Formation", "Exposed", "Riazelan, Gangzi Township, Leiwuqi County" ], [ "Riazenongyan Formation", "Lithology", "Basic volcanic rocks" ], [ "Riazenongyan Formation", "Distribution pattern", "Constructed block" ], [ "Riazenongyan Formation", "Earth tectonic location", "Northern Lancang River Combination Belt" ] ] }, { "text": "Light gray striped dolomite sodium schist 215.40m", "triple_list": [ [ "Light gray striped dolomite sodium perchlid", "thickness", "215.40m" ] ] }, { "text": "Gray block layered shallow metamorphic medium-fine-grained quartz sandstone, 46.33m ═════ Fault contact ════════ purplish quartz sandstone in the Dongdu Formation of Late Triassic", "triple_list": [ [ "Gray block layered shallow metamorphic medium-fine-grained quartz sandstone", "thickness", "46.33m" ], [ "Gray block layered shallow metamorphic medium-fine-grained quartz sandstone", "Fault contact", "The East-End Group of the Late Triassic" ], [ "The East-End Group of the Late Triassic", "Lithology", "Purple-red quartz sandstone" ] ] }, { "text": "Light gray-green fine-grained silt sandy clay slate 83.78m", "triple_list": [ [ "Light gray-green fine-grained silt clay slate", "thickness", "83.78m" ] ] }, { "text": "The Carboniferous strata in the Beilancang River strata zone include the Early Carboniferous Azenangyan Formation (C1r.) Kagonyan Formation (C1.).", "triple_list": [ [ "Carboniferous period of the Northern Lancang River Stratigraphic Zone", "Outcrop", "Azenongyan Formation in the Early Carboniferous Day" ], [ "Carboniferous period of the Northern Lancang River Stratigraphic Zone", "Outcrop", "Kagon Rock Formation" ] ] }, { "text": "Lower dark gray thin-layer strip-like limestone with shaping 9.5m", "triple_list": [ [ "Dark gray thin striped limestone", "Develop", "Corrugated stratigraphy" ], [ "Dark gray thin striped limestone", "thickness", "9.5m" ] ] }, { "text": "The most exposed area in Qingnidong, Jiangda County is 1:25 million. There are a small number of Drogodong Group (D3z∧) exposed to the west of Tuoba Township, with an area of 83m2.", "triple_list": [ [ "Bingqingni Cave in Jiangda County", "Outcrop", "Drogo Cave Group" ], [ "To the west of Tuoba Township", "Outcrop", "Drogo Cave Group" ], [ "Drogo Cave Group", "area", "83m2" ] ] }, { "text": "Off-white green mud dolomite quartz schist shattered silicated dolomite quartz schist, not seen, 197m", "triple_list": [ [ "Off-white green mud docile quartz schist fragmentation silicated docile quartz schist", "thickness", "197m" ] ] }, { "text": "Light gray striped dolomite sodium feldquartz schist 342.24m", "triple_list": [ [ "Light gray striped dolomite sodium feldquartz schist", "thickness", "342.24m" ] ] }, { "text": "Gray light gray medium-thick layer containing muddy powder crystal dolomite, containing coral and brachiopod fragments, 47.48m", "triple_list": [ [ "Gray light gray medium-thick layer containing mud powder crystal dolomite", "Paleontological", "coral" ], [ "Gray light gray medium-thick layer containing mud powder crystal dolomite", "Paleontological", "Brachiopod" ], [ "Gray light gray medium-thick layer containing mud powder crystal dolomite", "thickness", "47.48m" ] ] }, { "text": "Black thin layer crystal limestone with a small amount of gray-green metamorphic sandstone 15m", "triple_list": [ [ "Black thin layer of crystalline limestone with a small amount of gray-green metamorphic sandstone", "thickness", "15m" ] ] }, { "text": "The Carboniferous strata of the Chamdo-Mangkang strata are well developed, with early Carboniferous Wuqingna Formation (C1w), Machala Formation (C1m), and late Carboniferous Shiaoqu Formation (C2a).", "triple_list": [ [ "Carboniferous period of Chamdo-Mangkang stratigraphic zone", "Outcrop", "Early Carboniferous World Wuqingna Formation" ], [ "Carboniferous period of Chamdo-Mangkang stratigraphic zone", "Outcrop", "Machara Group" ], [ "Carboniferous period of Chamdo-Mangkang stratigraphic zone", "Outcrop", "Late Carboniferous World Aoqu Group" ] ] }, { "text": "The strata distribution area in this area is about 45085m2, and 112 main sections are collected and reviewed.", "triple_list": [ [ "This area", "area", "45085m2" ] ] }, { "text": "Dark gray serous quartz schist 100m", "triple_list": [ [ "Dark gray serous quartz schist", "thickness", "100m" ] ] }, { "text": "The actual test profile of Ding Zonglong Group (D2d) Drogo Dong Group (D3zˆ) in Jueong Village, Qingnidong Township, Jiangda County, Tibet was measured in 1986 by Zhang Zhenggui et al. of Chengdu Institute of Geology and Mineral Engineering and other departments, and this project was appropriately revised in 2006.", "triple_list": [ [ "Jueyong Village, Qingnidong Township, Jiangda County, Tibet", "Outcrop", "Devonian Haitong Formation" ], [ "Jueyong Village, Qingnidong Township, Jiangda County, Tibet", "Outcrop", "Ding Zonglong Group" ], [ "Jueyong Village, Qingnidong Township, Jiangda County, Tibet", "Outcrop", "Drogo Cave Group" ] ] }, { "text": "Light gray clay slate 143.70m", "triple_list": [ [ "Light gray clay slab", "thickness", "143.70m" ] ] }, { "text": "The Kagonite Formation is a set of gray, purple, green, gray, sericite, and metamorphic sandstone. Light, gray, metamorphic sandstone and dark, gray, green, stratigraphic bodies are occasionally seen with sand-clad limestone. The fracture folds are developed, small and orderly and large disorderly. It is a tectonic strata with a thickness of 1585m.", "triple_list": [ [ "Kagon Rock Formation", "Lithology", "Gray purple purple green gray serous clouds thousands of rocks" ], [ "Kagon Rock Formation", "Lithology", "Metamorphic Sandstone" ], [ "Kagon Rock Formation", "Lithology", "Light gray metamorphic sandstone" ], [ "Kagon Rock Formation", "Lithology", "Dark gray-green thousand rocks" ], [ "Kagon Rock Formation", "Lithology", "Sand chip limestone" ], [ "Kagon Rock Formation", "Develop", "fracture" ], [ "Kagon Rock Formation", "Develop", "Wrinkles" ], [ "Kagon Rock Formation", "thickness", "1585m" ] ] }, { "text": "Light gray middle layer serous quartz 174.41m", "triple_list": [ [ "Light gray middle layer serous quartz thousand rocks", "thickness", "174.41m" ] ] }, { "text": "In the area of Sangka-Laiba-Chalai Village, the Caoqu Group is a set of gray-green medium-basic volcanic rock crystalline limestone horned diffraction marble metamorphic conglomerate, metamorphic quartz sandstone transformed sandstone slate mica schist, and other combinations. The original rock is built with a set of coarse clastic rock fine clastic rock clay rock and medium-basic volcanic rock carbonate.", "triple_list": [ [ "Sangka-Laiba-Chalai Village", "Contained", "Caoqu Group" ], [ "Caoqu Group", "Lithology", "Gray-green mesobasic volcanic rocks" ], [ "Caoqu Group", "Lithology", "Crystalline limestone" ], [ "Caoqu Group", "Lithology", "horned schist" ], [ "Caoqu Group", "Lithology", "Dali Rock" ], [ "Caoqu Group", "Lithology", "Metamorphic gravel" ], [ "Caoqu Group", "Lithology", "Metamorphic quartz sandstone" ], [ "Caoqu Group", "Lithology", "Silty sandstone" ], [ "Caoqu Group", "Lithology", "Slate" ], [ "Caoqu Group", "Lithology", "Mica schist" ], [ "Caoqu Group", "Lithology", "Coarse clastic rock" ], [ "Caoqu Group", "Lithology", "Fine clastic rock" ], [ "Caoqu Group", "Lithology", "Clay rock" ], [ "Caoqu Group", "Lithology", "Mesoplasmic volcanic rocks" ], [ "Caoqu Group", "Lithology", "Carbonate rock" ] ] }, { "text": "Gray dicloss sodium schist diclossar diclossar and feldquartz schist, with a small amount of diclossar and mica schist, no bottom was seen, 325m", "triple_list": [ [ "Gray dicloss sodium schist diclossars and feldquartz schist", "thickness", "325m" ] ] }, { "text": "Dark gray green mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud feldschill 253m", "triple_list": [ [ "Dark gray green mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mu", "thickness", "253m" ] ] }, { "text": "The Qingnidong Group is distributed in the area of Fangshanggese Village-Reyong Village-Belt and Jueong Village-Qingnidong Township-Maidong Village, with an exposed area of about 563m2.", "triple_list": [ [ "Qingni Cave Group", "Exposed", "Jiangda County Fengshanggese Village-Reyong Village" ], [ "Qingni Cave Group", "Exposed", "Jueong Village-Qingnidong Township-Maidong Village" ], [ "Qingni Cave Group", "area", "563m2" ] ] }, { "text": "The tooth-shaped prick Polygnathus varcus is one of the fossils of the late Middle Devonian period.", "triple_list": [ [ "Polygnathus varcus", "Age", "Late Middle Devonian" ] ] }, { "text": "Gray-green green mud sericin thousand rock silt sandy green mud sericin thousand rocks thick-block layer metamorphic quartz mixed sandstone, 218.94m", "triple_list": [ [ "Gray-green green mud sericin thousand rock silt sandy green mud sericin thousand rocks intersected with thick-block metamorphic quartz mixed sandstone", "thickness", "218.94m" ] ] }, { "text": "Gray thick layer of blocky sand chip limestone and microcrystalline limestone 25.2m", "triple_list": [ [ "Gray thick layer of blocky sand chip limestone and microcrystalline limestone", "thickness", "25.2m" ] ] }, { "text": "The Machara Formation has a rich paleobiome with many species, including brachiopod coral plant bryozoa radioworm bivalves, foraminifera sea lily and algae, especially coral brachiopods.", "triple_list": [ [ "Machara Group", "Paleontological", "Brachiopod" ], [ "Machara Group", "Paleontological", "coral" ], [ "Machara Group", "Paleontological", "Snake plant" ], [ "Machara Group", "Paleontological", "Bruceworm" ], [ "Machara Group", "Paleontological", "Radioworms" ], [ "Machara Group", "Paleontological", "Bivalves" ], [ "Machara Group", "Paleontological", "Foraminifera" ], [ "Machara Group", "Paleontological", "sea lily" ], [ "Machara Group", "Paleontological", "Ancient algae" ], [ "Machara Group", "Paleontological", "coral" ], [ "Machara Group", "Paleontological", "Brachiopod" ] ] }, { "text": "Gray-black thin layer of crystalline limestone, 10m", "triple_list": [ [ "Gray-black thin layer of crystalline limestone", "thickness", "10m" ] ] }, { "text": "Limestone of the Aoqu Formation overlying strata ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Aoqu Formation Limestone", "Integration of contacts", "Wuqingna Group" ], [ "Aoqu Formation Limestone", "thickness", "790.4m" ] ] }, { "text": "Gray-black middle layer—block limestone, with flint strips, 88.6m", "triple_list": [ [ "Gray-black middle layer—block limestone", "Contained", "Flint strip" ], [ "Gray-black middle layer—block limestone", "thickness", "88.6m" ] ] }, { "text": "Dark gray medium-thin layered gravel-containing green mud schist 138.32m", "triple_list": [ [ "Dark gray medium-thin layered gravel-containing green mud schist", "thickness", "138.32m" ] ] }, { "text": "Jiapila Formation (3j) purple-red sandstone mudstone ═════ Fault contact ═══════ Youxi Formation ((Pt3Y)) thickness 1575m", "triple_list": [ [ "Kapila Group", "Lithology", "Purple-red sandstone mudstone" ], [ "Kapila Group", "Fault contact", "Youxi Group" ], [ "Kapila Group", "thickness", "1575m" ] ] }, { "text": "Metamorphic gravel-containing quartz sandstone with gravel-containing green mud schist serous 682.88m", "triple_list": [ [ "Metamorphic gravel-containing quartz sandstone with gravel-containing green mud schist serous green mud schist", "thickness", "682.88m" ] ] }, { "text": "In 1993, 1:200,000 Wuqibian Ladopa was divided into the Juetong group (D1j), Haitong group (D1h), Dzonglong group (D2d), Drogo cave group (D3z∧).", "triple_list": [ [ "Lewuqi Lado", "Outcrop", "Jue-entering group" ], [ "Lewuqi Lado", "Outcrop", "Haitong Group" ], [ "Lewuqi Lado", "Outcrop", "Ding Zonglong Group" ], [ "Lewuqi Lado", "Outcrop", "Drogo Cave Group" ] ] }, { "text": "Gray dark gray thick layer with thin layer of limestone biolimestone and black flint strips, foraminifera Ampipora sp.; tooth thorns Polygnathus varcus, P. xylusIcriodus aff. brevis, 24.8m", "triple_list": [ [ "Gray dark gray thick layer with thin layer of limestone biolimestone with black flint strips", "Paleontological", "Foraminifera Ampipora sp." ], [ "Gray dark gray thick layer with thin layer of limestone biolimestone with black flint strips", "Paleontological", "Tooth thorn Polygnathus varcus" ], [ "Gray dark gray thick layer with thin layer of limestone biolimestone with black flint strips", "Paleontological", "P. xylusIcriodus aff. brevis" ], [ "Gray dark gray thick layer with thin layer of limestone biolimestone with black flint strips", "thickness", "24.8m" ] ] }, { "text": "Green gray dark gray serous thousand-metre rock silty green mud serous thousand-metre rock and gray light green gray metamorphic quartz sandstone rock cuts quartz mixed sandstone interlayer, 135.31m", "triple_list": [ [ "Green gray dark gray serous Qianmei rock silt green mud serous Qianmei rock and gray light green gray metamorphic quartz sandstone rock cuttings quartz mixed sandstone interlayer", "thickness", "135.31m" ] ] }, { "text": "In 1992, the Nujiang-Lancang River-Jinsha River region was classified as the Former Carboniferous System (AnC).", "triple_list": [ [ "Nujiang-Lancang River-Jinsha River Regional Stratigraphy", "Belongs to", "Former Carboniferous" ] ] }, { "text": "Jitang Rock Group (Pt1-2J.) fake thickness 3299m", "triple_list": [ [ "Jitang Rock Group", "thickness", "3299m" ] ] }, { "text": "The above characteristics show that the Riazenangyan Formation belongs to a deep-sea environment.", "triple_list": [ [ "Riazenongyan Formation", "Belongs to", "Deep sea environment" ] ] }, { "text": "The overlying strata of Wuqingna Formation Quartz Sandstone ─────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Wuqingna Formation Quartz Sandstone", "Integration of contacts", "Drogo Cave Group" ], [ "Wuqingna Formation Quartz Sandstone", "thickness", "37.1m" ] ] }, { "text": "Light gray medium to thick layered green mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud schist sodium mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud", "triple_list": [ [ "Light gray medium to thick layered green mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud schist sodium mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud mud", "thickness", "282.3m" ] ] }, { "text": "Gray medium-thick layered shallow metamorphic medium-fine-grained quartz sandstone 101.58m", "triple_list": [ [ "Gray medium-thick layered shallow metamorphic medium-fine-grained quartz sandstone", "thickness", "101.58m" ] ] }, { "text": "The Machala Formation (C1m) of the Early Carboniferous Sea Wuqingna Formation (C1w) and the Late Carboniferous Sea Aoqu Formation (C2a) in the Chamdo-Mangkang Formation.", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Early Carboniferous World Wuqingna Formation" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Machara Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Late Carboniferous World Aoqu Group" ] ] }, { "text": "Gray dark gray blocky black cloud oblique length gneiss 260.0m", "triple_list": [ [ "Grey dark gray blocky black cloud oblique length gneis", "thickness", "260.0m" ] ] }, { "text": "Light gray striped sodium schist 53.37m", "triple_list": [ [ "Light gray striped sodium perchlid", "thickness", "53.37m" ] ] }, { "text": "Gray black clouds granite gneiss sandwich dark grey oblique long angle flash schist angle flash black cloud oblique long grain rock 60m", "triple_list": [ [ "Gray black clouds granite gneiss sandwich dark grey oblique long angle schist angular angular black cloud oblique long grain rock", "thickness", "60m" ] ] }, { "text": "Gray green - dark gray green green mud mud mud docuso sodium schist 419m", "triple_list": [ [ "Gray-green-dark gray-green green mud dolomite sodium perchillus", "thickness", "419m" ] ] }, { "text": "Zeng Ziding Group (Oz), thickness 717.07m", "triple_list": [ [ "Zeng Ziding Group", "thickness", "717.07m" ] ] }, { "text": "Light gray thin-sheet sericite quartz 327.00m ──────────────────Senza Formation (D2s), 830.57m thick", "triple_list": [ [ "Light gray thin-sheet-sheet-shaped serous quartz thousand rocks", "thickness", "327.00m" ], [ "Light gray thin-sheet-sheet-shaped serous quartz thousand rocks", "Integration of contacts", "Senza Group" ], [ "Senza Group", "thickness", "830.57m" ] ] }, { "text": "The Riazenangyan Formation and the Kagonyan Formation (C1.) fault are in contact with the tectonic blocks and are distributed in the North Lancang River junction. The main lithologies are gray-green, dark green, gray block-shaped flakes, physical and chemical basic volcanic rocks, mylonite, basic volcanic rocks, and dark gray serous slate light green, gray thick blocks, and physical and chemical quartz mixed sandstone, with a thickness greater than 1625m.", "triple_list": [ [ "Riazenongyan Formation", "Fault contact", "Kagon Rock Formation" ], [ "Riazenongyan Formation", "Distribution pattern", "Constructed block" ], [ "Riazenongyan Formation", "Earth tectonic location", "Northern Lancang River Combination Belt" ], [ "Riazenongyan Formation", "Lithology", "Physical and chemical basic volcanic rocks in gray green dark green gray blocks" ], [ "Riazenongyan Formation", "Lithology", "Mylonite-based volcanic rock" ], [ "Riazenongyan Formation", "Lithology", "Dark gray serous slate" ], [ "Riazenongyan Formation", "Lithology", "Light green gray thick-blocked quartz sandstone" ], [ "Riazenongyan Formation", "thickness", "1625m" ] ] }, { "text": "Gray-black block layered oblique elongated amphibole dark gray-green thick layer square horned amphibole schist with light gray-thin color-middle-layered quartz schist 74m", "triple_list": [ [ "Gray-black block layered oblique elongated amphibole dark gray-green thick-layer square-column horned amphibole interspersed with light gray-thin-middle-dimoss quartz schist", "thickness", "74m" ] ] }, { "text": "Brachiopods Cyrtospirifer sp., Pseudoatrpa sp., Caryorhynchus nana, Atrypa richthofeni, A. interruptta; coral Pseudozaphrentis minor, Paraamphipora zhougodongensis, Hexagonaria sp.; dentate prickly prickly Polygnathus xylus, Icriodus aff. brevis; Amphipora sp., et al.", "triple_list": [ [ "Qingni Cave Encounter Section", "Contained", "Drogo Cave Group" ], [ "Drogo Cave Group", "Paleontological", "Brachiopod Cytospirifer sp." ], [ "Drogo Cave Group", "Paleontological", "Pseudoatrpa sp." ], [ "Drogo Cave Group", "Paleontological", "Caryorhynchus nana" ], [ "Drogo Cave Group", "Paleontological", "Atrypa richthofeni" ], [ "Drogo Cave Group", "Paleontological", "A. interrupta" ], [ "Drogo Cave Group", "Paleontological", "Coral Pseudozaphrentis minor" ], [ "Drogo Cave Group", "Paleontological", "Paraamphipora zhougodonggensis" ], [ "Drogo Cave Group", "Paleontological", "Hexagonaria sp." ], [ "Drogo Cave Group", "Paleontological", "Tooth thorn Polygnathus xylus" ], [ "Drogo Cave Group", "Paleontological", "Icriodus aff. brevis" ], [ "Drogo Cave Group", "Paleontological", "Foraminifera Amphipora sp." ] ] }, { "text": "Dark gray blocky black cloud oblique elongated gneiss with a little thick layered black cloud oblique elongated gneiss and black cloud granular rock 233.0m", "triple_list": [ [ "Dark gray blocky black clouds oblique elongated gneiss with a little thick layered black cloud oblique elongated gneiss and black cloud granular rock", "thickness", "233.0m" ] ] }, { "text": "Green magnet mineralized schist 11m", "triple_list": [ [ "Green magnet mineralized schist", "thickness", "11m" ] ] }, { "text": "In the Sangzhi Akao area in Yushu County, Qinghai Province, the Dongla Formation is a set of gray fine-grained quartz sandstone calcareous slate limestone combinations, mainly sandstone and secondly slate. The limestone is produced in an interlayer, and belongs to the coast-shallow sea transition environment sedimentation.", "triple_list": [ [ "Sangzhi Akao, Yushu County, Qinghai Province", "Contained", "Donla Group" ], [ "Donla Group", "Lithology", "Gray fine-grained quartz sandstone" ], [ "Donla Group", "Lithology", "Calcium slate" ], [ "Donla Group", "Lithology", "Limestone" ], [ "Donla Group", "Lithology", "sandstone" ], [ "Donla Group", "Lithology", "Slate" ], [ "Donla Group", "Lithology", "Limestone" ], [ "Donla Group", "Belongs to", "Coastal-shallow sea transitional environment sedimentation" ] ] }, { "text": "The central part of Qingnidong Formation is characterized by limestone-mixed mud shale sandstone, and the bottom is a thin layer of black dark gray limestone, and crawling insects are seen on the level in a curved shape.", "triple_list": [ [ "Qingni Cave Group", "Lithology", "Limestone" ], [ "Qingni Cave Group", "Lithology", "Mud shale" ], [ "Qingni Cave Group", "Lithology", "sandstone" ], [ "Qingni Cave Group", "Lithology", "Thin layer of black dark grey limestone" ] ] }, { "text": "Black slate and thin layer of mud crystalline limestone interlayer 26m", "triple_list": [ [ "Black slate and thin layers of mud crystalline limestone interlayer", "thickness", "26m" ] ] }, { "text": "Light gray medium-thick layered quartz sandstone and gray calcareous slate interlayer thin layer of limestone, 160m", "triple_list": [ [ "Light gray medium-thick layered quartz sandstone and gray calcareous slate interlayer thin layer of limestone", "thickness", "160m" ] ] }, { "text": "There are also a small number of Drogo Cave Group (D3zˆ) exposed to the east of Bingxiaya Village, Changdu County at 1:25,000, with an exposed area of about 2m2.", "triple_list": [ [ "East of Fangxiaya Village, Changdu County", "Outcrop", "Drogo Cave Group" ], [ "Drogo Cave Group", "area", "2m2" ] ] }, { "text": "The survey area is located in the eastern part of the Qinghai-Tibet Plateau, with geographical coordinates of 96°00′97°30′English longitude, 31°00′33°00′North latitude (Nangqian County area Changdu County area), 97°30′99°00′English longitude, 31°00′32°00′North latitude (Jiangda County area), with a total area of about 47975m2.", "triple_list": [ [ "Test area", "Located at", "Eastern Qinghai-Tibet Plateau" ], [ "Test area", "Coordinates", "96°00′97°30′" ], [ "Test area", "Coordinates", "31°00′33°00′" ], [ "Test area", "Coordinates", "97°30′99°00′" ], [ "Test area", "Coordinates", "31°00′32°00′" ], [ "Test area", "area", "47975m2" ] ] }, { "text": "Yellow-gray thick layer of limestone with dark gray medium-layer biological clastic limestone 4.5m ────────────────────────────Doji Edition Group (D1dj), total thickness 139.2m", "triple_list": [ [ "Yellow-gray thick layer of limestone with dark gray medium-layer bioclad limestone", "thickness", "4.5m" ], [ "Yellow-gray thick layer of limestone with dark gray medium-layer bioclad limestone", "Integration of contacts", "Doji version group" ], [ "Doji version group", "thickness", "139.2m" ] ] }, { "text": "Brachiopod Cyrtospirif sp. is an important fossil of the Shetian Bridge Step in Hunan, my country, and is also commonly found in the Tuqiaozi Group and Shawozi Group of the Late Diwan Mountain in Longmen Mountain, Sichuan.", "triple_list": [ [ "Brachiopod Cytospirifer sp.", "Belongs to", "Shetian Bridge Steps in Hunan" ], [ "Brachiopod Cytospirifer sp.", "Exposed", "Sichuan Longmen Mountain Late Divon Shi Tuqiaozi Group" ], [ "Brachiopod Cytospirifer sp.", "Exposed", "Shawozi Group" ] ] }, { "text": "Gray block black cloud oblique long grain rock light gray block layered cross pomegranate quartz schist sandwiched gray-white medium-thick layer potassium feld quartz shallow grain rock 202m", "triple_list": [ [ "Gray blocky black cloud oblique length granular rock light gray block layered cross pomegranate quartz schist with gray-white medium-thick layer of potassium feld quartz shallow granular rock", "thickness", "202m" ] ] }, { "text": "Light gray striped dolomite schist and light gray striped dolomite schist are interlayered with different thicknesses of 1028.50m", "triple_list": [ [ "Light gray striped dolomite schist and light gray striped dolomite schist are interlayered with different thicknesses", "thickness", "1028.50m" ] ] }, { "text": "Ding Zonglong Formation is distributed in the area north of Jueong Village, Qingnidong Township, Jiangda County. It is composed of gray limestone thin-layered marl limestone coral reef-like dolomite and light gray-red quartz sandstone shale. It is 149,344m thick. It is in integrated contact with the Fudojiban Formation of the Overly Overlapping Drogodong Formation. It contains rich benthic organisms such as foraminiferous bivalves and gastropods, and other fossils such as mesophobia. Its rock formation unit characteristics are relatively stable throughout the region.", "triple_list": [ [ "Ding Zonglong Group", "Exposed", "The area north of Jueong Village, Qingnidong Township, Jiangda County" ], [ "Ding Zonglong Group", "Lithology", "Gray limestone" ], [ "Ding Zonglong Group", "Lithology", "Thin-layer tumor-like marl" ], [ "Ding Zonglong Group", "Lithology", "Coral reef-like dolomite" ], [ "Ding Zonglong Group", "Lithology", "Light gray light red quartz sandstone" ], [ "Ding Zonglong Group", "Lithology", "shale" ], [ "Ding Zonglong Group", "thickness", "149344m" ], [ "Ding Zonglong Group", "Integration of contacts", "Drogo Cave Group" ], [ "Ding Zonglong Group", "Integration of contacts", "Doji version group" ], [ "Ding Zonglong Group", "Paleontological", "Brachiopod" ], [ "Ding Zonglong Group", "Paleontological", "Coral layer" ], [ "Ding Zonglong Group", "Paleontological", "Foraminifera" ], [ "Ding Zonglong Group", "Paleontological", "Bivalves" ], [ "Ding Zonglong Group", "Paleontological", "Gastropod" ], [ "Ding Zonglong Group", "Paleontological", "Aphrodisiac" ] ] }, { "text": "Light gray white cloud sodium feldquartz schist 63.16m", "triple_list": [ [ "Light gray white cloud sodium feld quartz schist", "thickness", "63.16m" ] ] }, { "text": "Gray purple purple gray green mud sericin thousand rock silt sandy green mud sericin thousand rock, 81.57m", "triple_list": [ [ "Gray purple purple gray green mud sericin thousand rocks silt sandy green mud sericin thousand rocks", "thickness", "81.57m" ] ] }, { "text": "Gray medium-thick layer with thin layer of limestone 12.0m", "triple_list": [ [ "Gray medium-thick layer of thin layer of limestone", "thickness", "12.0m" ] ] }, { "text": "Therefore, the era of the Senza Group was classified as the Zhongdivon era.", "triple_list": [ [ "Senza Group", "Age", "Zhongdivonshi" ] ] }, { "text": "Light gray striped dolomite sodium longschist with striped dolomite feldquartz schist 293.50m", "triple_list": [ [ "Light gray striped dolomite sodium schist intersected striped dolomite sodium feldquartz schist", "thickness", "293.50m" ] ] }, { "text": "Light green gray diyun sodium longschilli mica sodium longschilli 159m", "triple_list": [ [ "Light green gray diyun sodium elongated schist mica sodium elongated schist", "thickness", "159m" ] ] }, { "text": "As early as 1959, Li Pu and others named the Jiayuqiao metamorphic rock system. Because no fossils were obtained, their era was classified as the Paleozoic era of the Precambrian Period (AnЄ-Pz1).", "triple_list": [ [ "Jiayuqiao metamorphic rock system", "Age", "Precambrian Paleozoic" ] ] }, { "text": "Gray medium-layered shallow metamorphic medium-fine-grained quartz sandstone with dark gray clay slate 95.41m", "triple_list": [ [ "Gray medium-layered shallow metamorphic medium-fine-grained quartz sandstone with dark gray clay slate", "thickness", "95.41m" ] ] }, { "text": "This project conducted a route geological survey on the Gangse Township-Requjitang rock group. The main lithologies are a set of gray, light gray gray-white angular angular slash black clouds plagiarism long gneiss plagiarism long gneiss angular slash black clouds plagiarism long gneiss 2 clouds plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss plagiarism long gneiss schist plagiarism long gneiss marble, etc.", "triple_list": [ [ "Gangse Township-Requjitang Rock Group", "Lithology", "Gray light gray gray white angular flash black cloud oblique length gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Eryun oblique length gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Black cloud horn flashing long gneiss" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Two clouds and two long gneiss" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Neck flash black cloud two long gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Glitter giraffe" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Silicon-containing two cloud oblique length gneiss" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Black Cloud Two Long Ginsels" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Two long gneisses containing pomegranate silicone" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Pomegranate mixed two-length gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Mixed two-length gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Silicone-containing pomegranate mixed two-length gneiss" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Neck flash black cloud oblique length gneis" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "oblique angular amphibole" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Granite gneiss" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "feldspar quartz schist" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "slanted quartz schist" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Black cloud quartz schist" ], [ "Gangse Township-Requjitang Rock Group", "Lithology", "Dali Rock" ] ] }, { "text": "Among them, the coral Pseudozaphrentis minor is a representative molecule in the early stage of the Late Devonian period.", "triple_list": [ [ "Coral Pseudozaphrentis minor", "Age", "Early Late Divonian" ] ] }, { "text": "The Administrative area of the test area is affiliated to Chaya County, Gongjue County, Jiangda County, Jiangda County, Jiangxi County, Leiwuqi County, Dingqing County, Tibet Autonomous Region.", "triple_list": [ [ "Test area", "Administrative area", "Dingqing County, Tibet Autonomous Region" ], [ "Test area", "Administrative area", "Leiwuqi County" ], [ "Test area", "Administrative area", "Luolong County" ], [ "Test area", "Administrative area", "Changdu County" ], [ "Test area", "Administrative area", "Jiangda County" ], [ "Test area", "Administrative area", "Gongjue County" ], [ "Test area", "Administrative area", "Chaya County" ] ] }, { "text": "Off-white weathered brown yellow mica quartz gneiss 50m", "triple_list": [ [ "Off-white weathered brown yellow mica quartz gneis", "thickness", "50m" ] ] }, { "text": "Light gray-green light gray dolomite sodium elongated schist sodium elongated tremolite schist intersected with dark gray medium-layer muddy crystalline limestone 174.36m ───────────────────────────Doji Pan Formation (D1dj) thickness 3427.66m", "triple_list": [ [ "Light gray-green light gray dolomite sodium elongated schist sodium elongated tremolite schist intersected with dark gray medium amid crystalline limestone", "thickness", "174.36m" ], [ "Light gray-green light gray dolomite sodium elongated schist sodium elongated tremolite schist intersected with dark gray medium amid crystalline limestone", "Integration of contacts", "Doji version group" ], [ "Doji version group", "thickness", "3427.66m" ] ] }, { "text": "The Jiayuqiao Rock Group era was placed in the late Paleozoic era.", "triple_list": [ [ "Jiayuqiao Rock Group", "Age", "Late Paleozoic" ] ] }, { "text": "Gray purple purple green gray sericin thousand rock sandy silt sandy green mud sericin thousand rocks intersected with thin layer of metamorphic calcium fine-grained quartz mixed sandstone, not seen, 118.25m", "triple_list": [ [ "Gray purple purple green gray sericin thousand rock sandy green mud sericin thousand rocks intersected with thin layer metamorphic calcium fine-grained quartz mixed sandstone", "thickness", "118.25m" ] ] }, { "text": "The Kagonite Formation (C1.) consists of a set of dark clastic rocks with shallow metamorphism, strong deformation, single lithology, and sparse fossils, mixed with lithostone and volcanic rocks. It is thicker than 1739m and is distributed in 1:25 Wanchangdu County. It is divided into a broken block in the northwest-south-east direction, with an area of 118.8m2, which may be deep-sea sediments in the North Lancang River junction.", "triple_list": [ [ "Kagon Rock Formation", "Lithology", "Clastite" ], [ "Kagon Rock Formation", "Lithology", "Limestone" ], [ "Kagon Rock Formation", "Lithology", "Volcanic rocks" ], [ "Kagon Rock Formation", "thickness", "1739m" ], [ "Kagon Rock Formation", "Exposed", "Changdu County Fenri Azenong-Majun Nong-Matsu-Taxilie-Natura" ], [ "Kagon Rock Formation", "Distribution pattern", "Distributed intermittently to the northwest-south eastward direction of the broken clamp" ], [ "Kagon Rock Formation", "area", "118.8m2" ], [ "Kagon Rock Formation", "Belongs to", "Deep-sea sediments in the Northern Lancang River Belt" ] ] }, { "text": "Grass Qun (Pt3C) thickness 3520.92m", "triple_list": [ [ "Caoqu Group", "thickness", "3520.92m" ] ] }, { "text": "In 1974, 1:1 million Chamdo's first Dignorant system was classified as the Downtown Group (D1h), Djonglong Group (D2d), Drogodong Group (D3z∧) from bottom to top.", "triple_list": [ [ "Chamdo", "Contained", "Mud pot system" ], [ "Mud pot system", "Outcrop", "Haitong Group" ], [ "Mud pot system", "Outcrop", "Ding Zonglong Group" ], [ "Mud pot system", "Outcrop", "Drogo Cave Group" ] ] }, { "text": "Light gray serous quartz thousand rocks with the same color medium-metamorphic feldspar quartz sandstone 99.66m", "triple_list": [ [ "Light gray serous quartz 100 rocks with the same color medium-metamorphic feldspar quartz sandstone", "thickness", "99.66m" ] ] }, { "text": "Light gray striped dolomite sodium feldquartz schist 114.18m", "triple_list": [ [ "Light gray striped dolomite sodium feldquartz schist", "thickness", "114.18m" ] ] }, { "text": "The lower purple-gray thick quartz sandstone is interspersed with thin sandstone and fine conglomerate 7.8m.", "triple_list": [ [ "Purple-gray thick quartz sandstone with thin sandstone and fine gravel rock", "thickness", "7.8m" ] ] }, { "text": "In 1986, the 1200,000 Luolong frame Changdu frame was adopted by the Early Ordovician Shiqing Nikong Formation, and it has been used to this day.", "triple_list": [ [ "Luolong Cangdu Cloth", "Contained", "Early Ordovician Qingni Cave Group" ] ] }, { "text": "Gray block-thick layer of limestone sees flint nodules and lens body 14.0m", "triple_list": [ [ "Gray block-thick limestone sees chert nodules and lens body", "thickness", "14.0m" ] ] }, { "text": "Light gray striped dolomite schist 167.26m", "triple_list": [ [ "Light gray striped dolomite schist", "thickness", "167.26m" ] ] }, { "text": "Gray dark gray serous quartz slate serous slate and light green gray thick-blocked layered physical and chemical quartz sandstone unequal thickness 531.00m", "triple_list": [ [ "Gray dark gray serous quartz slate serous slate and light green gray thick-blocked layered physical and chemical quartz sandstones are not equally thick and interlayered", "thickness", "531.00m" ] ] }, { "text": "There is the Youxi group (Pt3Y) in the Leiwuqi-Zuogong strata, with an exposed area of about 73.5m2", "triple_list": [ [ "Lewuqi-Zuogong Stratigraphic Division", "Contained", "Youxi Group" ], [ "Lewuqi-Zuogong Stratigraphic Division", "area", "73.5m2" ] ] }, { "text": "The Carboniferous strata in this area include the Azenongyan Formation (C1r.) in the North Lancang River Stratigraphic Zone.", "triple_list": [ [ "Carboniferous period", "Contained", "North Lancang River Stratigraphic Zone" ], [ "North Lancang River Stratigraphic Zone", "Outcrop", "Azenongyan Formation in the Early Carboniferous Day" ], [ "North Lancang River Stratigraphic Zone", "Outcrop", "Kagon Rock Formation" ] ] }, { "text": "The middle-class crystal limestone interlayers of the middle and upper crystalline limestone, fossils such as coral brachiopod algae, are in integrated contact with the overlying strata, and the Dojiban Formation, with a thickness of 830m.", "triple_list": [ [ "Crystalline limestone", "Paleontological", "coral" ], [ "Crystalline limestone", "Paleontological", "Brachiopod" ], [ "Crystalline limestone", "Paleontological", "Algae" ], [ "Crystalline limestone", "Paleontological", "Teeth thorn" ], [ "Crystalline limestone", "Paleontological", "sea lily" ], [ "Crystalline limestone", "Paleontological", "Jellyfish" ], [ "Crystalline limestone", "Integration of contacts", "Donla Group" ], [ "Crystalline limestone", "Integration of contacts", "Doji version group" ], [ "Crystalline limestone", "thickness", "830m" ] ] }, { "text": "Light gray striped dolomite sodium feldquartz schist 14665m", "triple_list": [ [ "Light gray striped dolomite sodium feldquartz schist", "thickness", "14665m" ] ] }, { "text": "Lily lily stem algae and brachiopod fossils in the limestone Contained shallow marine facies, and boreholes are found in some parts.", "triple_list": [ [ "Limestone", "Paleontological", "sea lily" ], [ "Limestone", "Paleontological", "Stem algae" ], [ "Limestone", "Paleontological", "Brachiopod" ], [ "Limestone", "Contained", "drilling" ] ] }, { "text": "Gray oblique long black cloud schist with gray dark gray quartz schist black cloud schist black cloud granite gneiss 69m", "triple_list": [ [ "Gray slanted black cloud schist with gray dark gray quartz schist black cloud schist black cloud granite gneis", "thickness", "69m" ] ] }, { "text": "Gray thick layered quartz sandstone 105m", "triple_list": [ [ "Gray thick layered quartz sandstone with calcified slate", "thickness", "105m" ] ] }, { "text": "The Zengziding Formation is a set of fine-grained quartz sandstone clay slate combinations, mainly clay slate, and fine-grained quartz sandstone.", "triple_list": [ [ "Zeng Ziding Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Zeng Ziding Group", "Lithology", "Clay slate" ], [ "Zeng Ziding Group", "Lithology", "Clay slate" ], [ "Zeng Ziding Group", "Lithology", "Fine-grained quartz sandstone" ] ] }, { "text": "The purple-red conglomerate sandstone in the late Triassic East Du Formation of the overlying formation is unconsistent. The false thickness of Ningduoyan Group (Pt1-2Nd.) is 1950m", "triple_list": [ [ "Late Triassic East Du Formation purple-red conglomerate sandstone", "Unconformity contact", "Ningduoyan Group" ], [ "Late Triassic East Du Formation purple-red conglomerate sandstone", "thickness", "1950m" ] ] }, { "text": "The Nujiang Rock Formation (Pz2n.) of Jiayuqiao Rock Group in this area is a set of metamorphic crust rock combinations, with the main lithologies of quartz schist green mud docusta quartz schist docusta schist pomegranate green mud docusta schist sodium longschist milita schist sodium longschist, etc., with a thickness of 3518m.", "triple_list": [ [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Belongs to", "Metamorphic Case Rock" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "Quartz schist" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "Green mud dolomite quartz schist" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "Mica schist" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "pomegranate green mud dolomite schist" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "Sodium perchlid" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "Lithology", "Mica sodium perchlid" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "thickness", "3518m" ] ] }, { "text": "Light gray striped dolomite sodium schist 46.34m", "triple_list": [ [ "Light gray striped dolomite sodium perchlid", "thickness", "46.34m" ] ] }, { "text": "Gray-black thin-medium-thick layered muddy sandy limestone, containing coral Kueichowpora sp. Zaphrentoides sp., 50.9m", "triple_list": [ [ "Gray-black thin-medium-thick layered muddy sandy limestone", "Paleontological", "Coral Kueichowpora sp." ], [ "Gray-black thin-medium-thick layered muddy sandy limestone", "Paleontological", "Zaphrentoides sp." ], [ "Gray-black thin-medium-thick layered muddy sandy limestone", "thickness", "50.9m" ] ] }, { "text": "In the same level as Longbanglan, Weimin also found the aphrodisiac Samaiella minuteta, Reetobaisdia elleriBairdia naumouae, 9.0m", "triple_list": [ [ "Dragon Help", "Paleontological", "Samaiella minuta" ], [ "Dragon Help", "Paleontological", "Reetobaisdia elleriBairdia naumouae" ], [ "Dragon Help", "thickness", "9.0m" ] ] }, { "text": "Gray-green thin-layer green mud sodium long dolomite schist green mud calcite dolomite schist intersected with mica sodium long schist, no bottoming, 211.7m - Fault contact - Marble crystalline limestone of the Xiarong Quyan Formation", "triple_list": [ [ "Gray-green thin-layer green mud sodium long mica schist green mud calcite docica schist intersected with mica sodium longichoke", "thickness", "211.7m" ], [ "Gray-green thin-layer green mud sodium long mica schist green mud calcite docica schist intersected with mica sodium longichoke", "Fault contact", "Crystal limestone of the marble of the Xiarong Quyan Formation" ] ] }, { "text": "The grass tutu group (Pt3C) in the Jiangda-Deqin stratigraphic area has an exposed area of about 1191m2.", "triple_list": [ [ "Jiangda-Deqin Stratigraphic Zone", "Contained", "Caoqu Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "area", "1191m2" ] ] }, { "text": "The Ordovician Zengziding Formation (Oz) is distributed in the area of the central and eastern part of Nangqian County, 1:25 million. The north side is covered by red clastic rock of the Late Triassic East Du Formation, and some areas on the south side are invaded by Paleocene granite bodies, with an exposed area of about 165m2.", "triple_list": [ [ "Ordovician Zengziding Group", "Exposed", "Jonnyku, central and eastern part of Nangqian County" ], [ "Ordovician Zengziding Group", "Integration of contacts", "Red clastic rock in the late Triassic East Duo Formation" ], [ "Ordovician Zengziding Group", "Invade", "Paleocene granite body" ], [ "Ordovician Zengziding Group", "area", "165m2" ] ] }, { "text": "In 1993, 1:20 million Wuqibian Ladou was divided into three rock groups from bottom to top of the Borisong Duoyan Formation (Ptb) steel group Nongyan Formation (Ptg) Qijiyan Formation (Ptp), and merged into the Jitang Rock Group of Proterozoic.", "triple_list": [ [ "Lewuqi Lado", "Contained", "Borisong Duoyan Formation" ], [ "Lewuqi Lado", "Contained", "Steel Group Rock Formation" ], [ "Lewuqi Lado", "Contained", "Jiyan Formation" ], [ "Lewuqi Lado", "Belongs to", "Jitang Rock Group in Proterozoic" ] ] }, { "text": "Overlapping formation Dongque Formation Bioclastic Limestone ────────────────────────────────────�", "triple_list": [ [ "Dongque Formation Bioclastic Limestone", "Integration of contacts", "Donla Group" ], [ "Dongque Formation Bioclastic Limestone", "thickness", "942m" ] ] }, { "text": "Light gray striped dolomite sodium feldquartz schist 154.89m", "triple_list": [ [ "Light gray striped dolomite sodium feldquartz schist", "thickness", "154.89m" ] ] }, { "text": "Gray green dark green gray block flakes physical and chemical basic volcanic rock alteration basic mylonite 863.00m", "triple_list": [ [ "Physical and chemical basic volcanic rock alteration of basic mylonites", "thickness", "863.00m" ] ] }, { "text": "Gray purple-green gray medium-thick layer metamorphic quartz mixed sandstone and sericite quartz silt sericite silt sandy sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite 110.83m", "triple_list": [ [ "Gray purple-green gray medium-thick layer metamorphic quartz mixed sandstone and sericite quartz thousand rock green mud sericite silt sand sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt sericite silt", "thickness", "110.83m" ] ] }, { "text": "Gray light green gray block layer metamorphic quartz mixed sandstone rocks and gray-green serous silt green mud serous thousand rocks are not equally thick and interlayered, 373.58m", "triple_list": [ [ "Gray light green gray block layer metamorphic quartz mixed sandstone rocks and gray-green serous silt green mud serous thousand rocks are not equally thick interlayered", "thickness", "373.58m" ] ] }, { "text": "Overlapping strata Carboniferous-Permian Russichiro Formation (CPe.)-Fault Contact-Jiayuqiao Rock Formation Nujiang Rock Formation (Pz2n.), with a thickness of 4568.4m.", "triple_list": [ [ "Carboniferous-Permian Russian Rock Formation", "Fault contact", "Nujiangyan Formation of Jiayuqiao Rock Group" ], [ "Nujiangyan Formation of Jiayuqiao Rock Group", "thickness", "4568.4m" ] ] }, { "text": "Caoqu Group (Pt3C) is distributed in 1:25 million areas of Sangka-Laiba-Chalai Village, Nangqian County, and Caoqu-Mose Nong.", "triple_list": [ [ "Caoqu Group", "Exposed", "Sangka-Laiba-Chalai Village, Nangqian County" ], [ "Caoqu Group", "Exposed", "Grass song - what color" ] ] }, { "text": "Overlapping formation Dongque Formation Quarz Sandstone Plywood ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Dongque Formation Quarz Sandstone Plywood", "Integration of contacts", "Donla Group" ], [ "Donla Group", "thickness", "500m" ] ] }, { "text": "The lower slate contains the slate Dichographus spp., Didymogrptus spp., etragraphus sp., Isographus sp., Phyllograptus sp., is the main molecule in the Didymograptus hirundo zone in southern my country, and is a common molecule in the early Ordovician Baowan stage.", "triple_list": [ [ "Slate", "Paleontological", "Bistone Dichographus spp." ], [ "Slate", "Paleontological", "Didymogrptus spp." ], [ "Slate", "Paleontological", "etragraphus sp." ], [ "Slate", "Paleontological", "Isographus sp." ], [ "Slate", "Paleontological", "Phyllograptus sp." ] ] }, { "text": "The Machara Formation is a sea-land interactive coal-based formation composed of gray, dark gray-gray black sandstone slate limestone biological clastic limestone marlstone and sea-closed silica rock coal lines and coal seams, with a thickness of more than 12161690m.", "triple_list": [ [ "Machara Group", "Lithology", "Gray dark gray gray black sandstone" ], [ "Machara Group", "Lithology", "Slate" ], [ "Machara Group", "Lithology", "Limestone" ], [ "Machara Group", "Lithology", "Bioclastic limestone" ], [ "Machara Group", "Lithology", "Marlite" ], [ "Machara Group", "Lithology", "Seacloser-containing silica rock" ], [ "Machara Group", "Lithology", "Coal line and coal layer" ], [ "Machara Group", "Belongs to", "Interactive coal-based strata of sea and land" ], [ "Machara Group", "thickness", "12161690m" ] ] }, { "text": "To sum up the above, the Machara Formation in this area is a sedimentation from the Datang period of the Early Carboniferous Sea to Dewu period.", "triple_list": [ [ "Machara Group", "Age", "Early Carboniferous World Datang Period-Dewu Period" ] ] }, { "text": "Gray yellow-gray medium-thin layer of amygdala limestone is mixed with a small amount of shale, producing rich foraminifera Ampipora sp., A. pervesiculata.", "triple_list": [ [ "Gray yellow-gray medium-thin layer of amygdala limestone with a small amount of shale", "Paleontological", "Foraminifera Ampipora sp." ], [ "Gray yellow-gray medium-thin layer of amygdala limestone with a small amount of shale", "Paleontological", "A.pervesiculata" ] ] }, { "text": "Kagon rock formation, false thickness 1585m", "triple_list": [ [ "Kagon Rock Formation", "thickness", "1585m" ] ] }, { "text": "Gray green black slate with gray thin layer of convex mirror-shaped muddy crystal limestone and a small amount of gray green or yellow metamorphic sandstone 73m", "triple_list": [ [ "Gray green black slate with gray thin layer of convex mirror-shaped muddy crystalline limestone and a small amount of gray green or yellow metamorphic sandstone", "thickness", "73m" ] ] }, { "text": "In the area of Caoqu-Mosenong, Caoqu Group is a set of metamorphic gravel serotonite quartz schist gravel quartz sandstone gravel green mud schist serotonite chromium schist serotonite chromium quartz schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist schist s", "triple_list": [ [ "Grass song - what color", "Outcrop", "Caoqu Group" ], [ "Caoqu Group", "Lithology", "Metamorphic gravel" ], [ "Caoqu Group", "Lithology", "serous quartz schist" ], [ "Caoqu Group", "Lithology", "Gravel-containing quartz sandstone" ], [ "Caoqu Group", "Lithology", "Gravel-containing green mud schist" ], [ "Caoqu Group", "Lithology", "Serous green mud schist" ], [ "Caoqu Group", "Lithology", "sericin quartz schist" ], [ "Caoqu Group", "Lithology", "Slate" ], [ "Caoqu Group", "Lithology", "Metamorphic olive basalt" ], [ "Caoqu Group", "Lithology", "Crystalline limestone" ], [ "Caoqu Group", "Lithology", "Qianmeiyan" ], [ "Caoqu Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "Caoqu Group", "Lithology", "Coarse clastic rock" ], [ "Caoqu Group", "Lithology", "Fine clastic rock" ], [ "Caoqu Group", "Lithology", "Clay rock" ], [ "Caoqu Group", "Lithology", "Mesoplasmic volcanic rocks" ], [ "Caoqu Group", "Lithology", "Carbonate rock" ] ] }, { "text": "The upper yellow-gray marl is sandwiched with calcareous shale and dark gray bioclad limestone, which produces poorly preserved brachiopods and corals, 16.3m", "triple_list": [ [ "Yellow-gray marl limestone with calcified shale and dark-gray bioclastic limestone", "Paleontological", "Brachiopod" ], [ "Yellow-gray marl limestone with calcified shale and dark-gray bioclastic limestone", "Paleontological", "coral" ], [ "Yellow-gray marl limestone with calcified shale and dark-gray bioclastic limestone", "thickness", "16.3m" ] ] }, { "text": "Light gray dolomite schist 239.63m", "triple_list": [ [ "Light grey dolomite schist", "thickness", "239.63m" ] ] }, { "text": "Jitang Rock Group (Pt1-2J.) false thickness 1798m", "triple_list": [ [ "Jitang Rock Group", "thickness", "1798m" ] ] }, { "text": "Light gray grey block layered cross pomegranate dolomite schist pomegranate dimoschist quartz schist with dark green thickness-block layered oblique amphibole oblique amphibole 261m", "triple_list": [ [ "Light gray-gray block layered cross-pomegranate musca schist pomegranate dimoschist quartz schist with dark green thickness-block layered oblique amphibole oblique amphibole oblique amphibole", "thickness", "261m" ] ] }, { "text": "Dark gray medium-thick layered black cloud oblique length gneiss 236.0m", "triple_list": [ [ "Dark gray medium-thick layered black cloud oblique length gneis", "thickness", "236.0m" ] ] }, { "text": "The Wuqingna Formation (C1w) is distributed in the Diga area of Zaduo County, northwest, Tubian, 1:25 million, 1:25 million, 1:30 million, 1:30 million, 1:30 million, 1:30 million, 1:30 million, 1:30 million, 10 million, 10 million, 10 million, 10 million, 10 million, 10 million, 10 million, scattered, with an exposed area of about 52.6m2.", "triple_list": [ [ "Wuqingna Group", "Exposed", "Nangqian County, North West Tubian Zaduo County Diga" ], [ "Wuqingna Group", "Exposed", "Changdu County, southeast map of Biantuoba Wuqingna" ], [ "Wuqingna Group", "Exposed", "Bingqingni Cave in Jiangda County" ], [ "Wuqingna Group", "area", "52.6m2" ] ] }, { "text": "There is the Jitang rock group (Pt1-2J.) in the Leiwuqi-Zuogong strata.", "triple_list": [ [ "Lewuqi-Zuogong Stratigraphic Division", "Contained", "Jitang Rock Group" ] ] }, { "text": "Black thin layer of crystalline limestone with gray-green metamorphic quartz sandstone and a small amount of black slate 46m", "triple_list": [ [ "Black thin layer of crystalline limestone with gray-green metamorphic quartz sandstone and a small amount of black slate", "thickness", "46m" ] ] }, { "text": "The lithologic part of the Dojiban Formation is light gray striped dolomite schist dolomite sodium feldquartz schist dolomite sodium feldquartz schist, and the interlayer is interlayered with a small amount of gray-dark gray lens-like crystal limestone. The strip-like structure is extremely developed, and no biological fossils are found. The lower part is gray-white thick layer of marble with green-gray medium-basic volcanic rocks and serosz schist, with a thickness of 3427m.", "triple_list": [ [ "Doji version group", "Lithology", "Light gray striped dolomite schist" ], [ "Doji version group", "Lithology", "Dolomite Feldquartz Schist" ], [ "Doji version group", "Lithology", "Dolomite Sodium Elongated Rock" ], [ "Doji version group", "Lithology", "Gray-dark gray lens-like crystalline limestone" ], [ "Doji version group", "Develop", "Strip structure" ], [ "Doji version group", "Develop", "Off-white thick layer of marble" ], [ "Doji version group", "Lithology", "Green-gray Medium-basic volcanic rock" ], [ "Doji version group", "Lithology", "serous quartz schist" ], [ "Doji version group", "thickness", "3427m" ] ] }, { "text": "Gray white gray dark gray medium-layer black clouds oblique length gneiss two clouds oblique length gneiss two clouds two long residual porcine gneiss and dark gray green black clouds oblique elongated amphibian two clouds oblique length granular rock two clouds quartz schist 243m", "triple_list": [ [ "Gray white gray dark gray - layered black clouds oblique length gneiss two clouds oblique length gneiss two clouds two long residual porcine gneiss and dark gray green black clouds oblique elongated amphibian two clouds oblique length granular rock two clouds quartz schist", "thickness", "243m" ] ] }, { "text": "From the above section, it can be seen that the lower part of the Qingnidong Formation is a set of variegated sandstone slate, and there are well-preserved fossils of fossils near the Qingnidong.", "triple_list": [ [ "Qingni Cave Group", "Lithology", "Variegated sandstone" ], [ "Qingni Cave Group", "Lithology", "Slate" ], [ "Qingni Cave Group", "Lithology", "Bilite fossil" ] ] }, { "text": "Gray clay slate 37.25m", "triple_list": [ [ "Gray clay slab", "thickness", "37.25m" ] ] }, { "text": "Micro horizontal stratigraphic Develop in slate.", "triple_list": [ [ "Slate", "Develop", "Horizontal stratification" ] ] }, { "text": "Dark gray thin-medium layered limestone 45m", "triple_list": [ [ "Dark gray thin-medium layered limestone", "thickness", "45m" ] ] }, { "text": "Sandstone slate of the Aoqu Formation overlying strata ─────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Sandstone slate of Aoqu Formation", "Integration of contacts", "Machara Group" ], [ "Machara Group", "thickness", "1215.86m" ] ] }, { "text": "There are no fossils found in the Dorjeban Formation in this area, but its integration is under the Senza Formation containing the fossils of the Middle Devonian, so its era is placed in the Early Devonian.", "triple_list": [ [ "Doji version group", "Integration of contacts", "Senza Formation containing Mesode Devonian Fossils" ], [ "Doji version group", "Age", "Early Mudfen World" ] ] }, { "text": "The Haitong Formation is concentrated in the area north of Jueong Village, Qingnidong Township, Jiangda County. It is composed of purple-red, gray, purple-red gravel, gravel-coarse sandstone-mudstone from bottom to top. It is 25212m thick and has red terrestrial sedimentary characteristics. It is angle-inconsistent overlaid on the Qingnidong Formation of the Early Ordovician Shi.", "triple_list": [ [ "Haitong Group", "Exposed", "North of Jueong Village, Qingnidong Township, Jiangda County" ], [ "Haitong Group", "Lithology", "Purple-red grey purple-red gravel rock" ], [ "Haitong Group", "Lithology", "Gravel-containing sandstone" ], [ "Haitong Group", "Lithology", "Gravel-containing coarse sandstone" ], [ "Haitong Group", "Lithology", "Mudstone" ], [ "Haitong Group", "thickness", "25212m" ], [ "Haitong Group", "Unconformity contact", "Early Ordovician Qingni Cave Group" ] ] }, { "text": "Dark gray thin-medium layered slate 15m", "triple_list": [ [ "Dark gray thin-medium layered slab", "thickness", "15m" ] ] }, { "text": "The lithology of Jitang rock group (Pt1-2J.) is black cloud oblique length gneiss black cloud sodium gneiss and a small amount of granite.", "triple_list": [ [ "Jitang Rock Group", "Lithology", "Black clouds oblique gneis" ], [ "Jitang Rock Group", "Lithology", "Black cloud sodium gneiss" ], [ "Jitang Rock Group", "Lithology", "Meatite" ] ] }, { "text": "Overlapping formation Wangbu Formation (J1w) purple-red thick layered complex medium conglomerate intersected with thin medium feldspar sandstone ────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Wang Bu Group", "Lithology", "Purple-red thick layered complex gravel rock" ], [ "Wang Bu Group", "Lithology", "Thin mid-sparish" ], [ "Wang Bu Group", "Lithology", "Chop sandstone" ], [ "Wang Bu Group", "Integration of contacts", "Gala group" ], [ "Gala group", "thickness", "1271.81m" ] ] }, { "text": "Light gray medium-thick layered pyrite-containing cryptocrystalline limestone, produced by brachiopod Cubanothyris copulentus Arcosarina pentagona Sanqiaothyris asymmetrical metros., 50.4m", "triple_list": [ [ "Light gray medium-thick layered pyrite-containing cryptocrystalline limestone", "Paleontological", "Brachiopod Cubanothyris copulentus Arcosarina pentagona Sanqiaothyris asymmetric." ], [ "Light gray medium-thick layered pyrite-containing cryptocrystalline limestone", "thickness", "50.4m" ] ] }, { "text": "The Late Jurassic Sokal Group (J3x) is distributed in the Changdu-Mangkang Stratigraphic Area, Jiaowuguolei, Wuqi County, Jiasangka Township, Changdu County, Jiaosangka Township, Changdu County, Jiaosangka Township, Changdu County, Jiangda-Deqin Stratigraphic Area, with an area of about 798.1m2 in the map.", "triple_list": [ [ "Late Jurassic Solo Card", "Exposed", "Changdu-Mangkang Stratigraphic Zone, Jiaowuguolei, Wuqi County, Jiasangka Township, Changdu County, Langda Ruoran" ], [ "Late Jurassic Solo Card", "Exposed", "Jiangda-Deqin Stratigraphic Area Chakaxi, Jiangda County" ], [ "Late Jurassic Solo Card", "area", "798.1m2" ] ] }, { "text": "The Jiapila Formation in this stratigraphic area consists of purple-red, blue-gray conglomerate gravel sandstone sandstone mudstone, etc. There are few fossils obtained on the profile. Amaryllite plant spore powder is produced on the route, with a total exposed thickness of 638.17m. The angle is not integrated and covered by the cave deck (3d), and is integrated and hidden under the Polila Formation (3b), which is a set of river-marine sand mud clastic rock sedimentation.", "triple_list": [ [ "Kapila Group", "Lithology", "Purple-red, blue-gray gravel rock" ], [ "Kapila Group", "Lithology", "Gravel-containing sandstone" ], [ "Kapila Group", "Lithology", "sandstone" ], [ "Kapila Group", "Lithology", "Mudstone" ], [ "Kapila Group", "Paleontological", "Chrysanthemum" ], [ "Kapila Group", "Paleontological", "Plant spore powder" ], [ "Kapila Group", "thickness", "638.17m" ], [ "Kapila Group", "Unconformity contact", "Hole deck" ], [ "Kapila Group", "Integration of contacts", "Polira group" ], [ "Kapila Group", "Belongs to", "River-Coastal Sand Clarinet Rock Sedimentation" ] ] }, { "text": "The lithology of the grass group (Pt3C) is metamorphic conglomerate-transformed sandstone slate metamorphic volcanic rocks, etc.", "triple_list": [ [ "Caoqu Group", "Lithology", "Metamorphic gravel" ], [ "Caoqu Group", "Lithology", "Sandstone" ], [ "Caoqu Group", "Lithology", "Slate" ], [ "Caoqu Group", "Lithology", "Metamorphic volcanic rocks" ] ] }, { "text": "Mixed siltstone with calcified quartz siltstone, Lepidodendron acutgulum Pecopteris sp. Compsopteris cf. contracta Annularia pingloensis, 29.17m", "triple_list": [ [ "Silty siltstone with calcified quartz siltstone", "Paleontological", "Plant Lepidodendron acutungulum Pecopteris sp." ], [ "Silty siltstone with calcified quartz siltstone", "Paleontological", "Compsopteris cf. contracta Annularia pingloensis" ], [ "Silty siltstone with calcified quartz siltstone", "thickness", "29.17m" ] ] }, { "text": "Gray thick layered gravel-containing unequal feldspar sandstone, 16.11m", "triple_list": [ [ "Gray thick layered gravel-containing feldspar sandstone", "thickness", "16.11m" ] ] }, { "text": "Wang Guo Group (C2w), 453.73m thick", "triple_list": [ [ "Wang Guo Group", "thickness", "453.73m" ] ] }, { "text": "Light purple, gray, green, yellow-brown block layer, medium-grained feldspar quartz sandstone splint and dark gray medium-layer biolimestone, produced by Sphaeroschwa Gerina sp., 116.95m", "triple_list": [ [ "Light purple, gray-green, yellow-brown block layer, medium-coarse feldspar quartz sandstone splint and dark gray medium-layer biolimestone", "Paleontological", "Sphaeroschwa Gerina sp." ], [ "Light purple, gray-green, yellow-brown block layer, medium-coarse feldspar quartz sandstone splint and dark gray medium-layer biolimestone", "thickness", "116.95m" ] ] }, { "text": "Overhead strata Kapila Formation (3j), purple-red conglomerate sandstone Angle unconsolidated Marathon multiple groups (1-2m), thickness 519.47m", "triple_list": [ [ "Kapila Group", "Lithology", "purple conglomerate sandstone" ], [ "purple conglomerate sandstone", "Unconformity contact", "Marathon multiple sets" ], [ "Marathon multiple sets", "thickness", "519.47m" ] ] }, { "text": "Light gray thin-medium-thick layer of crystalline limestone and marble with calcified schist, 418.1m", "triple_list": [ [ "Light gray thin-medium-thick layer of crystalline limestone and marble with calcified schist", "thickness", "418.1m" ] ] }, { "text": "Yingzhu Niang A group thickness 2989.85m", "triple_list": [ [ "Yingzhu Niang group", "thickness", "2989.85m" ] ] }, { "text": "In Tuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Mengrenxiong and other areas, the lithologies are mainly gray limestone 1,000 rocks slate metamorphic sandstone, intersecting siliceous rocks, containing radioworm gastropods Discohelix cf. caliulus, bivalve Chlamys sp. Nipponophycus zennicheloides N. sp., Hiorocodium aff. fertilis, Nautiloculina sp., Lithothamnium sp., Archaeocalothrix sp., Cladodinobryon sp.", "triple_list": [ [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Lithology", "Gray limestone" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Lithology", "Qianmeiyan" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Lithology", "Slate" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Lithology", "Metamorphic Sandstone" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Lithology", "Silicone rock" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Radioworms" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Gastropods Discohelix cf. caliulus" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "bivalve Chlamys sp." ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Ancient algae Nipponophycus zennicheloides N. sp." ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Hiorocodium aff. fertilis" ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Nautiloculina sp." ], [ "Cuoda Village, Leiwuqi County, Tialongxima Village, Xiemaxiong Dingqing County, Luodong Village, Basu County, Guoqing Township, Basu County", "Paleontological", "Lithothamnium sp." ], [ "Gastropods Discohelix cf. caliulus", "Paleontological", "Archaeocalothrix sp." ], [ "Gastropods Discohelix cf. caliulus", "Paleontological", "Cladodinobryon sp." ] ] }, { "text": "The early Triassic Pushuiqiao Formation volcanic rocks are distributed in the central and southern part of Jiangda County, extending to the south to the Gongjue County, with an area of more than 100m2 in the map.", "triple_list": [ [ "Volcanic rocks of Pushuiqiao Formation in the Early Triassic", "Exposed", "1:25 million Jiangda County Central and Southern" ], [ "Volcanic rocks of Pushuiqiao Formation in the Early Triassic", "Exposed", "1:250,000 Gongjue County" ], [ "Volcanic rocks of Pushuiqiao Formation in the Early Triassic", "area", "100m2" ] ] }, { "text": "Purple-red thick layer of gravel-containing tuff coarse sand tuff feldspar crush sandstone, 26m", "triple_list": [ [ "Purple-red thick layer of gravel-containing tuff coarse sand tuff feldspar sandstone", "thickness", "26m" ] ] }, { "text": "The era of the Degaila group was the middle and late triassic period.", "triple_list": [ [ "Gala group", "Age", "Middle-late Triassic" ] ] }, { "text": "The Dingqing Ophiolite Age was set in the Triassic period.", "triple_list": [ [ "Dingqing ophiolite", "Age", "Triassic" ] ] }, { "text": "The Chamdo-Mangkang stratigraphic divisions range from old to new have early Permian Lizha Group (P1l); the Middle Permian Mangcuo Group (P2mc) Jiaoga Group (P2j); the late Permian Tuoba Group (P3t) Xiaya Village Group (Pt3x).", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Early Permian investigation team" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Mid Permian Rumor" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Jiaoga Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Late Permian Tuoba Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Xiaya Village Group" ] ] }, { "text": "Sandstone slate of the Dugala Formation ─────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Sandstone slate of Duogaila Formation", "Integration of contacts", "The Adula Group of the Late Triassic" ], [ "The Adula Group of the Late Triassic", "thickness", "1707.04m" ] ] }, { "text": "Overhead strata Polila Formation limestone ───────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polila Formation Limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "132.2m" ] ] }, { "text": "The Dege-Baiyu Stratigraphic Zone develops in the late Triassic strata, exposed to the area east of the fault of the eastern border of the Jinsha River Belt. It is divided from bottom to top into Qugasi Formation (3q), Tumugou Formation (3t), Lanashan Formation (3l) and Yingzhunianga Formation (3yz).", "triple_list": [ [ "Dege-White Jade Stratigraphic Zone", "Outcrop", "Late Triassic strata" ], [ "Late Triassic strata", "Exposed", "The area east of the eastern border fault of Jinsha River Belt" ], [ "Late Triassic strata", "Outcrop", "Quga Temple Group" ], [ "Late Triassic strata", "Outcrop", "Tumugou Group" ], [ "Late Triassic strata", "Outcrop", "Rana Mountain Group" ], [ "Late Triassic strata", "Outcrop", "Yingzhu Niang group" ] ] }, { "text": "Permian Mangcuo Group limestone in the overlying strata──────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "The Mangcuo Group of the Middle Permian", "Integration of contacts", "Richa Group" ], [ "Richa Group", "thickness", "1206.56m" ] ] }, { "text": "The Kapila Formation (3j) is built for a set of purple-red clastic rocks.", "triple_list": [ [ "Kapila Group", "Belongs to", "Construction of purple clastic rock" ] ] }, { "text": "Gray thick layer thin strip-shaped fine-pink crystal dolomite with gray-white giant thick layered bioclad limestone, producing bivalve Halobia pluriradiata H. cf. cordillerana H. xizangensis, not seen, 50m", "triple_list": [ [ "Gray thick layer thin strip-shaped fine-pink crystal dolomite with gray-white giant thick layered bioclad limestone", "Paleontological", "Bivalve Halobia pluriradiata H. cf. cordillerana H. xizangensis" ], [ "Gray thick layer thin strip-shaped fine-pink crystal dolomite with gray-white giant thick layered bioclad limestone", "thickness", "50m" ] ] }, { "text": "Overhead formation Jiapila Formation purple-red conglomerate sandstone, angle unconsolidated, multiple marathon groups (1-2m), thickness 2272.05m", "triple_list": [ [ "Jiapila Formation Purple-red Conglomerate Sandstone", "Unconformity contact", "Marathon multiple sets" ], [ "Marathon multiple sets", "thickness", "2272.05m" ] ] }, { "text": "Ash-variegated thick layer contains biomud crystal powder crystal limestone, producing serpent Profusulinella sp. Eostaffella postmsquensis; coral Dibunophyllum sp., 75.26m", "triple_list": [ [ "Ash-variant thick layer containing biological mud crystal powder crystal limestone", "Paleontological", "Profusulinella sp. Eostaffella postmsquensis" ], [ "Ash-variant thick layer containing biological mud crystal powder crystal limestone", "Paleontological", "coral Dibunophyllum sp." ], [ "Ash-variant thick layer containing biological mud crystal powder crystal limestone", "thickness", "75.26m" ] ] }, { "text": "Overlapping strata Dongdaqiao Formation (J2d) gray-purple silt sandstone with marlstone ─────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "East Bridge Group", "Lithology", "Gray purple siltstone" ], [ "East Bridge Group", "Lithology", "Marlite" ], [ "East Bridge Group", "Integration of contacts", "Wang Bu Group" ], [ "Wang Bu Group", "thickness", "2583.84m" ] ] }, { "text": "Therefore, the Baitongyan Formation era was placed in the Permian-late Triassic period.", "triple_list": [ [ "Baitongyan Formation", "Age", "Permian-late Triassic" ] ] }, { "text": "Gray-dark gray medium-thick layer of particle crystalline limestone, producing bivalve Eumorphotis sp., 33.98m ───────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Gray-dark gray medium-thick layer of fine particle crystalline limestone", "Paleontological", "bivalve Eumorphotis sp." ], [ "Gray-dark gray medium-thick layer of fine particle crystalline limestone", "thickness", "33.98m" ], [ "Gray-dark gray medium-thick layer of fine particle crystalline limestone", "Integration of contacts", "Dongdu Formation Purple-red Conglomerate Sandstone" ] ] }, { "text": "Nillsonia sp., 283.8m", "triple_list": [ [ "Silty mudstone", "Paleontological", "Plant fossil Nillsonia sp." ], [ "Silty mudstone", "thickness", "283.8m" ] ] }, { "text": "Gray-black medium-thick layered mud slate, producing bivalves Halobia superbescens H. cf. buowinensis H. sp. 177.70m", "triple_list": [ [ "Gray-black medium-thick layered mud slab", "Paleontological", "Bivalves Halobia superbescens H. cf. buowinensis H. sp." ], [ "Gray-black medium-thick layered mud slab", "thickness", "177.70m" ] ] }, { "text": "Sodium long green curtain green mud sun rises from schist gray-green, and the broken particles-spotted structure is granular fibrous columnar metamorphic structure, and directional structure.", "triple_list": [ [ "Sodium long green curtain green mud sun schist", "Distribution pattern", "Crushed particles-spotted structure" ], [ "Sodium long green curtain green mud sun schist", "Distribution pattern", "Granular fibrous columnar metamorphic structure" ], [ "Sodium long green curtain green mud sun schist", "Develop", "Directional construction" ] ] }, { "text": "Overlapping strata Dongdaqiao Formation (J2d) gray-purple siltstone clay rock with marl stone ────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "East Bridge Group", "Lithology", "Gray purple siltstone" ], [ "East Bridge Group", "Lithology", "Clay rock" ], [ "East Bridge Group", "Lithology", "Marlite" ], [ "East Bridge Group", "Integration of contacts", "Wang Bu Group" ], [ "Wang Bu Group", "thickness", "505.7m" ] ] }, { "text": "Sandstone slate of the Walasi Formation ────────────────────Serong Temple Formation (1s), thickness 353.1m", "triple_list": [ [ "Sandstone slate of Wala Monastery", "Integration of contacts", "Serong Temple Group" ], [ "Serong Temple Group", "thickness", "353.1m" ] ] }, { "text": "In the Edu area of Cuodar Village, Leiwuqi County, its lithology is mainly gray-black slate with gray thin-layered grey limestone, containing spore-pollin uberculatsporites sp., Dictyophyllidites sp., Cycadopites sp., Pityosporites sp., Quadradraecullina anellaeformis, Classopollis sp., Cycadopites nitidus.", "triple_list": [ [ "Edu, Cuodar Village, Lewuqi County", "Lithology", "Grey black slate" ], [ "Edu, Cuodar Village, Lewuqi County", "Lithology", "Gray thin layer-middle mud crystal limestone" ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "spore uberculatosporites sp." ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Dictyophyllidites sp." ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Cycadopites sp." ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Pityosporites sp." ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Quadradraecullina anellaeformis" ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Classopollis sp." ], [ "Edu, Cuodar Village, Lewuqi County", "Paleontological", "Cycadopites nitidus" ] ] }, { "text": "Light gray thick layer of osamic limestone and thin layer of sand chips, fine-grained limestone and a small amount of tuff-like gravel limestone, brachiopod Athyris subquadrata; Michelinocevas sp., 147.60m", "triple_list": [ [ "Light gray thick layer of osaite limestone and thin layer of sand chips, fine-grained limestone and a small amount of tuff gravel limestone", "Paleontological", "Brachiopod Athyris subquadrata" ], [ "Light gray thick layer of osaite limestone and thin layer of sand chips, fine-grained limestone and a small amount of tuff gravel limestone", "Paleontological", "Michelinocevas sp." ], [ "Light gray thick layer of osaite limestone and thin layer of sand chips, fine-grained limestone and a small amount of tuff gravel limestone", "thickness", "147.60m" ] ] }, { "text": "Gray sandy limestone, 12.5m", "triple_list": [ [ "Gray sandy limestone", "thickness", "12.5m" ] ] }, { "text": "The late Permian Xiaya Village Group (P3x) is distributed in 1:25,000 Changdu County, Changdu County, Nabao Saikao, Chajinduo-Ompu, and 1:25,000 Jiangda County, Changdu County, Nanxiuma-Chaya County, Gajieka Cow Farm and other areas, with an exposed area of about 38.2m2.", "triple_list": [ [ "Late Permian Xiaya Village Group", "Exposed", "1:250,000 Changdu County, Changdu County, Nabao Scheme, you need to get Zhajinduo - Ompu" ], [ "Late Permian Xiaya Village Group", "Exposed", "1:25 million Jiangda County, Nanxiuma, Changdu County - Gajieka Cow Farm, Chaya County" ], [ "Late Permian Xiaya Village Group", "area", "38.2m2" ] ] }, { "text": "The Middle Jurassic East Bridge Formation (J2d) is widely distributed, exposed in the area of Ama-Renqingka-Kamado Township, Changdu County, 1:25,000, the area north of Bengduo Ri, Jiangna-Jiequ, Lugousha-Jido Township-Laji, Shangka-Yoluo Town-Tongxia Village, Yoba Township-Chaidu Township-Exi Township; 1:25,000, the area north of Bengniangxi Township, Jiangda County, Jiangda County, the area in the map is about 2735.5m2.", "triple_list": [ [ "Middle Jurassic East Bridge Group", "Exposed", "1:250,000 Changdu County, Ama-Renqingka-Kamado Township" ], [ "Middle Jurassic East Bridge Group", "Exposed", "Jiang Na - The Song of the" ], [ "Middle Jurassic East Bridge Group", "Exposed", "Lugousha-Jiduo Township-Laji" ], [ "Middle Jurassic East Bridge Group", "Exposed", "Shangka Township-Oluo Town-Tongxia Village" ], [ "Middle Jurassic East Bridge Group", "Exposed", "Yoba Township-Chaidui Township-Eisi Township" ], [ "Middle Jurassic East Bridge Group", "Exposed", "1:25 million Nangqian County Bengjiangba" ], [ "Middle Jurassic East Bridge Group", "Exposed", "1:25 million north of Bengniangxi Township, Jiangda County" ], [ "Middle Jurassic East Bridge Group", "area", "2735.5m2" ] ] }, { "text": "Richa Group (P1l), thickness 984.63m", "triple_list": [ [ "Richa Group", "thickness", "984.63m" ] ] }, { "text": "The Mesozoic cover layer is composed of the Jiapila Formation (3j), Polila Formation (3b), Adula Formation (3a), Dugail Formation (3d), Wangbu Formation (J1w), Dongdaqiao Formation (J2d), Xiaosoka Formation (J3x), Jingxing Formation (K1j), etc., and is generally constructed as a set of river and lake facies-marine-sea-land interaction-lake clastic rock carbonate rock.", "triple_list": [ [ "Mesozoic capping", "Contained", "Kapila Group" ], [ "Mesozoic capping", "Contained", "Polira group" ], [ "Mesozoic capping", "Contained", "Adula Group" ], [ "Mesozoic capping", "Contained", "Gala group" ], [ "Mesozoic capping", "Contained", "Wang Bu Group" ], [ "Mesozoic capping", "Contained", "East Bridge Group" ], [ "Mesozoic capping", "Contained", "Small Sole deck group" ], [ "Mesozoic capping", "Contained", "Jingxing Group" ], [ "Mesozoic capping", "Belongs to", "River and lake facies-marine facies-sea and land interplay-lake clastic rock carbonate clay rock construction" ] ] }, { "text": "Light gray thin layer-thick layer conglomerate and thin layer of lithotrix quartz sandstone interlayer, 78.00m", "triple_list": [ [ "Light gray thin layer-thick layer conglomerate and thin layer of lithotrix quartz sandstone interlayer", "thickness", "78.00m" ] ] }, { "text": "Only the Early Cretaceous Jingxing Formation (K1j) in the Cretaceous strata in this area is distributed in the Chamdo-Mangkang Stratigraphic Zone and the Jiangda-Deqin Stratigraphic Zone.", "triple_list": [ [ "Cretaceous strata", "Outcrop", "Early Cretaceous Scenic Star Group" ], [ "Early Cretaceous Scenic Star Group", "Stratigraphical zoning", "Chamdo-Mangkang Stratigraphic Zone" ], [ "Early Cretaceous Scenic Star Group", "Stratigraphical zoning", "Jiangda-Deqin Stratigraphic Zone" ] ] }, { "text": "The bamboo card group is distributed in the area of Fencuoga-Gazadou in Changdu County at 1:25 million, and is spread in the northwest to the southeast. It extends to the northwest to the west and into the Dingqing County in the northwest. It gradually fades to the southeast, with an exposed area of about 106.3m2.", "triple_list": [ [ "Bamboo card group", "Exposed", "1:250,000 Changdu County Fencuoga-Gazhaidou" ], [ "Bamboo card group", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Bamboo card group", "Exposed", "1:250,000 Dingqing County" ], [ "Bamboo card group", "area", "106.3m2" ] ] }, { "text": "The lithology of the Qingnidong Formation (O1q) is carbon slate sandstone, silt sandstone, etc.", "triple_list": [ [ "Qingni Cave Group", "Lithology", "Carbon slate" ], [ "Qingni Cave Group", "Lithology", "sandstone" ], [ "Qingni Cave Group", "Lithology", "Siltstone" ] ] }, { "text": "The schist is gray-green, with fibrous granular metamorphic structure and parallel flake structure.", "triple_list": [ [ "The sun is schist", "Distribution pattern", "Fibrogranular metamorphic structure" ], [ "The sun is schist", "Develop", "Parallel sheet structure" ] ] }, { "text": "Dark gray bioclad mud limestone, produced by Palaeofusulina cf. ellipsoidalis, P. tobensis, P. pulla, P. fusiformis, P. sp.; Brachiopod Oldhamina cf. squamosa, O. sp., Leptodus sp. L. sp. ind., Spirifer sp.; Coral Pseudobradgphyllum sp., Bradyphyllum sp. Lophophyllidium cf. pendulum, 6.92m", "triple_list": [ [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Palaeofusulina cf. ellipsoidalis" ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "P. tobensis" ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "P. pulla" ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "P. fusiformis" ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "P. sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Brachiopod Oldhamina cf. squamosa" ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "O. sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Leptodus sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "L. sp. ind." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "spirifer sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Coral Pseudobradgphyllum sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Bradyphyllum sp." ], [ "Dark gray bioclass mud crystal limestone", "Paleontological", "Lophophyllidium cf. pendulum" ], [ "Dark gray bioclass mud crystal limestone", "thickness", "6.92m" ] ] }, { "text": "Gray sandstone shale, plant Neocalamites cf. hoerensis N. cf. carcimoides, not seen, >50m", "triple_list": [ [ "Gray sandstone shale", "Paleontological", "Plant Neocalamites cf. hoerensis N. cf. carcimoides" ], [ "Gray sandstone shale", "thickness", "50m" ] ] }, { "text": "The Tumugou Group era was the Noli period of the late Triassic period.", "triple_list": [ [ "Tumugou Group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Purple-red medium quartz sandstone gray-green feldspar quartz sandstone, 26.3m", "triple_list": [ [ "Purple-red medium quartz sandstone gray-green feldspar quartz sandstone", "thickness", "26.3m" ] ] }, { "text": "In the Gadikao area, the Jidonglong Formation is composed of biolimestone containing diatom mud calcium biosiliceous rock silty silty silty calcium clay silty silty silty silty calcium clay silty hard sand feldstone sandstone mud calcium silty silty silty silty calcium silty silty silty silty silty calcium silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty silty", "triple_list": [ [ "Gadikao", "Outcrop", "Ji Donglong Group" ], [ "Ji Donglong Group", "Lithology", "Biolimestone" ], [ "Ji Donglong Group", "Lithology", "Diatom-containing marl" ], [ "Ji Donglong Group", "Lithology", "Calcium biosiliceous rock" ], [ "Ji Donglong Group", "Lithology", "Silty slab" ], [ "Ji Donglong Group", "Lithology", "Calcium clay slab containing fine silt" ], [ "Ji Donglong Group", "Lithology", "Hard sand feldstone" ], [ "Ji Donglong Group", "Lithology", "Calcium slab" ], [ "Ji Donglong Group", "Lithology", "Bioshell grain limestone" ], [ "Ji Donglong Group", "Lithology", "Limestone" ], [ "Ji Donglong Group", "Lithology", "Breccia" ], [ "Ji Donglong Group", "Lithology", "Limestone" ], [ "Ji Donglong Group", "Lithology", "Sandstone" ] ] }, { "text": "Light gray-green conglomerate, 25.6m, angle unconsistent, underdeveloped slabs of Jiaoga Formation", "triple_list": [ [ "Light gray-green gravel rock", "thickness", "25.6m" ], [ "Light gray-green gravel rock", "Unconformity contact", "Jiaoga Group Slate" ] ] }, { "text": "Gray-brown-medium-thick layer alteration medium-basic conglomerate dessert tuff tuff breccia, 155.16m", "triple_list": [ [ "Gray-brown-medium-thick layer alteration-basic conglomerate dessert tuff tuff breccia", "thickness", "155.16m" ] ] }, { "text": "Dark gray thin-medium-thick layer of fine-grained quartz sandstone and black sandy slate interlayer, producing ammonite Cucco ceras sp. Paracrochordiceras sp.; bivalve Posidonia pannonica Barbtis Jomdaensis Palaeoneilo sp., 70.60m", "triple_list": [ [ "Dark gray thin-medium-thick layer of fine-grained quartz sandstone and black sandy slate interlayer", "Paleontological", "Ammonite Cucco ceras sp." ], [ "Dark gray thin-medium-thick layer of fine-grained quartz sandstone and black sandy slate interlayer", "Paleontological", "Paracrochordiceras sp." ], [ "Dark gray thin-medium-thick layer of fine-grained quartz sandstone and black sandy slate interlayer", "Paleontological", "Bivalve Posidonia pannonica Barbtis Jomdaensis Palaeoneilo sp." ], [ "Dark gray thin-medium-thick layer of fine-grained quartz sandstone and black sandy slate interlayer", "thickness", "70.60m" ] ] }, { "text": "The Adula Formation of this strata is distributed in 1:25,000 Nangqian County, Nakka Nangqian County, Nakka Nangqian County, Jaduo County, Nakka Nangqian County, Jaduo County, Qinghai Province; 1:25,000 Changdu County, Chalong County, Chalan Dama Niuchang, Chaya County, Chaya County, Chaya County, and other areas. It extends to the west into 1:25,000 Zaduo County, Shiqu County, and Shiqu County, and the south into 1:25,000 Basu County, Gongjue County, with an exposed area of about 3,877m2.", "triple_list": [ [ "Adula Group", "Exposed", "1:25 million Nangqian County, Zaduo County, Qinghai Province, Naidoga Yushu County, Gequka Nangqian County, Gretto" ], [ "Adula Group", "Exposed", "1:250,000 Changdu County Case Changdu County Ding Longda" ], [ "Adula Group", "Exposed", "1:25 million Jiangda County Fenchaya County Chalan Dama Cow Farm" ], [ "Adula Group", "Exposed", "1:25 million Zaduo County" ], [ "Adula Group", "Exposed", "1:250,000 Shiqu County" ], [ "Adula Group", "Exposed", "1:250,000 Basu County Band Gongjue County Band" ], [ "Adula Group", "area", "3877m2" ] ] }, { "text": "Adula Formation with calcite-desert feldstone sandstone, fault contact, sand wood formation, thickness of 712.69m", "triple_list": [ [ "Adula Group", "Lithology", "Calcite-containing rock" ], [ "Adula Group", "Lithology", "Chissite sandstone" ], [ "Adula Group", "Fault contact", "Shamu Group" ], [ "Shamu Group", "thickness", "712.69m" ] ] }, { "text": "Gray medium-thick layered biolimestone with gray thin layered diatom-containing marl limestone, 29.47m", "triple_list": [ [ "Gray medium-thick layered biolimestone with gray thin layered diatom-containing marl", "thickness", "29.47m" ] ] }, { "text": "Gray-black thin-layered argillite slate and gray-brown medium-layered fine-grained feldspar fragment sandstone, 219.15m", "triple_list": [ [ "Gray-black thin-layered argillite slate and gray-brown medium-layered fine-grained feldspar cuttings sandstone", "thickness", "219.15m" ] ] }, { "text": "Gray-white thick layer of shiny crystal-clad spiny clay limestone, producing coral Lytvolosma sp. and brachiopod Enteletes ayseri, 165.8m", "triple_list": [ [ "Gray-white thick layer of lump-like crystal-bonded spiny-clad clay limestone", "Paleontological", "Coral Lytvolosma sp." ], [ "Gray-white thick layer of lump-like crystal-bonded spiny-clad clay limestone", "Paleontological", "Brachiopod Enteletes ayseri" ], [ "Gray-white thick layer of lump-like crystal-bonded spiny-clad clay limestone", "thickness", "165.8m" ] ] }, { "text": "The Permian-Late Triassic Kenanyan Group (P3K.) is distributed in the 1:25,000 area of the Baitong-Garrie-Dedaria area of the northeast corner of the northeast corner of the Nangqian County. It spreads in the Jinsha River junction belt in the northwest-south east direction, extending to the north into the 1:25,000 Yushu County, and extending to the east into the 1:25,000 Shiqu County, with an exposed area of about 506.94m2.", "triple_list": [ [ "Permian-Late Triassic Kenan Rock Group", "Exposed", "1:25 million Nangqian County area northeast corner Baitong-Jiarie-Tadaria" ], [ "Permian-Late Triassic Kenan Rock Group", "Distribution pattern", "Northwest-South East" ], [ "Permian-Late Triassic Kenan Rock Group", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Permian-Late Triassic Kenan Rock Group", "Exposed", "1:250,000 Yushu County" ], [ "Permian-Late Triassic Kenan Rock Group", "Exposed", "1:250,000 Shiqu County" ], [ "Permian-Late Triassic Kenan Rock Group", "area", "506.94m2" ] ] }, { "text": "The Jidonglong Formation of the Early Permian (P1j) is distributed in the Gadikao area in Bailiangniang Township, Yushu County, Nangqian County, 1:25 million, and the area west of Shengpa in Bangboluo Village, Jiangda County, 1:25 million, with an exposed area of about 13.4m2.", "triple_list": [ [ "Early Permian Jidonglong Group", "Exposed", "1:25 million Nangqian County Bian Gadikao Bailiangniang Township, Yushu County" ], [ "Early Permian Jidonglong Group", "Exposed", "1:25 Wan Jiangda County, Bangboluo Village, West of Payi" ], [ "Early Permian Jidonglong Group", "area", "13.4m2" ] ] }, { "text": "Dark gray thin layered fine silt sandstone sandstone intersected - thick layered lithotrix feldstone; insect traces are seen on the layer, fine horizontal stratigraphic Develop, and confined stratigraphic, bivalve Modiolus cf. jianchuanensis Mysidiella cf. yunnanensis; brachiopod Exca torhypchia deltoids imorhynchia cf. nimassica and plant fragments, 307.28m", "triple_list": [ [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Develop", "Insect traces" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Develop", "Horizontal stratification" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Develop", "Cover lamination" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Paleontological", "Bivalve Modiolus cf. jianchuanensis Mysidiella cf. yunnanensis" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Paleontological", "Brachiopod Exca torhypchia deltoids imorhynchia cf. nimassica" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "Paleontological", "Plant fragments" ], [ "Dark gray thin layered fine silt sandstone sandstone intersected-thick layered lithotrix feldstone sandstone", "thickness", "307.28m" ] ] }, { "text": "Diphyphyllum sp., 80.31m, fault contact, sandstone slate limestone of Wuqingna Formation of Carboniferous Systems under the underlying formation", "triple_list": [ [ "Biolimestone", "Paleontological", "coral Diphyphyllum sp." ], [ "Biolimestone", "thickness", "80.31m" ], [ "Biolimestone", "Fault contact", "Sandstone slate limestone of Wuqingna Formation in the Xia Carboniferous System" ] ] }, { "text": "The Adula Formation Stratigraphic Area of the Adula Formation is widely distributed, with exposures in the area of Binggangse Township, Changdu County 1:25,000, Changdu County, with an exposed area of about 750.12m2.", "triple_list": [ [ "Adula Formation Stratigraphic Division", "Outcrop", "Adula Group" ], [ "Adula Group", "Exposed", "1:250,000 Changdu County Finggangse Township-Changmaoling Township-Leiwuqi County" ], [ "Adula Group", "area", "750.12m2" ] ] }, { "text": "Light gray medium-layered fine-grained quartz sandstone, 110m", "triple_list": [ [ "Light gray medium layered fine-grained quartz sandstone", "thickness", "110m" ] ] }, { "text": "Gray silt sandstone, 12.5m", "triple_list": [ [ "Gray siltstone", "thickness", "12.5m" ] ] }, { "text": "The Wangguo Formation is in the area of Gucai Village, Jiangda County. The lower lithology is dark gray medium-block biological clastic limestone and light gray crystalline limestone interlayer, and a small amount of gray-green Andesan volcanic breccia.", "triple_list": [ [ "Wang Guo Group", "Exposed", "Gucai Village, Jiangda County" ], [ "Wang Guo Group", "Lithology", "Dark gray medium-block layer bioclastic limestone" ], [ "Wang Guo Group", "Lithology", "Light gray crystalline limestone" ], [ "Wang Guo Group", "Lithology", "Gray-green Andesan volcanic breccia" ] ] }, { "text": "The era of the Kapila group should be the Late Triassic Kani period.", "triple_list": [ [ "Kapila Group", "Age", "Late Triassic Kani" ] ] }, { "text": "Yellow-brown medium-thick layered sandy marlstone, 37.30m", "triple_list": [ [ "Yellow-brown medium-thick layered sandy marl", "thickness", "37.30m" ] ] }, { "text": "Serpentinite is dark green, with microscale crystalline structure and reticular structure.", "triple_list": [ [ "Serpentine", "Distribution pattern", "Microscopic scale crystallization structure" ], [ "Serpentine", "Develop", "Mesh structure" ] ] }, { "text": "Gray thick layered medium-coarse-grained rock sandstone interspersed with light gray fine conglomerates. It was damaged by faults and did not see the bottom. 179.70m, fault contact, Gangtuoyan Formation (P1g.) schist", "triple_list": [ [ "Gray thick layered medium-coarse-grained rock sandstone with light gray fine gravel rock", "thickness", "179.70m" ], [ "Gray thick layered medium-coarse-grained rock sandstone with light gray fine gravel rock", "Fault contact", "Gangtuoyan Formation" ], [ "Gangtuoyan Formation", "Lithology", "Rock Schist" ] ] }, { "text": "Ningduoyan group (Pt1-2Nd.) is mainly distributed in Changqingke Township, Yushu County, the northern section of the metamorphic rock belt, and the ancient toothed polo in the southern section is scattered, and the geological bodies are in the NW-SE direction.", "triple_list": [ [ "Ningduoyan Group", "Exposed", "Changqingke Township, Yushu County, northern section of the metamorphic rock belt" ], [ "Ningduoyan Group", "Exposed", "Ancient tooth poros" ], [ "Ningduoyan Group", "Distribution pattern", "NW-SE direction" ] ] }, { "text": "Gneiss is mainly found in the lower section of Ningduoyan Group, mainly black cloud oblique gneiss, followed by black cloud two long gneiss.", "triple_list": [ [ "Gneis", "Exposed", "The lower section of Ningduoyan group" ], [ "Gneis", "Contained", "Black clouds oblique gneis" ], [ "Gneis", "Contained", "Black Cloud Two Long Ginsels" ] ] }, { "text": "Overhead strata Dugala Formation (3d) silty rock-cut quartz sandstone amygdala sandstone────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Gala group", "Lithology", "Silty rock" ], [ "Gala group", "Lithology", "quartz sandstone" ], [ "Gala group", "Lithology", "Mud siltstone" ], [ "Gala group", "Integration of contacts", "Adula Group" ], [ "Gala group", "thickness", "1778.38m" ] ] }, { "text": "The foundation of the Baimahai rock is exposed in Jiangduosai-Baimahai area of Batang Township, Yushu Prefecture, Qinghai Province", "triple_list": [ [ "White Horse Sea Rock Foundation", "Exposed", "Jiangduosai in Batang Township, Yushu Prefecture, Qinghai Province-Baimahai" ] ] }, { "text": "Dark gray thin-layer silty fine-grained rock-cut feldspar sandstone intersected with thin-medium-layered muddy fine silty sandstone; the layer has symmetrical wave marks, interlaced stratigraphic Develop, and produces bivalve Burmesia lirata B. sp.; Plant Glossophylum sp. Neocalamites sp., 287.61m", "triple_list": [ [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "Develop", "Symmetrical wave marks" ], [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "Develop", "Interleaved hierarchy" ], [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "Paleontological", "Bivalve Burmesia lirata B. sp." ], [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "Paleontological", "Plant Glossophylum sp." ], [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "Paleontological", "Neocalamites sp." ], [ "Dark gray thin-layered silty fine-grained rock-cut feldspar sandstone sandstone intersected-medium-layered silty fine-silty sandstone", "thickness", "287.61m" ] ] }, { "text": "The black cloud quartz schist rock has a scale-grained metacrystalline structure, and the main minerals are quartz (56), mica (23), mica (4), sodium feldspar (16), etc.", "triple_list": [ [ "Black cloud quartz schist", "Distribution pattern", "Scale grainy metamorphic structure" ], [ "Black cloud quartz schist", "Develop", "Flake-like structure" ], [ "Black cloud quartz schist", "Contained", "quartz" ], [ "Black cloud quartz schist", "Contained", "Black Mouse" ], [ "Black cloud quartz schist", "Contained", "muscovite" ], [ "Black cloud quartz schist", "Contained", "Sodium longite" ] ] }, { "text": "Alternating rhizome porphyry is light gray, with spotty structure and blocky structure.", "triple_list": [ [ "Alternating rhizome porphyry", "Distribution pattern", "Spotted structure" ], [ "Alternating rhizome porphyry", "Develop", "Blocky structure" ] ] }, { "text": "Light gray thick layer of tuff limestone and green gray thick layer of argillic silt sandstone are interlayered, with bivalve rigonodus sp. at the bottom, 12.10m ─────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Light gray thick layer of tuff limestone and green gray thick layer of argill silt sandstone interlayer", "Paleontological", "bivalve rigonodus sp." ], [ "Light gray thick layer of tuff limestone and green gray thick layer of argill silt sandstone interlayer", "thickness", "12.10m" ], [ "Light gray thick layer of tuff limestone and green gray thick layer of argill silt sandstone interlayer", "Integration of contacts", "Pushuiqiao Formation Sandstone" ] ] }, { "text": "The Kenan Rock Group (P3K.) is a set of tectonic mixed rocks in the Jinsha River Belt.", "triple_list": [ [ "Kenan Rock Group", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Kenan Rock Group", "Lithology", "Tectonic mixed rock" ] ] }, { "text": "Luodongyan Group (3J1L.) fake thickness 615.23m", "triple_list": [ [ "Luodongyan Group", "thickness", "615.23m" ] ] }, { "text": "The Gariejee Fault (F12) moves northwestward and extends in a curved manner, extending out of the map at both ends of the north, southwest and east, and the length of this area is about 32m.", "triple_list": [ [ "Garietia fracture", "Distribution pattern", "North-west" ], [ "Garietia fracture", "Distribution pattern", "Curved extension" ], [ "Garietia fracture", "length", "32m" ] ] }, { "text": "The Carboniferous strata in the Sanjiangda-Deqin strata include the Early Carboniferous Dongque Formation (C1d) and the Late Carboniferous Wangguo Formation (C2w).", "triple_list": [ [ "Carboniferous strata of Sanjiangda-Deqin strata", "Outcrop", "The Dongque Group of the Early Carboniferous World" ], [ "Carboniferous strata of Sanjiangda-Deqin strata", "Outcrop", "Late Carboniferous World Wangguo Group" ] ] }, { "text": "Gray iron-containing silt sericite slate with a small amount of gray thin layer of metamorphic mud siltstone, bivalve Protocardia jianchanensis Utschamiella sp. Burmesia sp., 159.9m", "triple_list": [ [ "Gray iron-containing silt sericite slate with a small amount of gray thin layer of metamorphic mud silt", "Paleontological", "Bivalve Protocardia jianchanensis Utschamiella sp." ], [ "Gray iron-containing silt sericite slate with a small amount of gray thin layer of metamorphic mud silt", "Paleontological", "Burmesia sp." ], [ "Gray iron-containing silt sericite slate with a small amount of gray thin layer of metamorphic mud silt", "thickness", "159.9m" ] ] }, { "text": "Overhead strata Polila Formation grey limestone dolomite ─────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polila Formation Gray Limestone Dolomites", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "2440.03m" ] ] }, { "text": "Judging from the appearance of the fossil combination, the Wangguo group is undoubtedly in the late Carboniferous World.", "triple_list": [ [ "Wang Guo Group", "Age", "Late Carboniferous" ] ] }, { "text": "The tectonic invasion of the Japanese-Ji Bengba rock block group is located in the mixed rocks of the Russian rock formation.", "triple_list": [ [ "Tectonic invasion of Rijibengba rock block group", "Located at", "Mixed rocks of the Russian rocks" ] ] }, { "text": "The Gongyenong Group (3g) is distributed in 1:25,000 Nangqian County, Yushu County, Qinghai Province, Wulongxinya Longba-Duowuqiniuchang, 1:25,000 Jiangda County, Jiangda County, Gangga Gongyenong and other areas, extending to the northward 1:25,000 Yushu County and 1:25,000 Shiqu County, with an area of about 261m2 in the map.", "triple_list": [ [ "The man also works in groups", "Exposed", "1:25 million Nangqian County, Yushu County, Qinghai Province, Wulongxinyalongba—Duowuqiniuchang" ], [ "The man also works in groups", "Exposed", "1:25 million Jiangda County, Jiangda County, Ganggagong also" ], [ "The man also works in groups", "Exposed", "1:250,000 Yushu County" ], [ "The man also works in groups", "Exposed", "1:250,000 Shiqu County" ], [ "The man also works in groups", "area", "261m2" ] ] }, { "text": "Dark gray thick layer of metamorphic quartz sandstone with gray-black silty slate, containing plant fragments, 251.27m", "triple_list": [ [ "Dark gray thick layer of metamorphic quartz sandstone with gray-black silty slab", "Paleontological", "Plant fragments" ], [ "Dark gray thick layer of metamorphic quartz sandstone with gray-black silty slab", "thickness", "251.27m" ] ] }, { "text": "The volcanic rock of the Tumugou Formation is distributed in the upper part of the Tumugou Formation.", "triple_list": [ [ "Tumugou Formation volcanic rock", "Exposed", "The upper part of the Toumgou Group" ] ] }, { "text": "Gray lithotripsy silt sandstone with mud crystal limestone, produced by Palaeofusulina cf. ellipsoidalis, P. sp., 41.52m", "triple_list": [ [ "Gray rock debris silt sandstone with mud crystal limestone", "Paleontological", "Palaeofusulina cf. ellipsoidalis" ], [ "Gray rock debris silt sandstone with mud crystal limestone", "Paleontological", "P. sp." ], [ "Gray rock debris silt sandstone with mud crystal limestone", "thickness", "41.52m" ] ] }, { "text": "1:1 million Yushu plant was captured in the Permian coral Waagenophyllum sp. in the limestone in Juewu Temple in Shiqu County, Sichuan Province, and Neocrimites sp. Kufengceras sp., so its era was placed in the Permian-late Triassic period.", "triple_list": [ [ "1:1 million Yushu is located in Juewu Temple, Shiqu County, Sichuan Province", "Contained", "Limestone" ], [ "Limestone", "Paleontological", "Permian coral Waagenophyllum sp." ], [ "Limestone", "Paleontological", "Cephalopod Neocrimites sp." ], [ "Limestone", "Paleontological", "Kufengoceras sp." ], [ "Limestone", "Age", "Permian-late Triassic" ] ] }, { "text": "The ancient-Mid-Proterozoic volcanic rocks were distributed in the Jitang rock group (Pt1-2J.) in the Lewuqi area of Tañantawengshan and Ningdo rock group (Pt1-2Nd.) in the eastern Changqingke summer area, and both have metamorphic rocks.", "triple_list": [ [ "Ancient - Middle Proterozoic volcanic rocks", "Stratigraphical zoning", "In the western part of this area, he misses the Wengshan Leiwuqi area." ], [ "Ancient - Middle Proterozoic volcanic rocks", "Exposed", "Jitang Rock Group" ], [ "Ancient - Middle Proterozoic volcanic rocks", "Stratigraphical zoning", "East China Evergreen May in summer" ], [ "Ancient - Middle Proterozoic volcanic rocks", "Exposed", "Ningduoyan Group" ], [ "Ancient - Middle Proterozoic volcanic rocks", "Lithology", "Metamorphic rock" ] ] }, { "text": "Gray medium-thick layer of breccia-like powdered grey matter dolomite, producing Eostaffella cf. postmsoquensis Ozawainella sp. Pseudostffella confusa; Coral Arachnolasma sp. Hexaphyllum sp. Caninostrostion sp., 26.24m", "triple_list": [ [ "Gray medium-thick layer of breccia-like powdered grey matter dolomite", "Paleontological", "Eostaffella cf. postmsoquensis Ozawainella sp. Pseudostffella confusa" ], [ "Gray medium-thick layer of breccia-like powdered grey matter dolomite", "Paleontological", "Coral Arachnolasma sp. Hexaphyllum sp. Caninostrostion sp." ], [ "Gray medium-thick layer of breccia-like powdered grey matter dolomite", "thickness", "26.24m" ] ] }, { "text": "Silty sandstone with sand ripples corrugated strata two-way interlaced strata, 159.51m", "triple_list": [ [ "Siltstone", "Develop", "Sand ripple corrugated layering" ], [ "Siltstone", "Develop", "Two-way interlaced layering" ], [ "Siltstone", "thickness", "159.51m" ] ] }, { "text": "The Paleogene strata in this area include the Shixin Shizong Bai Group (E2Z) in the Jiayuqiao-Chawalong strata area; the Changdu-Mangkang strata area of the Leiwuqi-Zuogong strata area and the Gongjue strata area (Eg) in the Jiangda-Deqin strata area; the Relu Formation (Er) in the Dege-Baiyu strata area, with a total exposed area of about 4010m2.", "triple_list": [ [ "Paleogene strata", "Contained", "Jiayu Bridge-Chawalong Stratigraphic Zone" ], [ "Paleogene strata", "Contained", "Lewuqi-Zuogong Stratigraphic Division" ], [ "Paleogene strata", "Contained", "Chamdo-Mangkang Stratigraphic Zone" ], [ "Paleogene strata", "Contained", "Jiangda-Deqin Stratigraphic Zone" ], [ "Paleogene strata", "area", "4010m2" ], [ "Jiayu Bridge-Chawalong Stratigraphic Zone", "Outcrop", "The new Shizong Bai Qun" ], [ "Lewuqi-Zuogong Stratigraphic Division", "Outcrop", "Gongjue Group" ], [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Gongjue Group" ], [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Gongjue Group" ], [ "Dege-White Jade Stratigraphic Zone", "Outcrop", "Relu Group" ] ] }, { "text": "Black carbonaceous thousand rocks with light gray calcified schist and crystalline limestone strip-like siliceous rock, 522.1m ──────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Black carbonaceous thousand rocks with light gray calcified schist and crystalline limestone strip-like siliceous rock", "thickness", "522.1m" ], [ "Black carbonaceous thousand rocks with light gray calcified schist and crystalline limestone strip-like siliceous rock", "Integration of contacts", "Quga Temple Group" ], [ "Quga Temple Group", "Lithology", "Slate Sandstone" ] ] }, { "text": "Fine-grained feldspar quartz sandstone with calcified quartz silt sandstone, produces plant Pecopteris (Asterotheca) orientalis, 59.59m", "triple_list": [ [ "Fine-grained feldspar quartz sandstone with calcified quartz silt sandstone", "Paleontological", "Plant Pecopteris (Asterotheca) orientalis" ], [ "Fine-grained feldspar quartz sandstone with calcified quartz silt sandstone", "thickness", "59.59m" ] ] }, { "text": "Blue-gray calcium muddy silt sandstone, produces Sphenopteris sp. Fasoipteris (Ptychocarpus) densata, not seen, 159.59m", "triple_list": [ [ "Blue-gray calcium mud silt sandstone", "Paleontological", "Plant Sphenopteris sp." ], [ "Blue-gray calcium mud silt sandstone", "Paleontological", "Fasoipteris (Ptychocarpus) densata" ], [ "Blue-gray calcium mud silt sandstone", "thickness", "159.59m" ] ] }, { "text": "The grass qu group is only found in the south of Changqing Kexiang (Xiao Sumang), with an area of about 150m2, with a prism-shaped shape, with a long axis NW-SE direction, and a lithology of a shallow metamorphic clastic rock.", "triple_list": [ [ "Caoqu Group", "Exposed", "Changqingke Township (Xiao Sumang) South" ], [ "Caoqu Group", "area", "150m2" ], [ "Caoqu Group", "Distribution pattern", "Prismatic" ], [ "Caoqu Group", "Distribution pattern", "Long axis NW-SE direction" ], [ "Caoqu Group", "Lithology", "shallow metamorphic clastic rock" ] ] }, { "text": "Yellow-gray coarse quartz sandstone with thin layered gray-yellow fine-grained mica feldspar quartz sandstone, laminated and developed, containing plants Calamites sp., 316m", "triple_list": [ [ "Yellow-gray coarse quartz sandstone with thin layered gray-yellow fine-grained mica feldspar quartz sandstone", "Develop", "Layering" ], [ "Yellow-gray coarse quartz sandstone with thin layered gray-yellow fine-grained mica feldspar quartz sandstone", "Paleontological", "Plants Calamites sp." ], [ "Yellow-gray coarse quartz sandstone with thin layered gray-yellow fine-grained mica feldspar quartz sandstone", "thickness", "316m" ] ] }, { "text": "The lithology of the upper part of the Dongque Formation is biological clastic crystalline limestone and Andestone tuff, which is a shallow sea sedimentation on the edge of the active edge.", "triple_list": [ [ "Dong Que Group", "Lithology", "Bioclastic crystalline limestone" ], [ "Dong Que Group", "Lithology", "Andanyan" ], [ "Dong Que Group", "Lithology", "Tuff" ], [ "Dong Que Group", "Belongs to", "Shallow sea sedimentation at the edge" ] ] }, { "text": "The metamorphosis of the late Triassic formations include the Kapila Formation (3j), the Polila Formation (3b), the Adula Formation (3a) and the Dugala Formation (3d).", "triple_list": [ [ "Late Triassic strata", "Outcrop", "Kapila Group" ], [ "Late Triassic strata", "Outcrop", "Polira group" ], [ "Late Triassic strata", "Outcrop", "Adula Group" ], [ "Late Triassic strata", "Outcrop", "Gala group" ] ] }, { "text": "Anshan crystalline tuff, gray-white gray-green, variable tuff structure, layered structure.", "triple_list": [ [ "Anshan crystalline tuff", "Distribution pattern", "Variable tuff structure" ], [ "Anshan crystalline tuff", "Develop", "Layered structure" ] ] }, { "text": "Purple-red conglomerate, 20.4m", "triple_list": [ [ "Purple-red gravel", "thickness", "20.4m" ] ] }, { "text": "Gray yellow gray-green medium-thick layer contains bioclastic calcareous mudstone, producing bivalve Parallelodon sp. and brachiopod fossils, 69.57m", "triple_list": [ [ "Gray yellow gray-green medium-thick layer of bioclastocytic calcareous mudstone", "Paleontological", "bivalve Parallelodon sp." ], [ "Gray yellow gray-green medium-thick layer of bioclastocytic calcareous mudstone", "Paleontological", "Brachiopod fossils" ], [ "Gray yellow gray-green medium-thick layer of bioclastocytic calcareous mudstone", "thickness", "69.57m" ] ] }, { "text": "Dark gray gravel-like biological clastic limestone with marlstone, produced by Schwagerina sp., 83.15m", "triple_list": [ [ "Dark gray gravel-like biological clastic limestone with marl", "Paleontological", "Schwagerina sp." ], [ "Dark gray gravel-like biological clastic limestone with marl", "thickness", "83.15m" ] ] }, { "text": "Baitong fault (F11) extends in a north-west direction, with both ends extending out of the figure, about 43m long.", "triple_list": [ [ "White road break", "Distribution pattern", "Northwest bending and extending" ], [ "White road break", "length", "43m" ] ] }, { "text": "Limestone sandstone of the Jiapila Formation, fault contact, Licha Formation (P1l), thickness 674.6m", "triple_list": [ [ "Limestone sandstone of the Jiapila Formation", "Fault contact", "Richa Group" ], [ "Richa Group", "thickness", "674.6m" ] ] }, { "text": "The sub-district Duogala Formation consists of gray, light gray, dark gray, quartz sandstone, silt serous slate, thin layer of dolomelite scale limestone coal seam, etc., and produces bivalve plants, with a total thickness of 459.76m.", "triple_list": [ [ "Gala group", "Lithology", "Gray light gray dark gray quartz sandstone" ], [ "Gala group", "Lithology", "Silty serous slate" ], [ "Gala group", "Lithology", "Thin layer of dolomelite scale limestone" ], [ "Gala group", "Lithology", "Coal layer" ], [ "Gala group", "Paleontological", "Bivalves" ], [ "Gala group", "thickness", "459.76m" ] ] }, { "text": "Gray-black medium-thick layer of coarse-grained sandstone quartz feldspar sandstone sandstone intersected with black sandy shale argillary sandstone and black shale, 77.7m, fault contact, purple-red conglomerate sandstone in the Jiapila Formation.", "triple_list": [ [ "Gray-black medium-thick layer of coarse-grained sandstone quartz feldstone sandstone sandstone intersected with black sandy shale argillary sandstone and black shale", "thickness", "77.7m" ], [ "Gray-black medium-thick layer of coarse-grained sandstone quartz feldstone sandstone sandstone intersected with black sandy shale argillary sandstone and black shale", "Fault contact", "Jiapila Formation Purple-red Conglomerate Sandstone" ] ] }, { "text": "Dark gray-gray black slate silty slate containing silty clay slate with yellow-gray medium-layer sandstone, producing bivalve Halobia sp. H. superbercens and plant fragments, 141.13m", "triple_list": [ [ "Dark gray-gray black slate silty slate containing silty clay slate with yellow-gray middle-layer mixed sandstone", "Paleontological", "bivalve Halobia sp." ], [ "Dark gray-gray black slate silty slate containing silty clay slate with yellow-gray middle-layer mixed sandstone", "Paleontological", "H. superbercens" ], [ "Dark gray-gray black slate silty slate containing silty clay slate with yellow-gray middle-layer mixed sandstone", "Paleontological", "Plant fragments" ], [ "Dark gray-gray black slate silty slate containing silty clay slate with yellow-gray middle-layer mixed sandstone", "thickness", "141.13m" ] ] }, { "text": "Gray dark gray medium-thick layer of glossy crystal intercalculus limestone, 23.41m", "triple_list": [ [ "Gray dark gray medium-thick layer of glossy cemented intersected insect clay limestone", "thickness", "23.41m" ] ] }, { "text": "The rock has a granular crystal structure, a block-like structure, and some have a remnant layered structure.", "triple_list": [ [ "rock", "Distribution pattern", "Inlaid granular metamorphic structure" ], [ "rock", "Develop", "Blocky structure" ], [ "rock", "Develop", "Variable layered structure" ] ] }, { "text": "Gray-black slate with marl stone, no bottom, 50.0m", "triple_list": [ [ "Gray-black slate marl", "thickness", "50.0m" ] ] }, { "text": "Ash dark gray medium acidic tuff lava and limestone are interlayered with different thicknesses, producing ammonites Hollandites sp. Mataeinanites sp.; bivalve Entolium sichuanensis Eumorphotis sp.; brachiopod Oxyeolpd. Us sp. Holcorhynchia sp. et al., 50.00m", "triple_list": [ [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "Paleontological", "Ammonite Hollandites sp." ], [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "Paleontological", "Mataeinanites sp." ], [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "Paleontological", "bivalve Entolium sichuanensis Eumorphotis sp." ], [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "Paleontological", "Brachiopod Oxyeolpd. Us sp." ], [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "Paleontological", "Holcorhynchia sp." ], [ "Gray dark gray medium acid tuff lava and limestone are interlayered with different thicknesses", "thickness", "50.00m" ] ] }, { "text": "The Gajin Xueshan Rock Group (P1G.) only reveals its Gangtuo Rock Group (P1g) in this area, and is distributed in the Zhuoge Village-Ronama-Xagen Village-Gangtuo Township-Gedadi-Adang Village-Youba area in the central and eastern part of Jiangda County. It spreads in the Jinsha River Belt in a near north-south direction, extending to 1:25,000 Shiqu County to the north and 1:25,000 Gongjue County to the south, with an exposed area of about 1344.46m2.", "triple_list": [ [ "Gajin Snow Mountain Rock Group", "Outcrop", "Qigang Rock Formation" ], [ "Qigang Rock Formation", "Exposed", "1:25 million Jiangda County Zhuoge Village-Ronama-Xagen Village-Gangto Township-Gedadi-Adang Village-Youba" ], [ "Qigang Rock Formation", "Distribution pattern", "Near north-south" ], [ "Qigang Rock Formation", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Qigang Rock Formation", "Exposed", "1:250,000 Shiqu County" ], [ "Qigang Rock Formation", "Exposed", "1:250,000 Gongjue County" ], [ "Qigang Rock Formation", "area", "1344.46m2" ] ] }, { "text": "The brachiopod Gigantoproductus cdclburggens., Striatifera striata., belongs to the Early Carbonifera.", "triple_list": [ [ "Virgo Group", "Paleontological", "Brachiopod Gigantoproductus cdclburgens." ], [ "Virgo Group", "Paleontological", "Striatifera striata." ], [ "Virgo Group", "Age", "Early Carboniferous" ] ] }, { "text": "The Middle Permian volcanic rocks are produced in the Mangcuo Formation (P2mc) and Jiaoga Formation (P2j), and are distributed west of the Nangqian-Changdu line, and in the areas of Shanhongnabaqu, Leiwuqinga, Leiwuqinga, and Qinghai Nangqin County.", "triple_list": [ [ "Middle Permian volcanic rocks", "Located at", "Rude group" ], [ "Middle Permian volcanic rocks", "Located at", "Jiaoga Group" ], [ "Middle Permian volcanic rocks", "Exposed", "Nangqian-West of the Chamdo line" ], [ "Middle Permian volcanic rocks", "Exposed", "Shanhongnabaqu, Lewuqi County, east of the North Lancang River Fault" ], [ "Middle Permian volcanic rocks", "Exposed", "Gangzuoyongbiqinga, Nangqin County, Qinghai" ] ] }, { "text": "Rana Mountain Formation (3l), 3648.1m thick", "triple_list": [ [ "Rana Mountain Group", "thickness", "3648.1m" ] ] }, { "text": "Purple-red giant thick layer of fine-grained rock fragments mixed sandstone with ash-variety thin layer of muddy silt sandstone, horizontal stratigraphic Develop, 320.88m", "triple_list": [ [ "Purple-red giant thick layer of fine-grained rock fragments mixed sandstone with ash-variety thin layer of muddy silt sandstone", "Develop", "Horizontal stratification" ], [ "Purple-red giant thick layer of fine-grained rock fragments mixed sandstone with ash-variety thin layer of muddy silt sandstone", "thickness", "320.88m" ] ] }, { "text": "The Dongque Formation is in the area of Gucai Village, Jiangda County. The lithology is light gray-dark gray-mid-block layer containing biological clastic crystalline limestone with light gray-green altered andesite and tuffs. It is rich in foraminifera, followed by coral brachiopods, and is integrated and covered by the Late Devon Shidongla Formation.", "triple_list": [ [ "Dong Que Group", "Exposed", "Gucai Village, Jiangda County" ], [ "Dong Que Group", "Lithology", "Light gray-dark gray-block layer containing biological debris crystalline limestone" ], [ "Dong Que Group", "Lithology", "Light gray-green altered andesite" ], [ "Dong Que Group", "Lithology", "Tuff" ], [ "Dong Que Group", "Paleontological", "Foraminifera" ], [ "Dong Que Group", "Paleontological", "coral" ], [ "Dong Que Group", "Paleontological", "Brachiopod" ], [ "Dong Que Group", "Integration of contacts", "Late Devons Donra Group" ] ] }, { "text": "The Sanmu Formation is a sandstone siltstone biological clastic limestone or limestone lens body with shallow sea and sea land interaction, rich in serpentine fossils of the brachiopod and plant fragments, with an exposed thickness greater than 712.09m.", "triple_list": [ [ "Shamu Group", "Belongs to", "Shallow sea-land and sea interaction" ], [ "Shamu Group", "Lithology", "sandstone" ], [ "Shamu Group", "Lithology", "Siltstone" ], [ "Shamu Group", "Lithology", "Bioclastic limestone" ], [ "Shamu Group", "Lithology", "Limestone lens body" ], [ "Shamu Group", "Paleontological", "Snake" ], [ "Shamu Group", "Paleontological", "coral" ], [ "Shamu Group", "Paleontological", "Brachiopod fossil" ], [ "Shamu Group", "Paleontological", "Plant fragments" ], [ "Shamu Group", "thickness", "712.09m" ] ] }, { "text": "The Dugaila Formation Stratigraphic Zone of Dugaila Formation is distributed in the area of Longda-Qin State, Changdu County, with an exposed area of about 206.26m2.", "triple_list": [ [ "Terrain partition of the Dugaila Formation", "Outcrop", "Gala group" ], [ "Gala group", "Exposed", "1:250,000 Changdu County Longda-Qinbang" ], [ "Gala group", "area", "206.26m2" ] ] }, { "text": "Diorite vein rocks are gray, with a semi-self-shaped granular structure and a blocky structure.", "triple_list": [ [ "Diorite vein rock", "Distribution pattern", "Medium fine grain semi-self-shaped granular structure" ], [ "Diorite vein rock", "Develop", "Blocky structure" ] ] }, { "text": "Gray-black carbonaceous argillite and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green argill sandstone, containing bivalve Schizodus sp. Nuculana sp. Allorisma sp. Volsella sp. Liebea cf. sinensis, 461m", "triple_list": [ [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "Paleontological", "bivalve Schizodus sp." ], [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "Paleontological", "Nuculana sp." ], [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "Paleontological", "Allorisma sp." ], [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "Paleontological", "Volsella sp." ], [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "Paleontological", "Liebea cf. sinensis" ], [ "Gray-black carbonaceous arable rock and gray-yellow sandy shale interlayer thin layer of quartz sandstone and gray-green arable sandstone", "thickness", "461m" ] ] }, { "text": "Gray-black silty serous slate with gray-black medium-thin layer of metamorphic quartz silty sandstone, 13.7m", "triple_list": [ [ "Gray-black silty serous slate with gray-black medium-thin layer of metamorphic quartz silty", "thickness", "13.7m" ] ] }, { "text": "The diaboli vein rocks are gray-green-dark green, with altered diaboli structure and blocky structure.", "triple_list": [ [ "diaphragm vein rock", "Distribution pattern", "Alternating radiant green structure" ], [ "diaphragm vein rock", "Develop", "Blocky structure" ] ] }, { "text": "Serpentine petrochemical peridotite is dark green to dark green and black, and it explains the grid structure and the false spot structure, and blocky structure.", "triple_list": [ [ "serpentine petrochemical peridotite", "Distribution pattern", "Explain the grid structure" ], [ "serpentine petrochemical peridotite", "Distribution pattern", "Explain the false spot structure" ], [ "serpentine petrochemical peridotite", "Develop", "Blocky structure" ] ] }, { "text": "Neoprotrachyceras sp. Buchites cf. erneri, 109.30m, angle unconsolidated, submerged stratigraphic cave deck (3d) volcanic rocks intersected clastic rocks", "triple_list": [ [ "Mudstone", "Paleontological", "Ammonite Neoprotrachyceras sp. Buchites cf. erneri" ], [ "Mudstone", "thickness", "109.30m" ], [ "Mudstone", "Unconformity contact", "Hole deck" ], [ "Hole deck", "Lithology", "Volcanic rocks" ], [ "Hole deck", "Lithology", "Clastite" ] ] }, { "text": "The Early Jurassic Wangbu Formation (J1w) is distributed in the area of the Hela-Xiaogelong area of the Leiwuqi-Zuogong strata; the Changdu-Mangkang strata area Yuewarawa and Chennama; the Jiangda-Deqin strata area and other places, extending to the west into the Dingqing County area and 1:25,000 Gongjue County area and Basu County area, with an area of about 1331.98m2 in the map.", "triple_list": [ [ "Early Jurassic Wanbu Group", "Exposed", "Lewuqi-Zuogong strata zone - Xiao Gelon" ], [ "Early Jurassic Wanbu Group", "Exposed", "Chamdo-Mangkang Stratigraphic Zone Moon Walava and Chenama" ], [ "Early Jurassic Wanbu Group", "Exposed", "Jiangda-Deqin Stratigraphic Zone Jiangdaka Dune" ], [ "Early Jurassic Wanbu Group", "Exposed", "1:250,000 Dingqing County" ], [ "Early Jurassic Wanbu Group", "Exposed", "1:25 million Gongjue County picture" ], [ "Early Jurassic Wanbu Group", "area", "1331.98m2" ] ] }, { "text": "Black charcoal rocks with black sandy shale peaty sandstone and mesolayer mud sandy limestone, containing coral Asserculinia lophocarinophylloides Lophophyllidium stereoseptatum(sp. mov), imorphyllum sp. Schuchertella sp. Squarnuloria sp., 101.5m", "triple_list": [ [ "Black carbon rock with black sandy shale peaty sandstone and middle-layer mud sandy limestone", "Paleontological", "Coral Asserculinia lophocarinophylloides Lophophyllidium stereoseptatum(sp. mov)" ], [ "Black carbon rock with black sandy shale peaty sandstone and middle-layer mud sandy limestone", "Paleontological", "imorphyllum sp." ], [ "Black carbon rock with black sandy shale peaty sandstone and middle-layer mud sandy limestone", "Paleontological", "Brachiopod Schuchertella sp." ], [ "Black carbon rock with black sandy shale peaty sandstone and middle-layer mud sandy limestone", "Paleontological", "Squarnuloria sp." ], [ "Black carbon rock with black sandy shale peaty sandstone and middle-layer mud sandy limestone", "thickness", "101.5m" ] ] }, { "text": "The marathons are distributed in 1:25 million Jiangda County, with star squatting, and many other places, and are intermittently distributed in the northwest to southeast, extending to the south into the Gongjue County, with an area of about 178m2 in the map.", "triple_list": [ [ "Marathon multiple sets", "Exposed", "1:25 million Jiangda County star is wrong with the south Mang Marathon" ], [ "Marathon multiple sets", "Distribution pattern", "Distribution in the northwest-south east direction" ], [ "Marathon multiple sets", "Exposed", "1:250,000 Gongjue County" ], [ "Marathon multiple sets", "area", "178m2" ] ] }, { "text": "Gray purple-purple gray fine sandy clay quartz silt sandstone with gray purple-gray mud shale, containing bivalve Amiodon cf. fendengensis Prolocardia sp.", "triple_list": [ [ "Gray purple-purple gray fine sandy clay quartz silt sandstone with gray purple-gray mud shale", "Paleontological", "bivalve Amiodon cf. fendengensis Prolocardia sp." ] ] }, { "text": "Overhead bamboo trunk group──────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Bamboo card group", "Integration of contacts", "Russia team" ], [ "Russia team", "thickness", "1502.11m" ] ] }, { "text": "Holocene glacial accumulation (Qhgl) is distributed in the middle and alpine areas of glacier valleys and in the unend of modern glaciers. It mainly includes glacial mud gravel ice water deposits and ice edge accumulations, with an area of 40.7m2.", "triple_list": [ [ "Holocene glacier accumulation", "Exposed", "Modern glaciers in glacier valley" ], [ "Holocene glacier accumulation", "Exposed", "Alpine area" ], [ "Holocene glacier accumulation", "Contained", "glacier" ], [ "Holocene glacier accumulation", "Contained", "Mud and gravel" ], [ "Holocene glacier accumulation", "Contained", "Ice water deposit" ], [ "Holocene glacier accumulation", "Contained", "Ice edge accumulation" ], [ "Holocene glacier accumulation", "area", "40.7m2" ] ] }, { "text": "Overhead formation Boli Formation limestone, fault contact, Jiapila Formation (3j), thickness 1237.1m", "triple_list": [ [ "Poli Formation limestone", "Fault contact", "Kapila Group" ], [ "Kapila Group", "thickness", "1237.1m" ] ] }, { "text": "The Shamu Group in this area is undoubtedly in the late Permian period.", "triple_list": [ [ "Shamu Group", "Age", "Late Permian" ] ] }, { "text": "The Serong Temple Group has rich fossils, and ammonites dominate. The Owenites-Procarnites combination can be divided into the main molecules, including Owenites sp. , Procarnites oeni, P. latumbilicutus (sp.nov.), Isculitoides cf. origrnis, Calliholobus jomdaensis (sp.nov.), Meeoceras sp. , Xenoceltites sp. , Paranannites cf. Minutus, Pa. sp. , uculitoideslenticularis, Proptychitoides sp. , Pvosphingites cf. involutus, Eophyllites cf. erassus, Prohungarites delieatus (sp.nov.), etc.", "triple_list": [ [ "Serong Temple Group", "Paleontological", "Ammonites" ], [ "Serong Temple Group", "Contained", "Owenites—Procarnites combination" ], [ "Serong Temple Group", "Paleontological", "Owenites sp." ], [ "Serong Temple Group", "Paleontological", "Procarnites oeni" ], [ "Serong Temple Group", "Paleontological", "P. latumbilicutus (sp.nov.)" ], [ "Serong Temple Group", "Paleontological", "Isculitoides cf. origrnis" ], [ "Serong Temple Group", "Paleontological", "Calliholobus jomdaensis (sp.nov.)" ], [ "Serong Temple Group", "Paleontological", "Meeoceras sp." ], [ "Serong Temple Group", "Paleontological", "Xenoceltites sp." ], [ "Serong Temple Group", "Paleontological", "Paranannites cf. Minutus" ], [ "Serong Temple Group", "Paleontological", "Pa. sp." ], [ "Serong Temple Group", "Paleontological", "uculitoideslenticularis" ], [ "Serong Temple Group", "Paleontological", "Proptychitoides sp." ], [ "Serong Temple Group", "Paleontological", "Pvosphingites cf. involutus" ], [ "Serong Temple Group", "Paleontological", "Eophyllites cf. erassus" ], [ "Serong Temple Group", "Paleontological", "Prohungarites deliciousus (sp.nov.)" ] ] }, { "text": "The upper gray middle layer of silty limestone and calcified slate show rhythmic interlayers, thick-block tuff and Andanite gravel-containing crystal tuff; the lower dark gray carbon silty slate, calcified silty limestone, thin-layer (or lenticular) limestone shows rhythmic interlayers, and the bottom is gray thick-layer gravel-shaped limestone, 65.50m", "triple_list": [ [ "Gray thick gravel limestone", "thickness", "65.50m" ] ] }, { "text": "The Kapila Group era should be the Late Triassic Kani period.", "triple_list": [ [ "Kapila Group", "Age", "Late Triassic Kani" ] ] }, { "text": "The overlying formation of the Gongyelan Group of limestone ────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Gongyelian Group of Limestone", "Integration of contacts", "Dongdu Group" ], [ "Dongdu Group", "thickness", "377.21m" ] ] }, { "text": "The Yidun rear arc basin is a late Triassic sedimentary basin, with exposed strata including Qugasi Formation (3q), Tumugou Formation (3t), Lanashan Formation (3l), Yingzhunianga Formation (3y), and a small number of Paleogene Relu Formation (Er).", "triple_list": [ [ "Yidun rear arc basin", "Belongs to", "Late Triassic Sedimentary Basin" ], [ "Yidun rear arc basin", "Outcrop", "Quga Temple Group" ], [ "Yidun rear arc basin", "Outcrop", "Tumugou Group" ], [ "Yidun rear arc basin", "Outcrop", "Rana Mountain Group" ], [ "Yidun rear arc basin", "Outcrop", "Yingzhu Niang group" ], [ "Yidun rear arc basin", "Outcrop", "Paleogene Relu Formation" ] ] }, { "text": "Dark gray medium-thick layered limestone, 105m", "triple_list": [ [ "Dark gray medium-thick layered limestone", "thickness", "105m" ] ] }, { "text": "Purple-red thick layer of conglomerate sandstone, 59m", "triple_list": [ [ "Purple-red thick layer conglomerate sandstone", "thickness", "59m" ] ] }, { "text": "Gray dark gray medium-thick layer of rock-cut quartz fine sandstone arable quartz silt sandstone gray black serous clay slate interlayer, 77.32m", "triple_list": [ [ "Gray dark gray medium-thick layer of rock-cut quartz fine sandstone arable quartz silt sandstone gray black serous clay slate interlayer", "thickness", "77.32m" ] ] }, { "text": "Meng Axiongqun (3M) 985.52m", "triple_list": [ [ "Meng Axiong Qun", "thickness", "985.52m" ] ] }, { "text": "Zhengchang granite is light gray-green, and the Wenxiang granite is broken and blocky.", "triple_list": [ [ "Zhengchang granite", "Distribution pattern", "Wenxiang Granite Structure" ], [ "Zhengchang granite", "Distribution pattern", "Broken structure" ], [ "Zhengchang granite", "Develop", "Blocky structure" ] ] }, { "text": "Variety serous slate, 28.2m", "triple_list": [ [ "Misty serous slab", "thickness", "28.2m" ] ] }, { "text": "Light gray grey grey mud quartz silt sandstone, 45.4m", "triple_list": [ [ "Light grey grey mud quartz silt", "thickness", "45.4m" ] ] }, { "text": "Gray thick layered medium fine calcareous lithotripsy sandstone, 252.65m", "triple_list": [ [ "Gray thick layered medium fine calcareous lithotripsy sandstone", "thickness", "252.65m" ] ] }, { "text": "Coarse andylan is gray-dark gray, with a patchy structure intertwined structure and a stomatal-like structure.", "triple_list": [ [ "Cool Anyan", "Distribution pattern", "Coarse and interwoven structure" ], [ "Cool Anyan", "Distribution pattern", "Spotted structure" ] ] }, { "text": "Gray gray-gray black fine-grained thick layered mica quartz sandstone with black peaty shale, containing plant Pecopteris naingensis Protoblechnum sp. aeuipteris sp., Brachiopod Waagenites barusieus Compressoproductus compressus, 20m", "triple_list": [ [ "Gray gray-black fine-grained thick layered mica quartz sandstone with black peaty shale", "Paleontological", "Plant Pecopteris naingensis Protiblechnum sp." ], [ "Gray gray-black fine-grained thick layered mica quartz sandstone with black peaty shale", "Paleontological", "aeuipteris sp." ], [ "Gray gray-black fine-grained thick layered mica quartz sandstone with black peaty shale", "Paleontological", "Brachiopod Waagenites barusieusis Compressoproductus compressus" ], [ "Gray gray-black fine-grained thick layered mica quartz sandstone with black peaty shale", "thickness", "20m" ] ] }, { "text": "Gray dark gray thin medium-layer lithotrix quartz sandstone arable quartz silt sandstone gray black serous clay slate interlayer, producing bivalve hracia prisca.; gastropod Zygopleura sp. and vertebrate bone fragments, 141.20m", "triple_list": [ [ "Gray dark gray thin medium-layer lithotrix quartz sandstone arable quartz silt sandstone gray black serous clay slate interlayer", "Paleontological", "bivalve hracia prisca." ], [ "Gray dark gray thin medium-layer lithotrix quartz sandstone arable quartz silt sandstone gray black serous clay slate interlayer", "Paleontological", "Gastropods Zygopleura sp." ], [ "Gray dark gray thin medium-layer lithotrix quartz sandstone arable quartz silt sandstone gray black serous clay slate interlayer", "Paleontological", "Vertebrate bone slices" ], [ "Gray dark gray thin medium-layer lithotrix quartz sandstone arable quartz silt sandstone gray black serous clay slate interlayer", "thickness", "141.20m" ] ] }, { "text": "The Jiapila Formation of the Lewuqi-Zuogong District was exposed sporadically, with few fossils, and no fossils were found on the profile and route.", "triple_list": [ [ "Lewuqi-Zuogong Division", "Outcrop", "Kapila Group" ] ] }, { "text": "The Polila era is the Noli period.", "triple_list": [ [ "Polira group", "Age", "Noli period" ] ] }, { "text": "The strata sub-district Dugaila group is distributed in 1:25,000 Nangqian County Zhalangpo, Nangqian County, Nangqian County, 1:25,000 Changdu County, Deria, Changdu County, 1:25, Wanjiangda County, Gelong Gongjue County and other areas. It extends to the north into 1:25,000 Shiqu County, and 1:25,000 Basu County, and Gongjue County.", "triple_list": [ [ "Gala group", "Exposed", "1:25 million Nangqian County Zhalangpo" ], [ "Gala group", "Exposed", "1:250,000 Changdu County Case of Changdu County Desert" ], [ "Gala group", "Exposed", "1:25 Wanjiangda County, Biangelong Gongjue County Chala" ], [ "Gala group", "Exposed", "1:250,000 Shiqu County" ], [ "Gala group", "Exposed", "1:250,000 Basu County" ], [ "Gala group", "Exposed", "Gongjue County" ] ] }, { "text": "Purple medium-thick layer of blocky medium-grain sandy fine-grained rock-cut quartz sandstone with a small amount of purple mud silt sandstone, see corrugated sand pattern layering and groove mold, not seen, 16.65m", "triple_list": [ [ "Purple medium-thick layer of blocky medium-grained sandy fine-grained rock-cut quartz sandstone with a small amount of purple muddy silt sandstone", "Develop", "Wave mark sand pattern layering" ], [ "Purple medium-thick layer of blocky medium-grained sandy fine-grained rock-cut quartz sandstone with a small amount of purple muddy silt sandstone", "Develop", "Slot mold" ], [ "Purple medium-thick layer of blocky medium-grained sandy fine-grained rock-cut quartz sandstone with a small amount of purple muddy silt sandstone", "thickness", "16.65m" ] ] }, { "text": "Gray-changed quartz fine sandstone with gray marlstone, 24.4m", "triple_list": [ [ "Gray-changed quartz fine sandstone with gray marl", "thickness", "24.4m" ] ] }, { "text": "The lithology of the lower part of the Jiapila Formation is dark purple-red conglomerate gravel sandstone, siltstone, etc.; the lithology of the middle part is gray purple-red siltstone splintstone; the lithology of the upper part is gray gray-black purple-red siltstone feldspar quartz sandstone, etc., with a thickness of about 92.9m.", "triple_list": [ [ "Kapila Group", "Lithology", "Dark purple gravel" ], [ "Kapila Group", "Lithology", "Gravel-containing sandstone" ], [ "Kapila Group", "Lithology", "Siltstone" ], [ "Kapila Group", "Lithology", "Gray purple silt" ], [ "Kapila Group", "Lithology", "Slate" ], [ "Kapila Group", "Lithology", "Gray gray black purple silt" ], [ "Kapila Group", "Lithology", "Feldspar quartz sandstone" ], [ "Kapila Group", "Lithology", "Slate" ], [ "Kapila Group", "thickness", "92.9m" ] ] }, { "text": "Siltstone clay rock of the Adula Formation ───────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Siltstone clay rock of Adula Formation", "Integration of contacts", "Polira group" ], [ "Polira group", "thickness", "161.40m" ] ] }, { "text": "Alternating basalt has dark gray, thick block layer, with a change afterglow green structure, and a block structure.", "triple_list": [ [ "Alteration basalt", "Distribution pattern", "Change afterglow green structure" ], [ "Alteration basalt", "Develop", "Blocky structure" ] ] }, { "text": "Dark gray mica calcite-containing clastic siltstone, 10.54m", "triple_list": [ [ "Dark gray mica calcite-containing clastic siltstone", "thickness", "10.54m" ] ] }, { "text": "Purple-red Ying'an crystal tuff slate, 108.17m", "triple_list": [ [ "Purple-red Ying'an crystal tuff slab", "thickness", "108.17m" ] ] }, { "text": "The sediments are mainly riverbed alluvials with a thickness of 30153m.", "triple_list": [ [ "Sediments", "Belongs to", "Alluvial alluvials on the riverbed" ], [ "Sediments", "thickness", "30153m" ] ] }, { "text": "Gray-green block layer metamorphic fluid crystal crystal chip glass tuff, 62.98m", "triple_list": [ [ "Gray-green block layer metamorphic fluid crystal crystal chip glass tuff", "thickness", "62.98m" ] ] }, { "text": "The Pushuiqiao Formation (1p) is distributed in 1:25 million Jiangda County, Jiangda County, Pushuiqiao Chela-Cuolongdayabu-Gurgjue County and other areas, extending to the south by 1:25 million Gongjue County, with an area of about 535m2 in this area.", "triple_list": [ [ "Pushuiqiao Group", "Exposed", "1:25 million Jiangda County Fengjiangda County Pushuiqiao Chela - Cuolongda Yabu - Gorge County Garima" ], [ "Pushuiqiao Group", "Exposed", "1:250,000 Gongjue County" ], [ "Pushuiqiao Group", "area", "535m2" ] ] }, { "text": "The Permian-Triassic strata in this area are distributed in the Gangtuo-Xiqu River strata region, which is part of the material composed of the Jinsha River binding zone. It has the Permian-Late Triassic Kenan Rock Group (P3K.) Permian-Early Triassic Gajin Xueshan Rock Group (P1G.).", "triple_list": [ [ "Permian-Triassic strata", "Exposed", "Gangtuo-Xiquhe Stratigraphic Zone" ], [ "Permian-Triassic strata", "Belongs to", "Jinsha River Combination Belt" ], [ "Permian-Triassic strata", "Outcrop", "Permian-Late Triassic Kenan Rock Group" ], [ "Permian-Triassic strata", "Outcrop", "Permian-Early Triassic Gajin Snow Mountain Rock Group" ] ] }, { "text": "The Adula Group era should be the Noli period of the late Triassic period.", "triple_list": [ [ "Adula Group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Gray-white medium-thin layer of marlstone with gray quartz fine sandstone, containing bivalve Halobia sp. Geruillia sp., 71.8m", "triple_list": [ [ "Gray-white medium-thin layer of marlstone with gray quartz fine sandstone", "Paleontological", "bivalve Halobia sp." ], [ "Gray-white medium-thin layer of marlstone with gray quartz fine sandstone", "Paleontological", "Geruillia sp." ], [ "Gray-white medium-thin layer of marlstone with gray quartz fine sandstone", "thickness", "71.8m" ] ] }, { "text": "Gray Calcium Cuts Siltstone, 72.81m", "triple_list": [ [ "Gray Calcium Cuts Siltstone", "thickness", "72.81m" ] ] }, { "text": "Metamorphic horny Fluorite, metamorphic interlaced structure, patchy structure, block structure.", "triple_list": [ [ "Metamorphic Shrine", "Distribution pattern", "Variable interwoven structure" ], [ "Metamorphic Shrine", "Distribution pattern", "Spotted structure" ], [ "Metamorphic Shrine", "Develop", "Blocky structure" ] ] }, { "text": "The Wangbu group contains bivalve gastropod spore, etc.", "triple_list": [ [ "Wang Bu Group", "Paleontological", "Bivalves" ], [ "Wang Bu Group", "Paleontological", "Gastropod" ], [ "Wang Bu Group", "Paleontological", "Plant spore powder" ] ] }, { "text": "Overhead formation small sokka group (J3x) purple-red mudshale shale with siltstone ────────────────────────────────", "triple_list": [ [ "Small Sole deck group", "Lithology", "Purple-red mudstone" ], [ "Small Sole deck group", "Lithology", "shale" ], [ "Small Sole deck group", "Lithology", "Siltstone" ], [ "Small Sole deck group", "Integration of contacts", "East Bridge Group" ], [ "Small Sole deck group", "thickness", "162.73m" ] ] }, { "text": "Gray-brown medium-thick layered fine-grained feldspar crushed sandstone, 265.22m", "triple_list": [ [ "Gray-brown medium-thick layered fine-grained feldspar crushed sandstone", "thickness", "265.22m" ] ] }, { "text": "The ancient spores were captured in Suruka Carboniferous-Permian fine crystal limestone in Sangduo Township, Dingqing County, and the equivalent strata in the west, and was found in the fine crystal limestone of Leiotriletes, Punctatissporites sp., Laevigatosporites minutus, Granulatisporites sp., etc. (identified by Gaolianda, a researcher of the Chinese Academy of Geological Sciences), which belongs to the Early Permian.", "triple_list": [ [ "Suruka, Sangduo Township, Dingqing County", "Outcrop", "Carbonite-Permian" ], [ "Carbonite-Permian", "Lithology", "Fine crystal limestone" ], [ "Carbonite-Permian", "Age", "Early Permian" ], [ "Fine crystal limestone", "Paleontological", "Paleopore Leiotriletes sp." ], [ "Fine crystal limestone", "Paleontological", "Punctatisporites sp." ], [ "Fine crystal limestone", "Paleontological", "Laevigatosporites minutes" ], [ "Fine crystal limestone", "Paleontological", "Granulatisporites sp." ] ] }, { "text": "The Late Triassic-Early Jurassic strata are distributed in the Jiayuqiao-Chawalong strata zone in this area, producing tectonic mixed rocks, spreading in the Nujiang junction belt, with only the Luodong rock group.", "triple_list": [ [ "Late Triassic-Early Jurassic Stratigraphic", "Earth tectonic location", "Jiayu Bridge-Chawalong Stratigraphic Area of this District" ], [ "Late Triassic-Early Jurassic Stratigraphic", "Distribution pattern", "Tectonic mixed rock output" ], [ "Late Triassic-Early Jurassic Stratigraphic", "Exposed", "Nujiang Belt" ], [ "Late Triassic-Early Jurassic Stratigraphic", "Outcrop", "Luodongyan Group" ] ] }, { "text": "Jitang rock group metamorphic medium-medium-basic volcanic rock consists of plagiarismic radius gneiss black cloud horn radius gneiss plagiarism amphibian plagiarism amphibian radius gneiss plagiarism radius gneiss plagiarism radius gneiss plagiarism radius gneiss and a small amount of pyroxene.", "triple_list": [ [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "Glitter giraffe" ], [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "Black Cloud Corner Stroke Two Long Gins" ], [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "oblique angular amphibole" ], [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "Black cloud two-long grain rock" ], [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "Black Cloud Two Long Ginsels" ], [ "Metamorphic Medium-Medium-Basic Volcanic Rocks in Jitang Rock Group", "Lithology", "Pyroxene" ] ] }, { "text": "Gray-black lithotrix quartz sandstone radioworm siliceous sericite and sericite are interlayered, and there is no bottom, 193.75m, fault contact, purple-red sandstone mudstone of the Jiapila Formation", "triple_list": [ [ "Gray-black lithotrix quartz sandstone radioworm siliceous serous slate and serous slate interlayer", "thickness", "193.75m" ], [ "Gray-black lithotrix quartz sandstone radioworm siliceous serous slate and serous slate interlayer", "Fault contact", "Purple-red sandstone mudstone of the Jiapila Formation" ] ] }, { "text": "The Triassic strata of the Lewuqi-Zuogong strata are divided into the Late Triassic Jiapila Formation (3j), Polila Formation (3b), Adula Formation (3a), Dugail Formation (3d), which are distributed between the Nujiang Binding Belt and the Lancang River Binding Belt.", "triple_list": [ [ "Lewuqi-Zuogong Stratigraphic Division", "Outcrop", "Triassic strata" ], [ "Triassic strata", "Outcrop", "Late Triassic Apira Group" ], [ "Triassic strata", "Outcrop", "Polira group" ], [ "Triassic strata", "Outcrop", "Adula Group" ], [ "Triassic strata", "Outcrop", "Gala group" ], [ "Triassic strata", "Earth tectonic location", "Nujiang Belt" ], [ "Triassic strata", "Earth tectonic location", "Lancang River Combination Belt" ] ] }, { "text": "Serpentine petrochemical carbonate basalt dark green, with a change of afterglow green structure scale crystal structure.", "triple_list": [ [ "Serpentine petrochemical carbonate basalt", "Distribution pattern", "Change afterglow green structure" ], [ "Serpentine petrochemical carbonate basalt", "Distribution pattern", "Scale crystal structure" ] ] }, { "text": "Dark gray thin-medium-thick layered bioclad mud crystal limestone, producing bivalve Halobia yanandongensis Chen, 52.00m ──────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Dark gray thin-medium-thick layered bioclastic mud crystal limestone", "Paleontological", "Bivalve Halobia yandongensis Chen" ], [ "Dark gray thin-medium-thick layered bioclastic mud crystal limestone", "thickness", "52.00m" ], [ "Dark gray thin-medium-thick layered bioclastic mud crystal limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "Lithology", "Purple-red gravel" ], [ "Kapila Group", "Lithology", "sandstone" ] ] }, { "text": "Grab the Galla Group (3d) thickness 330.10m", "triple_list": [ [ "Gala group", "thickness", "330.10m" ] ] }, { "text": "According to the characteristics of rock combination, sedimentary structure and paleontology, the Licha Formation is a sedimentary environment for shallow sea shelves carbonate rocks sand amy rocks and pyroclastic rocks.", "triple_list": [ [ "Richa Group", "Belongs to", "Sedimentary environment of carbonate rocks and sand amy rocks with pyroclastic rocks in shallow sea sheds" ] ] }, { "text": "The late Permian Tuoba Formation (P3t) is distributed in the east of Soluoyong East and Ziqu River in Yushu County, Nangqian County, Nangqian County, 1:25 million, Changdu County, Kangdu County, Changdu County, Kaoyao Nong Niuchangka Township, Bainong, 1:25 million, Jiangda County, Jiangda County, Gaqu and other areas, extending to the southward 1:25 million Gongjue County, with an exposed area of about 140.22m2.", "triple_list": [ [ "Late Permian Tuoba Group", "Exposed", "1:25 million Nangqian County, Yushu County Soluo Yongdong" ], [ "Late Permian Tuoba Group", "Exposed", "Both sides of Ziqu River" ], [ "Late Permian Tuoba Group", "Exposed", "1:250,000 Changdu County Case of Changdu County Test-Bainong Niuchang Kaxiangda" ], [ "Late Permian Tuoba Group", "Exposed", "1:25 million Jiangda County Bian Gaqu Township, Tuoba Township, Changdu County" ], [ "Late Permian Tuoba Group", "Exposed", "1:250,000 Gongjue County" ], [ "Late Permian Tuoba Group", "area", "140.22m2" ] ] }, { "text": "Sodium long tremolite is light gray-green, with a granular fibrous metacrystalline structure and a sheet-like structure.", "triple_list": [ [ "Sodium tremolite", "Distribution pattern", "Granular fibrous crystal structure" ], [ "Sodium tremolite", "Develop", "Flake-like structure" ] ] }, { "text": "Dingqing ophiolite group (D.) serpentine petrochemical oblique peridotite, fault contact, Luodong rock group (3J1L.), false thickness 5180m", "triple_list": [ [ "Dingqing ophiolite group", "Lithology", "Serpentine petrochemical peridotite" ], [ "Dingqing ophiolite group", "Fault contact", "Luodongyan Group" ], [ "Luodongyan Group", "thickness", "5180m" ] ] }, { "text": "Gray thin-medium-layered granular limestone bioclastic limestone crystalline limestone, ammonite-producing Juvenites sp. and gastropod Natiria sp., 182.24m", "triple_list": [ [ "Gray thin-medium-layered granular limestone bioclastic limestone crystalline limestone", "Paleontological", "Ammonite Juvenites sp." ], [ "Gray thin-medium-layered granular limestone bioclastic limestone crystalline limestone", "Paleontological", "Gastropodon Natiria sp." ], [ "Gray thin-medium-layered granular limestone bioclastic limestone crystalline limestone", "thickness", "182.24m" ] ] }, { "text": "Dark gray gray black gray-white serpentine petrochemical peridotite, 240m wide, fault contact, gray green dark black serpentine, 110m wide", "triple_list": [ [ "Dark gray gray black gray white serpentine petrochemical peridotite", "thickness", "240m" ], [ "Dark gray gray black gray white serpentine petrochemical peridotite", "Fault contact", "Gray green dark black serpentine rock" ], [ "Gray green dark black serpentine rock", "thickness", "110m" ] ] }, { "text": "Bamboo card group thickness 2051.65m", "triple_list": [ [ "Bamboo card group", "thickness", "2051.65m" ] ] }, { "text": "The rock mass invaded the strata of the Dongduoyan Group (Pt1-2Nd.) Dongdu Formation (3d), Pushuiqiao Formation (1p), Walasi Formation (2w).", "triple_list": [ [ "Rock body", "Invade", "Ningduoyan Group" ], [ "Rock body", "Invade", "Dongdu Group" ], [ "Rock body", "Invade", "Pushuiqiao Group" ], [ "Rock body", "Invade", "Wala Temple Group" ] ] }, { "text": "Hal obia aff. dilatata H. yandongensis; plant Glossophyllum sp. Neocalamiiees sp., 476.04m", "triple_list": [ [ "sandstone", "Develop", "Volume construction" ], [ "sandstone", "Paleontological", "Bivalve Hal obia aff. dilatata H. yandongensis" ], [ "sandstone", "Paleontological", "Plant Glossophyllum sp." ], [ "sandstone", "Paleontological", "Neocalamiiees sp." ], [ "sandstone", "thickness", "476.04m" ] ] }, { "text": "The era of the Adula group should be the Noli period of the late Triassic period.", "triple_list": [ [ "Adula Group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Olive basalt is dark green, with spotty structure and blocky structure.", "triple_list": [ [ "Olive basalt", "Distribution pattern", "Spotted structure" ], [ "Olive basalt", "Develop", "Blocky structure" ] ] }, { "text": "Light gray yellow metamorphic quartz silt sandstone with dark gray shale, 916.70m ──────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Light gray yellow metamorphic quartz silt sandstone sandstone sandstone sandstone sandstone sandstone", "thickness", "916.70m" ], [ "Light gray yellow metamorphic quartz silt sandstone sandstone sandstone sandstone sandstone sandstone", "Integration of contacts", "Polila Formation Limestone" ] ] }, { "text": "Grey limestone of the overlying strata, producing brachiopods ─────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Polila Formation Grey Limestone", "Paleontological", "Brachiopod" ], [ "Polila Formation Grey Limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "495.4m" ] ] }, { "text": "Sandstone of the overlying strata of Ranashan Formation (3l) ────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Rana Mountain Group", "Lithology", "sandstone" ], [ "Rana Mountain Group", "Integration of contacts", "Tumugou Group" ], [ "Tumugou Group", "thickness", "2073.2m" ] ] }, { "text": "Dark gray-black slate and metamorphic sandstone interlayer siliceous rock, 409.65m", "triple_list": [ [ "Dark gray-black slate and metamorphic sandstone interlayer siliceous rock", "thickness", "409.65m" ] ] }, { "text": "Blue-gray giant thick layered conglomerate, 98.02m", "triple_list": [ [ "Green-gray giant thick layered gravel rock", "thickness", "98.02m" ] ] }, { "text": "Overhead Stratigraphic Jingxing Formation (K1j) purple-red purple-gray giant thick layer of calcareous conglomerate rocks intersected with purple-red giant thick layer of conglomerate fragments sandstone - parallel unconsolidation - small solo set (J3x), thickness 359.32m", "triple_list": [ [ "Jingxing Group", "Lithology", "Purple-red purple-gray giant thick layer of calcium brigade" ], [ "Jingxing Group", "Lithology", "Magenta-red thick layer of gravel rock" ], [ "Jingxing Group", "Lithology", "Chop sandstone" ], [ "Jingxing Group", "Integration of contacts", "Small Sole deck group" ], [ "Small Sole deck group", "thickness", "359.32m" ] ] }, { "text": "Gray light gray-white giant layer of glittery cemented algae clay limestone, producing misellina sp. Pseudofusuli-na sp. P. jiaogensis Schwagerina sp., 51.91m", "triple_list": [ [ "Gray light gray-white giant layer of glitter cemented algae clay limestone", "Paleontological", "Misellina sp." ], [ "Gray light gray-white giant layer of glitter cemented algae clay limestone", "Paleontological", "Pseudofusuli-na sp." ], [ "Gray light gray-white giant layer of glitter cemented algae clay limestone", "Paleontological", "P. jiaogensis Schwagerina sp." ], [ "Gray light gray-white giant layer of glitter cemented algae clay limestone", "thickness", "51.91m" ] ] }, { "text": "Anshan crystalline tuff is light gray, with a subtuff structure and a layered structure.", "triple_list": [ [ "Anshan crystalline tuff", "Distribution pattern", "Variable tuff structure" ], [ "Anshan crystalline tuff", "Develop", "Layered structure" ] ] }, { "text": "Light gray medium-layered calcium silt sandstone, 75m", "triple_list": [ [ "Light gray medium layered calcium siltstone", "thickness", "75m" ] ] }, { "text": "The green curtain has a gray-green schist, a granular fibrous columnar metamorphic structure, and a directional structure.", "triple_list": [ [ "Green curtain sodium longyang schist", "Distribution pattern", "Granular fibrous columnar metamorphic structure" ], [ "Green curtain sodium longyang schist", "Develop", "Directional construction" ] ] }, { "text": "The alkaline rough rocks mainly include black clouds, bright and thick rocks.", "triple_list": [ [ "Alkaline rough rock", "Contained", "Black clouds and radiance thick rock" ], [ "Alkaline rough rock", "Contained", "Fang Fei Nihui Coarse Rock" ] ] }, { "text": "The Russian Rock Formation (CPe.) drawn in this area is part of the Jiayu Bridge Group drawn in Luolongbing 1:200,000, and is a set of tectonic mixed rocks.", "triple_list": [ [ "Russian Rock Formation", "Belongs to", "1:200,000 Jiayu Bridge Group drawn by Luolong Bing" ], [ "Russian Rock Formation", "Belongs to", "Tectonic mixed rock" ] ] }, { "text": "The Adula Formation in this strata is composed of gray, dark gray, gray-black slate, sandstone marl, etc., and produces bivalve ammonite brachiopods, with a total exposed thickness of 780.22m, which is a marine sand amylin deposit.", "triple_list": [ [ "Adula Group", "Lithology", "Gray dark gray gray black slate" ], [ "Adula Group", "Lithology", "sandstone" ], [ "Adula Group", "Lithology", "Marlite" ], [ "Adula Group", "Paleontological", "Bivalves" ], [ "Adula Group", "Paleontological", "Chrysanthemum" ], [ "Adula Group", "Paleontological", "Brachiopods" ], [ "Adula Group", "thickness", "780.22m" ], [ "Adula Group", "Belongs to", "Coastal sand amylin sedimentation" ] ] }, { "text": "Andesan rocks are gray-green, with spotty structures and blocky structures.", "triple_list": [ [ "Andesan Rock", "Distribution pattern", "Spotted structure" ], [ "Andesan Rock", "Develop", "Blocky structure" ] ] }, { "text": "Dark gray silty silty pulverized limestone with gray thick layer of calcified sandstone, horizontal fine layer Develop, production of serpentine Rugosofusulina valida, Schwagerina jewetti, Ozawainella sp.; Coral Aagophyllum sp., 225.78m", "triple_list": [ [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "Develop", "Horizontal microstructure" ], [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "Paleontological", "Rugosofusulina valida" ], [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "Paleontological", "Schwagerina jewetti" ], [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "Paleontological", "Ozawainella sp." ], [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "Paleontological", "Coral Aagophyllum sp." ], [ "Dark gray silty sandy pulverized limestone with gray thick layer of calcareous sandstone", "thickness", "225.78m" ] ] }, { "text": "Anshan rock-cut crystal tuff, dark gray-green, variable tuff structure, layered structure.", "triple_list": [ [ "Anshan rock crystal tuff", "Distribution pattern", "Variable tuff structure" ], [ "Anshan rock crystal tuff", "Develop", "Layered structure" ] ] }, { "text": "Gray thin-layer mud calcium biological silty rock with gray-black silty slate, 3.13m", "triple_list": [ [ "Gray thin-layer mud calcium biological silty rock with gray black silty slab", "thickness", "3.13m" ] ] }, { "text": "The Adula Group in the subdistrict is distributed in the area of Riagulan-Shengenbato Niuchang, Jiangda County, 1:25,000 Jiangda County, extending to the north into the Shiqu County, and 1:25,000 Gongjue County, extending to the south into the area of about 302.2m2.", "triple_list": [ [ "Adula Group", "Exposed", "1:25 million Jiangda County Fenjiangda County Riaguolan-Shengenbato Niuchang" ], [ "Adula Group", "Exposed", "1:250,000 Shiqu County" ], [ "Adula Group", "Exposed", "1:250,000 Gongjue County" ], [ "Adula Group", "area", "302.2m2" ] ] }, { "text": "The rock types of the Shamu Formation include both siltstone in the low-energy zone and sandstone bioclass limestone in higher energy environments, which Contained local plant fragments.", "triple_list": [ [ "Shamu Group", "Lithology", "Siltstone" ], [ "Shamu Group", "Lithology", "sandstone" ], [ "Shamu Group", "Lithology", "Bioclastic limestone" ], [ "Shamu Group", "Paleontological", "Plant fragments" ] ] }, { "text": "The gaze is dark gray-green, and becomes afterglow-glow-glow-glow structure. Occasionally, there are long-grained structures and blocky structures. The main minerals include basal plagioclase (5055), pyroxene (3540) and a small amount of quartz.", "triple_list": [ [ "Galloped gag", "Distribution pattern", "Change afterglow green-glow structure" ], [ "Galloped gag", "Distribution pattern", "Crystalline long structure" ], [ "Galloped gag", "Develop", "Blocky structure" ], [ "Galloped gag", "Contained", "Basal plagioclase" ], [ "Galloped gag", "Contained", "Pyrox" ], [ "Galloped gag", "Contained", "quartz" ] ] }, { "text": "The Nanqiangtang-Zuogong continental block is located between the Bangong Lake-Nujiang junction belt and the Lancang River junction belt, and develops the crystal base of the Jitang rock group in the Paleo-Midproterozoic period, the fold base of the Youxi group in the Neo-Proterozoic period and the Mesozoic region cap layer.", "triple_list": [ [ "Nanqiangtang-Zuogong Land Block", "Located at", "Pangong Lake-Nujiang Combination Belt" ], [ "Nanqiangtang-Zuogong Land Block", "Located at", "Lancang River Combination Belt" ], [ "Nanqiangtang-Zuogong Land Block", "Develop", "Crystallization base of Jitang rock group in ancient times in the Middle Proterozoic period" ], [ "Nanqiangtang-Zuogong Land Block", "Develop", "Neoproterozoic Youxi Group fold base" ], [ "Nanqiangtang-Zuogong Land Block", "Develop", "Mesozoic capping" ] ] }, { "text": "The stratigraphic era of the Luodong rock group should be the Late Triassic-Early Jurassic.", "triple_list": [ [ "Luodongyan Group", "Age", "Late Triassic-Early Jurassic" ] ] }, { "text": "The pre-Paleozoic continental marginal sediment mainly exposed the Zengziding Formation (Oz), which was built for a set of terrestrial clastic rocks and carbonate rocks.", "triple_list": [ [ "Early Paleozoic continental marginal sedimentation", "Outcrop", "Zeng Ziding Group" ], [ "Early Paleozoic continental marginal sedimentation", "Belongs to", "Construction of land-source clastic rocks with carbonate rocks" ] ] }, { "text": "The Aoqu Formation consists of gray-dark gray-black limestone bio-limestone amylin limestone crystal limestone mudstone shale slate sandstone, dolomite grey-green crystalline tuff, etc., and produces brachiopod coral bryozoosomes and aphropods, with a total thickness of 287.5m. According to the characteristics of rock combination, sedimentary structure and paleontology, it belongs to the active continental margin shallow sea shed sedimentary environment.", "triple_list": [ [ "Aoqu Group", "Lithology", "Gray dark gray black limestone" ], [ "Aoqu Group", "Lithology", "Biolimestone" ], [ "Aoqu Group", "Lithology", "Mixed limestone" ], [ "Aoqu Group", "Lithology", "Crystalline limestone" ], [ "Aoqu Group", "Lithology", "Mudstone" ], [ "Aoqu Group", "Lithology", "shale" ], [ "Aoqu Group", "Lithology", "Slate" ], [ "Aoqu Group", "Lithology", "sandstone" ], [ "Aoqu Group", "Lithology", "Dolomite" ], [ "Aoqu Group", "Lithology", "Gray-green crystal chip tuff" ], [ "Aoqu Group", "Paleontological", "Brachiopod" ], [ "Aoqu Group", "Paleontological", "coral" ], [ "Aoqu Group", "Paleontological", "Snake" ], [ "Aoqu Group", "Paleontological", "Bruceworm" ], [ "Aoqu Group", "Paleontological", "Aphrodisiac" ], [ "Aoqu Group", "Paleontological", "Gastropod" ], [ "Aoqu Group", "Belongs to", "Activity of the shallow sea shed sedimentary environment on the edge of the continent" ] ] }, { "text": "Green curtain sun schist green scale fibrous columnar metamorphic structure, mellopterytic structure, directional structure, stretched, wrinkled and twisted structure.", "triple_list": [ [ "Green curtain sun schist", "Distribution pattern", "Scale-shaped fibrous columnar metamorphic structure" ], [ "Green curtain sun schist", "Distribution pattern", "Mylon-like structure" ], [ "Green curtain sun schist", "Develop", "Directional construction" ], [ "Green curtain sun schist", "Develop", "Stretching and wrinkling twisted structure" ] ] }, { "text": "Gray-green complex conglomerate, 7.9m", "triple_list": [ [ "Gray-green complex gravel rock", "thickness", "7.9m" ] ] }, { "text": "Gray Crystal Black Mica Schist, 138.55m", "triple_list": [ [ "Gray crystal black mica schist", "thickness", "138.55m" ] ] }, { "text": "The Yingzhu Niang'a Group is only distributed in the Hudexia Nisongduo area of Baiyu County, Sichuan, southeast of this district. It extends to the south into the Gongjue County area and 1:25,000 Ganzi County area in the east, with an area of about 54m2 in the map.", "triple_list": [ [ "Yingzhu Niang group", "Exposed", "Hudexia Songduo, Baiyu County, Sichuan Province, southeast of this area" ], [ "Yingzhu Niang group", "Exposed", "1:250,000 Gongjue County" ], [ "Yingzhu Niang group", "Exposed", "1:250,000 Ganzi County" ], [ "Yingzhu Niang group", "area", "54m2" ] ] }, { "text": "The Pushuiqiao Formation era was the early Triassic era.", "triple_list": [ [ "Pushuiqiao Group", "Age", "Early Triassic" ] ] }, { "text": "The Bolila Group of this stratigraphic area is distributed in 1:25,000 Nangqian County, Longmala, Ziqunangqian County, Yushu County, Yinghai, Zaduo County, Qinghai Province, 1:25,000 Changdu County, Danzha, Leiwuqi County, Tibet, Naitong, Changdu County, 1:25,000 Jiangda County, Changdu County, Zongreyuzi and other areas. It extends to the west into 1:25,000 Zadu County, Yushu County, north into 1:25,000 Yushu County, south into 1:25,000 Basu County, Gongjue County, exposed area in this area is about 4,648m2.", "triple_list": [ [ "Polira group", "Exposed", "1:25 million Nangqian County, Qinghai Province, Longmala, Ziqunangqian County, Yushu County, Yinghai Province" ], [ "Polira group", "Exposed", "1:250,000 Changdu County, Dazha, Lewuqi County, Tibet" ], [ "Polira group", "Exposed", "Changdu County Naitong" ], [ "Polira group", "Exposed", "1:25 million Jiangda County, Changdu County Zongreyuzi" ], [ "Polira group", "Exposed", "1:25 million Zaduo County" ], [ "Polira group", "Exposed", "1:250,000 Yushu County" ], [ "Polira group", "Exposed", "1:250,000 Basu County" ], [ "Polira group", "Exposed", "Gongjue County" ], [ "Polira group", "area", "4648m2" ] ] }, { "text": "The Aoqu Group is mainly distributed in the southwest of Nangqian County, the northwest of Jinkou, Jinkou, Aga, and the west of Dangqubaqu, Zaduo County, Soluo Yongxiaofugongba and other places, with an exposed area of about 376.3m2.", "triple_list": [ [ "Aoqu Group", "Exposed", "1:25 million Nangqian County, southwest Nangqian County, northwest Nangqian County, northwest Jinkou Aga North South" ], [ "Aoqu Group", "Exposed", "Dangqubaqu West" ], [ "Aoqu Group", "Exposed", "Zaduo County Solo Yong Xiaofu Gongba" ], [ "Aoqu Group", "area", "376.3m2" ] ] }, { "text": "Sandstone slate of the Walasi Formation ────────────────────Serong Temple Formation (1s), thickness 843.48m", "triple_list": [ [ "Sandstone slate of Wala Monastery", "Integration of contacts", "Serong Temple Group" ], [ "Serong Temple Group", "thickness", "843.48m" ] ] }, { "text": "The Kamado East Fault (F106) extends in a northwest direction, and the north, southwest and eastern ends extend out of the map. The length of this area is about 90m.", "triple_list": [ [ "Kamadodong break", "Distribution pattern", "Northwest bending and extending" ], [ "Kamadodong break", "thickness", "90m" ] ] }, { "text": "Gray medium-thick layered unequal grain hard sandy feldstone, 16.80m", "triple_list": [ [ "Gray medium-thick layered unequal grained hard sandy feldstone", "thickness", "16.80m" ] ] }, { "text": "The Jiapila Formation in this section is very small, only found in places north of Leiwuqi Town, Zhongda Village, Lewuqi Town, Changdu County, 1:25 million, with an exposed area of about 3.5m2, and the angle is not integrated above the Late Triassic rock mass and the ancient Jitang rock group in the Paleo-Middle Proterozoic.", "triple_list": [ [ "Kapila Group", "Exposed", "1:250,000 north of Lewuqi Town, Zhongda Village, Bengleiwuqi Town, Changdu County" ], [ "Kapila Group", "area", "3.5m2" ], [ "Kapila Group", "Unconformity contact", "Late Triassic rock body" ], [ "Kapila Group", "Unconformity contact", "Ancient - Jitang Rock Group in the Middle Proterozoic" ] ] }, { "text": "Dark purple-red coarse grained gravel hard sandstone and dark purple-red gray conglomerate interlayer, 42.6m", "triple_list": [ [ "Dark purple-red coarse grained gravel hard sandstone and dark purple-red gray conglomerate interlayer", "thickness", "42.6m" ] ] }, { "text": "The paleobiome of the Dongdaqiao Formation includes bivalve brachiopod gastropods paleoalgae vertebrates, etc.", "triple_list": [ [ "East Bridge Group", "Paleontological", "Bivalves" ], [ "East Bridge Group", "Paleontological", "Brachiopod" ], [ "East Bridge Group", "Paleontological", "Gastropods" ], [ "East Bridge Group", "Paleontological", "Ancient algae" ], [ "East Bridge Group", "Paleontological", "vertebrate" ] ] }, { "text": "The Dedari Ayan Formation (P3d.) is distributed in the northeast corner of Nangqian County, Dedari A-dong Guri A area, spreading in the Jinsha River junction belt in the northwest-south east direction, with an exposed area of about 156.85m2.", "triple_list": [ [ "Have to fight against RiAyan Group", "Exposed", "1:25 million Nangqian County area northeast corner can be beaten - Dongguri" ], [ "Have to fight against RiAyan Group", "Distribution pattern", "Northwest-South East" ], [ "Have to fight against RiAyan Group", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Have to fight against RiAyan Group", "area", "156.85m2" ] ] }, { "text": "Dark gray calcareous feldspar silt sandstone, 149.70m", "triple_list": [ [ "Dark gray calcareous feldspar crush siltstone", "thickness", "149.70m" ] ] }, { "text": "The bivalve Myophoria (Costatoria) cf. inaequicastataPosidonia wengensis is a mid-to-late Triassic molecule.", "triple_list": [ [ "bivalve Myophoria (Costatoria) cf. inaequicastataPosidonia wengensis", "Age", "The Triassic Period" ] ] }, { "text": "Off-white thin-medium-thick layered fine crystal marble, 115.53m", "triple_list": [ [ "Off-white thin-medium-thick layered fine crystal marble", "thickness", "115.53m" ] ] }, { "text": "Gala Group (3d), 941.21m", "triple_list": [ [ "Gala group", "thickness", "941.21m" ] ] }, { "text": "Jidonglong group produced Pseudofusulina cf. gruperaensis (homppsonet Miller), Pseudofusulina ueichowensis Sheng.", "triple_list": [ [ "Ji Donglong Group", "Paleontological", "Pseudofusulina cf. gruperaensis (homppsonet Miller)" ], [ "Ji Donglong Group", "Paleontological", "Pseudofusulina ueichwensis Sheng" ] ] }, { "text": "Dark gray thin layered muddy silt sandstone intersected with yellow thick layered rock-cut sandstone, 148.49m", "triple_list": [ [ "Dark gray thin layered mud silt sandstone inlaid yellow thick layered rock-cut sandstone", "thickness", "148.49m" ] ] }, { "text": "Brown gray thick layered fine-grained calcium silt sandstone sandstone with dark gray thin layered argillic calcium shale, 408.40m", "triple_list": [ [ "Brown gray thick layered fine-grained calcium silt sandstone sandstone sandstone with dark gray thin layered muddy calcium shale", "thickness", "408.40m" ] ] }, { "text": "Overlapping formation Jidonglong Formation Slate with Siltstone ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Jidonglong Formation Slate and Silt Sandstone", "Integration of contacts", "Wang Guo Group" ], [ "Wang Guo Group", "thickness", "1250m" ] ] }, { "text": "Dongque Formation has abundant biological fossils and can be divided into the Eostaffella belt. The main snake molecules include Eostaffella hohsienica, E. mosquensis, E. galinae, E. accepta, E. endothyroidea, E. ozawainellaeformis, Millerella marblensis, Ozawainella sp. wait.", "triple_list": [ [ "Dong Que Group", "Paleontological", "Snake" ], [ "Dong Que Group", "Paleontological", "Eostaffella hohsienica" ], [ "Dong Que Group", "Paleontological", "E. mosquensis" ], [ "Dong Que Group", "Paleontological", "E. galinae" ], [ "Dong Que Group", "Paleontological", "E. accepta" ], [ "Dong Que Group", "Paleontological", "E. endothyroidea" ], [ "Dong Que Group", "Paleontological", "E. ozawainellaeformis" ], [ "Dong Que Group", "Paleontological", "Millerella marblensis" ], [ "Dong Que Group", "Paleontological", "Ozawainella sp." ] ] }, { "text": "The Youxi group is a set of volcanic rock systems such as calcium-alkali basalt andshanyan Ying'anite, with a thickness of more than 2350m.", "triple_list": [ [ "Youxi Group", "Lithology", "Calcium alkaline basalt" ], [ "Youxi Group", "Lithology", "Andanyan" ], [ "Youxi Group", "Lithology", "Ying'an Rock" ], [ "Youxi Group", "Belongs to", "Volcanic rock system" ], [ "Youxi Group", "thickness", "2350m" ] ] }, { "text": "The volcanic rocks in the Xiayacun Group of the Late Permian are distributed in the Tuoba area of Changdu County. They are a set of neutral volcanic clastic rock-medium-basic lava. They consist of four eruption rhythms of Anshan tuff Anshan volcanic breccia Anshan lava, with a thickness of up to 165m.", "triple_list": [ [ "Volcanic rocks in Xiaya Village Group, Late Permian", "Exposed", "Tauba, Changdu County" ], [ "Volcanic rocks in Xiaya Village Group, Late Permian", "Belongs to", "Neutral volcanic rock-medium lava" ], [ "Volcanic rocks in Xiaya Village Group, Late Permian", "Lithology", "Andesan tuff" ], [ "Volcanic rocks in Xiaya Village Group, Late Permian", "Lithology", "Andesan volcanic breccia" ], [ "Volcanic rocks in Xiaya Village Group, Late Permian", "Lithology", "Andan Lava" ], [ "Volcanic rocks in Xiaya Village Group, Late Permian", "thickness", "165m" ] ] }, { "text": "The geological era of Licha Group in this district was the early Permian.", "triple_list": [ [ "Richa Group", "Age", "Early Permian" ] ] }, { "text": "Quga Temple Group (3q) thickness 1179m", "triple_list": [ [ "Quga Temple Group", "thickness", "1179m" ] ] }, { "text": "To sum up, the Mangcuo Formation in this area is composed of gray-dark gray limestone biological clastic limestone dolomite limestone shale sandstone, etc., and produces erpentine brachiopods bryozoa hilaria sea lily coral foraminifer trilobites interstitial aphrodisiac tung-shaped piercing gastropods, etc., with a total thickness of 580.5m.", "triple_list": [ [ "Rude group", "Lithology", "Grey dark grey limestone" ], [ "Rude group", "Lithology", "Bioclastic limestone" ], [ "Rude group", "Lithology", "Dolomites limestone" ], [ "Rude group", "Lithology", "shale" ], [ "Rude group", "Lithology", "sandstone" ], [ "Rude group", "Paleontological", "Snake" ], [ "Rude group", "Paleontological", "Brachiopod" ], [ "Rude group", "Paleontological", "Bruceworm" ], [ "Rude group", "Paleontological", "Chrysanthemum" ], [ "Rude group", "Paleontological", "sea lily" ], [ "Rude group", "Paleontological", "coral" ], [ "Rude group", "Paleontological", "Foraminifera" ], [ "Rude group", "Paleontological", "Trileleaf" ], [ "Rude group", "Paleontological", "Aphrodisiac" ], [ "Rude group", "Paleontological", "Teeth thorn" ], [ "Rude group", "Paleontological", "Gastropod" ], [ "Rude group", "thickness", "580.5m" ] ] }, { "text": "The Dongque Formation is relatively stable in the region, but the biological appearance changes greatly, mainly carbonate rocks and volcanic rocks, with the increase of sandstones to the north, which generally reflects the active marginal sea sedimentation.", "triple_list": [ [ "Dong Que Group", "Lithology", "Carbonate rock" ], [ "Dong Que Group", "Lithology", "Volcanic rocks" ], [ "Dong Que Group", "Lithology", "sandstone" ], [ "Dong Que Group", "Belongs to", "marginal sea sedimentation" ] ] }, { "text": "The Polila Group era was the Noli period of the late Triassic period.", "triple_list": [ [ "Polira group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Overhead strata Polila Formation (3b) Bioclastic limestone ────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polira group", "Lithology", "Bioclastic limestone" ], [ "Polira group", "Integration of contacts", "Kapila Group" ], [ "Polira group", "thickness", "141.21m" ] ] }, { "text": "The fake thickness of the Jiarieyan Formation (P3j.) is 1377.91m", "triple_list": [ [ "Gariei rock formation", "thickness", "1377.91m" ] ] }, { "text": "Gray metamorphic medium-grained quartz sandstone, 44.01m", "triple_list": [ [ "Gray metamorphic medium-grained quartz sandstone", "thickness", "44.01m" ] ] }, { "text": "Gray medium-thick layer contains shiny limestone in biological debris, producing Ozawainella sp. O.vozhgalica, 7.76m", "triple_list": [ [ "Gray medium-thick layer of grey limestone containing biological debris inner clastics", "Paleontological", "Ozawainella sp. O.vozhgalica" ], [ "Gray medium-thick layer of grey limestone containing biological debris inner clastics", "thickness", "7.76m" ] ] }, { "text": "Gray light gray medium-thick layer of rock-cut quartz fine sandstone rock-cut quartz silt sandstone gray-black serous clay slate is interlayered, 120.78m", "triple_list": [ [ "Gray light gray medium-thick layer of rock-cut quartz fine sandstone rock-cut quartz silt sandstone gray-black serous clay slate interlayer", "thickness", "120.78m" ] ] }, { "text": "Light gray thick layer of limestone with oligate limestone and light fleshy red limestone, producing parasalites Paranannites sp. Proptychitoioides sp. Prosphingites cf.involutus, 189.00m", "triple_list": [ [ "Light gray thick layer limestone with ovalite limestone and light fleshy red limestone", "Paleontological", "Ammonites Paranannites sp." ], [ "Light gray thick layer limestone with ovalite limestone and light fleshy red limestone", "Paleontological", "Proptychitoioides sp." ], [ "Light gray thick layer limestone with ovalite limestone and light fleshy red limestone", "Paleontological", "Prosphingites cf.involutus" ], [ "Light gray thick layer limestone with ovalite limestone and light fleshy red limestone", "thickness", "189.00m" ] ] }, { "text": "Gray thick layered medium-fine-grained feldspar sandstone sandstone with gray medium-thick layered bioclad powder-containing limestone, producing bivalve Halobia pluriradiata H. rugosa H. cordillerana, 466.75m", "triple_list": [ [ "Gray thick layered medium-fine-grained feldspar sandstone sandstone with gray medium-thick layered bioclad powder crystal limestone", "Paleontological", "Bivalve Halobia pluriradiata H. rugosa H. cordillerana" ], [ "Gray thick layered medium-fine-grained feldspar sandstone sandstone with gray medium-thick layered bioclad powder crystal limestone", "thickness", "466.75m" ] ] }, { "text": "From the above section, it can be seen that the Jiapila Formation in this stratigraphic area consists of purple-red, gray-green sandstone conglomerate mudstone, etc., and produces bivalves, which are super-covered and discontinuous on the Proterozoic Carboniferous-Permian system, and integrate with the overly covered Borila Formation (3b), and are deposited in a set of river-shore shallow marine sand amycladic clastic rocks.", "triple_list": [ [ "Kapila Group", "Lithology", "purple-red gray-green sandstone" ], [ "Kapila Group", "Lithology", "Polygon" ], [ "Kapila Group", "Lithology", "Mudstone" ], [ "Kapila Group", "Lithology", "Marlite" ], [ "Kapila Group", "Paleontological", "Bivalves" ], [ "Kapila Group", "Unconformity contact", "Carboniferous-Permian" ], [ "Kapila Group", "Integration of contacts", "Polira group" ], [ "Kapila Group", "Belongs to", "River-Shallow Marine Sand Clarinet Rock Sedimentation" ] ] }, { "text": "Proterozoic granite was distributed in the Lewuqi-Dongdashan invading rock belt and the Jiangda-Decin invading rock belt, and was produced in the Paleozoic-Mid-Proterozoic strata.", "triple_list": [ [ "Proterozoic granite", "Exposed", "Lewuqi-Dongdashan invasion rock belt" ], [ "Proterozoic granite", "Exposed", "Jiangda-Deqin invades the rock belt" ], [ "Proterozoic granite", "Located at", "Ancient—Midproterozoic strata" ] ] }, { "text": "Neocalamites meriani aenoopteris leclerei is produced in the area of Shazhaguo, Lewuqi County; Neocalamites meriani aenoopteris leclerei is produced in the section, and integrated under the Early Jurassic Wanbu Formation.", "triple_list": [ [ "Lewuqi County Shazaguo", "Paleontological", "bivalve Cardium(ulongocardium) nequam" ], [ "Lewuqi County Shazaguo", "Paleontological", "Plant Neocalamites meriani aeniopteris leclerei" ], [ "Lewuqi County Shazaguo", "Integration of contacts", "Early Jurassic Wanbu Group" ] ] }, { "text": "Gray-white middle layer glitter cemented bioclass limestone with gray-yellow thin layer containing bioclass clay rock, producing serpentodofusulina cf. Houchangensis, Schwagerinidae; Coral achylasma sp. Allotropiophyllum sp. Lonocyclicus sp. Trilobite Phillipsia sp. Baircia sp. Acratia sp.; Teeth-shaped spines Streptognathodus sp. and brachiopods, 32.5m ──────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Psendofusulina cf. Houchangensis" ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Schwagerinidae" ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "coral achylasma sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Allotropiophyllum sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Lonocyclicus sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Trilobite Phillipsia sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Bairclia sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Acratia sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Streptognathodus sp." ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Paleontological", "Brachiopod" ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "thickness", "32.5m" ], [ "Gray gray-white middle layer glitter cemented bioclass limestone with gray yellow thin layer of bioclass clay rock", "Integration of contacts", "Licha Group limestone slate" ] ] }, { "text": "The fake thickness of Dedari Ayan Formation (P3d.) is 2785.99m", "triple_list": [ [ "Have to fight against RiAyan Group", "thickness", "2785.99m" ] ] }, { "text": "The lithologies of Ningduoyan Group (Pt1-2Nd.) are gneiss granite schist marble oblique amphibole, etc.", "triple_list": [ [ "Ningduoyan Group", "Lithology", "Gneis" ], [ "Ningduoyan Group", "Lithology", "Granular rock" ], [ "Ningduoyan Group", "Lithology", "Rock Schist" ], [ "Ningduoyan Group", "Lithology", "Dali Rock" ], [ "Ningduoyan Group", "Lithology", "oblique angular amphibole" ] ] }, { "text": "The lithology of the lower part of the Serongsi Formation is mainly gray-white thick-block layer oasis limestone pseudoasis limestone, with light fleshy red gray clastic limestone tuff gravel limestone and gray-green calcified Andanite tuff.", "triple_list": [ [ "Serong Temple Group", "Lithology", "Off-white thick block layer oasis limestone" ], [ "Serong Temple Group", "Lithology", "Pseudo-oalite limestone" ], [ "Serong Temple Group", "Lithology", "Light fleshy red grey clastic limestone" ], [ "Serong Temple Group", "Lithology", "Tuffy gravel limestone" ], [ "Serong Temple Group", "Lithology", "Gray-green Calcium Andesan Tuff" ] ] }, { "text": "The Yurang Formation was built for a set of continental marginal clastic clay rock-sand carbonate rock. The main lithologies were sericite silt sandy sericite bioclastic limestone tuff slate limestone quartz sandstone silt sandstone, etc., which were deposited on the coast of the continental marginal shore - shallow sea.", "triple_list": [ [ "Russia team", "Belongs to", "Construction of clay rocks and carbonate rocks on the edge of continental edges" ], [ "Russia team", "Lithology", "Serous slab" ], [ "Russia team", "Lithology", "Silty serous slate" ], [ "Russia team", "Lithology", "Bioclass limestone" ], [ "Russia team", "Lithology", "Tuff matter slate" ], [ "Russia team", "Lithology", "Rock cutting quartz sandstone" ], [ "Russia team", "Lithology", "Siltstone" ], [ "Russia team", "Belongs to", "Continental margin coast—shallow sea sedimentation" ] ] }, { "text": "In summary, the Tuoba Group belongs to the late Permian.", "triple_list": [ [ "Tuoba Group", "Age", "Late Permian" ] ] }, { "text": "Variety silt-containing bioamilite and clay interlayer, 27.64m", "triple_list": [ [ "Variety silt-containing biological amylin and clay interlayer", "thickness", "27.64m" ] ] }, { "text": "The Qugasi Formation consists of a dark gray crystalline limestone slate sandstone, a mixed medium-basal volcanic rock, etc., and a dental shaped spiny sea lily bivalve brachiopod coral, with a total exposed thickness of >1179m.", "triple_list": [ [ "Quga Temple Group", "Lithology", "Gray dark gray crystalline limestone" ], [ "Quga Temple Group", "Lithology", "Slate" ], [ "Quga Temple Group", "Lithology", "Qianmeiyan" ], [ "Quga Temple Group", "Lithology", "sandstone" ], [ "Quga Temple Group", "Lithology", "Basal medium-basal volcanic rocks" ], [ "Quga Temple Group", "Paleontological", "Teeth thorn" ], [ "Quga Temple Group", "Paleontological", "sea lily" ], [ "Quga Temple Group", "Paleontological", "Bivalves" ], [ "Quga Temple Group", "Paleontological", "Brachiopod" ], [ "Quga Temple Group", "Paleontological", "coral" ] ] }, { "text": "Gray light gray (local flesh-red) giant layer of glittery cemented algae gravel limestone, producing Schubertella sp. Schwagerinidae and coral Paotomichelinia sp., 60.08m", "triple_list": [ [ "Gray light gray (local flesh red) giant layer of glitter cemented algae gravel limestone", "Paleontological", "Schubertella sp." ], [ "Gray light gray (local flesh red) giant layer of glitter cemented algae gravel limestone", "Paleontological", "Schwagerinidae" ], [ "Gray light gray (local flesh red) giant layer of glitter cemented algae gravel limestone", "Paleontological", "Coral Paotomichelinia sp." ], [ "Gray light gray (local flesh red) giant layer of glitter cemented algae gravel limestone", "thickness", "60.08m" ] ] }, { "text": "Overhead siltstone clay rock of Dugala Formation ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Siltstone clay rock of the Dugala Formation", "Integration of contacts", "Adula Group" ], [ "Adula Group", "thickness", "1897.90m" ] ] }, { "text": "Erchang Granular porphyry is concentrated in the area of Chongbo Longduoxiasongduo, Mangma, Changdu County, and invaded the Jiapila Group (3j) marathon group (1-2m).", "triple_list": [ [ "Erchang granite", "Exposed", "Changdu County Mangmai Chongbo Longduo Xia Songduo" ], [ "Erchang granite", "Invade", "Kapila Group" ], [ "Erchang granite", "Invade", "Marathon multiple sets" ] ] }, { "text": "Gray-black sandy limestone gravel limestone, brachiopod-producing Dictyoclostus sp., 58.10m", "triple_list": [ [ "Gray-black sandy limestone gravel limestone", "Paleontological", "Brachiopod Dictyoclostus sp." ], [ "Gray-black sandy limestone gravel limestone", "thickness", "58.10m" ] ] }, { "text": "Black Thousand-shaped serous slate, >171.2m, fault contact, Gangtuoyan Formation (P1g.) schist", "triple_list": [ [ "Black Thousand-shaped serous slate", "thickness", "171.2m" ], [ "Black Thousand-shaped serous slate", "Fault contact", "Gangtuoyan Formation" ], [ "Gangtuoyan Formation", "Lithology", "Rock Schist" ] ] }, { "text": "The Wangbu Formation is generally mainly composed of gray-gray green purple-red purple sandstone mudstone, and is composed of a small amount of limestone, which produces bivalve gastropod spores, and has a total exposed thickness of 505.72-583.84m, which is a river phase deposition.", "triple_list": [ [ "Wang Bu Group", "Lithology", "Gray gray green purple red purple sandstone" ], [ "Wang Bu Group", "Lithology", "Mudstone" ], [ "Wang Bu Group", "Lithology", "Limestone" ], [ "Wang Bu Group", "Paleontological", "Bivalves" ], [ "Wang Bu Group", "Paleontological", "Gastropod" ], [ "Wang Bu Group", "Paleontological", "Plant spore powder" ], [ "Wang Bu Group", "thickness", "505.72-583.84m" ], [ "Wang Bu Group", "Belongs to", "River phase sedimentation" ] ] }, { "text": "Gray-dark gray thick layered limestone with gray thin layer of feldspar quartz sandstone, producing bivalve Crurirhynchia bagenae, Eumorphotis (Asosella) sp., 281.2m ───────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Gray-dark gray thick layered limestone with gray thin layer of feldspar quartz sandstone", "Paleontological", "bivalve Crurirhynchia bagenae" ], [ "Gray-dark gray thick layered limestone with gray thin layer of feldspar quartz sandstone", "Paleontological", "Eumorphotis (Asosella) sp." ], [ "Gray-dark gray thick layered limestone with gray thin layer of feldspar quartz sandstone", "thickness", "281.2m" ], [ "Gray-dark gray thick layered limestone with gray thin layer of feldspar quartz sandstone", "Integration of contacts", "Sandstone slate of Adula Formation" ] ] }, { "text": "Light gray green block layer altered rhizomorphic crystalline crystalline tuff with a fluid structure, 318.81m", "triple_list": [ [ "Light gray green block layer altered rhizomorphic crystalline crystalline tuff", "Develop", "Flow-like structure" ], [ "Light gray green block layer altered rhizomorphic crystalline crystalline tuff", "thickness", "318.81m" ] ] }, { "text": "Light gray medium-thick layer of crystalline limestone, weathered to see many calcite particles or clumps, 150m", "triple_list": [ [ "Light gray medium-thick layer of crystalline limestone", "Contained", "Calcite granules" ], [ "Light gray medium-thick layer of crystalline limestone", "Contained", "Clusters" ], [ "Light gray medium-thick layer of crystalline limestone", "thickness", "150m" ] ] }, { "text": "Gray light gray metamorphic plate-like muddy siltstone, horizontal laminar Develop, 9.03m", "triple_list": [ [ "Gray light gray metamorphic silt sandstone", "Develop", "Horizontal stratification" ], [ "Gray light gray metamorphic silt sandstone", "thickness", "9.03m" ] ] }, { "text": "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone; Eostaffella sp. (E. mosquensis); Lithostrotion cf. irregular Caninia sp. Correnia sp. Dibunophyllum sp.; Gigantoproductus cf. rectestrius G. edelbogensis, 23.22m────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone", "Paleontological", "Eostaffella sp.(E. mosquensis)" ], [ "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone", "Paleontological", "Lithostrotion cf. irregulare Caninia sp. Correnia sp. Dibunophyllum sp." ], [ "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone", "Paleontological", "Brachiopod Gigantoproductus cf. rectestrius G. edelbogensis" ], [ "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone", "thickness", "23.22m" ], [ "Off-white medium-thin layer of powder crystal limestone intersected with biolimestone", "Integration of contacts", "Wuqingna Formation Sandstone Limestone" ] ] }, { "text": "Dark gray-grey-black thin-middle siliceous rock, 6.76m", "triple_list": [ [ "Dark gray-grey-black thin-middle siliceous rock", "thickness", "6.76m" ] ] }, { "text": "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone, 95.1m", "triple_list": [ [ "Light gray medium-thick layered medium-fine-grained feldspar quartz sandstone", "thickness", "95.1m" ] ] }, { "text": "The Tuoba Formation (P3t) is composed of gray-gray black silt quartz sandstone shale charcoal shale marl, limestone coal line, etc., and produces plant bivalve brachiopod corals, etc., with a total thickness of 1362.9m.", "triple_list": [ [ "Tuoba Group", "Lithology", "Gray-gray black siltstone" ], [ "Tuoba Group", "Lithology", "Quartz sandstone" ], [ "Tuoba Group", "Lithology", "shale" ], [ "Tuoba Group", "Lithology", "Carbon shale" ], [ "Tuoba Group", "Lithology", "Marlite" ], [ "Tuoba Group", "Lithology", "Limestone" ], [ "Tuoba Group", "Lithology", "Coal line" ], [ "Tuoba Group", "Paleontological", "Plant bivalves" ], [ "Tuoba Group", "Paleontological", "Brachiopod" ], [ "Tuoba Group", "Paleontological", "coral" ], [ "Tuoba Group", "Paleontological", "Snake" ], [ "Tuoba Group", "thickness", "1362.9m" ] ] }, { "text": "The distribution of schist is relatively small, mainly seen in the upper section of Ningduoyan Group, including sericite schist and dolomite schist.", "triple_list": [ [ "Rock Schist", "Exposed", "Ningduoyan Group Shangyan Section" ], [ "Rock Schist", "Contained", "serous quartz schist" ], [ "Rock Schist", "Contained", "Dolomite Quartz Schist" ] ] }, { "text": "Paracrochordiceras sp. Hollandites sp. Leiophyllites sp., invaded by the late Triassic quartz diorite (ο3), 180.10m", "triple_list": [ [ "Slate", "Paleontological", "Paracrochordiceras sp." ], [ "Slate", "Paleontological", "Hollandites sp." ], [ "Slate", "Paleontological", "Leiophyllites sp." ], [ "Slate", "Invade", "Late Triassic Quartz Diorite" ], [ "Slate", "thickness", "180.10m" ] ] }, { "text": "The Holocene loose deposits are distributed in various parts of this area. According to the main landforms of the formation type of deposits, lithologic equality characteristics include alluvial (Qhal), flooding (Qhpl), spring and Hua accumulation (Qhcas), slope accumulation (Qhdl), glacier accumulation (Qhgl), underground river accumulation (Qhcall), etc.", "triple_list": [ [ "Loose accumulations of Holocene", "Contained", "Alluvial" ], [ "Loose accumulations of Holocene", "Contained", "Hong Ji" ], [ "Loose accumulations of Holocene", "Contained", "Quanhua accumulation" ], [ "Loose accumulations of Holocene", "Contained", "Slope accumulation" ], [ "Loose accumulations of Holocene", "Contained", "Remaining" ], [ "Loose accumulations of Holocene", "Contained", "Glacier accumulation" ], [ "Loose accumulations of Holocene", "Contained", "Underground river accumulation" ] ] }, { "text": "Overhead strata Polila Formation limestone ───────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polila Formation Limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "650.9m" ] ] }, { "text": "Gray medium-thick layered limestone conglomerate, 69.84m", "triple_list": [ [ "Gray medium-thick layered limestone gravel", "thickness", "69.84m" ] ] }, { "text": "The Permian strata are distributed in the Chamdo-Mangkang strata and the Jiangda-Deqin strata.", "triple_list": [ [ "Permian strata", "Stratigraphical zoning", "Chamdo-Mangkang Stratigraphic Zone" ], [ "Permian strata", "Stratigraphical zoning", "Jiangda-Deqin Stratigraphic Zone" ] ] }, { "text": "Late Triassic II-Change Granite, 5.00m, angle not integrated late Triassic II-Change Granite (η3)", "triple_list": [ [ "Late Triassic Granite", "thickness", "5.00m" ], [ "Late Triassic Granite", "Unconformity contact", "Late Triassic Granite" ] ] }, { "text": "Dark gray medium-thick layered impure limestone sandstone, 120m", "triple_list": [ [ "Dark gray medium-thick layered impure limestone sandstone", "thickness", "120m" ] ] }, { "text": "The Russian Formation is a shallow marine terrestrial sand mud carbonate sedimentation.", "triple_list": [ [ "Russia team", "Belongs to", "Shallow marine terrestrial sand mud carbonate sedimentation" ] ] }, { "text": "The era of the Degaila group belongs to the middle and late triassic period.", "triple_list": [ [ "Gala group", "Age", "Late Triassic" ] ] }, { "text": "Gray medium-grained quartz sandstone, 26.64m", "triple_list": [ [ "Gray medium-grained quartz sandstone", "thickness", "26.64m" ] ] }, { "text": "The irregular rock plants in the Erchang granite mass invaded multiple marathon groups and were then covered by the Kapila group.", "triple_list": [ [ "Second Chang granite body", "Distribution pattern", "Irregular rock plants" ], [ "Second Chang granite body", "Invade", "Marathon multiple sets" ], [ "Second Chang granite body", "Unconformity contact", "Kapila Group" ] ] }, { "text": "Medium acidic crystal chip glass tuff is gray-white gray-green, with a changeable tuff structure and a layered structure.", "triple_list": [ [ "Medium acidic crystal chip glass tuff", "Distribution pattern", "Variable tuff structure" ], [ "Medium acidic crystal chip glass tuff", "Develop", "Layered structure" ] ] }, { "text": "Gray green thick-block layer altered andes, 39.47m", "triple_list": [ [ "Gray green thick-block layer alteration andesite", "thickness", "39.47m" ] ] }, { "text": "Gray-green medium-layered medium-acid tuff, 50m", "triple_list": [ [ "Gray-green medium-layered medium-acid tuff", "thickness", "50m" ] ] }, { "text": "The late Permian brachiopod group Leptodus—Oldhamina—Spirifer combination zone, the main species are Leptodus sp. Oldhamina sp., O. cf. squamosa Spirifer sp.", "triple_list": [ [ "Late Permian brachiopods Leptodus—Oldhamina—Spirifer combination belt", "Paleontological", "Leptodus sp." ], [ "Late Permian brachiopods Leptodus—Oldhamina—Spirifer combination belt", "Paleontological", "Oldhamina sp." ], [ "Late Permian brachiopods Leptodus—Oldhamina—Spirifer combination belt", "Paleontological", "O. cf. squamosa Spirifer sp." ] ] }, { "text": "Purple-red thick layer of muddy silt sandstone intersected with purple-red thick layer of rock-cut sandstone, 38.44m ──────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Purple-red thick layer of muddy silt sandstone intersects with purple-red thick layer of rock-cut sandstone", "thickness", "38.44m" ], [ "Purple-red thick layer of muddy silt sandstone intersects with purple-red thick layer of rock-cut sandstone", "Integration of contacts", "East Bridge Group" ], [ "East Bridge Group", "Lithology", "Fine-grained rock" ], [ "East Bridge Group", "Lithology", "Chop sandstone" ], [ "East Bridge Group", "Lithology", "Purple-gray gravel coarse sandstone" ] ] }, { "text": "The rock mass is exposed in Niangxi Township, Jiangda County, Jiaduoling, Xiaosumang Township, and is spread in NW-SE.", "triple_list": [ [ "Rock body", "Exposed", "Dizhong, Niangxi Township, Jiangda County, Jiaduoling, Xiaosumang Township" ], [ "Rock body", "Distribution pattern", "NW-SE to the spread cloth" ] ] }, { "text": "The bivalve Hiatella-Lilingella combination belt is produced in the lower part of the Renqingka Wangbu Form in Lewuqi County.", "triple_list": [ [ "Bivalve Hiatella-Lilingella combination belt", "Located at", "Lewuqi County Renqingka Wangbu Group" ] ] }, { "text": "The Luodongyan group is a set of deep-water ocean basin-trench sedimentary environment.", "triple_list": [ [ "Luodongyan Group", "Belongs to", "Deepwater ocean basin-trench sedimentary environment" ] ] }, { "text": "Black clouds (two clouds) Two long gneisses have scale-grained metamorphic structures and scalyx-like structures.", "triple_list": [ [ "Black clouds (two clouds) Two lengths of gneis", "Distribution pattern", "Scale grainy metamorphic structure" ], [ "Black clouds (two clouds) Two lengths of gneis", "Develop", "Throttle structure" ] ] }, { "text": "Permian Mangcuo Group limestone in the overlying strata──────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "The Mangcuo Group of the Middle Permian", "Integration of contacts", "Richa Group" ], [ "Richa Group", "thickness", "1316.05m" ] ] }, { "text": "The Wujiangda-Deqin strata are well developed in the Triassic strata, and from bottom to top are divided into the Early Triassic Pushuiqiao Serong Temple Group (1s), the Middle Triassic Wala Temple Group (2w), the Late Triassic East Unit Group (3dd), Gongye Nong Group (3g) Cave Deck (3d), Apira Group (3j) Polila Group (3b) Adula Group (3a) Digaira Group (3d).", "triple_list": [ [ "Wujiangda-Deqin Stratigraphic Zone", "Outcrop", "Triassic strata" ], [ "Triassic strata", "Outcrop", "Serong Temple Group of Pushuiqiao in the Early Triassic Period" ], [ "Triassic strata", "Outcrop", "The Wala Monastery of the Middle Triassic" ], [ "Triassic strata", "Outcrop", "The East-End Group of the Late Triassic" ], [ "Triassic strata", "Outcrop", "The man also works in groups" ], [ "Triassic strata", "Outcrop", "Hole deck" ], [ "Triassic strata", "Outcrop", "Kapila Group" ], [ "Triassic strata", "Outcrop", "Polira group" ], [ "Triassic strata", "Outcrop", "Adula Group" ], [ "Triassic strata", "Outcrop", "Gala group" ] ] }, { "text": "The metamorphic rock types of the Russian-Rang Formation include sericite silt sandy sericite metamorphic fine-grained quartz hybrid sandstone metamorphic fine-grained quartz sandstone metamorphic fine-medium-grained quartz sandstone metamorphic quartz sandstone metamorphic quartz fine conglomerates, etc.", "triple_list": [ [ "The Russian group metamorphic rock", "Lithology", "Serous slab" ], [ "The Russian group metamorphic rock", "Lithology", "Silty serous slate" ], [ "The Russian group metamorphic rock", "Lithology", "Metamorphic fine-grained rock" ], [ "The Russian group metamorphic rock", "Lithology", "quartz sandstone" ], [ "The Russian group metamorphic rock", "Lithology", "Metamorphic fine-grained rock" ], [ "The Russian group metamorphic rock", "Lithology", "Chissite sandstone" ], [ "The Russian group metamorphic rock", "Lithology", "Metamorphic fine-medium-grain rock" ], [ "The Russian group metamorphic rock", "Lithology", "quartz sandstone" ], [ "The Russian group metamorphic rock", "Lithology", "Metamorphic quartz fine gravel" ] ] }, { "text": "Off-white thick-block layer osa limestone, 143.61m", "triple_list": [ [ "Off-white thick-block layer oasis limestone", "thickness", "143.61m" ] ] }, { "text": "Gray thick-block layered metamorphic medium-medium-fine-grained quartz sandstone; not seen, 473.01m", "triple_list": [ [ "Gray thick-block layered metamorphic medium-medium-fine-grained quartz sandstone", "thickness", "473.01m" ] ] }, { "text": "The Gongjue Formation of the Paleo-Monarchy was deposited in the Nangqian-Gongjuela sub-basin, distributed in the 1:25,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-125,000-126, in the map, the area in the map was about 3746m2, which was deposited in a set of red coarse debris grinding stone.", "triple_list": [ [ "Gongjue Group of the Paleo-Morning", "Belongs to", "Sedimentation of Nangqian-Gongjuelafen Basin" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:250,000 Changdu County, Malan Leliniang, Malong Nangqian County, and Ka Changdu County Gong Gun Lane" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:25 million Nangqian County, Nangqian County, Longmuda, Yushu County, Nangqian County, Nangqian County" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:25 million Jiangda County Fenjiangda County Sori Village, Baima Village, Zedi Niuchang, Baima Village - Xiangpi, Gongjue County (check the bottom)" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:25 million Zaduo County" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:250,000 Dingqing County" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:250,000 Yushu County" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:250,000 Shiqu County" ], [ "Gongjue Group of the Paleo-Morning", "Exposed", "1:250,000 Gongjue County" ], [ "Gongjue Group of the Paleo-Morning", "area", "3746m2" ], [ "Gongjue Group of the Paleo-Morning", "Belongs to", "Red coarse debris grinding stone deposit" ] ] }, { "text": "Gray-green mesolayer meso-basic crystalline tuff, 34.18m", "triple_list": [ [ "Gray-green mesolayer mesoplasmic crystalline tuff", "thickness", "34.18m" ] ] }, { "text": "Small sole set (J3x) thickness 1264.03m", "triple_list": [ [ "Small Sole deck group", "thickness", "1264.03m" ] ] }, { "text": "The geological era of the Aoqu Formation should be the late Carboniferous Luosu period-Dala period.", "triple_list": [ [ "Aoqu Group", "Age", "Late Carboniferous Luosu Period-Dala Period" ] ] }, { "text": "Andesite is gray-green, with interlaced structures and block-like structures.", "triple_list": [ [ "Andanyan", "Distribution pattern", "Spotted structure" ], [ "Andanyan", "Distribution pattern", "Interwoven structure" ], [ "Andanyan", "Develop", "Blocky structure" ] ] }, { "text": "The Holocene flood accumulation materials (Qhpl) are mainly distributed in the areas of water systems such as the Qulancang River and the Jinsha River and their tributary valleys, and are often in a fan-shaped landform.", "triple_list": [ [ "Holocene Hong accumulation", "Exposed", "Ziquzhao Quziqugai Qugai Qulancang River and Jinsha River and its tributary valleys" ], [ "Holocene Hong accumulation", "Distribution pattern", "Fan-shaped landform" ] ] }, { "text": "The Russian-Jian-Zhuka strata are divided into the Triassic strata, including the Mid-Triassic strata, and the Mid-Late Triassic strata.", "triple_list": [ [ "Russia-Zhuka Stratigraphic Zone", "Outcrop", "Triassic strata" ], [ "Triassic strata", "Outcrop", "The Russian group of the Middle Triassic" ], [ "Triassic strata", "Outcrop", "Middle-late Three-Stillary Bamboo Card Group" ] ] }, { "text": "The andesite is light green, the residual filling structure is changed, the pore-like structure, and the block-like structure.", "triple_list": [ [ "Andyama", "Distribution pattern", "Structure of the variable residual filling room" ], [ "Andyama", "Develop", "Stomatal structure" ], [ "Andyama", "Develop", "Blocky structure" ] ] }, { "text": "The Lewuqi-Zuogong metamorphic rock belt is located in the southwest of this area, and is spread toward NW-SE.", "triple_list": [ [ "Lewuqi-Zuogong metamorphic rock belt", "Located at", "Southwest of this area" ], [ "Lewuqi-Zuogong metamorphic rock belt", "Distribution pattern", "NW-SE Towards" ] ] }, { "text": "The Ningduoyan group is followed by gneiss as the main schist, and a small amount of pyroxene granular rock appears in the lower part.", "triple_list": [ [ "Ningduoyan Group", "Lithology", "Gneis" ], [ "Ningduoyan Group", "Lithology", "Pyroxene Granular Rock" ] ] }, { "text": "Diorite species are exposed in Jiezonglong Xiewolong Renda North Dongpu North and other places.", "triple_list": [ [ "Diorite", "Exposed", "Xie Zonglong Xie Wolong Renda North Dongpu North" ] ] }, { "text": "The plagiaract amphibole has a cylindrical crystal structure and a block-like structure. The main mineral components are ordinary amphibole (3869), plagiaractite, and a small amount of mica quartz.", "triple_list": [ [ "oblique angular amphibole", "Distribution pattern", "Cylindrical crystal structure" ], [ "oblique angular amphibole", "Develop", "Blocky structure" ], [ "oblique angular amphibole", "Contained", "Azurite" ], [ "oblique angular amphibole", "Contained", "Plagioclase" ], [ "oblique angular amphibole", "Contained", "Mica quartz" ] ] }, { "text": "The Wala Monastery era was the Middle Triassic period.", "triple_list": [ [ "Wala Temple Group", "Age", "Middle Triassic" ] ] }, { "text": "Gray-black slate with fine-grained cuts feldspar sandstone, 16.89m", "triple_list": [ [ "Gray-black slate with fine-grained cuts feldspar sandstone", "thickness", "16.89m" ] ] }, { "text": "Ash-blue-gray medium-thick layer of metamorphic silty fine-grained feldspar quartz hybrid sandstone, 32.36m", "triple_list": [ [ "Ash-green medium-thick layer of metamorphic silt fine-grained feldspar quartz hybrid sandstone", "thickness", "32.36m" ] ] }, { "text": "Yellow-gray medium-thick layer of metamorphic unequal grained rock debris quartz sandstone with dark gray slate, 36.12m", "triple_list": [ [ "Yellow-gray medium-thick layer metamorphic unequal grained rock debris quartz sandstone sandstone with dark gray slate", "thickness", "36.12m" ] ] }, { "text": "Granular porphyry is exposed in Ruoyela Yulong Duoxia Songduobei and other places, with a total area of 7.85m2, accounting for 0.35% of the total area of invading rocks.", "triple_list": [ [ "Granular porphyry", "Exposed", "If you also pull the jade dragon, the clouds, the pine trees, the north" ], [ "Granular porphyry", "area", "7.85m2" ] ] }, { "text": "The original rock of the Riazenangyan Formation is a set of basic volcanic rocks with a small amount of clastic rock clay formations.", "triple_list": [ [ "Riazenongyan Formation", "Lithology", "Basic volcanic rocks" ], [ "Riazenongyan Formation", "Lithology", "Clastite" ], [ "Riazenongyan Formation", "Lithology", "Clay rock" ] ] }, { "text": "Grey light grey glitter cemented bioclastic limestone, produced by winding Pseudofusulina crassispira Schwagerina sp., 59.7m", "triple_list": [ [ "Grey light grey glitter cemented bioclastic limestone", "Paleontological", "snail Pseudofusulina crassispira Schwagerina sp." ], [ "Grey light grey glitter cemented bioclastic limestone", "thickness", "59.7m" ] ] }, { "text": "Jidonglong Group (P1j), 509.4m", "triple_list": [ [ "Ji Donglong Group", "thickness", "509.4m" ] ] }, { "text": "Medium-thick layered medium-fine-grained feldspar fragment quartz sandstone, thinning or sharply extinct along the direction, 32.36m", "triple_list": [ [ "Medium-thick layered medium-fine-grained feldspar cuttings quartz sandstone", "thickness", "32.36m" ] ] }, { "text": "Siltstone of the Adula Formation ────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Siltstone of Adula Formation", "Integration of contacts", "Polira group" ], [ "Polira group", "thickness", "1303.5m" ] ] }, { "text": "Late Paleozoic volcanic rocks were produced in the Nujiangyan Formation (Pz2J.) of Jiayuqiao Rock Group of the Late Paleozoic, and were exposed at the southwest corner of Changdu County with an area of about 13m2.", "triple_list": [ [ "Late Paleozoic Volcanic Rocks", "Located at", "Nujiangyan Formation in Jiayuqiao Rock Group in Late Paleozoic" ], [ "Late Paleozoic Volcanic Rocks", "Exposed", "1:250,000 Southwest corner of Changdu County" ], [ "Late Paleozoic Volcanic Rocks", "area", "13m2" ] ] }, { "text": "The Pleistocene Lake accumulations (Qpl) are mainly distributed in the area of the Zhumuqu-Zhuangqukang Garden, Yushu County, Wannangqian County. The lithology of the lake accumulations is mainly composed of sand, gravel, soil, and clay layers, with a thickness of 15m.", "triple_list": [ [ "Pleistocene Lake accumulation", "Exposed", "1:25 Wannangqian County, Yushu County Award-winning Wood Ququkang Garden Treasure Fruit and Cow Farm" ], [ "Pleistocene Lake accumulation", "Lithology", "Gravel" ], [ "Pleistocene Lake accumulation", "Lithology", "soil" ], [ "Pleistocene Lake accumulation", "Lithology", "Clay layer" ], [ "Pleistocene Lake accumulation", "thickness", "15m" ] ] }, { "text": "The Luodong Rock Group (3J1L.) is a set of tectonic mixed rocks, which are covered by the angle of the Shixun White Group in the Shixun. They are distributed in 1:25,000 places in the southwest corner of the Changdu County area. They extend to the west into the Dingqing County area and 1:25,000 to the south into the Basu County area. The area in the map is about 642.78m2.", "triple_list": [ [ "Luodongyan Group", "Lithology", "Tectonic mixed rock" ], [ "Luodongyan Group", "Unconformity contact", "The new Shizong Bai Qun" ], [ "Luodongyan Group", "Exposed", "1:250,000. Ladui Maselongda, Luodong Township, southwest corner of Changdu County" ], [ "Luodongyan Group", "Exposed", "1:250,000 Dingqing County" ], [ "Luodongyan Group", "Exposed", "1:250,000 Basu County" ], [ "Luodongyan Group", "area", "642.78m2" ] ] }, { "text": "Light gray-green chlorite quartz thousand rocks, not bottomed, 138.8m", "triple_list": [ [ "Light gray-green chlorite quartz thousand rocks", "thickness", "138.8m" ] ] }, { "text": "Dark gray weathered light gray serpentine, 550m wide, fault contact, dark gray weathered gray white sub-amphite serpentine", "triple_list": [ [ "Dark gray weathered light gray serpentine rock", "thickness", "550m" ], [ "Dark gray weathered light gray serpentine rock", "Fault contact", "Dark gray weathered off-white sub-amphite serpentine" ] ] }, { "text": "The Gangzi-Cumammylonite belt is located in the Jitang rock group from the southwest Gangzi Township to Zhongda Yuangujie. It has an NW-SE direction and is about 80m long.", "triple_list": [ [ "Steel-Mammalite Belt", "Located at", "Southwest Gangzi Township to Jitang Rock Group of Zhongda Yuangujie" ], [ "Steel-Mammalite Belt", "Distribution pattern", "NW-SE direction" ], [ "Steel-Mammalite Belt", "length", "80m" ] ] }, { "text": "1:200,000 kinds of Uzira is called Borisong multiple hemp-shaped two-long granite unit, produced in Beizhongda Borisongo ancient-Middle Proterozoic Jitang rock group (Pt1-2J.)", "triple_list": [ [ "1:200,000 Uzira many pictures called Borisong multiple pieces of hemp-shaped 2-chang granite", "Exposed", "Beizhong Daborisongduo Ancient - Jitang Rock Group in the Middle Protozoic Period" ] ] }, { "text": "Gangtuoyan Formation (P1g.) false thickness 2454.90m", "triple_list": [ [ "Gangtuoyan Formation", "thickness", "2454.90m" ] ] }, { "text": "Gray purple medium-thick layered complex conglomerate with dark purple gravel-containing unequal grained rock sandstone, 125.10m, angle unconsistent, underlying stratigraphic cave deck (3d) tuffy lava tuffy breccia lava", "triple_list": [ [ "Gray-purple medium-thick layered complex conglomerate with dark purple gravel-containing uneven grained rock sandstone", "thickness", "125.10m" ], [ "Gray-purple medium-thick layered complex conglomerate with dark purple gravel-containing uneven grained rock sandstone", "Unconformity contact", "Hole deck" ], [ "Hole deck", "Lithology", "Tuff lava" ], [ "Hole deck", "Lithology", "tuff breccia lava" ] ] }, { "text": "Gray bioclastic limestone, Neoschwagerina sp., not seen, 48.9m", "triple_list": [ [ "Gray bioclastic limestone", "Paleontological", "Neoschwagerina sp." ], [ "Gray bioclastic limestone", "thickness", "48.9m" ] ] }, { "text": "Gray-black medium-thick layered feldspar quartz sandstone with fragmented gravel-containing uneven grained sandstone, 92.4m", "triple_list": [ [ "Gray-black medium-thick layered feldspar quartz sandstone with fragmented gravel-containing uneven grained sandstone", "thickness", "92.4m" ] ] }, { "text": "The Dongdaqiao Formation of Wangbu Formation (J1w) is built for a set of purple-red clastic rock carbonate.", "triple_list": [ [ "Wang Bu Group", "Belongs to", "Construction of purple-red clastic rock carbonate rock" ], [ "East Bridge Group", "Belongs to", "Construction of purple-red clastic rock carbonate rock" ] ] }, { "text": "The geological era of the Jiaoga Formation was the early stage of the Middle Permian period to the middle and late stages.", "triple_list": [ [ "Jiaoga Group", "Age", "Early Middle Permian-middle-late" ] ] }, { "text": "The Tumugou Formation (3t) is distributed in the areas of Wangbuding Township, Jiangda County, Tibet - Chapu - Xingbanda Kelu Cave - Maisu Baiyu County, Zhaban - Shedan, etc., extending to the north, extending to the 125,000 Shiqu County, and extending to the east, 125,000 Ganzi County, with an area of about 1435m2 in the map.", "triple_list": [ [ "Tumugou Group", "Exposed", "Wangbuding Township, Jiangda County, Tibet - Ouphe Niuchang Chapu - Xingbanda Kelu Cave - Maisu Baiyu County - Shooting Gallbladder" ], [ "Tumugou Group", "Exposed", "1:250,000 Shiqu County" ], [ "Tumugou Group", "Exposed", "1:250,000 Ganzi County" ], [ "Tumugou Group", "area", "1435m2" ] ] }, { "text": "Late Carboniferous Formation (C2a) is distributed in the Dachaqujujulong area of Lewuqi County, this district. It is mainly composed of Anshan Ying'an tuff, with a small amount of Andesite.", "triple_list": [ [ "Late Carboniferous World Aoqu Group", "Exposed", "Lewuqi County Dachaqujue Zulong" ], [ "Late Carboniferous World Aoqu Group", "Lithology", "Anshan Ying'an Tuff" ], [ "Late Carboniferous World Aoqu Group", "Lithology", "Andanyan" ] ] }, { "text": "Gray fragmented powdery limestone, produced by Sphaeroschwagerina subrtunda, S. sphaerica, Pseudoschwagerina sp., Zellia colaniae Rugosofusulina sp. Pseudosulina sp. Pseudosulina sp. P. cf. yunnanica, 135.58m", "triple_list": [ [ "Gray chipped powder limestone", "Paleontological", "Sphaeroschwagerina subrtunda" ], [ "Gray chipped powder limestone", "Paleontological", "S. sphaerica" ], [ "Gray chipped powder limestone", "Paleontological", "Pseudoschwagerina sp." ], [ "Gray chipped powder limestone", "Paleontological", "Zellia colaniaeRugosofusulina sp." ], [ "Gray chipped powder limestone", "Paleontological", "Pseudofusulina sp." ], [ "Gray chipped powder limestone", "Paleontological", "P. cf. yunnanica" ], [ "Gray chipped powder limestone", "thickness", "135.58m" ] ] }, { "text": "Gray-black subammogram serpentine, 110m wide", "triple_list": [ [ "Gray-black subammogram serpentine", "thickness", "110m" ] ] }, { "text": "The sandstone of the Gongyelan group, fault contact, Polila group (3b), thickness 356m", "triple_list": [ [ "Gongyelan sandstone", "Fault contact", "Polira group" ], [ "Polira group", "thickness", "356m" ] ] }, { "text": "Gray-green complex conglomerate (bottom conglomerate), 4.5m, fault contact, Mangcuo formation sandstone", "triple_list": [ [ "Gray-green complex conglomerate (bottom conglomerate)", "thickness", "4.5m" ], [ "Gray-green complex conglomerate (bottom conglomerate)", "Fault contact", "Mangcuo Group Sandstone" ] ] }, { "text": "According to the characteristics of paleontology, the Mangcuo Formation is a shallow sea shed carbonate sedimentary environment.", "triple_list": [ [ "Rude group", "Belongs to", "Silky sea shelter carbonate sedimentary environment" ] ] }, { "text": "Light gray off-white thin layered muddy siltstone, produced by Danaeopsis sp. Nilssonia pterophylloides, 178.45m", "triple_list": [ [ "Light gray off-white thin layered muddy siltstone", "Paleontological", "Plant Danaeopsis sp." ], [ "Light gray off-white thin layered muddy siltstone", "Paleontological", "Nilssonia pterophylloides" ], [ "Light gray off-white thin layered muddy siltstone", "thickness", "178.45m" ] ] }, { "text": "The Paleo-Medieval Relu Formation (Er) is distributed in the Dege-Baiyu Stratigraphic Zone. It is built with red mola stone in the mountain fault basin. There is less exposure in this area, only seen in the Shangmana-Garonglan Belt of Babang Township, Dege County, eastern Jiangda County, with an exposed area of about 14m2.", "triple_list": [ [ "Paleogene Relu Formation", "Stratigraphical zoning", "Dege-White Jade Stratigraphic Zone" ], [ "Paleogene Relu Formation", "Belongs to", "Construction of red mullard stone in the mountain fault basin" ], [ "Paleogene Relu Formation", "Exposed", "1:25 million Jiangda County Bendang Shangmana-Garongnong" ], [ "Paleogene Relu Formation", "area", "14m2" ] ] }, { "text": "The rocks of the horn diorama vein are gray-green, with crystalline structures and block-like structures.", "triple_list": [ [ "Horned diagonal vein rock", "Distribution pattern", "Change afterglow structure" ], [ "Horned diagonal vein rock", "Distribution pattern", "Crystalline structure" ], [ "Horned diagonal vein rock", "Develop", "Blocky structure" ] ] }, { "text": "Gray-black thin-middle metamorphic feldspar quartz fine sandstone and gray-black slate interlayer, the bottom layer of mask heavy load mold, not seen, 42.00m", "triple_list": [ [ "Gray-black thin-middle metamorphic feldspar quartz fine sandstone and gray-black slate interlayer", "Contained", "Heavy load model" ], [ "Gray-black thin-middle metamorphic feldspar quartz fine sandstone and gray-black slate interlayer", "thickness", "42.00m" ] ] }, { "text": "The Gongyenong Formation is composed of gray-dark gray limestone crystal limestone biological clastic limestone mudstone, mixed with silt sandstone, etc., and produces bivalve ammonite brachiopod corals, with a total exposed thickness of >1346m, which is a set of shallow marine sedimentation.", "triple_list": [ [ "The man also works in groups", "Lithology", "Grey dark grey limestone" ], [ "The man also works in groups", "Lithology", "Crystalline limestone" ], [ "The man also works in groups", "Lithology", "Bioclastic limestone" ], [ "The man also works in groups", "Lithology", "Mudstone" ], [ "The man also works in groups", "Lithology", "Siltstone" ], [ "The man also works in groups", "Paleontological", "Bivalves" ], [ "The man also works in groups", "Paleontological", "Chrysanthemum" ], [ "The man also works in groups", "Paleontological", "Brachiopod" ], [ "The man also works in groups", "Paleontological", "coral" ], [ "The man also works in groups", "thickness", "1346m" ], [ "The man also works in groups", "Belongs to", "shallow ocean sedimentation" ] ] }, { "text": "Dongdu Formation consists of purple-red, gray-green conglomerate, sandstone, mudstone, slate, etc., and produces bivalve gastropods, with a total thickness of 377.21m, which is a set of coastal sedimentation.", "triple_list": [ [ "Dongdu Group", "Lithology", "Purple red gray green gravel rock" ], [ "Dongdu Group", "Lithology", "Sandstone" ], [ "Dongdu Group", "Lithology", "sandstone" ], [ "Dongdu Group", "Lithology", "Mudstone" ], [ "Dongdu Group", "Lithology", "Slate" ], [ "Dongdu Group", "Paleontological", "Bivalves" ], [ "Dongdu Group", "Paleontological", "Gastropod" ], [ "Dongdu Group", "thickness", "377.21m" ], [ "Dongdu Group", "Belongs to", "Maritime sedimentation" ] ] }, { "text": "The Riazenangyan Formation is built for a set of large Yanjian volcanic rocks with a small amount of clastic clay rocks. The main lithologies include gray-green dark gray-green block-shaped flakes of physical and chemical basic volcanic rocks, and intersected with seric slate flakes of physical and chemical quartz hybrid sandstone.", "triple_list": [ [ "Riazenongyan Formation", "Belongs to", "Construction of large Yankee volcanic rocks with a small amount of clastic rocks and clay rocks" ], [ "Riazenongyan Formation", "Lithology", "Physical and chemical basic volcanic rocks with gray-green dark gray-green blocks" ], [ "Riazenongyan Formation", "Lithology", "Basal mylonite" ], [ "Riazenongyan Formation", "Lithology", "Alternating base mylonite" ], [ "Riazenongyan Formation", "Lithology", "Serous slab" ], [ "Riazenongyan Formation", "Lithology", "Physical and chemical quartz sandstone" ] ] }, { "text": "The cave deck consists of gray-green andylanite inanite basalt tuff volcanic breccia clusters, sandstone slate limestone, etc., and produces bivalve ammonite brachiopods gastropod coral plants, with a total exposed thickness of >4206m, which is a set of shore-shallow marine fine clastic rocks and volcanic rocks.", "triple_list": [ [ "Hole deck", "Lithology", "Gray green andyama" ], [ "Hole deck", "Lithology", "Ying'an Rock" ], [ "Hole deck", "Lithology", "Basalt" ], [ "Hole deck", "Lithology", "Tuff" ], [ "Hole deck", "Lithology", "Volcanic breccia" ], [ "Hole deck", "Lithology", "Cluster rock" ], [ "Hole deck", "Lithology", "sandstone" ], [ "Hole deck", "Lithology", "Slate" ], [ "Hole deck", "Lithology", "Limestone" ], [ "Hole deck", "Paleontological", "Bivalves" ], [ "Hole deck", "Paleontological", "Chrysanthemum" ], [ "Hole deck", "Paleontological", "Brachiopod" ], [ "Hole deck", "Paleontological", "Gastropod" ], [ "Hole deck", "Paleontological", "Coral plants" ], [ "Hole deck", "thickness", "4206m" ], [ "Hole deck", "Belongs to", "Coastal-shallow marine fine clastic rocks and volcanic rock sedimentation" ] ] }, { "text": "Limestone is rich in coral brachiopod algae, followed by foraminifera.", "triple_list": [ [ "Limestone", "Paleontological", "coral" ], [ "Limestone", "Paleontological", "Brachiopod" ], [ "Limestone", "Paleontological", "Algae" ], [ "Limestone", "Paleontological", "Foraminifera" ] ] }, { "text": "Alternating andestone green-gray, spotty structure filled structure, block-like structure.", "triple_list": [ [ "altered andes", "Distribution pattern", "Spotted structure" ], [ "altered andes", "Distribution pattern", "Filling structure" ], [ "altered andes", "Develop", "Blocky structure" ] ] }, { "text": "The Adula group's era was the late Triassic Noli period.", "triple_list": [ [ "Adula Group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Gray gravel sand and gravel layer, top subsandal soil, 2-level terrace accumulation, 10m, angle unconsistent, Pleistocene alluvial accumulation (Qpal), thickness 30m", "triple_list": [ [ "Gray gravel gravel layer", "thickness", "10m" ], [ "Gray gravel gravel layer", "Unconformity contact", "Pleistocene alluvial accumulation" ], [ "Pleistocene alluvial accumulation", "thickness", "30m" ] ] }, { "text": "In Zhongda Village, Leiwuqi Town, I saw that the Late Triassic Jiapila Formation (3j) was not integrated on the Erchang granite body.", "triple_list": [ [ "See the Late Triassic Apila Group in Zhongda Village, Leiwuqi Town", "Unconformity contact", "Second Chang granite body" ] ] }, { "text": "The main lithologies of the Adula Formation are gray-black and gray slate serous slate sandstone, with a small amount of thin-layered crustal limestone, etc., and bivalve gastropods, brachiopods, etc., with a total thickness of >2095.18m, which is a shallow sea-marine sedimentary environment.", "triple_list": [ [ "Adula Group", "Lithology", "Gray black grey slate" ], [ "Adula Group", "Lithology", "Serous slab" ], [ "Adula Group", "Lithology", "sandstone" ], [ "Adula Group", "Lithology", "Thin layer scale limestone" ], [ "Adula Group", "Paleontological", "Bivalves" ], [ "Adula Group", "Paleontological", "Gastropod" ], [ "Adula Group", "Paleontological", "Brachiopod" ], [ "Adula Group", "thickness", "2095.18m" ], [ "Adula Group", "Belongs to", "Shallow sea-marine sedimentary environment" ] ] }, { "text": "Dongdaqiao Formation (J2d) thickness 2282.82m", "triple_list": [ [ "East Bridge Group", "thickness", "2282.82m" ] ] }, { "text": "Anshan rock-crystal crystal tuff is gray-green, with a variable tuff structure and a block structure.", "triple_list": [ [ "Anshan rock crystal tuff", "Distribution pattern", "Variable tuff structure" ], [ "Anshan rock crystal tuff", "Develop", "Blocky structure" ] ] }, { "text": "The Early Cretaceous Jingxing Formation (K1j) in the Changdu-Mangkang Stratigraphic Zone is distributed in the Duodu Belt in the southwest corner of Nangqian County, Qinghai Province; the Bendoreka area in Changdu County, Changdu County, and Baotou Lane in Mangda Township; the Cangda County, 1:25 million Jiangda County, the Chakaxi area in Niangxi Township, Jiangda County, Jiangda County, with an exposed area of about 143.51m2.", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Early Cretaceous Scenic Star Group" ], [ "Early Cretaceous Scenic Star Group", "Exposed", "1:250,000 Nangqian County, southwest corner of Qinghai Province, Duodu" ], [ "Early Cretaceous Scenic Star Group", "Exposed", "1:250,000 Changdu County hot card" ], [ "Early Cretaceous Scenic Star Group", "Exposed", "Baotou Lane, Mangda Township" ], [ "Early Cretaceous Scenic Star Group", "Exposed", "1:25 million Jiangda County, Jiangda County, Niangxi Township, Niangxi Township, Jiangda County" ], [ "Early Cretaceous Scenic Star Group", "area", "143.51m2" ] ] }, { "text": "According to the characteristics of paleontology, the Tuba Formation is a coal-containing sedimentary environment for sea and land interaction.", "triple_list": [ [ "Tuoba Group", "Belongs to", "Interactive coal-containing sedimentary environment for sea and land" ] ] }, { "text": "The Dugaila Formation was in integrated contact with the Late Triassic Adula Formation of the Underground Stratigraphic and the Early Jurassic Wanbu Formation of the Overlying Stratigraphic.", "triple_list": [ [ "Gala group", "Integration of contacts", "The Adula Group of the Late Triassic" ], [ "Gala group", "Integration of contacts", "Early Jurassic Wanbu Group" ] ] }, { "text": "Gray-black fine-grained quartz sandstone with a muddy sandy shale and carbonaceous shale, containing a small amount of feldspar quartz sandstone, containing a plant Keriotheca lungtanensis Pecopteris sp., 40m, fault contact, green gray-black a muddy silt sandstone with a shale sandy shale and a small amount of quartz sandstone, containing a plant Gigantopteris sp. Lobatannularia sp. Pecopteris sp., 119m", "triple_list": [ [ "Gray-black fine-grained quartz sandstone with muddy sandy shale and carbonaceous shale a small amount of feldspar quartz sandstone", "Paleontological", "Plant Keriotheca lungtanensis Pecopteris sp." ], [ "Gray-black fine-grained quartz sandstone with muddy sandy shale and carbonaceous shale a small amount of feldspar quartz sandstone", "thickness", "40m" ], [ "Gray-black fine-grained quartz sandstone with muddy sandy shale and carbonaceous shale a small amount of feldspar quartz sandstone", "Fault contact", "Green gray black muddy silt sandstone with shale sandy shale and a small amount of quartz sandstone" ], [ "Green gray black muddy silt sandstone with shale sandy shale and a small amount of quartz sandstone", "Paleontological", "Plant Gigantopteris sp. Lobatannularia sp." ], [ "Green gray black muddy silt sandstone with shale sandy shale and a small amount of quartz sandstone", "Paleontological", "Pecopteris sp." ], [ "Green gray black muddy silt sandstone with shale sandy shale and a small amount of quartz sandstone", "thickness", "119m" ] ] }, { "text": "Variegated alteration Andylantic tuff Andylantic tuff, 5.72m ───────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Variety alteration Andshan tuff Andshan tuff crystal crystal tuff", "thickness", "5.72m" ], [ "Variety alteration Andshan tuff Andshan tuff crystal crystal tuff", "Integration of contacts", "Sandstone slate of Tuoba Formation" ] ] }, { "text": "Gray purple-red calcareous quartz sandstone with gray thin layer of limestone, containing bivalve Palaeocardita sp. P. aff. langnongensis Pleuromya sp., 87.4m", "triple_list": [ [ "Gray purple-red calcareous quartz sandstone with gray thin layer of limestone", "Paleontological", "bivalve Palaeocardita sp." ], [ "Gray purple-red calcareous quartz sandstone with gray thin layer of limestone", "Paleontological", "P. aff. langnogensis Pleuromya sp." ], [ "Gray purple-red calcareous quartz sandstone with gray thin layer of limestone", "thickness", "87.4m" ] ] }, { "text": "Purple-red blocky metamorphic yinganin breccia tuff lava metamorphic yinganin fume breccia, 485.63m", "triple_list": [ [ "purple-red blocky metamorphic yinganin breccia tuff lava metamorphic yinganin fusion volcanic breccia", "thickness", "485.63m" ] ] }, { "text": "Gray-brown argilled lithotrix feldspar silt sandstone, 5.12m", "triple_list": [ [ "Taupe argic rock-cut feldspar silt sandstone", "thickness", "5.12m" ] ] }, { "text": "Sandstone of the early Triassic Pushuiqiao Formation in the overlying formation, the angle is not integrated, the Licha Formation (P1l), the total thickness is 1360.65m", "triple_list": [ [ "Sandstone of Pushuiqiao Formation in Early Triassic", "Unconformity contact", "Richa Group" ], [ "Richa Group", "thickness", "1360.65m" ] ] }, { "text": "The Late Triassic Jiapila Formation is a set of marine coarse clastic rock fine clastic rock deposits.", "triple_list": [ [ "Late Triassic Apira Group", "Belongs to", "Coarse clastic rock fine clastic rock sedimentation" ] ] }, { "text": "Gray-brown medium-grained rock fragment sandstone intersects limestone lens body, producing coral Bradyphyllum sp., 21.50m", "triple_list": [ [ "Gray-brown medium-grained rock fragment sandstone intersecting limestone lens body", "Paleontological", "Coral Bradyphyllum sp." ], [ "Gray-brown medium-grained rock fragment sandstone intersecting limestone lens body", "thickness", "21.50m" ] ] }, { "text": "Light grey - grey limestone breccia, 48.51m", "triple_list": [ [ "Light grey - grey limestone breccia", "thickness", "48.51m" ] ] }, { "text": "The volcanic rocks in the Shisenza Formation of Zhongdevon are distributed in the Zengguosenza area of Fanggucai Village, Jiangda County 1:25 million, with a total thickness of 173.95m.", "triple_list": [ [ "volcanic rocks in Shisenza Formation in the Middle Devon", "Exposed", "1:25 million Jiangda County Zengguosenza" ], [ "volcanic rocks in Shisenza Formation in the Middle Devon", "thickness", "173.95m" ] ] }, { "text": "Light gray-dark gray-thick-thick layer of siliceous rock, 25.76m", "triple_list": [ [ "Light gray-dark gray-thick-thick layer of siliceous rock", "thickness", "25.76m" ] ] }, { "text": "Coarse-grained dolomite lithotrix quartz sandstone in the gray thick layer to the block layer, containing plant fragments and bivalve Paranoceramus cf. matsumotoi Astarte sp. Corbula sp. Inoceramus sp. Lilingella cf. xinyunensis, 44.15m", "triple_list": [ [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "Paleontological", "Plant fragments" ], [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "Paleontological", "bivalve Paranoceramus cf. matsumotoi Astarte sp." ], [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "Paleontological", "Corbula sp." ], [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "Paleontological", "Inoceramus sp." ], [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "Paleontological", "Lilingella cf. xinyunensis" ], [ "Coarse grained dolomite quartz sandstone in gray thick layer to block layer", "thickness", "44.15m" ] ] }, { "text": "Overhead strata cave deck (3d) Light green and gray altered medium-basic tuff ─────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Hole deck", "Lithology", "Light green gray alteration medium-basic tuff" ], [ "Hole deck", "Integration of contacts", "The man also works in groups" ], [ "The man also works in groups", "thickness", "853.75m" ] ] }, { "text": "Gambling grey - light gray-green, variable afterglow long structure contains long structures and blocky structures. The main minerals are basal plagioclase (4547), ordinary pyroxene (48), and a small amount of quartz and chlorite.", "triple_list": [ [ "Gambling", "Distribution pattern", "Change afterglow structure" ], [ "Gambling", "Distribution pattern", "Long structure" ], [ "Gambling", "Contained", "Basal plagioclase" ], [ "Gambling", "Contained", "Ordinary pyrosine" ], [ "Gambling", "Contained", "quartz" ], [ "Gambling", "Contained", "Green clay" ] ] }, { "text": "The Bolila Formation Stratigraphic Area of the Bolila Formation is very small, only seen in Zhongda Village, Bengleiwuqi Town, Changdu County 1:25 million, with an exposed area of about 0.5m2.", "triple_list": [ [ "Polila Formation Stratigraphic Division", "Outcrop", "Polira group" ], [ "Polira group", "Exposed", "1:250,000 Zhongda Village, Bengleiwuqi Town, Changdu County" ], [ "Polira group", "area", "0.5m2" ] ] }, { "text": "Dark gray gray-green mud calcium slate sandy slate with limestone, producing brachiopod Leptodus nobilis; Agathiceras sp., 211.58m", "triple_list": [ [ "Dark gray gray green mud calcium slate sandy slate limestone", "Paleontological", "Brachiopod Leptodus nobilis" ], [ "Dark gray gray green mud calcium slate sandy slate limestone", "Paleontological", "Agathiceras sp." ], [ "Dark gray gray green mud calcium slate sandy slate limestone", "thickness", "211.58m" ] ] }, { "text": "Gray green purple-red quartz sandstone feldspar quartz sandstone silt sandstone with gray thin layer of marlstone, 81.7m", "triple_list": [ [ "Gray green purple-red quartz sandstone feldspar quartz sandstone silt sandstone with gray thin layer of marlstone", "thickness", "81.7m" ] ] }, { "text": "The Licha group (P1l) was distributed in 1:25,000. The Licha group was distributed in 1:25,000. The Zayalongwadiga Nangqian County, Qinghai Province, Zayalongwadiga Nangqian County, Qinghai Province, 1:25,000. The exposed area in this area is about 166.37m2.", "triple_list": [ [ "Richa Group", "Exposed", "1:25 million Nangqian County, Zaya Longwadiga Nangqian County, Qinghai Province Chajina Rongpu" ], [ "Richa Group", "Exposed", "1:250,000 Changdu County Bengnangqian County Jiangpu, Tibet, Machala Changdu County, Chamdo County, Lewuqi County, Tibet" ], [ "Richa Group", "Exposed", "1:25 million Jiangda County Bend Qingni Cave, Jiangda County, Nylon Xiong, Jiangda County, Tuoba Township, Changdu County" ], [ "Richa Group", "area", "166.37m2" ] ] }, { "text": "The era of Xiaya Village Group should be in the late Permian period.", "triple_list": [ [ "Xiaya Village Group", "Age", "Late Permian" ] ] }, { "text": "Caoqu Group schist transformed into sandstone, fault contact, Baitongyan Formation (P3b.), false thickness 3460.65m", "triple_list": [ [ "Caoququ Group schist sandstone", "Fault contact", "Baitongyan Formation" ], [ "Baitongyan Formation", "thickness", "3460.65m" ] ] }, { "text": "The Chamdo-Mangkang strata have multiple groups of early-middle Triassic marathons (1-2m), and the Late Triassic Apira Group (3j), Polila Group (3b), Adula Group (3a) Digala Group (3d).", "triple_list": [ [ "Chamdo-Mangkang Stratigraphic Zone", "Outcrop", "Triassic strata" ], [ "Triassic strata", "Outcrop", "Early-Middle Triassic Marathon Multiple Groups" ], [ "Triassic strata", "Outcrop", "Late Triassic Apira Group" ], [ "Triassic strata", "Outcrop", "Polira group" ], [ "Triassic strata", "Outcrop", "Adula Group" ], [ "Triassic strata", "Outcrop", "Gala group" ] ] }, { "text": "Jidonglong Formation is a set of shallow marine carbonate and fine clastic rock deposits.", "triple_list": [ [ "Ji Donglong Group", "Belongs to", "Shallow marine carbonate and fine clastic rock sedimentation" ] ] }, { "text": "Gray medium-thick layer of silty slate with unequal grained rock-cut feldspar sandstone and gray medium-thick layer of fine-pink limestone, producing serpentine Ozawainella sp. 169.74m", "triple_list": [ [ "Gray medium-thick layer of silty slate with unequal grained rock-cut feldspar sandstone and gray medium-thick layer of fine-filled limestone", "Paleontological", "Ozawainella sp." ], [ "Gray medium-thick layer of silty slate with unequal grained rock-cut feldspar sandstone and gray medium-thick layer of fine-filled limestone", "thickness", "169.74m" ] ] }, { "text": "The subdistrict Digaila group is distributed in the area of Shenqinglong Fuma Niuchang, Jiangda County, Jiangda County, and extends to the north by 125,000 Shiqu County, with an area of about 108.3m2 in the map.", "triple_list": [ [ "Gala group", "Exposed", "1:25 million Jiangda County Fenjiangda County Shenqinglong Fuma Niuchang" ], [ "Gala group", "Exposed", "1:250,000 Shiqu County" ], [ "Gala group", "area", "108.3m2" ] ] }, { "text": "Late Triassic Adula Formation (3a), total thickness 2095.18m", "triple_list": [ [ "The Adula Group of the Late Triassic", "thickness", "2095.18m" ] ] }, { "text": "Light gray thick layered fine-grained feldstone sandstone, with insect traces on the layer, large interlaced stratigraphic, containing plant fragments, 311.26m", "triple_list": [ [ "Light gray thick layered fine-grained feldspar sandstone", "Develop", "Insect traces" ], [ "Light gray thick layered fine-grained feldspar sandstone", "Develop", "Interleaved hierarchy" ], [ "Light gray thick layered fine-grained feldspar sandstone", "Paleontological", "Plant fragments" ], [ "Light gray thick layered fine-grained feldspar sandstone", "thickness", "311.26m" ] ] }, { "text": "Silicated dolomel ultramafic rocks have alternating structures or residual grid structures and block-like structures.", "triple_list": [ [ "Silicated Dolomel Superbasic Rock", "Distribution pattern", "Explain the structure" ], [ "Silicated Dolomel Superbasic Rock", "Distribution pattern", "Residual mesh structure" ], [ "Silicated Dolomel Superbasic Rock", "Develop", "Blocky structure" ] ] }, { "text": "The Baitongyan Formation (P3b.) of the Kenanyan Group can be determined that the fossils of the era are mainly bivalve Halobia sp. Halobia suprbescens, which are the late Triassic Kani-Nori period; the brachiopod Yidunella magna, which is the late Triassic Kani-Second period.", "triple_list": [ [ "The Baitongyan Formation of Kenanyan Group", "Paleontological", "bivalve Halobia sp." ], [ "The Baitongyan Formation of Kenanyan Group", "Paleontological", "Halobia suprbescens" ], [ "The Baitongyan Formation of Kenanyan Group", "Age", "Late Triassic Kani-Nori period" ], [ "The Baitongyan Formation of Kenanyan Group", "Paleontological", "Brachiopod Yidunella magna" ], [ "The Baitongyan Formation of Kenanyan Group", "Age", "Late Triassic Kani" ] ] }, { "text": "Gray dark gray thin-middle calcareous silt sandstone and gray-black shale interlayer, sand pattern lamination Develop, 34.18m", "triple_list": [ [ "Gray dark gray thin-middle calcareous siltstone and gray-black shale interlayer", "Develop", "Sand pattern layering" ], [ "Gray dark gray thin-middle calcareous siltstone and gray-black shale interlayer", "thickness", "34.18m" ] ] }, { "text": "Alternating alkaline basalt gray-green, rough and mysterious structure, and blocky structure.", "triple_list": [ [ "Alkaline basalt", "Distribution pattern", "Coarse and mysterious structure" ], [ "Alkaline basalt", "Develop", "Blocky structure" ] ] }, { "text": "In 1993, 1:200,000 Uqi Lado was once classified as the Longzaida Group (J1l) Go-to-buy group (J1q) E-to-buy group (J1a) sequence.", "triple_list": [ [ "1:200,000 types of Uqi Lado", "Outcrop", "Longzaida Group" ], [ "1:200,000 types of Uqi Lado", "Outcrop", "Go buy a group" ], [ "1:200,000 types of Uqi Lado", "Outcrop", "Aimai Group" ] ] }, { "text": "Gray-black fine silt calcare clay slate, 21.60m", "triple_list": [ [ "Gray-black fine silt calcare clay slab", "thickness", "21.60m" ] ] }, { "text": "The Polila Group in the subdistrict is distributed in 1:25,000 Jiangda County, Jiangda County, and the area of Luoba, Marisong Duozanzhayong Gongjue Group in Cuori Village, Jiangda County, extends to the north and 1:25,000 Gongjue County in the south, with an area of about 400.3m2 in the map.", "triple_list": [ [ "Polira group", "Exposed", "1:25 million Jiangda County Fenjiangda County Marisong thorns and Gongjue Group Luoba" ], [ "Polira group", "Exposed", "1:250,000 Shiqu County" ], [ "Polira group", "Exposed", "1:250,000 Gongjue County" ], [ "Polira group", "area", "400.3m2" ] ] }, { "text": "Gray-green-dark purple gray block layer volcanic breccia, 9.90m", "triple_list": [ [ "Gray-green-dark purple gray block layer volcanic breccia", "thickness", "9.90m" ] ] }, { "text": "Jidonglong Formation is a set of shallow marine carbonate and fine clastic rock deposits.", "triple_list": [ [ "Ji Donglong Group", "Belongs to", "Shallow marine carbonate and fine clastic rock sedimentation" ] ] }, { "text": "The Adula group fossils are rich in bivalves, and the period is the late Triassic period. Among them, the bivalve Burmesia lirata B. cf., etc. are important species of the late Triassic Noli period in southwestern my country.", "triple_list": [ [ "Adula Group", "Paleontological", "Bivalves" ], [ "Adula Group", "Age", "Late Triassic" ], [ "Adula Group", "Paleontological", "Bivalve Burmesia lirata B. cf." ], [ "Adula Group", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Gray thick block limestone, 102.00m", "triple_list": [ [ "Gray thick block limestone", "thickness", "102.00m" ] ] }, { "text": "The Garieyan Formation (P3j.) produces many types of paleontological fossils, and the period was the late Triassic.", "triple_list": [ [ "Gariei rock formation", "Paleontological", "Paleontological fossils" ], [ "Gariei rock formation", "Age", "Late Triassic" ] ] }, { "text": "Common rocks of mica slant-long grain rocks include black cloud slant-long grain rocks and two clouds slant-long grain rocks.", "triple_list": [ [ "Mica slant-length-grained rock", "Contained", "Black clouds slanted long grain rock" ], [ "Mica slant-length-grained rock", "Contained", "Eryun slant-length-variable grain rock" ] ] }, { "text": "Gray-brown thick layered conglomerate sandstone, 84.99m", "triple_list": [ [ "Gray-brown thick layered conglomerate sandstone", "thickness", "84.99m" ] ] }, { "text": "Gray gray-black thin-middle-fine crystal dolomite, containing brachiopod Genet sp. indet., 159.78m", "triple_list": [ [ "Gray gray black thin-middle fine crystal dolomite", "Paleontological", "Brachiopod Genet sp. indet." ], [ "Gray gray black thin-middle fine crystal dolomite", "thickness", "159.78m" ] ] }, { "text": "Purple-red thick mudstone with a small amount of thin mudstone, 122.6m", "triple_list": [ [ "Purple-red thick mudstone with a small amount of thin mudstone", "thickness", "122.6m" ] ] }, { "text": "Myoporia (Neoschizodus) sp. Modiolus sp. Baevellia sp. rigonodus sp. Mytilus sp. Neomegalodon sp., 145.00m ───────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Mixed limestone", "Paleontological", "bivalve Myoporia (Neoschizodus) sp." ], [ "Mixed limestone", "Paleontological", "Modiolus sp." ], [ "Mixed limestone", "Paleontological", "Baevelia sp." ], [ "Mixed limestone", "Paleontological", "rigonodus sp." ], [ "Mixed limestone", "Paleontological", "Mytilus sp." ], [ "Mixed limestone", "Paleontological", "Neomegalodon sp." ], [ "Mixed limestone", "thickness", "145.00m" ], [ "Mixed limestone", "Integration of contacts", "Polila Formation Limestone" ] ] }, { "text": "The Russian group was integrated under the bamboo group, so it placed its era in the Middle Triassic.", "triple_list": [ [ "Russia team", "Integration of contacts", "Bamboo card group" ], [ "Russia team", "Age", "Middle Triassic" ] ] }, { "text": "The Jiapila Group of the subdistrict is distributed in 1:25,000 Jiangda County, Jiangda County, Gencaike Shida Long Niuchang Zuolong Gongba and other areas. It extends to the north by 1:25,000 Shiqu County and 1:25,000 Gongjue County and the area in the map is about 345.9m2.", "triple_list": [ [ "Kapila Group", "Exposed", "1:25 million Jiangda County Fenjiangda County Gencai Shida Long Niuchang Zuolong Gongba" ], [ "Kapila Group", "Exposed", "1:250,000 Shiqu County" ], [ "Kapila Group", "Exposed", "1:250,000 Gongjue County" ], [ "Kapila Group", "area", "345.9m2" ] ] }, { "text": "Gray thin layered silt sandstone sandstone with conglomerate limestone, 220m", "triple_list": [ [ "Gray thin-layered silt sandstone sandstone with conglomerate limestone", "thickness", "220m" ] ] }, { "text": "Purple-red medium-thin layered silty sandstone, 26.50m", "triple_list": [ [ "Purple-red medium-thin layered silty sandstones containing uneven grains", "thickness", "26.50m" ] ] }, { "text": "Purple mud silty sandstone silty shale quartz silty sandstone interlayer grey quartz fine sandstone, visible sand pattern layering 21.92m", "triple_list": [ [ "Purple mud silt sandstone silt shale quartz silt sandstone interlayer grey quartz fine sandstone", "Develop", "Sand pattern layering" ], [ "Purple mud silt sandstone silt shale quartz silt sandstone interlayer grey quartz fine sandstone", "thickness", "21.92m" ] ] }, { "text": "Gray-brown calcium fine-grained rock fragment sandstone, 253.83m", "triple_list": [ [ "Gray-brown calcium fine-grained sandstone", "thickness", "253.83m" ] ] }, { "text": "Light gray serous quartz thousand rock, 165.6m", "triple_list": [ [ "Light gray serous quartz thousand rocks", "thickness", "165.6m" ] ] }, { "text": "The Baitongyan Formation (P3b.) is distributed in the area of Xiewu-Baitong-Benda Township, northeast corner of Nangqian County, with an exposed area of about 211.72m2.", "triple_list": [ [ "Baitongyan Formation", "Exposed", "1:25 million Nangqian County, Hewu-Baitong-Benda Township" ], [ "Baitongyan Formation", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Baitongyan Formation", "area", "211.72m2" ] ] }, { "text": "Gray medium-thick layer metamorphic quartz sandstone gray yellow medium-thin layer metamorphic calcified quartz sandstone dark gray black gray silty rocks are not equally thick interlayered, producing bivalve Baevellia sp., 183.00m", "triple_list": [ [ "Gray medium-thick layer metamorphic quartz sandstone gray yellow medium-thin layer metamorphic calcified quartz sandstone dark gray black gray silty rock unequal thick interlayer", "Paleontological", "Bivalves Baevellia sp." ], [ "Gray medium-thick layer metamorphic quartz sandstone gray yellow medium-thin layer metamorphic calcified quartz sandstone dark gray black gray silty rock unequal thick interlayer", "thickness", "183.00m" ] ] }, { "text": "Yellow-gray thin middle layer of calcareous silt sandstone mud shale with marlstone, horizontal stratigraphic Develop, bivalve Ceratomya cf. concentrica Amiodon jinguensis, 166.17m", "triple_list": [ [ "Yellow-gray thin middle layer of calcareous silt sandstone mud shale with marl", "Develop", "Horizontal stratification" ], [ "Yellow-gray thin middle layer of calcareous silt sandstone mud shale with marl", "Paleontological", "Bivalve Ceratomya cf. concentrica Amiodon jinguensis" ], [ "Yellow-gray thin middle layer of calcareous silt sandstone mud shale with marl", "thickness", "166.17m" ] ] }, { "text": "The late Paleozoic volcanic rocks in this volcanic rock belt are mainly found in the Azenang rock formation in the Early Carboniferous Azenang rock formation, distributed in the Lancang River junction belt, and spreading in the northwest-south eastward direction.", "triple_list": [ [ "Late Paleozoic volcanic rocks in volcanic rocks", "Located at", "Azenongyan Formation in the Early Carboniferous Day" ], [ "Late Paleozoic volcanic rocks in volcanic rocks", "Earth tectonic location", "Lancang River Combination Belt" ], [ "Late Paleozoic volcanic rocks in volcanic rocks", "Distribution pattern", "Northwest-south eastward expansion" ] ] }, { "text": "Gray-yellow gravel sand and gravel layer with binary structure, 3-level terrace accumulation, 12m", "triple_list": [ [ "Gray yellow gravel gravel layer", "Distribution pattern", "Binary structure" ], [ "Gray yellow gravel gravel layer", "thickness", "12m" ] ] }, { "text": "The period of the Fusulina-Fusulinella belt in the Wangguo Formation was the late Carboniferous period.", "triple_list": [ [ "Wang Guo Group Fusulina—Fusulinella belt", "Age", "Late Carboniferous" ] ] }, { "text": "In the area of Muri Ezhako-Waji, the main lithologies are gray-dark gray limestone bio-limestone marlstone crystalline limestone slate sandstone, with gray-green Andesan tuff, and are rich in serpentine Neomisellina sp. N. lepida Neoschwagerina sp. N. ueichowensis N. wangsiana Cancellina sp. Parafusulina sp. P. cinta P. splendens P. houae P. gruperaensis P. aasarsis P. yunnanica P. subbrotunda Yangchienia sp. Sumatrina sp. Neosehwagerina margheriti N. wangchiensis Afghanella megaspherica Verbeeina sp. Pseudodolina sp.; Brachiopod Linoproductus sp. Spiriferella salter Spinomarginifera lopingensis Dictyoclostus gratiosus D. margaritatus Hustedia indica H. gradicosta Uncinunellina timorensis; marl stone coral Allotropiophyllum sp. Yatsengia sp. and ammonite trilobites bivalve sea lily, with an exposed thickness of 1082.33m.", "triple_list": [ [ "Marlite", "Paleontological", "Coral Allotropiophyllum sp." ], [ "Marlite", "Paleontological", "Yatsengia sp." ], [ "Marlite", "Paleontological", "Chrysanthemum" ], [ "Marlite", "Paleontological", "Trileleaf" ], [ "Marlite", "Paleontological", "Bivalves" ], [ "Marlite", "Paleontological", "sea lily" ], [ "Marlite", "thickness", "1082.33m" ] ] }, { "text": "Luotang Fault (F162) extends in a northwest direction, with both ends extending out of the diagram, and the length of this area is about 45m.", "triple_list": [ [ "Luotang fault", "Distribution pattern", "Northwest bending and extending" ], [ "Luotang fault", "length", "45m" ] ] }, { "text": "The gabbro groups of the cull waves are exposed in the southeast of Baiyu County, with an area of 13.44m2.", "triple_list": [ [ "The gabbro groups", "Exposed", "Nandong, Baiyu County" ], [ "The gabbro groups", "area", "13.44m2" ] ] }, { "text": "The Mangcuo Group of the Middle Permian (P2mc) was distributed in 1:25,000 Nangqian County, Nangqian County, Yushu County, Qinghai Province, Zhaxitang-Jiuba Adamkong Juewuwujiajiugaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogaogao", "triple_list": [ [ "Mid Permian Rumor", "Exposed", "1:25 million Nangqian County, Yushu County, Qinghai Province, Zhaxitang, Nangqian County, Guoqu, Nangqian County - Jiuba A Dangkong Juewu Gives the Russian Championship" ], [ "Mid Permian Rumor", "Exposed", "1:250,000 Changdu County Bing Nangqi County Mai Rang Tibet Lewuqi County Table Densai Sai" ], [ "Mid Permian Rumor", "Exposed", "1:25 million Jiangda County Fenjiangda County Jiarima Gongjue County Ranma Dun" ], [ "Mid Permian Rumor", "Exposed", "1:25 million Zaduo County" ], [ "Mid Permian Rumor", "area", "286.74m2" ] ] }, { "text": "Lewuqibian Lado (1993) is divided into Guoxuepu Group (3gx), Luanniba Group (3l) Sando Group (3s).", "triple_list": [ [ "Lewuqi Lado", "Contained", "Guoxuepu Group" ], [ "Lewuqi Lado", "Contained", "Random Niba Group" ], [ "Lewuqi Lado", "Contained", "Sando Group" ] ] }, { "text": "Dark gray medium-thick layered bioshell grain-clad limestone, produced by snaking Pseudofusulina cf. gruperaensis (homppsonet Miller), Pseu dofusulina ueichowensis Sheng, 110.49m", "triple_list": [ [ "Dark gray medium-thick layered bioshell grain chip limestone", "Paleontological", "Pseudofusulina cf. gruperaensis (homppsonet Miller)" ], [ "Dark gray medium-thick layered bioshell grain chip limestone", "Paleontological", "Pseu dofusulina ueichiwensis Sheng" ], [ "Dark gray medium-thick layered bioshell grain chip limestone", "thickness", "110.49m" ] ] }, { "text": "The limestone is rich in foraminifera corals, etc., and is integrated and covered by the Dongque Group.", "triple_list": [ [ "Limestone", "Paleontological", "Snake" ], [ "Limestone", "Paleontological", "Foraminifera" ], [ "Limestone", "Paleontological", "coral" ], [ "Limestone", "Integration of contacts", "Dong Que Group" ] ] }, { "text": "The Polila Formation is a set of limestone mixed with mud limestone, which is locally deformed, has slab physicochemical, and is integrated with the Jiapila Formation of the underlying formation.", "triple_list": [ [ "Polira group", "Lithology", "Limestone" ], [ "Polira group", "Lithology", "Mixed limestone" ], [ "Polira group", "Develop", "Physics and Chemistry" ], [ "Polira group", "Integration of contacts", "Kapila Group" ] ] }, { "text": "The small Sokar group consists of purple-red dark purple-red sandstone mudstone shale, etc., sporophore-producing vertebrates, with an exposed thickness of >1264.03m, and is a river and lake phase deposition.", "triple_list": [ [ "Small Sole deck group", "Lithology", "Purple-red dark purple-red sandstone" ], [ "Small Sole deck group", "Lithology", "Mudstone" ], [ "Small Sole deck group", "Lithology", "shale" ], [ "Small Sole deck group", "Paleontological", "Spore powder" ], [ "Small Sole deck group", "Paleontological", "vertebrate" ], [ "Small Sole deck group", "thickness", "1264.03m" ], [ "Small Sole deck group", "Belongs to", "River and lake sedimentation" ] ] }, { "text": "Light gray medium-layered quartz sandstone with gray slate, 90m ──────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Light gray medium layered quartz sandstone with grey slate", "thickness", "90m" ], [ "Light gray medium layered quartz sandstone with grey slate", "Integration of contacts", "Donla Formation Limestone Plywood" ] ] }, { "text": "The Quier Mountain-Yidun invading rock zone exposed less late Triassic granite rock mass, with a total area of 89.8m2.", "triple_list": [ [ "Queer Mountain-Yidun invades the rock belt", "Contained", "Late Triassic granite rock body" ], [ "Late Triassic granite rock body", "area", "89.8m2" ] ] }, { "text": "Overhead Adula Formation (3a) gray medium-thick layered medium-fine-grained feldspar fragment sandstone ─────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Adula Group", "Lithology", "Gray medium-thick layered medium-fine-grained feldspar" ], [ "Adula Group", "Lithology", "Chop sandstone" ], [ "Adula Group", "Integration of contacts", "Polira group" ], [ "Polira group", "thickness", "52.00m" ] ] }, { "text": "Dark gray thick-block layered shiny crystal gravel ovalite limestone, producing ammonite Discophyllites sp., 22.94m", "triple_list": [ [ "Dark gray thick-block layered shiny crystal gravel ovalite limestone", "Paleontological", "Ammonite Discophyllites sp." ], [ "Dark gray thick-block layered shiny crystal gravel ovalite limestone", "thickness", "22.94m" ] ] }, { "text": "The ancient algae Stenoporidium sp., Lithothamnum sp., was harvested from the limestone of Nanonggou, Luodong Village, Dingqing County.", "triple_list": [ [ "Nalangou in Luodong Village, Dingqing County", "Contained", "Limestone" ], [ "Limestone", "Paleontological", "Stenoporidium sp." ], [ "Limestone", "Paleontological", "Lithothamnum sp." ] ] }, { "text": "The late Permian Shamu Formation is rarely distributed in this area, only found in Mangda, Bengniangxi Township, Jiangda County 1:25 million, and is produced in broken blocks, with an exposed area of about 1.5m2.", "triple_list": [ [ "Late Permian Sanmu Group", "Exposed", "1:25 million east of Mangda, Bingniangxi Township, Jiangda County" ], [ "Late Permian Sanmu Group", "Distribution pattern", "Output of broken clamp block" ], [ "Late Permian Sanmu Group", "area", "1.5m2" ] ] }, { "text": "1:200,000 Shangla Xiubing was captured in the Wangguo group in Sangzhi Akao area, Yushu County, Kinophyllum sp., Echinoconcha punctatus., which was the late Carboniferous World.", "triple_list": [ [ "1:200,000 yuan to pull up the show in Sangzhi Akao, Yushu County", "Outcrop", "Wang Guo Group" ], [ "Wang Guo Group", "Paleontological", "Brachiopod Kinophyllum sp." ], [ "Wang Guo Group", "Paleontological", "Echinoconcha punctatus." ], [ "Wang Guo Group", "Age", "Late Carboniferous" ] ] }, { "text": "The left seat grid is broken (F166) and heads northwest, extending out of the diagram at both ends, with a length of more than 21m.", "triple_list": [ [ "Left seat lattice break", "Distribution pattern", "North-west" ], [ "Left seat lattice break", "length", "21m" ] ] }, { "text": "The Permian granite in the Jiangda-Deqin invasion rock zone is mainly late Permian granite, and the main rock types are mica granite and echinite.", "triple_list": [ [ "Permian granite in the Jiangda-Deqin invasion rock belt", "Lithology", "Late Permian granite" ], [ "Permian granite in the Jiangda-Deqin invasion rock belt", "Lithology", "Mica granite" ], [ "Permian granite in the Jiangda-Deqin invasion rock belt", "Lithology", "Yingyun Diorite" ] ] }, { "text": "Sand sericite quartz thousand rocks, with light yellow on the upper part and light gray-white on the lower part, 1951.1m", "triple_list": [ [ "Sand serous quartz thousand rocks", "thickness", "1951.1m" ] ] }, { "text": "The plagioclase rock is inlaid with granular metacrystalline structure and block-like structure.", "triple_list": [ [ "plagioclase", "Distribution pattern", "Inlaid granular metamorphic structure" ], [ "plagioclase", "Develop", "Blocky structure" ] ] }, { "text": "The Jiapila Group in the subdistrict is widely distributed, exposed to 1:25,000 Nangqian County, Rimasemaqiongda, Yushu County, Qinghai Province, Quritoshi, Nangqian County, Quritoshi, Gorha, 1:25,000 Changdu County, Zaranda, Binda, Banna Niuchang, Changdu County, 1:25,000 Jiangda County, Chaya County, Chela, Jiangda County, Shengga and other areas, extending to the west into 1:25,000 Zaduo County, and extending to the south into 1:25,000 Basu County, Gongjue County, with an exposed area of about 2308m2.", "triple_list": [ [ "Kapila Group", "Exposed", "1:25 million Nangqian County, Yushu County, Qinghai Province" ], [ "Kapila Group", "Exposed", "Nangqian County Quri arrives for Sha Hongkao" ], [ "Kapila Group", "Exposed", "1:250,000 Changdu County, Zharenda, Wuqi County - Binda Changdu County Bana Cow Farm - How Given" ], [ "Kapila Group", "Exposed", "1:25 million Jiangda County Fenchaya County to Lajiangda County Shengga" ], [ "Kapila Group", "Exposed", "1:25 million Zaduo County" ], [ "Kapila Group", "Exposed", "1:250,000 Basu County Band Gongjue County Band" ], [ "Kapila Group", "area", "2308m2" ] ] }, { "text": "The brachiopod bivalve gastropods are abundant in limestone, and they are integrated and hidden under the Wala Monastery of the Middle Triassic.", "triple_list": [ [ "Limestone", "Paleontological", "Brachiopod" ], [ "Limestone", "Paleontological", "Bivalves" ], [ "Limestone", "Paleontological", "Gastropod" ], [ "Limestone", "Integration of contacts", "The Wala Monastery of the Middle Triassic" ] ] }, { "text": "Purple-red mesostratigraphic conglomerate, 50.5m, angle unconsistent, and the underlying formation Machala Formation sandstone", "triple_list": [ [ "Purple-red medium gravel rock", "thickness", "50.5m" ], [ "Purple-red medium gravel rock", "Unconformity contact", "Machara Formation Sandstone" ] ] }, { "text": "The Yingzhu Nianga Formation is composed of gray, dark gray, gray-black conglomerate sandstone, shale slate marl, limestone, etc., and produces bivalves, with a total exposed thickness of 2989.85m, which is a coast-shallow marine sedimentary environment.", "triple_list": [ [ "Yingzhu Niang group", "Lithology", "Gray dark gray gray black gravel rock" ], [ "Yingzhu Niang group", "Lithology", "sandstone" ], [ "Yingzhu Niang group", "Lithology", "shale" ], [ "Yingzhu Niang group", "Lithology", "Slate" ], [ "Yingzhu Niang group", "Lithology", "Marlite" ], [ "Yingzhu Niang group", "Lithology", "Limestone" ], [ "Yingzhu Niang group", "Paleontological", "Bivalves" ], [ "Yingzhu Niang group", "thickness", "2989.85m" ], [ "Yingzhu Niang group", "Belongs to", "Coastal-shallow marine sedimentary environment" ] ] }, { "text": "The Dongque Formation is distributed in the area of Sangzhi Akao in Bailiangniang Township, Yushu County, Nangqian County, and the Dongque in Gucai Village, Jiangda County, 1:25 million. The exposed area is about 5.5m2, and it is in integrated contact with the Dongla Formation (D3d) of the underlying strata and the Wangguo Formation (C2w) of the overlying strata.", "triple_list": [ [ "Dong Que Group", "Exposed", "1:25 million Nangqian County Band Sangzhi Akao" ], [ "Dong Que Group", "Exposed", "1:25 million Dong Que, Fanggucai Village, Jiangda County" ], [ "Dong Que Group", "area", "5.5m2" ], [ "Dong Que Group", "Integration of contacts", "Donla Group" ], [ "Dong Que Group", "Integration of contacts", "Wang Guo Group" ] ] }, { "text": "The Anshan gravel-containing crystal chips are gray-green, and the residual tuff structure is layered.", "triple_list": [ [ "Anshan gravel-containing crystal tuff", "Distribution pattern", "Variable tuff structure" ], [ "Anshan gravel-containing crystal tuff", "Develop", "Layered structure" ] ] }, { "text": "The lithologies of Luodong rocks are slate 100 rock metamorphic sandstone, mud crystal limestone siliceous rocks, spore-pollinated ancient algae bivalve gaspods, and are mixed with ultra-basic rock gabbros diaboli siliceous volcanic rocks, with a thickness of 615.23m", "triple_list": [ [ "Luodongyan Group", "Lithology", "Slate" ], [ "Luodongyan Group", "Lithology", "Qianmeiyan" ], [ "Luodongyan Group", "Lithology", "Metamorphic Sandstone" ], [ "Luodongyan Group", "Lithology", "Mud crystal limestone" ], [ "Luodongyan Group", "Lithology", "Silicone rock" ], [ "Luodongyan Group", "Paleontological", "Spore powder" ], [ "Luodongyan Group", "Paleontological", "Ancient algae" ], [ "Luodongyan Group", "Paleontological", "Bivalves" ], [ "Luodongyan Group", "Paleontological", "Gastropod" ], [ "Luodongyan Group", "Paleontological", "Radioworms" ], [ "Luodongyan Group", "Lithology", "Superbasal rock" ], [ "Luodongyan Group", "Lithology", "Gambling" ], [ "Luodongyan Group", "Lithology", "Diamondite" ], [ "Luodongyan Group", "Lithology", "Basic volcanic rocks" ], [ "Luodongyan Group", "Lithology", "Silicone strip limestone blocks" ], [ "Luodongyan Group", "thickness", "615.23m" ] ] }, { "text": "Gray thin-layer microcrystalline-pink crystalline limestone, gastropod Natiria sp., 60.29m", "triple_list": [ [ "Gray thin-layer microcrystalline-pink crystalline limestone", "Paleontological", "Gastropodon Natiria sp." ], [ "Gray thin-layer microcrystalline-pink crystalline limestone", "thickness", "60.29m" ] ] }, { "text": "The Dongdaqiao Formation is a set of sedimentary fine clastic rock clay rock carbonate rock, etc., with its era from the Baro period of the Middle Jurassic to the Carlo period.", "triple_list": [ [ "East Bridge Group", "Belongs to", "Sedimentation of fine clastic rock clay rock carbonate rock and other intercourse in sea and land" ], [ "East Bridge Group", "Age", "The Baro period of the Middle Jurassic-Carlo period" ] ] }, { "text": "Gray-changed quartz sandstone with silty slate, 62.05m", "triple_list": [ [ "Gray-changed quartz sandstone with silty slab", "thickness", "62.05m" ] ] }, { "text": "Gray-black weathered, light gray silty serous slate, 45.5m", "triple_list": [ [ "Gray black weathered with light gray silty serous slab", "thickness", "45.5m" ] ] }, { "text": "Based on the above data, the era of the Russian Rock Formation (CPe.) is placed in the Carboniferous-Permian period.", "triple_list": [ [ "Russian Rock Formation", "Age", "Carboniferous-Permian" ] ] }, { "text": "Light gray thick layered silty fine-grained feldspar crushed sandstone sandstone intersected with dark gray thin layered amidal silty sandstone, producing bivalve Cardium (ulongo cardium) cf. martini C. sp.; plant Glossophlum shensiensis, 446.55m ──────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Light gray thick layered silty fine-grained feldspar crushed sandstone sandstone with dark gray thin layered muddy silty sandstone", "Paleontological", "bivalve Cardium (ulongo cardium) cf. martini C. sp." ], [ "Light gray thick layered silty fine-grained feldspar crushed sandstone sandstone with dark gray thin layered muddy silty sandstone", "Paleontological", "Plant Glossophlum shensiensis" ], [ "Light gray thick layered silty fine-grained feldspar crushed sandstone sandstone with dark gray thin layered muddy silty sandstone", "thickness", "446.55m" ], [ "Light gray thick layered silty fine-grained feldspar crushed sandstone sandstone with dark gray thin layered muddy silty sandstone", "Integration of contacts", "Adula Group" ], [ "Adula Group", "Lithology", "Dark gray thin layer of muddy silt" ], [ "Adula Group", "Lithology", "Feldspar rock" ], [ "Adula Group", "Lithology", "Chop sandstone" ] ] }, { "text": "The Dongdu Group (3dd) is distributed in 1:25,000 Nangqian County, Shaning Dalalongda, Yushu County, Qinghai Province, and Oma type in Jiangda County, Tibet; 1:25,000 Jiangda County, Jiangda County, Aosai Juniuchang Zhongbei and other areas, extending to the northward 1:25,000 Yushu County and 1:25,000 Shiqu County, with an area of about 298m2 in the map.", "triple_list": [ [ "Dongdu Group", "Exposed", "1:25 million Nangqian County, Shaning Dalalongda, Yushu County, Qinghai Province" ], [ "Dongdu Group", "Exposed", "Oma type in Jiangda County, Tibet" ], [ "Dongdu Group", "Exposed", "1:25 million Jiangda County Fenjiangda County Aosai Ju Niuchang Zhongbei" ], [ "Dongdu Group", "Exposed", "1:250,000 Yushu County" ], [ "Dongdu Group", "Exposed", "1:250,000 Shiqu County" ], [ "Dongdu Group", "area", "298m2" ] ] }, { "text": "The Triassic invasion rocks in the Chamdo-Mangkang invasion rock belt are mainly invasion rocks in the Middle Triassic invasion rocks, exposed in Kurumamyong, northeast of Rado Township, and are intermittently distributed in NW-SE. They are composed of six invasion bodies of varying sizes, with a total area of 163.88m2, accounting for 7.25% of the total area of invasion rocks.", "triple_list": [ [ "Chamdo-Mangkang invades the rock belt", "Contained", "Triassic invasion rock" ], [ "Triassic invasion rock", "Lithology", "Middle Triassic Invasion Rock" ], [ "Triassic invasion rock", "Exposed", "Kuruma in the northeast of Rado Township" ], [ "Triassic invasion rock", "Distribution pattern", "NW-SE direction intermittent distribution" ], [ "Triassic invasion rock", "area", "163.88m2" ] ] }, { "text": "The Shixin Shizong Bai Group (E2Z) is only distributed in the southwest corner of Changdu County, Tongran Qingpuguo Xiama Riji and other areas. It extends to the west into the Dingqing County, and 1:25,000 to the south into the Basu County, with an area of about 250m2 in the map, which is a set of red coarse debris-silted sedimentation after the orogenic period.", "triple_list": [ [ "The new Shizong Bai Qun", "Exposed", "1:250,000 Changdu County's southwest corner velvet Tongran Qingpu fruit dismounted and Riji" ], [ "The new Shizong Bai Qun", "Exposed", "1:250,000 Dingqing County" ], [ "The new Shizong Bai Qun", "Exposed", "1:250,000 Basu County" ], [ "The new Shizong Bai Qun", "area", "250m2" ], [ "The new Shizong Bai Qun", "Belongs to", "Red coarse debris-silt sedimentation after orogenic period" ] ] }, { "text": "Permian granite is found in the Chamdo-Mangkang invasion zone and the Jiangda-Deqin invasion zone. It has less exposed and produces rock plants.", "triple_list": [ [ "Permian granite", "Exposed", "Chamdo-Mangkang invades the rock belt" ], [ "Permian granite", "Exposed", "Jiangda-Deqin invades the rock belt" ], [ "Permian granite", "Distribution pattern", "Rock plant output" ] ] }, { "text": "The Wangbu Formation is a set of purple-red fine clastic rocks and clay rock marlstones, which have the characteristics of arid Huanzhangxia Lake Facies.", "triple_list": [ [ "Wang Bu Group", "Lithology", "Purple-red fine clastic rock" ], [ "Wang Bu Group", "Lithology", "Clay rock" ], [ "Wang Bu Group", "Lithology", "Marlite" ], [ "Wang Bu Group", "Belongs to", "Characteristics of the sedimentary characteristics of the lake phase in the dry Huanzhangxia" ] ] }, { "text": "The thickness of the Relu Formation (Er) is 415.89m", "triple_list": [ [ "Relu Group", "thickness", "415.89m" ] ] }, { "text": "Yellow, gray, green, purple, red, medium-thick layer of radioworm siliceous serous slate with a small amount of gray-green acidic glass tuff, containing gastropods Cylicioscapa sp. Eumophalus sp.; radioworm Cenosphaera sp. and brachiopods, 77.77m", "triple_list": [ [ "Yellow, gray, green, purple, red medium-thick layer of radioworm siliceous serous slate with a small amount of gray, green acidic glass tuff", "Paleontological", "Gastropods Cylicioscapa sp." ], [ "Yellow, gray, green, purple, red medium-thick layer of radioworm siliceous serous slate with a small amount of gray, green acidic glass tuff", "Paleontological", "Eumophalus sp." ], [ "Yellow, gray, green, purple, red medium-thick layer of radioworm siliceous serous slate with a small amount of gray, green acidic glass tuff", "Paleontological", "radioworm Cenosphaera sp." ], [ "Yellow, gray, green, purple, red medium-thick layer of radioworm siliceous serous slate with a small amount of gray, green acidic glass tuff", "Paleontological", "Brachiopod" ], [ "Yellow, gray, green, purple, red medium-thick layer of radioworm siliceous serous slate with a small amount of gray, green acidic glass tuff", "thickness", "77.77m" ] ] }, { "text": "Overhead siltstone clay rock of Dugala Formation ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Siltstone clay rock of the Dugala Formation", "Integration of contacts", "Adula Group" ], [ "Adula Group", "thickness", "780.2m" ] ] }, { "text": "Green curtain green mud sodium elongated schist green, remnant spot-like structure, scaly grainy metamorphic structure, flaky structure.", "triple_list": [ [ "Green curtain green mud sodium elongated rock", "Distribution pattern", "Spot-like structure" ], [ "Green curtain green mud sodium elongated rock", "Distribution pattern", "Scale-like granular metamorphic structure" ], [ "Green curtain green mud sodium elongated rock", "Develop", "Flake-like structure" ] ] }, { "text": "The exposed area of Jiayuqiao Rock Group in the survey area is only about 30m2, and only the Nujiang Rock Group in the upper part is seen.", "triple_list": [ [ "Jiayuqiao Rock Group", "area", "30m2" ], [ "Jiayuqiao Rock Group", "Outcrop", "Nujiangyan Formation" ] ] }, { "text": "Gambling rocks are exposed in several places in Dongpu Village (111) Niangxi Township (141) and Dangda (146147) in Jiangda County, Tibet, Yushu Prefecture, Qinghai Province. The rock mass invades the strata of the cave deck (3d), Gongyelan Group (3g), Pushuiqiao Group (1p).", "triple_list": [ [ "Gambling", "Exposed", "Nanmabaose, Batang Township, Yushu Prefecture, Qinghai Province" ], [ "Gambling", "Exposed", "Dongpu Village, Jiangda County, Tibet" ], [ "Gambling", "Exposed", "Niangxi Township" ], [ "Gambling", "Exposed", "Dianda" ], [ "Gambling", "Invade", "Hole deck" ], [ "Gambling", "Invade", "The man also works in groups" ], [ "Gambling", "Invade", "Pushuiqiao Group" ] ] }, { "text": "The Meng Axiong Group (3M) in the late Triassic Period spreads in the Nujiang junction belt in a tectonic block, with no comparison in the region, and is distributed in the southwest corner of Changdu County, 1:25 million, and is spread in the northwest to southeast. The area inside the picture is about 293.34m2.", "triple_list": [ [ "The late Triassic Meng Axiong group", "Distribution pattern", "Constructed block" ], [ "The late Triassic Meng Axiong group", "Earth tectonic location", "Nujiang Belt" ], [ "The late Triassic Meng Axiong group", "Exposed", "1:250,000 Changdu County's southwest corner green union-Shama Riji" ], [ "The late Triassic Meng Axiong group", "Distribution pattern", "Northwest-south eastward expansion" ], [ "The late Triassic Meng Axiong group", "area", "293.34m2" ] ] }, { "text": "The mud limestone in the overlying strata───────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Licha Group amylin limestone", "Integration of contacts", "Aoqu Group" ], [ "Aoqu Group", "thickness", "566.54m" ] ] }, { "text": "Holocene alluvial accumulation (Qhal) thickness 3m", "triple_list": [ [ "Holocene alluvial accumulation", "thickness", "3m" ] ] }, { "text": "Gray dark gray medium-thick layer of rock-cut quartz fine sandstone and gray-black serous clay slate, etc., produce small bivalve Myophriopis sp. Palaeocardita sp., 134.65m", "triple_list": [ [ "Gray dark gray medium-thick layer of rock cuttings quartz fine sandstone and gray-black serous clay slate and other thick interlayers", "Paleontological", "bivalve Myophriopis sp." ], [ "Gray dark gray medium-thick layer of rock cuttings quartz fine sandstone and gray-black serous clay slate and other thick interlayers", "Paleontological", "Palaeocardita sp." ], [ "Gray dark gray medium-thick layer of rock cuttings quartz fine sandstone and gray-black serous clay slate and other thick interlayers", "thickness", "134.65m" ] ] }, { "text": "Gray-black thin-middle metamorphic quartz silt sandstone with gray medium-thick layer metamorphic quartz fine sandstone and gray-black slate, with wavy marks on the layer, 116.3m", "triple_list": [ [ "Gray-black thin-middle metamorphic quartz silt sandstone with gray medium-thick layer metamorphic quartz fine sandstone and gray-black slate", "Develop", "Wave trace" ], [ "Gray-black thin-middle metamorphic quartz silt sandstone with gray medium-thick layer metamorphic quartz fine sandstone and gray-black slate", "thickness", "116.3m" ] ] }, { "text": "Gray-green block layer Anshan tuff breccia, 11.04m", "triple_list": [ [ "Gray-green block layer Andesan tuff breccia", "thickness", "11.04m" ] ] }, { "text": "The geological era of the Gongjue Formation should be Paleogene.", "triple_list": [ [ "Gongjue Group", "Age", "Paleogene" ] ] }, { "text": "Pleistocene cave accumulation (Qpca) is mainly found in Duoqu, Deden Township, Jiangda County, Fengjiangda County, Jiangda County, and is distributed in caves or dissolution pits about 4,000m.", "triple_list": [ [ "Pleistocene cave accumulation", "Exposed", "1:25 million Jiangda County Fengjiangda County Dedeng Township Duoqu" ] ] }, { "text": "The Jiapila Formation purple-red conglomerate sandstone of the overlying formation, unconformed angle, Tuoba Formation (P3t), thickness 493.52m", "triple_list": [ [ "Jiapila Formation Purple-red Conglomerate Sandstone", "Unconformity contact", "Tuoba Group" ], [ "Tuoba Group", "thickness", "493.52m" ] ] }, { "text": "Avonia tuberculatus Linoproductus cf. cora Dictyoclostus sp. Chori stites sp. Fusulinella boci was obtained in this layer in Fan Yingnian (1977).", "triple_list": [ [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Contained", "Flint clumps" ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Contained", "tuberculosis" ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Paleontological", "Eostaffella sp." ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Paleontological", "Pseudostaffella antiqua P. compressa" ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Paleontological", "Brachiopod Avonia tuberculatus Linoproductus cf. cora Dictyoclostus sp." ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Paleontological", "Chori stites sp." ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "Paleontological", "Fusulinella boci" ], [ "Gray-gray-black thick layer of dense limestone and white thick layer of crystalline limestone", "thickness", "148.90m" ] ] }, { "text": "Serong Temple Group was exposed in 1:25 million areas south of Minda Village, south of Jiangba Village, Pushuiqiao, Ya'an, Jiangda County, with an area of about 125m2.", "triple_list": [ [ "Serong Temple Group", "Exposed", "1:25 million Jiangda County, south of Jiangba Village, Nongpushuiqiao, Ya'an" ], [ "Serong Temple Group", "Exposed", "South of Minda Village" ], [ "Serong Temple Group", "Exposed", "East of Menda" ], [ "Serong Temple Group", "area", "125m2" ] ] }, { "text": "The Russian-Jian Group (2e) is distributed in the area of the Russian-Jian-Guoqiu area in the northwest to the south, and extends to the northwest to the west to the northwest to the 1:25,000 Dingqing County area, gradually disappearing to the southeast, with an exposed area of about 109.77m2.", "triple_list": [ [ "Russia team", "Exposed", "1:250,000 Changdu County's Russian-Jian-Jian-Jiang" ], [ "Russia team", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Russia team", "Exposed", "1:250,000 Dingqing County" ], [ "Russia team", "area", "109.77m2" ] ] }, { "text": "The invading rock belt of Leiwuqi-Dongdashan is mainly composed of late Triassic granite, exposed in the area of Watong-Lewuqi Town-Gangse Township. The rock mass number is 4750525462-17879, intermittently exposed in NW-SE direction, mainly two-chang granite, with a small amount of granite, with a total area of 76.03m2.", "triple_list": [ [ "Lewuqi-Dongdashan invasion rock belt", "Lithology", "Late Triassic Granite" ], [ "Lewuqi-Dongdashan invasion rock belt", "Exposed", "Watong-Leiwuqi Town-Gangse Township" ], [ "Lewuqi-Dongdashan invasion rock belt", "Distribution pattern", "NW-SE exposes intermittently" ], [ "Lewuqi-Dongdashan invasion rock belt", "Lithology", "Second Chang Granite" ], [ "Lewuqi-Dongdashan invasion rock belt", "Lithology", "Grandiorite" ], [ "Lewuqi-Dongdashan invasion rock belt", "area", "76.03m2" ] ] }, { "text": "The flow tuff is mainly gray, and the second is purple-red, with a variable tuff structure and a block-like layer structure.", "triple_list": [ [ "Flow-grained tuff", "Distribution pattern", "Variable tuff structure" ], [ "Flow-grained tuff", "Develop", "Block layer structure" ] ] }, { "text": "Gray-green block metamorphic Angular crystalline clay-cut tuff with light purple-red striped metamorphic Angular subgrade tuff, 91.02m ─────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Gray-green block metamorphic Ying'an crystal clastic tuff with light purple-red striped metamorphic Ying'an sedimentary tuff", "thickness", "91.02m" ], [ "Gray-green block metamorphic Ying'an crystal clastic tuff with light purple-red striped metamorphic Ying'an sedimentary tuff", "thickness", "Russia team" ] ] }, { "text": "The volcanic rock of the Walasi Formation is 850m thick, accounting for 38% of the total thickness of the strata. Among them, volcanic clastic rocks are the main ones, andesite and Andesite volcanic breccia lava.", "triple_list": [ [ "Volcanic rocks of Wala Monastery", "thickness", "850m" ], [ "Volcanic rocks of Wala Monastery", "Lithology", "Pyroclastic rock" ], [ "Volcanic rocks of Wala Monastery", "Lithology", "Andanyan" ], [ "Volcanic rocks of Wala Monastery", "Lithology", "Andesan volcanic breccia lava" ] ] }, { "text": "Accordingly, the Serong Temple Group period was the Early Triassic period, and its lower part was the Orennik rank of the Early Triassic period.", "triple_list": [ [ "Serong Temple Group", "Age", "Early Triassic" ], [ "Serong Temple Group", "Belongs to", "The Orenik rank in the early Triassic" ] ] }, { "text": "Permian-Triassic volcanic rocks in this area are distributed in the Jinsha River junction belt, and are produced in the Permian-Late Triassic Kenan rock group Garieite Formation (P3j.) and the Permian-Early Triassic Gajinxue Mountain Rock Group Gangtoshi Formation (P1g.) and are part of the Jinsha River volcanic rock belt.", "triple_list": [ [ "Permian-Triassic volcanic rocks", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Permian-Triassic volcanic rocks", "Located at", "Permian-late Triassic Kanan Rock Group Gariei Rock Formation" ], [ "Permian-Triassic volcanic rocks", "Located at", "Permian-Early Triassic Gajin Snow Mountain Rock Group Gangtuoyan Formation" ], [ "Permian-Triassic volcanic rocks", "Belongs to", "Jinsha River Volcanic Rock Belt" ] ] }, { "text": "The porphyry vein rock has a luxuriant spot structure and a blocky structure.", "triple_list": [ [ "Porphyry vein rock", "Distribution pattern", "Splendid Structure" ], [ "Porphyry vein rock", "Develop", "Blocky structure" ] ] }, { "text": "Purple-red, gray-green medium-thick layer dolomite lithotripsy feldspar sandstone with mud gravel conglomerate lens body, with siderite nodules and large wedge-shaped plate-like stratigraphy, containing brachiopod Avonothyris sp.; bivalve Protocardia sp. and vertebrate fossil fragments, 37.22m", "triple_list": [ [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "Develop", "siderite nodule" ], [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "Develop", "Wedge-shaped plate-shaped layering" ], [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "Paleontological", "Brachiopod Avonothyris sp." ], [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "Paleontological", "Bivalve Protocardia sp." ], [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "Paleontological", "Fossil fragments of vertebrate animals" ], [ "Purple-red, gray-green medium-thick layer dolomite rock fragment feldstone sandstone with mud grey conglomerate lens body", "thickness", "37.22m" ] ] }, { "text": "Dark gray medium-thick layered bioclass limestone, 230m", "triple_list": [ [ "Dark gray medium-thick layered bioclastic limestone", "thickness", "230m" ] ] }, { "text": "Off-white medium-thick tuff sandstone, 66.64m ─────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Off-white medium-thick tuff sandstone", "thickness", "66.64m" ], [ "Off-white medium-thick tuff sandstone", "Integration of contacts", "Lizha Formation of Early Permian" ] ] }, { "text": "Light gray medium-thick layered bioclad mud crystal limestone, producing bivalve Halobia rugosa H. pluriradiata Posidonia aff. wengensis Entolium sp. norv., 63.42m", "triple_list": [ [ "Light gray medium-thick layered bioclastic mud crystal limestone", "Paleontological", "Bivalve Halobia rugosa H. pluriradiata Posidonia aff. wengensis Entolium sp. norv." ], [ "Light gray medium-thick layered bioclastic mud crystal limestone", "thickness", "63.42m" ] ] }, { "text": "Gray-black slate and dark gray thin-medium-thick sandstone interlayer, producing ammonites Protrachyceras sp. Paracrochordicreas sp. Balatonites sp. Gymnites sp. Bivalve Posidonia sp.; plant Neocalamites sp., 35.50m", "triple_list": [ [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Ammonite Protrachyceras sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Paracrochordicreas sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Balatonites sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Gymnites sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Bivalve Posidonia sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "Paleontological", "Plant Neocalamites sp." ], [ "Gray-black slate and dark gray thin-medium-thick sandstone interlayer", "thickness", "35.50m" ] ] }, { "text": "The Kamado rock block group tectonic invasion is located in the Dongdaqiao Formation (J2d) formation of Luodong Rock Group (3J1L.).", "triple_list": [ [ "Kamado rock mass tectonic invasion", "Located at", "Luodongyan Group" ], [ "Kamado rock mass tectonic invasion", "Located at", "East Bridge Group" ] ] }, { "text": "Light gray medium-thick layered medium-fine grain quartz sandstone, 320m", "triple_list": [ [ "Light gray medium-thick layered medium-fine grain quartz sandstone", "thickness", "320m" ] ] }, { "text": "The Lanashan Formation is composed of gray, dark gray, gray-black slate sandstone, limestone, calcified schist seric schist, etc., with a total exposed thickness of 3648.1m, which is a marine quartz sedimentation.", "triple_list": [ [ "Rana Mountain Group", "Lithology", "Gray dark gray gray black slate" ], [ "Rana Mountain Group", "Lithology", "sandstone" ], [ "Rana Mountain Group", "Lithology", "Limestone" ], [ "Rana Mountain Group", "Lithology", "Qianmeiyan" ], [ "Rana Mountain Group", "Lithology", "Calcium schist" ], [ "Rana Mountain Group", "Lithology", "seric schist" ], [ "Rana Mountain Group", "thickness", "3648.1m" ], [ "Rana Mountain Group", "Belongs to", "Marine refraction" ] ] }, { "text": "Gray-black slate with gray thin to medium-layer metamorphic fine-grained sandstone, 17.35m", "triple_list": [ [ "Gray-black slate with gray thin to medium metamorphic fine-grained sandstone", "thickness", "17.35m" ] ] }, { "text": "The granodiorite mass invaded the marathon multiple groups (1-2m) and was unconformally covered by the Kapila group (3j).", "triple_list": [ [ "Grandiorite body", "Invade", "Marathon multiple sets" ], [ "Grandiorite body", "Unconformity contact", "Kapila Group" ] ] }, { "text": "Grandiorite is exposed in Xiaosumang Township, Yushu Prefecture, Qinghai Province, Dongpuboluo Township, Jiangda County, Tibet and other places.", "triple_list": [ [ "Grandiorite", "Exposed", "Xiaosumang Township, Yushu Prefecture, Qinghai Province" ], [ "Grandiorite", "Exposed", "Dongpuboluo Township, Jiangda County, Tibet" ] ] }, { "text": "To sum up, the Jiaoga Formation is composed of gray-dark gray limestone biological class limestone marstone shale sandstone, etc., and the snake-producing coral brachiopods have foraminiferous bivalve tricyclohexandria sea lily, with a total thickness of 1082.33m.", "triple_list": [ [ "Jiaoga Group", "Lithology", "Grey dark grey limestone" ], [ "Jiaoga Group", "Lithology", "Bioclastic limestone" ], [ "Jiaoga Group", "Lithology", "Marlite" ], [ "Jiaoga Group", "Lithology", "shale" ], [ "Jiaoga Group", "Lithology", "sandstone" ], [ "Jiaoga Group", "Paleontological", "Snake" ], [ "Jiaoga Group", "Paleontological", "coral" ], [ "Jiaoga Group", "Paleontological", "Brachiopod" ], [ "Jiaoga Group", "Paleontological", "Foraminifera" ], [ "Jiaoga Group", "Paleontological", "Bivalves" ], [ "Jiaoga Group", "Paleontological", "Trileleaf" ], [ "Jiaoga Group", "Paleontological", "Chrysanthemum" ], [ "Jiaoga Group", "Paleontological", "sea lily" ], [ "Jiaoga Group", "thickness", "1082.33m" ] ] }, { "text": "Dark green block layer volcanic breccia, 8.49m", "triple_list": [ [ "Dark green block volcanic breccia", "thickness", "8.49m" ] ] }, { "text": "Metamorphic olive basalt, with a microspot-like structure, matrix interwoven structure, and block-like structure.", "triple_list": [ [ "Metamorphic olive basalt", "Distribution pattern", "Microscopic structure" ], [ "Metamorphic olive basalt", "Distribution pattern", "Matrix interwoven structure" ], [ "Metamorphic olive basalt", "Develop", "Blocky structure" ] ] }, { "text": "1:200,000 Dege is called Dongpu duplex granite body (the era is Hualixi period), exposed between Dongpu Village and Pushui Bridge in Jiangda County, with an area of 264.49m2.", "triple_list": [ [ "1:200,000 DeGe format is called Dongpu compound granite body", "Exposed", "Dongpu Village, Jiangda County - Pushui Bridge" ], [ "1:200,000 DeGe format is called Dongpu compound granite body", "area", "264.49m2" ] ] }, { "text": "The Quga Temple Group (3q) is distributed in the areas of Xiarixiuyong, Jiangda County, Tibet - Gongya-Baimeng Temple, Dege County, Sichuan Province, Heirushe Niuchang-Babang Township, Doergagou-Napshe Niuchang Baiyu County, Xiarixi, etc., extending to the north into the Shiqu County area, and extending to the east into the Ganzi County area, with an area of about 740m2.", "triple_list": [ [ "Quga Temple Group", "Exposed", "Tibet Jiangda County, Tibet—Gongya, Gongya, Dege County, Sichuan—Baimeng Temple" ], [ "Quga Temple Group", "Exposed", "Heirushe cattle farm-Dorgagou, Babang Township-Napshe cattle farm Xiarixi" ], [ "Quga Temple Group", "Exposed", "1:250,000 Shiqu County" ], [ "Quga Temple Group", "Exposed", "1:250,000 Ganzi County" ], [ "Quga Temple Group", "area", "740m2" ] ] }, { "text": "Total thickness of Toba Group (P3t) is 1362.9m", "triple_list": [ [ "Tuoba Group", "thickness", "1362.9m" ] ] }, { "text": "The purple-red thick layer of quartz fine conglomerate and quartz sandstone arable feldspar quartz silt sandstone, 236.60m ―――――――――――――――――――――――――――――――――――――――――――――――――――――――――――――――――――�", "triple_list": [ [ "Interlayer of purple-red thick quartz fine conglomerates and quartz sandstone amid feldspar quartz siltstone", "thickness", "236.60m" ], [ "Interlayer of purple-red thick quartz fine conglomerates and quartz sandstone amid feldspar quartz siltstone", "Integration of contacts", "Limestone sandstone of Wala Monastery" ] ] }, { "text": "Gray light gray thick layer—block layer of rock cuttings quartz fine sandstone with gray black clay slate, 116.84m", "triple_list": [ [ "Gray light gray thick layer—block layer of rock cuttings quartz fine sandstone with gray black clay slate", "thickness", "116.84m" ] ] }, { "text": "The Mesozoic cover layer was constructed with the Jiapila Group (3j), Polila Group (3b), Adula Group (3a), Dugail Group (3d), Wangbu Group (J1w) Dongdaqiao Group (J2d).", "triple_list": [ [ "Mesozoic capping construction", "Contained", "Kapila Group" ], [ "Mesozoic capping construction", "Contained", "Polira group" ], [ "Mesozoic capping construction", "Contained", "Adula Group" ], [ "Mesozoic capping construction", "Contained", "Gala group" ], [ "Mesozoic capping construction", "Contained", "Wang Bu Group" ], [ "Mesozoic capping construction", "Contained", "East Bridge Group" ] ] }, { "text": "Serpentine petrochemical pure perlite is dark green, has a grid structure, a block-like structure.", "triple_list": [ [ "Serpentine petrochemical pure perlite", "Distribution pattern", "Grid structure" ], [ "Serpentine petrochemical pure perlite", "Distribution pattern", "False spot structure" ], [ "Serpentine petrochemical pure perlite", "Develop", "Blocky structure" ] ] }, { "text": "Gray-black radiated silicone serous slate with rock-cut quartz sandstone, 62.48m", "triple_list": [ [ "Gray-black radiated silicone serous slate with rock cuttings quartz sandstone", "thickness", "62.48m" ] ] }, { "text": "The only fossils in the Dedari Ayan Formation (P3d.) can be determined that the only fossils in the era are Cyclocyclicus cf. rotiformis, which is the Triassic period.", "triple_list": [ [ "Have to fight against RiAyan Group", "Paleontological", "Sea lily stem Cyclocyclicus cf. rotiformis" ], [ "Have to fight against RiAyan Group", "Age", "Triassic" ] ] }, { "text": "Light gray thick layered biological clastic mud crystal limestone with gray-white medium-thick layered sandy limestone, producing bivalve Posidonia aff. wengensis Halobia pluriradiata H. xizangensis, 72.60m", "triple_list": [ [ "Light gray thick layered biological clastic mud crystal limestone with gray-white medium-thick layered sandy limestone", "Paleontological", "Bivalve Posidonia aff. wengensis Halobia pluriradiata H. xizangensis" ], [ "Light gray thick layered biological clastic mud crystal limestone with gray-white medium-thick layered sandy limestone", "thickness", "72.60m" ] ] }, { "text": "The Tumugou Formation is composed of gray-dark gray-grey black crystalline limestone sandstone slate 100 rock calcified quartz schist serotonite serotonite schist, acidic volcanic conglomerates, etc., and produces bivalves, gastropod coral tooth-shaped thorns, etc., with a total exposed thickness >2103m.", "triple_list": [ [ "Tumugou Group", "Lithology", "Gray dark gray gray black crystal limestone" ], [ "Tumugou Group", "Lithology", "sandstone" ], [ "Tumugou Group", "Lithology", "Slate" ], [ "Tumugou Group", "Lithology", "Qianmeiyan" ], [ "Tumugou Group", "Lithology", "Calcium schist" ], [ "Tumugou Group", "Lithology", "serous quartz schist" ], [ "Tumugou Group", "Lithology", "Medium-acid volcanic rocks" ], [ "Tumugou Group", "Lithology", "Polygon" ], [ "Tumugou Group", "Paleontological", "Bivalves" ], [ "Tumugou Group", "Paleontological", "Gastropod" ], [ "Tumugou Group", "Paleontological", "coral" ], [ "Tumugou Group", "Paleontological", "Teeth thorn" ], [ "Tumugou Group", "thickness", "2103m" ] ] }, { "text": "The main Late Paleozoic volcanic rocks in the Chamdo-Mangkang volcanic rocks include the Early Carboniferous Machala Formation, the Late Carboniferous Aoqu Formation, the Middle Permian Mangcuo Formation, and the Late Permian Xiayacun Formation.", "triple_list": [ [ "Late Paleozoic volcanic rocks in Chamdo-Mangkang Volcanic Rock Belt", "Contained", "Early Carboniferous Machara Formation Volcanic Rock" ], [ "Late Paleozoic volcanic rocks in Chamdo-Mangkang Volcanic Rock Belt", "Contained", "Late Carboniferous Aoqu Formation Volcanic Rock" ], [ "Late Paleozoic volcanic rocks in Chamdo-Mangkang Volcanic Rock Belt", "Contained", "The volcanic rock of the Mangcuo Group of Jiaoga Formation in the Middle Permian" ], [ "Late Paleozoic volcanic rocks in Chamdo-Mangkang Volcanic Rock Belt", "Contained", "Volcanic rocks in Xiaya Village Group, Late Permian" ] ] }, { "text": "The Jiaoga Formation in the Middle Permian (P2j) is distributed in 1:25,000. The Jiaoga Formation in the Oqinlan, Nangqin County, Nangqin County, Nangqin County, 1:25,000. The exposed area is about 253.13m2.", "triple_list": [ [ "Middle Permian Jiaoga Group", "Exposed", "1:25 million Nangqian County, Nangqinong Gazizabu, Oqinong" ], [ "Middle Permian Jiaoga Group", "Exposed", "1:250,000 Changdu County Bianqian County Town Balan" ], [ "Middle Permian Jiaoga Group", "Exposed", "Tibet Lewuqi County Qiumuri Ezaguo-Waji" ], [ "Middle Permian Jiaoga Group", "Exposed", "1:25 million Jiangda County, Chaodu County" ], [ "Middle Permian Jiaoga Group", "area", "253.13m2" ] ] }, { "text": "Coarse basalt gray-green, rough and mysterious structure, block-like structure.", "triple_list": [ [ "Crude basalt", "Distribution pattern", "Coarse and mysterious structure" ], [ "Crude basalt", "Develop", "Blocky structure" ] ] }, { "text": "Therefore, the Mangcuo Group era belonged to the early stage of the Middle Permian period.", "triple_list": [ [ "Rude group", "Age", "Early Middle Permian" ] ] }, { "text": "Grey thin-medium-layered microcrystalline limestone, ammonite production Discotropites sp., Gastropods Anulifera cf. yunnanensis, 59.80m", "triple_list": [ [ "Gray thin-medium-layered microcrystalline limestone", "Paleontological", "Ammonite Discotropites sp." ], [ "Gray thin-medium-layered microcrystalline limestone", "Paleontological", "Gastropods Anulifera cf. yunnanensis" ], [ "Gray thin-medium-layered microcrystalline limestone", "thickness", "59.80m" ] ] }, { "text": "Gray-black thin-layer silt sandstone shale containing charcoal-bearing limestone intersects strip-like medium acidic tuff, limestone medium-sized aphrodisiac. Coelonella subcardiopetala Cyathus sp. Bairdia subnitida B. hassi Ceratobai longicalida C. subfirmata Orthobai rdia molliuscula O. cestriensis Bairdiacypris benxiensis Fabalicypris shidelari, Silenites mui, and gastropod Lopho spira sp., 33.47m", "triple_list": [ [ "Gray-black thin-layer silt sandstone shale carbon-containing aleite limestone intersects strip-like medium acidic tuff", "thickness", "33.47m" ], [ "Limestone", "Paleontological", "Coelonella subcardiopetala Cyathus sp. Bairdia subnitida B. hassi Ceratobai longicalida C. subfirmata Orthobai rdia molliuscula O. cestriensis Bairdiacypris benxiensis Fabalicypris shidelari" ], [ "Limestone", "Paleontological", "Silenites mui" ] ] }, { "text": "The mud limestone in the overlying strata───────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Licha Group amylin limestone", "Integration of contacts", "Aoqu Group" ], [ "Aoqu Group", "thickness", "287.54m" ] ] }, { "text": "Dark gray medium-thick layered limestone with thin layer of sandstone, 126.3m ───────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Dark gray medium-thick layered limestone with thin layer of sandstone", "thickness", "126.3m" ], [ "Dark gray medium-thick layered limestone with thin layer of sandstone", "Integration of contacts", "Sandstone slate of the Jiapila Formation" ] ] }, { "text": "The marathon groups are composed of gray-green rhyolite rhyolite rhyolite sandstone shale slate conglomerates, with an exposed thickness of 2272.05m.", "triple_list": [ [ "Marathon multiple sets", "Lithology", "Gray-gray-green rhyolite" ], [ "Marathon multiple sets", "Lithology", "Flow-grained tuff" ], [ "Marathon multiple sets", "Lithology", "sandstone" ], [ "Marathon multiple sets", "Lithology", "shale" ], [ "Marathon multiple sets", "Lithology", "Slate" ], [ "Marathon multiple sets", "Lithology", "Polygon" ], [ "Marathon multiple sets", "thickness", "2272.05m" ] ] }, { "text": "Purple-red thin to medium-layer lithotrix quartz sandstone mudstone interlayer tuffy biological detritus gray matter dolomite, 54.53m────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Purple-red thin to medium-layer lithotrix quartz sandstone mudstone interlayer tuffy bioclad grey matter dolomite", "thickness", "54.53m" ], [ "Purple-red thin to medium-layer lithotrix quartz sandstone mudstone interlayer tuffy bioclad grey matter dolomite", "Integration of contacts", "Machara Formation Limestone" ] ] }, { "text": "The lower part of the bamboo group contains more volcanic breccia, 235.93m", "triple_list": [ [ "Bamboo card group", "Lithology", "Volcanic horns" ], [ "Bamboo card group", "thickness", "235.93m" ] ] }, { "text": "The Polila Formation in this strata is thin, but very stable. The lithology is composed of a set of shallow marine carbonate sedimentation gray-white limestone biological clastic limestone mixed with mudstone. There are fewer fossils on the profile. Bivalve brachiopod corals, etc. are obtained on the route, with a total thickness of 29,230m.", "triple_list": [ [ "Polira group", "Belongs to", "Shallow marine carbonate sedimentation" ], [ "Polira group", "Lithology", "Gray white limestone" ], [ "Polira group", "Lithology", "Bioclastic limestone" ], [ "Polira group", "Lithology", "Mudstone" ], [ "Polira group", "Paleontological", "Bivalves" ], [ "Polira group", "Paleontological", "Brachiopod" ], [ "Polira group", "Paleontological", "coral" ], [ "Polira group", "thickness", "29230m" ] ] }, { "text": "On this section, the sand wood group is damaged by faults, the expose is wedge-shaped, with good outcropping, and the lithology is shallow sea-sea-land-interaction sandstone, biological clastic mud crystal limestone or limestone lens body, rich in marine fossils and plant fragments, no top and bottom are found, and the wrist-pods and corals are produced.", "triple_list": [ [ "Shamu Group", "Distribution pattern", "Wedge-shaped" ], [ "Shamu Group", "Belongs to", "Shallow sea-land and sea interaction" ], [ "Shamu Group", "Lithology", "sandstone" ], [ "Shamu Group", "Lithology", "Siltstone" ], [ "Shamu Group", "Lithology", "Bioclass mud crystal limestone" ], [ "Shamu Group", "Lithology", "Limestone lens body" ], [ "Shamu Group", "Paleontological", "Marine fossils" ], [ "Shamu Group", "Paleontological", "Plant fragments" ], [ "Shamu Group", "Paleontological", "Wrist foot" ], [ "Shamu Group", "Paleontological", "Snake" ], [ "Shamu Group", "Paleontological", "coral" ] ] }, { "text": "Light gray medium-layered muddy siltstone, 210m──────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Light gray medium layered muddy siltstone", "thickness", "210m" ], [ "Light gray medium layered muddy siltstone", "Integration of contacts", "Dongque Formation Limestone" ] ] }, { "text": "Gray-brown thick layered fine-grained feldspar crushed sandstone sandstone with gray silty slate, producing bivalve Halobia superbescens H. rugosa, 202.22m", "triple_list": [ [ "Gray-brown thick layered fine-grained feldspar crushed sandstone with gray silty slab", "Paleontological", "Bivalve Halobia superbescens H. rugosa" ], [ "Gray-brown thick layered fine-grained feldspar crushed sandstone with gray silty slab", "thickness", "202.22m" ] ] }, { "text": "Brick red thick layered dolomite fine-grained rock fragment quartz sandstone and brick red medium-thick layered dolomite sandstone, 20.06m", "triple_list": [ [ "Brick red thick layered dolomite fine-grained quartz sandstone and brick red medium-thick layered dolomite sandstone are not equally thick interlayered", "thickness", "20.06m" ] ] }, { "text": "Dark gray thin layer of microcrystalline limestone intersects several layers of transformed rhyolite, 149.9m", "triple_list": [ [ "Dark gray thin layer of microcrystalline limestone intersects several layers of rheology", "thickness", "149.9m" ] ] }, { "text": "Off-white medium-thick layer of powdery limestone, producing snail Pseudostaffella sp.; Coral Fomitherella sp., 69.84m", "triple_list": [ [ "Off-white medium-thick layer of powdery limestone", "Paleontological", "Pseudostaffella sp." ], [ "Off-white medium-thick layer of powdery limestone", "Paleontological", "Coral Fomitherella sp." ], [ "Off-white medium-thick layer of powdery limestone", "thickness", "69.84m" ] ] }, { "text": "According to the characteristics of rock combination, sedimentary structure, paleontology, etc., the Jiaoga Formation is mainly a set of shallow sea shed carbonate sedimentation.", "triple_list": [ [ "Jiaoga Group", "Belongs to", "Carbonate rock sedimentation in shallow sea shelter" ] ] }, { "text": "Overlapping strata of Wangguo Formation Biological Clastula Dolomite Crystallisstone ───────────────────── Dongque Formation (C1d), thickness 104.61m", "triple_list": [ [ "Bioclastic dolomite crystalline limestone of Wangguo Formation", "Integration of contacts", "Dong Que Group" ], [ "Dong Que Group", "thickness", "104.61m" ] ] }, { "text": "The angular radics are gray-green, with fibrous metamorphic structure and directional structure.", "triple_list": [ [ "horned schist", "Distribution pattern", "Fragile crystal structure" ], [ "horned schist", "Develop", "Directional construction" ] ] }, { "text": "Parallelodon sp. Posidonia sp.; Coelonella sp. Paraparchites sp. Roundyella sp. Fabalicypris sp., 132.15m", "triple_list": [ [ "Limestone", "Paleontological", "bivalve Parallelodon sp." ], [ "Limestone", "Paleontological", "Posidonia sp." ], [ "Limestone", "Paleontological", "Coelonella sp." ], [ "Limestone", "Paleontological", "Paraparchites sp." ], [ "Limestone", "Paleontological", "Roundyella sp." ], [ "Limestone", "Paleontological", "Fabalicypris sp." ], [ "Limestone", "thickness", "132.15m" ] ] }, { "text": "The Jiangda-Deqin strata are less exposed and distributed scattered. From old to new, there are early Permian Jidonglong Formation (P1j) and late Permian Shamu Formation.", "triple_list": [ [ "Jiangda-Deqin Stratigraphic Zone", "Outcrop", "Permian strata" ], [ "Permian strata", "Outcrop", "Early Permian Jidonglong Group" ], [ "Permian strata", "Outcrop", "Late Permian Sanmu Group" ] ] }, { "text": "The Jinsha River invading rock zone exposed a small amount of late Triassic rock mass, with a total area of 56.77m2, and was exposed sporadically in Jiezonglong, Gapo, Xiewolong and other places in Yushu Prefecture, Qinghai Province, and Boluo Township, Jiangda County, Tibet. The rock types seen include diorite quartz diorite 2 Changya granite granite granite granite granite.", "triple_list": [ [ "Jinsha River invades the rock belt", "Contained", "Late Triassic rock body" ], [ "Late Triassic rock body", "area", "56.77m2" ], [ "Late Triassic rock body", "Exposed", "Xiewolong, Jiezonglong, Gapo, Yushu Prefecture, Qinghai Province" ], [ "Late Triassic rock body", "Exposed", "Boluo Township, Jiangda County, Tibet" ], [ "Late Triassic rock body", "Lithology", "Diorite" ], [ "Late Triassic rock body", "Lithology", "Quartz diorite" ], [ "Late Triassic rock body", "Lithology", "Erchang granite" ], [ "Late Triassic rock body", "Lithology", "Grandiorite" ], [ "Late Triassic rock body", "Lithology", "granite" ] ] }, { "text": "The thickness of the rude group (P2mc) is 632.82m", "triple_list": [ [ "Rude group", "thickness", "632.82m" ] ] }, { "text": "Overhead formation Polila Formation (3b) gray limestone ──────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polira group", "Lithology", "Gray limestone" ], [ "Polira group", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "638.17m" ] ] }, { "text": "Dark gray rock cuttings siltstone, 21.08m", "triple_list": [ [ "Dark gray rock cuttings siltstone", "thickness", "21.08m" ] ] }, { "text": "The era of Yingzhu Niang A Group was the early period of the late Triassic period - Noli period.", "triple_list": [ [ "Yingzhu Niang group", "Age", "Early Carnie period in the Late Triassic period-Nori period" ] ] }, { "text": "Light gray block layered limestone conglomerate, not seen, 80.59m", "triple_list": [ [ "Light gray block layered limestone gravel", "thickness", "80.59m" ] ] }, { "text": "The Jurassic system in this area is relatively developed and is distributed in the Jiangda-Deqin stratigraphic division of the Lewuqi-Zuogong stratigraphic division of the Changdu-Mangkang stratigraphic division. It is divided from old to new into the early Jurassic Wanbu Formation (J1w), middle Jurassic East Bridge Formation (J2d), late Jurassic Small Sokha Formation (J3x) stratigraphic sequence from old to new.", "triple_list": [ [ "Jurassic", "Stratigraphical zoning", "Lewuqi-Zuogong Stratigraphic Division" ], [ "Jurassic", "Stratigraphical zoning", "Chamdo-Mangkang Stratigraphic Zone" ], [ "Jurassic", "Stratigraphical zoning", "Jiangda-Deqin Stratigraphic Zone" ], [ "Jurassic", "Outcrop", "Early Jurassic Wanbu Group" ], [ "Jurassic", "Outcrop", "Middle Jurassic East Bridge Group" ], [ "Jurassic", "Outcrop", "Late Jurassic Solo Card" ] ] }, { "text": "The bamboo group of this subdistrict consists of gray-green, gray-purple-red, turmeric tuff, inanite volcanic breccia, dark-gray tuff, slate tuff, etc., with a total thickness of 2051.65m.", "triple_list": [ [ "Bamboo card group", "Lithology", "Gray green gray purple purple-red Ying'an flow tuff" ], [ "Bamboo card group", "Lithology", "Ying'an Rock" ], [ "Bamboo card group", "Lithology", "Volcanic breccia" ], [ "Bamboo card group", "Lithology", "Dark gray tuff slate" ], [ "Bamboo card group", "Lithology", "Tuff" ], [ "Bamboo card group", "thickness", "2051.65m" ] ] }, { "text": "Paleobiological fossils are rare, and only coral Myriophyllum sp. is obtained in the limestone in Balipu area of Dege County. According to its integration and coverage on the Tumugou Formation, its era is placed in the Noli period of the late Triassic period.", "triple_list": [ [ "Balipu, Dege County", "Contained", "Limestone" ], [ "Limestone", "Paleontological", "Coral Myriophyllum sp." ], [ "Limestone", "Integration of contacts", "Tumugou Group" ], [ "Limestone", "Age", "The Late Triassic Noli period" ] ] }, { "text": "Light gray-bricked grey block layer breccia limestone with mid-layer bioclastic limestone with gray-white bioclastic limestone, producing coral Favosi chaetet sp. Guizhouchaetets sp. Dermasophyllum sp., 38.99m", "triple_list": [ [ "Light gray-brick-layered breccia-like limestone with mid-layer bioclastic limestone with gray-white bioclastic limestone", "Paleontological", "coral Favosi chaetet sp." ], [ "Light gray-brick-layered breccia-like limestone with mid-layer bioclastic limestone with gray-white bioclastic limestone", "Paleontological", "Guizhouchaetets sp." ], [ "Light gray-brick-layered breccia-like limestone with mid-layer bioclastic limestone with gray-white bioclastic limestone", "Paleontological", "Dermasophyllum sp." ], [ "Light gray-brick-layered breccia-like limestone with mid-layer bioclastic limestone with gray-white bioclastic limestone", "thickness", "38.99m" ] ] }, { "text": "The Pleistocene flood accumulation materials (Qpppl) are mainly distributed in the Lancang River in Zhaqu Changdu County, Jiqu Changdu County, Ziqu Jiasangka Township, Leiwuqi County, Leiwuqi County, and the rivers and their tributary ditches and mountain passes, and are often fan-shaped landforms, and are all superimposed on the 2nd stages of the riverbed or form a 23-level flood accumulation platform.", "triple_list": [ [ "Pleistocene flood accumulation", "Exposed", "Lancang River, Jiquchangdu County, Zhaquchangdu County, Changdu County, Ziqujiasangka Township, Leiwuqi County" ], [ "Pleistocene flood accumulation", "Exposed", "Jiangda County Gaiqu Jinsha River" ], [ "Pleistocene flood accumulation", "Distribution pattern", "Fan-shaped landform" ] ] }, { "text": "Gray-black slate lithotripsy sandstone and conglomerate interlayer, containing ammonites Japonitesa sp. Balatonites sp.; Paracrochordices sp. Cuccoceras sp. Gymnites sp. Leiophhyllites sp., 360.00m", "triple_list": [ [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Ammonites Japonitesa sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Balatonites sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Paracrochordicera s sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Cuccoceras sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Gymnites sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "Paleontological", "Leiophhyllites sp." ], [ "Gray-black slate cuttings sandstone and conglomerate interlayer", "thickness", "360.00m" ] ] }, { "text": "Gray purple gray block layer metamorphic unequal grain sandy quartz conglomerate, 128.10m", "triple_list": [ [ "Gray purple gray block layer metamorphic unequal grain sandy quartz gravel", "thickness", "128.10m" ] ] }, { "text": "According to its fossil data, the geological era of the Wangbu Formation was the early-late Jurassic period.", "triple_list": [ [ "Wang Bu Group", "Age", "Early Jurassic Early-late" ] ] }, { "text": "The Russian Rock Formation (CPe.) is a set of tectonic mixed rocks with complex lithology and strong deformation and shallow metamorphism. The main lithology is a set of quartz schist slate metamorphic sandstone siliceous rocks, etc., mixed with metamorphic peridotite serpentine petrified peridotite serpentine serpentine crystal rocks and other rock blocks.", "triple_list": [ [ "Russian Rock Formation", "Belongs to", "Tectonic hybrid rocks in deep-sea sedimentation" ], [ "Russian Rock Formation", "Lithology", "Quartz schist" ], [ "Russian Rock Formation", "Lithology", "Slate" ], [ "Russian Rock Formation", "Lithology", "Metamorphic Sandstone" ], [ "Russian Rock Formation", "Lithology", "Silicone rock" ], [ "Russian Rock Formation", "Lithology", "Metamorphic peridotite" ], [ "Russian Rock Formation", "Lithology", "serpentine petrochemical peridotite" ], [ "Russian Rock Formation", "Lithology", "Serpentine" ], [ "Russian Rock Formation", "Lithology", "Crystal rock" ] ] }, { "text": "Off-white medium-thick layered fine-grained feldspar rock-cut sandstone with a small amount of dark gray thin-layered argillic silt sandstone, containing plant fragments, 187.06m", "triple_list": [ [ "Off-white medium-thick layered fine-grained feldspar crushed sandstone with a small amount of dark gray thin-layered muddy silt sandstone", "Paleontological", "Plant fragments" ], [ "Off-white medium-thick layered fine-grained feldspar crushed sandstone with a small amount of dark gray thin-layered muddy silt sandstone", "thickness", "187.06m" ] ] }, { "text": "Gray light gray with gray black glitter cemented spiny clay limestone with gray white medium-thick layer of glitter cemented algae gravel limestone, containing snail Schwagerina criticala, Pseudodoliolilina sp., 60.5m", "triple_list": [ [ "Gray light gray with gray black glitter cemented spiny clay limestone with gray white medium-thick layer of glitter cemented algae gravel limestone", "Paleontological", "Schwagerina criticala" ], [ "Gray light gray with gray black glitter cemented spiny clay limestone with gray white medium-thick layer of glitter cemented algae gravel limestone", "Paleontological", "Pseudodolina sp." ], [ "Gray light gray with gray black glitter cemented spiny clay limestone with gray white medium-thick layer of glitter cemented algae gravel limestone", "thickness", "60.5m" ] ] }, { "text": "Light gray-black thick-medium-thick layer of limestone, with flint tuberculosis on the upper part, containing bryozoosin Fenestella sp.; Brachipods Spirifer sp., Choris tites sp., Pugnax sp., Buxtonia sp., Brachythyrina sp., Cleiothyridina sp.; Coral Bradyphyllum sp.; Barrandeophyllum sp., 163.30m", "triple_list": [ [ "Light gray gray black thick-medium thick limestone", "Contained", "Flint tuberculosis" ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Bryomyces Fenestella sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Brachiopod Spirifer sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Choris tites sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Pugnax sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Buxtonia sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Brachythyrina sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Cleiothyridina sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Coral Bradyphyllum sp." ], [ "Light gray gray black thick-medium thick limestone", "Paleontological", "Barrandeophyllum sp." ], [ "Light gray gray black thick-medium thick limestone", "thickness", "163.30m" ] ] }, { "text": "The Polila Formation (3b) is built for a set of carbonate rocks.", "triple_list": [ [ "Polira group", "Belongs to", "Carbonate rock construction" ] ] }, { "text": "Gray-black mud calcium slate, 89.63m", "triple_list": [ [ "Gray-black mud calcium slab", "thickness", "89.63m" ] ] }, { "text": "In the Shengpa area, the Jidonglong Formation is composed of sandy limestone limestone limestone limestone limestone fine-grained limestone feldstone medium-basic tuff limestone limestone calcified limestone calcified limestone calcified limestone limestone calcified limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone limestone", "triple_list": [ [ "Raw Pa", "Outcrop", "Ji Donglong Group" ], [ "Ji Donglong Group", "Lithology", "Sandy limestone" ], [ "Ji Donglong Group", "Lithology", "Rock cuttings sandstone" ], [ "Ji Donglong Group", "Lithology", "Gravel-containing silt sandstone" ], [ "Ji Donglong Group", "Lithology", "Black silty slab" ], [ "Ji Donglong Group", "Lithology", "Granular limestone" ], [ "Ji Donglong Group", "Lithology", "Fine-grained rock" ], [ "Ji Donglong Group", "Lithology", "Chop sandstone" ], [ "Ji Donglong Group", "Lithology", "Calcium rock" ], [ "Ji Donglong Group", "Lithology", "Chissite sandstone" ], [ "Ji Donglong Group", "Lithology", "Mesobasic tuff" ], [ "Ji Donglong Group", "Lithology", "Pink limestone" ], [ "Ji Donglong Group", "Lithology", "Calcium Sandstone" ], [ "Ji Donglong Group", "Lithology", "Flyssil sandstone" ] ] }, { "text": "The Wangguo Formation is distributed in the area of Sangzhi Akao in Bailiangniang Township, Yushu County, Nangqian County, and 1:25 million yuan. The exposed area is about 10.5m2, and it is in integrated contact with the Dongque Formation (C1d) of the underlying formation and Jidonglong Formation (P1j) of the overlying formation.", "triple_list": [ [ "Wang Guo Group", "Exposed", "1:25 million Nangqian County Band Sangzhi Akao" ], [ "Wang Guo Group", "Exposed", "1:25 million Wang Guo, Fanggucai Village, Jiangda County" ], [ "Wang Guo Group", "area", "10.5m2" ], [ "Wang Guo Group", "Integration of contacts", "Dong Que Group" ], [ "Wang Guo Group", "Integration of contacts", "Ji Donglong Group" ] ] }, { "text": "The sub-district Duogaila Formation consists of gray-dark gray quartz sandstone sandstone mudstone, sandstone mudstone, mixed with a small amount of coal line, and produces bivalve plants, with a total exposed thickness of >1271.81m, which is a set of sea and land-based interactive sand mud-containing coal deposits.", "triple_list": [ [ "Gala group", "Lithology", "Grey dark grey quartz sandstone" ], [ "Gala group", "Lithology", "sandstone" ], [ "Gala group", "Lithology", "Mudstone" ], [ "Gala group", "Lithology", "Coal line" ], [ "Gala group", "Paleontological", "Bivalves" ], [ "Gala group", "thickness", "1271.81m" ], [ "Gala group", "Belongs to", "Sea-land interaction sand mud coal-containing sedimentation" ] ] }, { "text": "Gray-green dense blocky Anshan crystalline crystal tuff, 11.04m", "triple_list": [ [ "Gray-green dense blocky Andesan crystalline tuff", "thickness", "11.04m" ] ] }, { "text": "Gray white light gray thick blocky glitter crystal intercalculus limestone glitter crystal cf, containing flint clumps, yielding sinus Quasifusulina cf. cayeuxi Minojapanella sp. Schubertella sp. Sphaeroschwagerina sp. Naninella rhomboidea Rubustoschwagerina sp. R. schellwieni Rugosorusulina sp. R. cf. steadyis Schwagerinidae Schwagerina sp. , 69.9m", "triple_list": [ [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Contained", "Flint clumps" ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "Quasifusulina cf. cayeuxi Minojapanella sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "Schubertella sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "Sphaeroschwagerina sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "Naninella rhomboidea Rubustoschwagerina sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "R. schellwieni Rugosorusulina sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "Paleontological", "R. cf. steadyis Schwagerinidae Schwagerina sp." ], [ "Gray white light gray thick block glitter crystal intercalculus limestone glitter crystal clay limestone", "thickness", "69.9m" ] ] }, { "text": "Jingxing Group (K1j) thickness 1046.03m", "triple_list": [ [ "Jingxing Group", "thickness", "1046.03m" ] ] }, { "text": "Dark gray thin-medium layered biolimestone, 39.24m, fault contact, Donla formation limestone", "triple_list": [ [ "Dark gray thin-medium layered biolimestone", "thickness", "39.24m" ], [ "Dark gray thin-medium layered biolimestone", "Fault contact", "Donla Formation Limestone" ] ] }, { "text": "The original rock of Zhukaqun is a neutral medium acidic volcanic rock with a small number of clastic rock formations.", "triple_list": [ [ "Bamboo card group", "Lithology", "Neutral medium acidic volcanic rocks" ], [ "Bamboo card group", "Lithology", "Clastite" ] ] }, { "text": "Brown-gray tuff slate and serous slate interlayer, 20.30m", "triple_list": [ [ "Brown-gray tuff slate and serous slate interlayer", "thickness", "20.30m" ] ] }, { "text": "Medium acidic crystalline crystalline tuff is gray-green, with a change of tuff structure and a layered structure.", "triple_list": [ [ "Medium acidic crystalline crystallis tuff", "Distribution pattern", "Variable tuff structure" ], [ "Medium acidic crystalline crystallis tuff", "Develop", "Layered structure" ] ] }, { "text": "Calcium quartz siltstone, produced by Fascipteris (Ptychocarpus)densata Gigonto pteris sp. Pecopteris sp. Compsopt eris sp. Annularia hunaensis Sphenophyllum cf. minor and bivalve Schizodus sp., not bottomed, 199.00m", "triple_list": [ [ "Calcium quartz siltstone", "Paleontological", "Plant Fascipteris (Ptychocarpus)densata Gigonto pteris sp." ], [ "Calcium quartz siltstone", "Paleontological", "Pecopteris sp." ], [ "Calcium quartz siltstone", "Paleontological", "Compsopt eris sp." ], [ "Calcium quartz siltstone", "Paleontological", "Annularia hunaensis Sphenophyllum cf. minor" ], [ "Calcium quartz siltstone", "Paleontological", "bivalve Schizodus sp." ], [ "Calcium quartz siltstone", "thickness", "199.00m" ] ] }, { "text": "Light gray medium-thick layered quartz sandstone with dark gray slate, 210m", "triple_list": [ [ "Light gray medium-thick layered quartz sandstone with dark gray slate", "thickness", "210m" ] ] }, { "text": "Purple-red thick layer of quartz conglomerate lithotripsum quartz silt sandstone and a small amount of mudstone interlayer, 27.21m", "triple_list": [ [ "Purple-red thick layer of quartz conglomerate lithotripsy quartz silt sandstone and a small amount of mudstone interlayer", "thickness", "27.21m" ] ] }, { "text": "Off-white unequal grain calcite-rich limestone, produced by Millerella sp. Eostaffella mosquensis E. aceepta E. prciensis Mediocris mediocris; Palaeotextularia sp. Climacammina sp., 30.94m", "triple_list": [ [ "Off-white, unequal grained calcite-rich limestone", "Paleontological", "Millerella sp. Eostaffella mosquensis E. aceepta E. prciensis Mediocris mediocris" ], [ "Off-white, unequal grained calcite-rich limestone", "Paleontological", "foraminifera Palaeutextularia sp. Climacammina sp." ], [ "Off-white, unequal grained calcite-rich limestone", "thickness", "30.94m" ] ] }, { "text": "Dark gray-black slate metamorphic sandstone with siliceous rock, 247.98m", "triple_list": [ [ "Dark gray-black slate metamorphic sandstone intersecting siliceous rock", "thickness", "247.98m" ] ] }, { "text": "Gray-black slate with gray thin-thick layer of fine-grained cuts feldspar sandstone, 33.78m, fault contact, carbonate rock block (ca), false thickness 158.45m", "triple_list": [ [ "Gray-black slate with gray thin-thick layer of fine-grained cuts feldspar sandstone", "thickness", "33.78m" ], [ "Gray-black slate with gray thin-thick layer of fine-grained cuts feldspar sandstone", "Fault contact", "Carbonate rock blocks" ], [ "Carbonate rock blocks", "thickness", "158.45m" ] ] }, { "text": "Purple-red blocky dolomite feldspar crushed coarse sandstone, not topped, 15.73m", "triple_list": [ [ "purple-red blocky dolomite feldspar crushed coarse sandstone", "thickness", "15.73m" ] ] }, { "text": "Yellow-brown thick layer - fine-grained rock fragment sandstone with silty slate, 147.22m", "triple_list": [ [ "Yellow-brown thick layer-fine-grained rock sandstone sandstone with silty slab", "thickness", "147.22m" ] ] }, { "text": "Gray calcareous rock feldspar silt sandstone, fault damage has not bottomed out, 103.92m, fault contact, volcanic sandstone slate of Walasi Formation", "triple_list": [ [ "Gray calcareous lithotris feldspar silt sandstone", "thickness", "103.92m" ], [ "Gray calcareous lithotris feldspar silt sandstone", "Fault contact", "Volcanic rock sandstone slate in Walasi Formation" ] ] }, { "text": "Holocene alluvial accumulation (Qhal), thickness 22.7m", "triple_list": [ [ "Holocene alluvial accumulation", "thickness", "22.7m" ] ] }, { "text": "Off-white serous quartz thousand rocks, 111.7m", "triple_list": [ [ "Off-white serous quartz thousand rocks", "thickness", "111.7m" ] ] }, { "text": "The lithology of Jiayuqiao rock group (Pz2J.) is Qianmeiyan slate-transformed sandstone schist, etc.", "triple_list": [ [ "Jiayuqiao Rock Group", "Lithology", "Qianmeiyan" ], [ "Jiayuqiao Rock Group", "Lithology", "Slate" ], [ "Jiayuqiao Rock Group", "Lithology", "Sandstone" ], [ "Jiayuqiao Rock Group", "Lithology", "Rock Schist" ] ] }, { "text": "The Jiapila Formation purple-red conglomerate sandstone of the overlying formation, unconsistent angle, Xiaya Village Formation (P3x), thickness 164.71m", "triple_list": [ [ "Jiapila Formation Purple-red Conglomerate Sandstone", "Unconformity contact", "Xiaya Village Group" ], [ "Xiaya Village Group", "thickness", "164.71m" ] ] }, { "text": "Diorite is exposed in the northwest and southeast of Gentu Village, Niangxi Township, Chesuo Township, Jiangda County.", "triple_list": [ [ "Diorite", "Exposed", "Chesuo Township, Jiangda County" ], [ "Diorite", "Exposed", "Gentu Village, Niangxi Township, Northwest and Southeast" ] ] }, { "text": "The Adula Formation (3a) and the Dugala Formation (3d) are constructed for a set of dark grey clastic rocks, clay rocks, seas and lands.", "triple_list": [ [ "Adula Group", "Belongs to", "Dark gray clastic rock and clay rock, sea and land construction" ], [ "Gala group", "Belongs to", "Dark gray clastic rock and clay rock, sea and land construction" ] ] }, { "text": "Gray-brown medium-thick layered gravel-containing unequal grained calcareous rock-cut sandstone, 55.96m", "triple_list": [ [ "Gray-brown medium-thick layered gravel-containing unequal grained calcareous rock fragments sandstone", "thickness", "55.96m" ] ] }, { "text": "The volcanic rocks of the Carboniferous Machala Formation are distributed in the area of Naisegui Jiamailang, Nangqi County, Dachaqu, Qinghai Province.", "triple_list": [ [ "Early Carboniferous Machara Formation Volcanic Rock", "Exposed", "Lewuqi County Dachaqun Naisegui Jiamai Nong, Nangqi County, Qinghai Province" ] ] }, { "text": "Purple-red conglomerate sandstone in the Dongdu Formation of the overlying formation - - - - Parallel and unconformal contact - - - - Wala Monastery Formation (2w), thickness 1282.44m", "triple_list": [ [ "Dongdu Formation purple-red conglomerate sandstone", "Integration of contacts", "Wala Temple Group" ], [ "Wala Temple Group", "thickness", "1282.44m" ] ] }, { "text": "Judging from the majority of the serpentaceae fossils in the Jidonglong Formation, their era was undoubtedly the early Permian.", "triple_list": [ [ "Ji Donglong Group", "Age", "Early Permian" ] ] }, { "text": "The original rock of the Russian group was a set of clastic rocks and clay rocks.", "triple_list": [ [ "Russia team", "Lithology", "Clastite" ], [ "Russia team", "Lithology", "Clay rock" ] ] }, { "text": "Overlapping strata Dongdaqiao Formation (J2d) gray-purple silt sandstone with marlstone ─────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "East Bridge Group", "Lithology", "Gray purple siltstone" ], [ "East Bridge Group", "Lithology", "Marlite" ], [ "East Bridge Group", "Integration of contacts", "Wang Bu Group" ], [ "East Bridge Group", "thickness", "710.88m" ] ] }, { "text": "Adula Group (3a), thickness 1309.9m", "triple_list": [ [ "Adula Group", "thickness", "1309.9m" ] ] }, { "text": "Gray dark gray middle-layer rock fragment coarse silt sandstone containing dolomite silt sandstone gray black rock fragment silt sandstone, 83.64m ────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Gray dark gray medium-layer rock fragment coarse silt sandstone containing dolomite silt sandstone gray black rock fragment silt sandstone", "thickness", "83.64m" ], [ "Gray dark gray medium-layer rock fragment coarse silt sandstone containing dolomite silt sandstone gray black rock fragment silt sandstone", "Integration of contacts", "Sandstone slate of Adula Formation" ] ] }, { "text": "Pyroxene granular rocks are only found in the lower part of the Ningduoyan group and are rarely distributed. The rocks are mainly composed of pyroxene (30), meseafossil (30), quartz (20), mica (15), etc.", "triple_list": [ [ "Pyroxene Granular Rock", "Exposed", "The lower part of the lower section of Ningduoyan Group" ], [ "Pyroxene Granular Rock", "Contained", "Pyrox" ], [ "Pyroxene Granular Rock", "Contained", "Medium-stone" ], [ "Pyroxene Granular Rock", "Contained", "quartz" ], [ "Pyroxene Granular Rock", "Contained", "Black Mouse" ] ] }, { "text": "Gray medium-thick layer of fine-grained feldspar sandstone with a small amount of black serous slate. The bottom of the sandstone is heavy-loaded film, but it has not been seen at the top, 2.78m", "triple_list": [ [ "Gray medium-thick layer of fine-grained feldspar sandstone with a small amount of black sericite slate", "Contained", "Heavy loading membrane" ], [ "Gray medium-thick layer of fine-grained feldspar sandstone with a small amount of black sericite slate", "thickness", "2.78m" ] ] }, { "text": "Gray quartz schist, 887.42m, angle unconsistent, purple-red conglomerate gravel", "triple_list": [ [ "Gray dimos quartz schist", "thickness", "887.42m" ], [ "Gray dimos quartz schist", "Unconformity contact", "The white group of purple-red conglomerate gravel" ] ] }, { "text": "The cave deck (3d) is distributed in the area of Zamacha Congsongla-Lawuga-Subra in Yushu County, Qinghai Province 1:25 million Jiangda County, Tibet Ria County-Moza, Luogen Niuchang-Keduo Niuchang Dongka and other areas, extending to the north by 1:25 million Yushu County and 1:25 million Shiqu County, with an area of about 839m2 in the map.", "triple_list": [ [ "Hole deck", "Exposed", "1:25 million Nangqian County, Zamacha Congsongla-Lawuga-Subura, Yushu County, Qinghai Province" ], [ "Hole deck", "Exposed", "1:25 million Jiangda County, Jiangda County, Tibet - the last smash" ], [ "Hole deck", "Exposed", "Root Cattle Farm—Keto Cattle Farm Hole Card" ], [ "Hole deck", "Exposed", "1:250,000 Yushu County" ], [ "Hole deck", "Exposed", "1:250,000 Shiqu County" ], [ "Hole deck", "area", "839m2" ] ] }, { "text": "The grass quint group is distributed in the grass quint area south of Changqingke Township, Yushu County, this area has an area of about 140m2. It consists of metamorphic gravel-containing green mud schist chlorite quartz schist serous quartz schist, gray-green metamorphic olive basalt metamorphic horns Fluorite metamorphic andandrosite, etc.", "triple_list": [ [ "Caoqu Group", "Exposed", "Caoqu south of Changqingke Township, Yushu County" ], [ "Caoqu Group", "area", "140m2" ], [ "Caoqu Group", "Lithology", "Metamorphic gravel-containing green mud schist" ], [ "Caoqu Group", "Lithology", "Chlorite quartz schist" ], [ "Caoqu Group", "Lithology", "serous quartz schist" ], [ "Caoqu Group", "Lithology", "Gray-green metamorphic olive basalt" ], [ "Caoqu Group", "Lithology", "Metamorphic Shrine" ], [ "Caoqu Group", "Lithology", "Metamorphic Andesite" ] ] }, { "text": "The main rocks of Chamdo-Mangkang metamorphic rocks include metamorphic sandstone slate thousand-corrosive crystal limestone and metamorphic basalt, metamorphic andandyrostone andyrosite and rhyolite, etc.", "triple_list": [ [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Metamorphic Sandstone" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Slate" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Qianmeiyan" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Crystalline limestone" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Metamorphic basalt" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Andyama" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Turning into Ying'an Rock" ], [ "Chamdo-Mangkang Metamorphic Rock", "Lithology", "Rheomorph" ] ] }, { "text": "The Jiapila Formation purple-red conglomerate sandstone of the overlying formation, unconsistent angle, Mangcuo Formation (P2mc), thickness 310.46m", "triple_list": [ [ "Jiapila Formation Purple-red Conglomerate Sandstone", "Unconformity contact", "Rude group" ], [ "Rude group", "thickness", "310.46m" ] ] }, { "text": "The Adula Formation in this section consists of dark gray grey slate sandstone charcoal shale, etc., and produces bivalve brachiopod ammonite sea lily plants, with a total exposed thickness of 778.38m, which is a set of inter-sea and land deposits.", "triple_list": [ [ "Adula Group", "Lithology", "Dark gray slate" ], [ "Adula Group", "Lithology", "sandstone" ], [ "Adula Group", "Lithology", "Carbon shale" ], [ "Adula Group", "Paleontological", "Bivalves" ], [ "Adula Group", "Paleontological", "Brachiopod" ], [ "Adula Group", "Paleontological", "Chrysanthemum" ], [ "Adula Group", "Paleontological", "Sea lily plant" ], [ "Adula Group", "thickness", "778.38m" ], [ "Adula Group", "Belongs to", "Interaction of sea and land" ] ] }, { "text": "Balatonites sp. Japonites magnus Gymnites sp. Hollanmdites sp. Paraceratites sp., and bivalves and plant fragments, 73.00m", "triple_list": [ [ "Slate", "Paleontological", "Ammonites Balatonites sp." ], [ "Slate", "Paleontological", "Japonites magnus Gymnites sp." ], [ "Slate", "Paleontological", "Hollanmdites sp." ], [ "Slate", "Paleontological", "Paraceratites sp." ], [ "Slate", "Paleontological", "Bivalves" ], [ "Slate", "Paleontological", "Plant fragments" ], [ "Slate", "thickness", "73.00m" ] ] }, { "text": "The lithologies of Zengziding Formation (Oz) are sandstone slate and limestone.", "triple_list": [ [ "Zeng Ziding Group", "Lithology", "sandstone" ], [ "Zeng Ziding Group", "Lithology", "Slate" ], [ "Zeng Ziding Group", "Lithology", "Limestone" ] ] }, { "text": "Overlapping silt sandstone of Wangguo Formation ─────────────────────── Dongque Formation (C1d), 750m", "triple_list": [ [ "Wangguo Formation Mud Silty Sandstone", "Integration of contacts", "Dong Que Group" ], [ "Dong Que Group", "thickness", "750m" ] ] }, { "text": "Purple thick layer of coarse sandy gravel dolomite coarse sandstone and dolomite coarse sandy medium-grained quartz sandstone interlayer, 15.55m", "triple_list": [ [ "Purple thick layer of coarse sandy gravel dolomite coarse sandstone and dolomite coarse sandy medium-grained quartz sandstone interlayer", "thickness", "15.55m" ] ] }, { "text": "The Lana Mountain Formation (3l) is distributed in the Dege County, Sichuan Province. On the day, the Maize School in Baiyu County, Dongzha Village, Gongjue County, Tibet - Nazhe Pass of Baiyu County, Baiyu County, Baiyu County, and other areas, extending to the north into 1:25,000 Shiqu County and extending to the east into 1:25,000 Ganzi County, with an area of about 1164m2.", "triple_list": [ [ "Rana Mountain Group", "Exposed", "Sichuan Dege County Geguzhayou wrong trucks and lots of woodland velvet wheat cattle farms that day" ], [ "Rana Mountain Group", "Exposed", "Baiyu County Mai Xue" ], [ "Rana Mountain Group", "Exposed", "Dongzha Village, Gongjue County, Tibet - Nazhe Pass, Baiyu County, Sichuan" ], [ "Rana Mountain Group", "Exposed", "Baiyu County" ], [ "Rana Mountain Group", "Exposed", "1:250,000 Shiqu County" ], [ "Rana Mountain Group", "Exposed", "1:250,000 Ganzi County" ], [ "Rana Mountain Group", "area", "1164m2" ] ] }, { "text": "Dark gray thin middle layer of calcified sandstone and calcified slate interlayers with bioclastic limestone, 105.25m ──────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Dark gray thin middle layer calcareous sandstone mixed sandstone and calcareous slate interlayer interlayers containing biological clastic limestone", "thickness", "105.25m" ], [ "Dark gray thin middle layer calcareous sandstone mixed sandstone and calcareous slate interlayer interlayers containing biological clastic limestone", "Integration of contacts", "Polira group" ] ] }, { "text": "Ying'an crystal-clear tuff is light gray-green, with tuff structure and block-like layer structure.", "triple_list": [ [ "Ying'an crystal chip tuff", "Distribution pattern", "Tuff structure" ], [ "Ying'an crystal chip tuff", "Develop", "Block layer structure" ] ] }, { "text": "Almond-like basalt is green-gray, microcrystalline long structure, and almond structure.", "triple_list": [ [ "Almond-like basalt", "Distribution pattern", "Microcrystalline long-containing structure" ], [ "Almond-like basalt", "Develop", "Almond structure" ] ] }, { "text": "Nujiangyan Formation (Pz2n.), fault contact, Russian rock formation (CPe.), false thickness 1593.66m", "triple_list": [ [ "Nujiangyan Formation in Jiayuqiao Rock Group in Late Paleozoic", "Fault contact", "Russian Rock Formation" ], [ "Russian Rock Formation", "thickness", "1593.66m" ] ] }, { "text": "The Garieiyan Formation (P3j.) is distributed in the Biris-Garei area in the northeast corner of Nangqian County at 1:25 million, and is spread in the Jinsha River junction belt in the northwest-south east direction, with an exposed area of about 128.37m2.", "triple_list": [ [ "Gariei rock formation", "Exposed", "1:25 million Nangqian County area, the northeast corner of the night - Garie" ], [ "Gariei rock formation", "Distribution pattern", "Northwest-South East" ], [ "Gariei rock formation", "Earth tectonic location", "Jinsha River Combination Belt" ], [ "Gariei rock formation", "area", "128.37m2" ] ] }, { "text": "The Wala Temple Group (2w) is distributed in 1:25 million Jiangda County, Jiangda County, Aixudogenxiongdanda Cuba Village, Minda Village, Jiba Village, Jiangda County, Jiangda County, and other areas. It extends to the south by 1:25 million Gongjue County, with an area of about 482m2 in the map.", "triple_list": [ [ "Wala Temple Group", "Exposed", "1:25 million Jiangda County Fenjiangda County Minda Village Sesha Village Aixudogen Xiongdanda Cuba Village" ], [ "Wala Temple Group", "Exposed", "1:250,000 Gongjue County" ], [ "Wala Temple Group", "area", "482m2" ] ] }, { "text": "The fake thickness of the Jiarieyan Formation (P3j.) is 1845.63m", "triple_list": [ [ "Gariei rock formation", "thickness", "1845.63m" ] ] }, { "text": "Gongjue Group (Eg) thickness 4764.45m", "triple_list": [ [ "Gongjue Group", "thickness", "4764.45m" ] ] }, { "text": "The volcanic rocks in the Pushuiqiao area of Jiangda County are 943m thick, and the main lithologies are Anshan tuff green-gray and pyroclastic structures.", "triple_list": [ [ "Pushui Bridge, Jiangda County", "Contained", "Volcanic rocks" ], [ "Volcanic rocks", "thickness", "943m" ], [ "Volcanic rocks", "Lithology", "Andesan tuff" ], [ "Volcanic rocks", "Distribution pattern", "Pyroclastic structure" ] ] }, { "text": "The Jidonglong Formation is rich in fossils, and produces serpentine Rugosofusulina valida, Schwagerina jewetti, Ozawainella sp.; Sphaeroschwagerina subtunda, S. sphaerica, Pseudoschwagerina sp., Zellia colaniae, Rugosofusulina sp. Pseudosulina sp. P. cf. yunnanica., Coral Aagophyllum sp.", "triple_list": [ [ "Ji Donglong Group", "Paleontological", "Rugosofusulina valida" ], [ "Ji Donglong Group", "Paleontological", "Schwagerina jewetti" ], [ "Ji Donglong Group", "Paleontological", "Ozawainella sp." ], [ "Ji Donglong Group", "Paleontological", "Sphaeroschwagerina subrtunda" ], [ "Ji Donglong Group", "Paleontological", "S. sphaerica" ], [ "Ji Donglong Group", "Paleontological", "Pseudoschwagerina sp." ], [ "Ji Donglong Group", "Paleontological", "Zellia colaniaeRugosofusulina sp." ], [ "Ji Donglong Group", "Paleontological", "Pseudofusulina sp." ], [ "Ji Donglong Group", "Paleontological", "P. cf. yunnanica." ], [ "Ji Donglong Group", "Paleontological", "Coral Aagophyllum sp." ] ] }, { "text": "Off-white thick block layer shiny cement containing bioclass sand gravel limestone, producing brachiopod Costiferina cf. indica; Bothrophyllum sp., 53.48m", "triple_list": [ [ "Off-white thick block layer glitter cemented with bio-clad sand gravel gravel limestone", "Paleontological", "Brachiopod Costiferina cf. indica" ], [ "Off-white thick block layer glitter cemented with bio-clad sand gravel gravel limestone", "Paleontological", "Bothrophyllum sp." ], [ "Off-white thick block layer glitter cemented with bio-clad sand gravel gravel limestone", "thickness", "53.48m" ] ] }, { "text": "Carboniferous volcanic rocks are distributed in the Dongque-Jiangguo area of Fanggucai Village, Jiangda County 1:25 million, and are produced in the Dongque Formation of Early Carboniferous (C1d) and the Wangguo Formation of Late Carboniferous (C2w).", "triple_list": [ [ "Carboniferous volcanic rocks", "Exposed", "1:25 million Dongque-Jiangguo Village, Fenggucai Village, Jiangda County" ], [ "Carboniferous volcanic rocks", "Located at", "The Dongque Group of the Early Carboniferous World" ], [ "Carboniferous volcanic rocks", "Located at", "Late Carboniferous World Wangguo Group" ] ] }, { "text": "Light gray medium-layered siltstone with light gray thin layered calcareous siltstone, 125m", "triple_list": [ [ "Light gray medium-layered siltstone with light gray thin layered calcareous siltstone", "thickness", "125m" ] ] }, { "text": "The main accumulations of Quanhua are travertine silicone, sulfur and salt flowers, etc., with a thickness of up to 15m.", "triple_list": [ [ "Quanhua accumulation", "Belongs to", "Travertine Silicon Flower" ], [ "Quanhua accumulation", "Belongs to", "Sulfur Hua Yan Hua" ], [ "Quanhua accumulation", "thickness", "15m" ] ] }, { "text": "Sphae roschwagerina sp. S. cf. subrotunda Pseudoendothyra sp. Rugosofusulina sp. Pseudoschwagerina sp.; Coral Canina sp. Chaetetes zhuogeodonggensis, 356.57m", "triple_list": [ [ "Limestone", "Paleontological", "Sphae roschwagerina sp." ], [ "Limestone", "Paleontological", "S. cf. subrotunda Pseudoendothyra sp." ], [ "Limestone", "Paleontological", "Rugosofusulina sp." ], [ "Limestone", "Paleontological", "Pseudoschwagerina sp." ], [ "Limestone", "Paleontological", "Coral Canina sp." ], [ "Limestone", "Paleontological", "Chaetetes zhuogeodonggensis" ], [ "Limestone", "thickness", "356.57m" ] ] }, { "text": "Only the Carboniferous-Permian strata in this area is the Russian rock formation (CPe.), which is distributed in the Waquzuozhage area of the southwest corner of Bangbeng, Changdu County, spreading in the northwest to southeast. The exposed area in this area is about 58.48m2.", "triple_list": [ [ "Carboniferous-Permian strata", "Outcrop", "Russian Rock Formation" ], [ "Russian Rock Formation", "Exposed", "1:250,000 Changdu County's southwest corner of the tile quad" ], [ "Russian Rock Formation", "Distribution pattern", "Northwest-south eastward expansion" ], [ "Russian Rock Formation", "area", "58.48m2" ] ] }, { "text": "The Dongdaqiao Formation is composed of gray-green purple-red sandstone mudstone shale, gravel-sized limestone, etc., and produces bivalve brachiopod gastropod vertebrate fossils, etc. The total exposed thickness is 2282.82m, which is a river and lake facies-shallow marine facies sedimentation.", "triple_list": [ [ "East Bridge Group", "Lithology", "Gray gray green purple-red sandstone" ], [ "East Bridge Group", "Lithology", "Mudstone" ], [ "East Bridge Group", "Lithology", "shale" ], [ "East Bridge Group", "Lithology", "Polygon" ], [ "East Bridge Group", "Lithology", "Limestone" ], [ "East Bridge Group", "Paleontological", "Bivalves" ], [ "East Bridge Group", "Paleontological", "Brachiopod" ], [ "East Bridge Group", "Paleontological", "Gastropod" ], [ "East Bridge Group", "Paleontological", "Vertebrate fossils" ], [ "East Bridge Group", "thickness", "2282.82m" ], [ "East Bridge Group", "Belongs to", "River and lake phases-shade sedimentation" ] ] }, { "text": "Gray giant layer micro-fine-grained crystalline limestone, 52.40m", "triple_list": [ [ "Gray giant layer micro-fine-grained crystalline limestone", "thickness", "52.40m" ] ] }, { "text": "Therefore, the Karieiyan Formation period was placed in the Permian-late Triassic period.", "triple_list": [ [ "Gariei rock formation", "Age", "Permian-late Triassic" ] ] }, { "text": "The oblique length two cloud schist rock has a granular scale crystal structure and a sheet-like structure.", "triple_list": [ [ "slanted length two cloud schist", "Distribution pattern", "Granular scale crystal structure" ], [ "slanted length two cloud schist", "Develop", "Flake-like structure" ] ] }, { "text": "Light gray purple with gray green medium-thick layered arable quartz silt sandstone, 180.7m", "triple_list": [ [ "Light gray purple with gray green medium-thick layered mud quartz siltstone", "thickness", "180.7m" ] ] }, { "text": "The lithologies of the Youxi Group (Pt3Y) are quartz schist sodium long-dragon schist green mud schist metamorphic conglomerate, etc.", "triple_list": [ [ "Youxi Group", "Lithology", "quartz schist" ], [ "Youxi Group", "Lithology", "Sodium 2-millichrys" ], [ "Youxi Group", "Lithology", "Green mud schist" ], [ "Youxi Group", "Lithology", "Metamorphic gravel" ] ] }, { "text": "To sum up, the Licha Formation in this area consists of gray, dark gray, gray, black limestone, biological clastic limestone, aquatic limestone, dolomite, gravel-like limestone, slate sandstone, siliceous rock, gray-green tuff (local regions), etc., and produces erpentine brachiopods, gastropods, foraminifera bivalves, radioworms, sea lilies, bryoworms, tooth-shaped thorny algae, etc., with a total thickness of 674.61m.", "triple_list": [ [ "Richa Group", "Lithology", "Gray dark gray gray black limestone" ], [ "Richa Group", "Lithology", "Bioclastic limestone" ], [ "Richa Group", "Lithology", "Mixed limestone" ], [ "Richa Group", "Lithology", "Dolomites limestone" ], [ "Richa Group", "Lithology", "Gravel-like limestone" ], [ "Richa Group", "Lithology", "Mudstone" ], [ "Richa Group", "Lithology", "Slate" ], [ "Richa Group", "Lithology", "sandstone" ], [ "Richa Group", "Lithology", "Silicone rock" ], [ "Richa Group", "Lithology", "Gray-green tuff" ], [ "Richa Group", "Paleontological", "Snake" ], [ "Richa Group", "Paleontological", "Brachiopod" ], [ "Richa Group", "Paleontological", "coral" ], [ "Richa Group", "Paleontological", "Gastropod" ], [ "Richa Group", "Paleontological", "Chrysanthemum" ], [ "Richa Group", "Paleontological", "Foraminifera" ], [ "Richa Group", "Paleontological", "Bivalves" ], [ "Richa Group", "Paleontological", "Aphrodisiac" ], [ "Richa Group", "Paleontological", "Radioworms" ], [ "Richa Group", "Paleontological", "sea lily" ], [ "Richa Group", "Paleontological", "Bruceworm" ], [ "Richa Group", "Paleontological", "Teeth thorn" ], [ "Richa Group", "Paleontological", "Algae" ], [ "Richa Group", "thickness", "674.61m" ] ] }, { "text": "Olive basalt, gray-green, with spotty structure, rough basalt structure, and block-like structure.", "triple_list": [ [ "Olive basalt", "Distribution pattern", "Spotted structure" ], [ "Olive basalt", "Distribution pattern", "Coarse black treasure structure" ], [ "Olive basalt", "Develop", "Blocky structure" ] ] }, { "text": "The types of metamorphic rocks of Zhuka Group include metamorphic Ying'anite crystalline tuff metamorphic Ying'anite crystalline tuff metamorphic Ying'anite crystalline tuff metamorphic Ying'anite volcanic tuff metamorphic Buckler metamorphic rhizome glassycladic crystalline tuff metamorphic Andestone slate metamorphic sandstone, etc.", "triple_list": [ [ "Bamboo card group metamorphic rock", "Lithology", "Metamorphic Ying'an crystal chip tuff" ], [ "Bamboo card group metamorphic rock", "Lithology", "Metamorphic Ying'an crystal crystal rock" ], [ "Bamboo card group metamorphic rock", "Lithology", "Clast volcanic breccia" ], [ "Bamboo card group metamorphic rock", "Lithology", "Metamorphic Yinganite volcanic tuff breccia" ], [ "Bamboo card group metamorphic rock", "Lithology", "Metamorphic fluidic glass-clad crystal tuff" ], [ "Bamboo card group metamorphic rock", "Lithology", "Metamorphic Andesite" ], [ "Bamboo card group metamorphic rock", "Lithology", "Slate" ], [ "Bamboo card group metamorphic rock", "Lithology", "Sandstone" ] ] }, { "text": "Silty marlstone with calcified quartz fine sandstone, produces plants Annularia huntonensis, 40.17m", "triple_list": [ [ "Silty marl stone with calcified quartz fine sandstone", "Paleontological", "Plant Annularia huntonensis" ], [ "Silty marl stone with calcified quartz fine sandstone", "thickness", "40.17m" ] ] }, { "text": "Triassic granite is widely exposed, mainly distributed in the Chamdo-Mangkang invasion rock belt, Jiangda-Deqin invasion rock belt, Jinsha River invasion rock belt, Quershan-Yidun invasion rock belt, and secondly, there are a small number of them in the Lancang River invasion rock belt and the Yurang-Zhuka invasion rock belt.", "triple_list": [ [ "Triassic granite", "Earth tectonic location", "Lewuqi-Dongdashan invasion rock belt" ], [ "Triassic granite", "Earth tectonic location", "Chamdo-Mangkang invades the rock belt" ], [ "Triassic granite", "Earth tectonic location", "Jiangda-Deqin invades the rock belt" ], [ "Triassic granite", "Earth tectonic location", "Jinsha River invades the rock belt" ], [ "Triassic granite", "Earth tectonic location", "Queer Mountain-Yidun invades the rock belt" ], [ "Triassic granite", "Earth tectonic location", "Lancang River invades rock belt" ], [ "Triassic granite", "Earth tectonic location", "Russia-Bamboo card invades the rock belt" ] ] }, { "text": "Overhead formation Polila Formation limestone────────────────────────────────────────────────────────────────────────────────�", "triple_list": [ [ "Polila Formation Limestone", "Integration of contacts", "Kapila Group" ], [ "Kapila Group", "thickness", "92.90m" ] ] }, { "text": "Blue-gray variegated giant thick layered conglomerate, 261.40m", "triple_list": [ [ "Blue-gray variegated huge thick layered gravel rock", "thickness", "261.40m" ] ] }, { "text": "The Devonian Dojiban Formation (D1dj), Senza Formation (D2s) Dongla Formation (D3d); the Carboniferous Dongque Formation (C1d) Wangguo Formation (C2w); and the Permian Jidonglong Formation (P1j) Shamu Formation (P3s).", "triple_list": [ [ "Late Paleozoic continental marginal sedimentation", "Contained", "Devonian Doji Edition Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Senza Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Donla Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Carboniferous Dongque Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Wang Guo Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Permian Jidonglong Group" ], [ "Late Paleozoic continental marginal sedimentation", "Contained", "Shamu Group" ] ] }, { "text": "Fossils such as Claraia, the early Triassic bivalve, were harvested in multiple marathon areas, so their era was placed in the early-Mid-Triassic period.", "triple_list": [ [ "Marathon multiple sets", "Paleontological", "Early Triassic Bivalve Claraia" ], [ "Marathon multiple sets", "Age", "Early-Middle Triassic" ] ] }, { "text": "Gray medium-thick layer of bioclass limestone marlstone, producing bivalve ancredia triangularis Nanogyra sp. and gastropod Amplovata aff. jiangguensis, 85.55m", "triple_list": [ [ "Gray medium-thick layer of bioclass limestone", "Paleontological", "bivalve ancredia triangularis Nanogyra sp." ], [ "Gray medium-thick layer of bioclass limestone", "Paleontological", "Gastropods Amplovata aff. jiangguensis" ], [ "Gray medium-thick layer of bioclass limestone", "thickness", "85.55m" ] ] }, { "text": "Gray-white, light gray-green striped medium acidic crystal chip glass tuff, 39.88m", "triple_list": [ [ "Gray white light gray-green stripe medium acidic crystal chip glass chip tuff", "thickness", "39.88m" ] ] }, { "text": "Overhead slate clay rock siltstone of Adula Formation ───────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────────", "triple_list": [ [ "Slate clay rock siltstone in Adula Formation", "Integration of contacts", "Polira group" ], [ "Polira group", "thickness", "228.2m" ] ] }, { "text": "Dark gray medium-thick layered feldspar sandstone, 150m", "triple_list": [ [ "Dark gray medium-thick layered feldspar sandstone", "thickness", "150m" ] ] }, { "text": "1:200,000 Uzira, many of the Gaugulan Erchang granite units were exposed in the area east of Gouguda, Gelong Township, Changdu County. They invaded the gneiss in Ningduoyan group and were unconformally covered by the Jiapila Formation of the Upper Triassic.", "triple_list": [ [ "1:200,000 Uzirado's picture said that Goukuannong Erchang Granite", "Exposed", "Gouqianda, Gelong Township, Changdu County" ], [ "1:200,000 Uzirado's picture said that Goukuannong Erchang Granite", "Distribution pattern", "Long-shaped rock plant" ], [ "1:200,000 Uzirado's picture said that Goukuannong Erchang Granite", "Invade", "Ningduoyan group gneis" ], [ "1:200,000 Uzirado's picture said that Goukuannong Erchang Granite", "Unconformity contact", "The upper triassic regime Apira group" ] ] }, { "text": "Gray gravel (pimple) limestone, 4.7m", "triple_list": [ [ "Gray gravel (pimples) limestone", "thickness", "4.7m" ] ] }, { "text": "Jiaoga Group (P2j) thickness 418.63m", "triple_list": [ [ "Jiaoga Group", "thickness", "418.63m" ] ] }, { "text": "Andesite is green, gray-green, with interlaced structures and blocky structures.", "triple_list": [ [ "Andanyan", "Distribution pattern", "Spotted structure" ], [ "Andanyan", "Distribution pattern", "Interwoven structure" ], [ "Andanyan", "Develop", "Blocky structure" ] ] }, { "text": "Off-white medium-thick layer of crystalline limestone fragmented and glittery cemented sand-clad limestone, produced by Martinia semiglo-bosa Echinocochus sp. Reticularia cf. linenta Martininopsis sp. Mesolobus sp. Squamularia sp. Brachythyrina sp. Erebratulidea sp.; Misellina sphaerica Schwagerinida Schwagerina aff. grperaensis sp. et al., 54.59m", "triple_list": [ [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Brachiopod Martinia semiglo-bosa Echinocochus sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Reticularia cf. linenta Martininopsis sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Mesolobus sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Squamularia sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Brachythyrina sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "erebratulidea sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "Paleontological", "Misellina sphaerica Schwagerinidae Schwagerina aff. grperaensis sp." ], [ "Off-white medium-thick layer of crystalline limestone fragmented glitter cemented sand chip limestone", "thickness", "54.59m" ] ] }, { "text": "Black carbon shale black brown calcareous sandstone sandy shale carbon argill sandstone interlayer, containing brachiopod Orthotetina sp. Orthoticia sp., 51.7m", "triple_list": [ [ "Black carbon shale black brown calcareous sandstone sandy shale carbon amid sandstone interlayer", "Paleontological", "Brachiopod Orthotetina sp." ], [ "Black carbon shale black brown calcareous sandstone sandy shale carbon amid sandstone interlayer", "Paleontological", "Orthoticia sp." ], [ "Black carbon shale black brown calcareous sandstone sandy shale carbon amid sandstone interlayer", "thickness", "51.7m" ] ] }, { "text": "There are only many groups of volcanic rocks in the Chamdo-Mangkang volcanic rocks in the early-Mid-Triassic marathon, distributed in 1:25,000 Jiangda County, Xiare Nongmang Marathon, and other places. It extends to 1:25,000 Gongjue County in the southeast, with an exposed area of about 67m2 in this area.", "triple_list": [ [ "Chamdo-Mangkang Volcanic Rock Belt", "Contained", "Triassic volcanic rocks" ], [ "Triassic volcanic rocks", "Lithology", "Early-Middle Triassic Marathon Multiple Groups of Volcanic Rocks" ], [ "Triassic volcanic rocks", "Exposed", "1:25 million Jiangda County Shrimp Hot Ring Mang Marathon" ], [ "Triassic volcanic rocks", "Exposed", "1:250,000 Gongjue County" ], [ "Triassic volcanic rocks", "area", "67m2" ] ] }, { "text": "Dolomelized serpentinite is grayish-white, with an interpretive structure or a scale structure, and a block-like structure.", "triple_list": [ [ "Dolomite serpentine", "Distribution pattern", "Explain the structure" ], [ "Dolomite serpentine", "Distribution pattern", "Scallop structure" ], [ "Dolomite serpentine", "Develop", "Blocky structure" ] ] }, { "text": "The main rocks of the grass quint group are metamorphic conglomerates, gravel-containing thousand rocks metamorphic feldspar quartz sandstones, thunderstones, chlorite quartz schist sericin quartz schist sericin quartz schist sericin quartz schist sericin quartz schist sericin quartz schist quartz quartz schist, etc., and two layers of metamorphic olive basalt are interspersed in the middle.", "triple_list": [ [ "Caoqu Group", "Lithology", "Metamorphic gravel" ], [ "Caoqu Group", "Lithology", "Thousands of gravels" ], [ "Caoqu Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "Caoqu Group", "Lithology", "Qianmeiyan" ], [ "Caoqu Group", "Lithology", "Serous green mud schist" ], [ "Caoqu Group", "Lithology", "Chlorite quartz schist" ], [ "Caoqu Group", "Lithology", "serous quartz schist" ], [ "Caoqu Group", "Lithology", "Quartzite" ], [ "Caoqu Group", "Lithology", "Metamorphic olive basalt" ] ] }, { "text": "The era of the Degaila group belongs to the middle and late triassic period.", "triple_list": [ [ "Gala group", "Age", "Late Triassic" ] ] }, { "text": "The Wangguo Formation has abundant biological fossils, which can be divided into the Profusulinella-Pseudostaffella belt and the Fusulina-Fusulinella belt.", "triple_list": [ [ "Wang Guo Group", "Contained", "Profusulinella—Pseudostaffella belt" ], [ "Wang Guo Group", "Contained", "Fusulina—Fusulinella belt" ] ] }, { "text": "Gray thick layer of calcareous rock-cut feldspar sandstone sandstone with dark gray silty slate and gray sand-cut limestone, producing serpentine Sphaeroschwagerina sp., 227.72m", "triple_list": [ [ "Gray thick layer of calcareous rock fragment feldspar sandstone sandstone with dark gray silty slate and gray sand fragment limestone", "Paleontological", "Sphaeroschwagerina sp." ], [ "Gray thick layer of calcareous rock fragment feldspar sandstone sandstone with dark gray silty slate and gray sand fragment limestone", "thickness", "227.72m" ] ] }, { "text": "To sum up the above, the Dongque Formation should be deposited in the Datang period of the Early Carboniferous Period.", "triple_list": [ [ "Dong Que Group", "Belongs to", "Sedimentation in Datang Period of Early Carboniferous" ] ] }, { "text": "Gray thin layer of limestone and metamorphic feldspar quartz sandstone carbonaceous amidite are interlayered, producing tooth-shaped thorns Ozarodina sp. Enatiognathus sp. Prioniodella sp. Neogonolella sp.; Sea lily stem Isocrinus sp. Enorinus sp. et al.", "triple_list": [ [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Ozarodina sp." ], [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Enatiognathus sp." ], [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Prioniodella sp." ], [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Neogonolella sp." ], [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Sea lily stem Isocrinus sp." ], [ "Interlayer of gray thin layer limestone and metamorphic feldspar quartz sandstone carbonaceous amid rock", "Paleontological", "Enorinus sp." ] ] }, { "text": "Sandstone lenses are seen in siltstone, with symmetrical wavy marks on the level, producing bivalve Cardium (ulongocardium) cf. martini; plant Glossophyllum sp. Neocalamites sp. Marattiopsis sp. Sphenobaiera sp. Equisetites sp., 277.14m", "triple_list": [ [ "Siltstone", "Contained", "Sandstone lens" ], [ "Siltstone", "Develop", "Symmetrical wave marks" ], [ "Siltstone", "Paleontological", "bivalve Cardium(ulongocardium) cf. martini" ], [ "Siltstone", "Paleontological", "Plant Glossophyllum sp." ], [ "Siltstone", "Paleontological", "Neocalamites sp." ], [ "Siltstone", "Paleontological", "Marattiopsis sp." ], [ "Siltstone", "Paleontological", "Sphenobaira sp." ], [ "Siltstone", "Paleontological", "Equisetites sp." ], [ "Siltstone", "thickness", "277.14m" ] ] }, { "text": "Gray-gray medium-thick layer of crystalline limestone glitter cemented gravel limestone, producing Schwagerinidae Verbeeina sp.; Brachiopod yloplecta sp. and coral sea lily fragments, 77.84m", "triple_list": [ [ "Gray-gray medium-thick layer of crystalline limestone glitter cemented gravel limestone", "Paleontological", "Schwagerinidae Verbeeina sp." ], [ "Gray-gray medium-thick layer of crystalline limestone glitter cemented gravel limestone", "Paleontological", "Brachiopod yloplecta sp." ], [ "Gray-gray medium-thick layer of crystalline limestone glitter cemented gravel limestone", "Paleontological", "Coral Sea Lily Fragments" ], [ "Gray-gray medium-thick layer of crystalline limestone glitter cemented gravel limestone", "thickness", "77.84m" ] ] }, { "text": "Hole deck (3d), thickness >1919.16m", "triple_list": [ [ "Hole deck", "thickness", "1919.16m" ] ] }, { "text": "Gray thin-thick layered crystalline gray matter dolomite, 221.14m", "triple_list": [ [ "Thin gray-thick layered crystalline gray matter dolomite", "thickness", "221.14m" ] ] }, { "text": "Gray gray matter dolomite, 21.14m", "triple_list": [ [ "Gray gray matter dolomite", "thickness", "21.14m" ] ] }, { "text": "1:50,000 Guiyi area, the actual exposure of Longjiaotang-energy plate is complete and representative. The stratigraphic sequence is the Luodong Formation, the black cloud and red columns are oblique stone rocks. ——————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Luodong Group", "Lithology", "Black clouds, red columns, oblique curtains, stone horns" ], [ "Luodong Group", "Integration of contacts", "Luo Hong Group" ], [ "Luo Hong Group", "thickness", "2518m" ] ] }, { "text": "The ancient tomb group in the survey area should Belongs to to the early Shiliushi.", "triple_list": [ [ "Ancient Tomb Group", "Age", "Early Shili" ] ] }, { "text": "The limestone lens body or calcified siltstone layer at the bottom of the Bali Formation and the top of the Daganshan Formation, and the upper part are in integrated contact with the Laohutang Formation, with a thickness of 1400~1600m.", "triple_list": [ [ "Bali Group", "Integration of contacts", "Dakanshan Group" ], [ "Bali Group", "Integration of contacts", "Tiger Pond Group" ], [ "Bali Group", "thickness", "1400~1600m" ], [ "Dakanshan Group", "Lithology", "Limestone lens body" ], [ "Dakanshan Group", "Lithology", "Calcium silt sandstone layer" ] ] }, { "text": "Overlapping Chunwan Formation, off-white quartz sandstone ————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Chunwan Group", "Lithology", "Off-white quartz sandstone" ], [ "Chunwan Group", "Integration of contacts", "Guitou Group" ], [ "Guitou Group", "thickness", "922.1m" ] ] }, { "text": "Dark - black shale, with stone on top Orthographus sp. Pristiographus aff hisingeri Streptographus nodife; Monographus aff aff. Priodon, 6.0m", "triple_list": [ [ "Dark-black shale", "Paleontological", "Bistone Orthographus sp." ], [ "Dark-black shale", "Paleontological", "Pristiographus aff hisingeri Streptographus nodife" ], [ "Dark-black shale", "Paleontological", "Monographus aff. Priodon" ], [ "Dark-black shale", "thickness", "6.0m" ] ] }, { "text": "Light gray blue-gray medium-thin layered mudstone, 13m", "triple_list": [ [ "Light gray blue-gray medium-thin layered mudstone", "thickness", "13m" ] ] }, { "text": "Floating soil, 42m", "triple_list": [ [ "surface dust", "thickness", "42m" ] ] }, { "text": "The lithology of the Laohutang Formation is metamorphic (feldspar) quartz sandstone quartzite quartzite with carbonaceous serous rock and sandy silty slate, etc., with a thickness of 950m.", "triple_list": [ [ "Tiger Pond Group", "Lithology", "Metamorphic (feldspar) quartz sandstone" ], [ "Tiger Pond Group", "Lithology", "Quartzite" ], [ "Tiger Pond Group", "Lithology", "Carbon-containing sericinous rock" ], [ "Tiger Pond Group", "Lithology", "Sandy silty slab" ], [ "Tiger Pond Group", "thickness", "950m" ] ] }, { "text": "The Lanweng Formation consists of a stratigraphic sequence mainly composed of fine-grained sandstone and Qianmei rocks. It has a large thickness and develops horizontal stratigraphic and strip-like structures, showing the characteristics of the Bauma sequence. There are more conglomerate interlayers in locally, indicating the Develop of the waterway phase.", "triple_list": [ [ "Orchid group", "Lithology", "Fine-grained sandstone" ], [ "Orchid group", "Lithology", "Qianmeiyan" ], [ "Orchid group", "Develop", "Horizontal stratification" ], [ "Orchid group", "Develop", "Strip structure" ], [ "Orchid group", "Develop", "Bauma Sequence" ], [ "Orchid group", "Develop", "Sandstone" ], [ "Orchid group", "Belongs to", "Waterway phase" ] ] }, { "text": "Gray-green thick layered mica quartzite with thin layered quartz mica microschist, 39.3m", "triple_list": [ [ "Gray-green thick layered mica quartzite", "thickness", ".3m" ] ] }, { "text": "The interfacial deformation and metamorphism of various rocks in the Precambrian basal base, especially the research on the multi-layered basal structure characteristics of the Yunkai area, its interface properties, the geographic tectonic properties and paleogeographic location changes.", "triple_list": [ [ "Yunkai area", "Lithology", "Multi-layered base structure" ] ] }, { "text": "The Tianziling Formation of the Shangfu Formation, gray-black limestone ———————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Tianziling Group", "Lithology", "Gray-black limestone" ], [ "Tianziling Group", "Integration of contacts", "Chunwan Group" ], [ "Chunwan Group", "thickness", "510.8m" ] ] }, { "text": "Under the Bali Formation, the limestone lens body or calcified silt sandstone layer at the top of the Daganshan Formation was in integrated contact with the Laohutang Formation, with a thickness of 14001600m.", "triple_list": [ [ "Bali Group", "Integration of contacts", "Dakanshan Group" ], [ "Bali Group", "thickness", "14001600m" ], [ "Dakanshan Group", "Lithology", "Limestone lens body" ], [ "Dakanshan Group", "Lithology", "Calcium silt sandstone layer" ], [ "Dakanshan Group", "Lithology", "Tiger Pond Group" ] ] }, { "text": "The first group of Yunkai Group (QnY1) refers to a group at the lower part of Yunkai Group, which is widely distributed in the Luoding-Xinyi-Yangchun area, with a large exposed area of about 924.27m2, accounting for 5.46% of the total area of the survey area.", "triple_list": [ [ "The first group of Yunkai Group", "Exposed", "Luo Ding-Xinyi-Yangchun" ], [ "The first group of Yunkai Group", "area", "924.27m2" ] ] }, { "text": "The lithology of the Chunwan Formation is composed of gray-dark gray thin-layered argillary belt limestone mud crystal limestone powder limestone dolomite limestone, etc., and is partially pseudooxic limestone bioclass limestone granular clastic limestone amidst sericite shale calcified mudstone siltstone.", "triple_list": [ [ "Chunwan Group", "Lithology", "Gray-dark gray thin-layered mud strip limestone" ], [ "Chunwan Group", "Lithology", "Mud crystal limestone" ], [ "Chunwan Group", "Lithology", "Pink limestone" ], [ "Chunwan Group", "Lithology", "Dolomites limestone" ], [ "Chunwan Group", "Lithology", "Pseudoolithic limestone" ], [ "Chunwan Group", "Lithology", "Bioclastic limestone" ], [ "Chunwan Group", "Lithology", "Crystal-grained limestone" ], [ "Chunwan Group", "Lithology", "mud sericite shale" ], [ "Chunwan Group", "Lithology", "Calcium mudstone" ], [ "Chunwan Group", "Lithology", "Siltstone" ] ] }, { "text": "Gray-black, gray-white striped marble and magnesium calcite quartz mica microschist 2.7m", "triple_list": [ [ "Gray-black, gray-white striped magnesium marble", "thickness", "2.7m" ], [ "magnesium calcite quartz mica microschist", "thickness", "2.7m" ] ] }, { "text": "The Daganshan Formation in the survey area is distributed in Luodingweidi-Yun'an County Zhen'an-Yunfuyaoguyangchun-Helang and other places, with wide exposure, about 772.46m2, accounting for 4.57% of the total area of the survey area.", "triple_list": [ [ "Dakanshan Group", "area", "About 772.46m2" ], [ "Dakanshan Group", "Exposed", "Luodingweidi-Yunan County Zhen'an-Yunfuyao Guyangchun-Helang and other places" ] ] }, { "text": "The lithology of the Dagangding Formation is mainly composed of silty-silty strip mudstone mixed with silty mudstone fine sandstone mixed with mudstone, which is thicker and thinner from bottom to top. Petalolihus hispanicus, Spiroptus sp., S. minor, Streptograptus sp.", "triple_list": [ [ "Dagang Ding Group", "Lithology", "Silty sandy strip mudstone" ], [ "Dagang Ding Group", "Lithology", "Silty mudstone" ], [ "Dagang Ding Group", "Lithology", "Fine sandstone" ], [ "Dagang Ding Group", "Lithology", "Mudstone" ], [ "Dagang Ding Group", "Paleontological", "Petalolihus hispanicus" ], [ "Dagang Ding Group", "Paleontological", "spirographus sp." ], [ "Dagang Ding Group", "Paleontological", "Streptographus sp." ] ] }, { "text": "Gray-green gray-red slate and gray-red silt sandstone and sandstone interlayer, 683.27m", "triple_list": [ [ "Gray-green gray-red slate and gray-red silt sandstone and sandstone interlayer", "thickness", "683.27m" ] ] }, { "text": "The Ordovician strata in the southeastern Guizhou and Yunkai strata are from bottom to top of the Luohong Formation, Luodong Formation, Dongchong Formation, and Lanwen Formation.", "triple_list": [ [ "Ordovician strata", "Stratigraphical zoning", "South East Gui" ], [ "Ordovician strata", "Stratigraphical zoning", "Cloud open" ], [ "Ordovician strata", "Outcrop", "Luo Hong Group" ], [ "Ordovician strata", "Outcrop", "Luodong Group" ], [ "Ordovician strata", "Outcrop", "Dongchong Group" ], [ "Ordovician strata", "Outcrop", "Orchid group" ] ] }, { "text": "The second group of Yunkai Group, not seen the peak, the total thickness is >2703.3m", "triple_list": [ [ "The second group of Yunkai Group", "thickness", "Total thickness >2703.3m" ] ] }, { "text": "The Guitou group in the survey area is mainly composed of red mixed conglomerate quartz conglomerate sandstone sandstone silt sandstone silt sandstone silt sandstone volcanic conglomerate, and is partially intertwined with gravel-containing sandstone volcanic conglomerate.", "triple_list": [ [ "Guitou Group", "Lithology", "Red gravel" ], [ "Guitou Group", "Lithology", "Quartz gravel" ], [ "Guitou Group", "Lithology", "sandstone" ], [ "Guitou Group", "Lithology", "Siltstone" ], [ "Guitou Group", "Lithology", "Silty mudstone" ], [ "Guitou Group", "Lithology", "Gravel-containing sandstone" ], [ "Guitou Group", "Lithology", "Volcanic gravel" ] ] }, { "text": "Overlapping strata Hazifeng Formation Muddy Silty Sandstone ————————————————————————————————————————— Tianziling Formation, total thickness 787.6m", "triple_list": [ [ "Hat Peak Group", "Lithology", "Mud siltstone" ], [ "Hat Peak Group", "Integration of contacts", "Tianziling Group" ], [ "Tianziling Group", "thickness", "787.6m" ] ] }, { "text": "The Guitou group in the survey area is distributed in Taishan, Nafuen Pinghongjiaoliang Xiniujiang Shahu, Yangchun Weiguo Heshui Xinxingjinzhuhetou Yunfudashi and other places, with an exposed area of about 459.44m2, accounting for 2.72% of the total area.", "triple_list": [ [ "Guitou Group", "Exposed", "Taishan Nafuen Pinghong Jiaoliang Xiniujiang Shahu Yangchun Weiguo Heshui Xinxing Jinzhuhetou Yunfudashi" ], [ "Guitou Group", "area", "459.44m2" ] ] }, { "text": "Gray white dark gray metamorphic feldspar quartz sandstone, thick layered, horizontally layered, 152.7m", "triple_list": [ [ "Gray white dark gray metamorphic feldspar quartz sandstone", "Develop", "Horizontal stratification" ], [ "Gray white dark gray metamorphic feldspar quartz sandstone", "thickness", "152.7m" ] ] }, { "text": "The Fangcheng group in the survey area produced brachiopods Mollngia sp., M.cf. Uniqlicata (Grabuw), Orthis sp., Retzia sp., Camarotoechia sp., Eosprifer sp., Zygospira sp., and the maria lily algae mesophobia.", "triple_list": [ [ "Fangcheng Group", "Paleontological", "Brachiopod Mollngia sp." ], [ "Fangcheng Group", "Paleontological", "M.cf.Uniqlicata(Grabuw)" ], [ "Fangcheng Group", "Paleontological", "Orthis sp." ], [ "Fangcheng Group", "Paleontological", "Retzia sp." ], [ "Fangcheng Group", "Paleontological", "Camarotoechia sp." ], [ "Fangcheng Group", "Paleontological", "Eosprifer sp." ], [ "Fangcheng Group", "Paleontological", "Zygospira sp." ], [ "Fangcheng Group", "Paleontological", "sea lily" ], [ "Fangcheng Group", "Paleontological", "Algae" ], [ "Fangcheng Group", "Paleontological", "Aphrodisiac" ] ] }, { "text": "Ash-dark gray silty slate and purple-purple silty slate with a small amount of metamorphic sandstone, 20.59m", "triple_list": [ [ "Gray-dark gray silty slate and purple-purple silty slate with a small amount of metamorphic sandstone", "thickness", "20.59m" ] ] }, { "text": "The Cambrian strata are called Gaotan Formation and Shuishi Formation.", "triple_list": [ [ "Gaotan Group", "Belongs to", "Cambrian strata" ], [ "Water stone group", "Belongs to", "Cambrian strata" ] ] }, { "text": "Light yellow gray-white medium-thick layered fine-grained quartz sandstone with muddy silt sandstone, 14m", "triple_list": [ [ "Light yellow, gray-white medium-thick layered fine-grained quartz sandstone with muddy silt sandstone", "thickness", "14m" ] ] }, { "text": "Tawny quartz mica schist, 87.2m", "triple_list": [ [ "Tawny quartz mica schist", "thickness", "87.2m" ] ] }, { "text": "The second group of the submerged strata is formed by the second group of the clouds, and the cross-stone garnet quartz dimica schist, garnet mica granules and mica granules and mica granules are interlayered. This group is clastic rock at the bottom of the survey area.", "triple_list": [ [ "The second group of clouds in the underlying strata", "Lithology", "Cross stone garnet quartz dimica schist" ], [ "The second group of clouds in the underlying strata", "Lithology", "Garnet mica granular rock" ], [ "The second group of clouds in the underlying strata", "Lithology", "Clastite" ] ] }, { "text": "The lithologies in the survey area are yellow, green, purple and red shale, which are mainly sandstones, and are in integrated contact with the Hushan Formation of the Underwater Water Stone Formation, with a thickness of >133m.", "triple_list": [ [ "Investigation Area", "Lithology", "Variety shale such as yellow, green, purple and red" ], [ "Investigation Area", "Lithology", "sandstone" ], [ "Investigation Area", "Integration of contacts", "Water stone group" ], [ "Investigation Area", "Integration of contacts", "Hushan Group" ], [ "Investigation Area", "thickness", "133m" ] ] }, { "text": "Gray-green thin-medium-thick layered sheets of physical and chemical mica quartzite with yellow-brown purple-red micro-thin layered quartz schist, >266.1m, no bottom is seen", "triple_list": [ [ "Gray-green thin-medium-thick layered sheets of physicochemical mica quartzite with yellow-brown purple-red micro-thin layered quartz schist", "thickness", "266.1m" ] ] }, { "text": "The Tiger Pond Group (Z2lh), created in the Tiger Pond in Shangxiang, Xiajiang County, Jiangxi Province, refers to a set of rematerials. The survey area is only found in the east of Yangchun City, with an exposed area of about 39.14m2, accounting for 0.23% of the total area of the survey area.", "triple_list": [ [ "Tiger Pond Group", "Exposed", "Tiger pond, Shangxiang, Xiajiang County, Jiangxi Province" ], [ "Tiger Pond Group", "Belongs to", "Rematerial construction" ], [ "Tiger Pond Group", "Exposed", "East of Yangchun City" ], [ "Tiger Pond Group", "area", "39.14m2" ] ] }, { "text": "The first group of clouds in the underlying strata, gray-green quartz mica slices.", "triple_list": [ [ "The first group of clouds in the underlying formation", "Lithology", "Gray-green quartz mica tablets" ] ] }, { "text": "Light yellow gray blue-gray medium-thin layered silty serous slate, horizontally layered, 5m", "triple_list": [ [ "Light yellow gray blue gray medium-thin layered silty serous slab", "Develop", "Horizontal stratification" ], [ "Light yellow gray blue gray medium-thin layered silty serous slab", "thickness", "5m" ] ] }, { "text": "Liantan Formation (S1l) originally refers to a strata containing black, gray, black, yellow and green striped shale with thin sandstone near Wentou Mountain in Liantan, Yunan, Guangdong.", "triple_list": [ [ "Liantan Group", "Exposed", "Near Wentou Mountain, Liantan, Yunan, Guangdong" ], [ "Liantan Group", "Lithology", "Black gray, black yellow green striped shale" ], [ "Liantan Group", "Lithology", "Thin layer of sandstone" ] ] }, { "text": "The upper part of the Daganshan Formation is mainly gray, gray-white medium-thick layered mica quartzite and quartzite, and there are many blue-gray thin-medium-thick layered sericite thousand rocks and quartz mica schist.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Ash, off-white medium-thick layered mica quartzite" ], [ "Dakanshan Group", "Lithology", "Quartzite" ], [ "Dakanshan Group", "Contained", "Blue-gray thin-medium-thick layered sericite thousand rock" ], [ "Dakanshan Group", "Contained", "Quartz mica schist" ] ] }, { "text": "Developmental asymmetric wavy stratigraphy in sandstone", "triple_list": [ [ "sandstone", "Develop", "Asymmetric wavy stratigraphy" ] ] }, { "text": "Light gray dark gray thick layered metamorphic feldspar quartz sandstone with black mica schist, 37.9m", "triple_list": [ [ "Light gray dark gray thick layered metamorphic feldspar quartz sandstone", "Contained", "Mica schist" ], [ "Light gray dark gray thick layered metamorphic feldspar quartz sandstone", "thickness", "37.9m" ] ] }, { "text": "Overlying formation Liujiang Formation, thin-layer siliceous mudstone containing siliceous mudstone siliceous Qianmei Rock, etc. ————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Liujiang Group", "Lithology", "Thin layered siliceous mudstone containing siliceous mudstone siliceous thousand rocks" ], [ "Liujiang Group", "Integration of contacts", "Donggangling Group" ], [ "Donggangling Group", "thickness", "118m" ] ] }, { "text": "The lithology of Liantan Formation is strip-shaped shale sandstone and sandstone, which is in integrated contact with the underlying ancient tomb formation and has a thickness greater than 224m.", "triple_list": [ [ "Liantan Group", "Lithology", "Striped shale" ], [ "Liantan Group", "Lithology", "Siltstone" ], [ "Liantan Group", "Lithology", "sandstone" ], [ "Liantan Group", "Integration of contacts", "Ancient Tomb Group" ], [ "Liantan Group", "thickness", "224m" ] ] }, { "text": "Gray medium-thick layered fine-grained sheets of physical and chemical quartz sandstone with ash-grey black thin layered Qianmei rock, 120.46m", "triple_list": [ [ "Gray medium-thick layered fine-grained sheets of physical and chemical quartz sandstone with ash-grey black thin layered thousand rocks", "thickness", "120.46m" ] ] }, { "text": "Dongchong Formation (O2d) refers to a set of fine clastic formation sequences of yellow, white, gray, yellow, light purple, gray, calcium-containing fine-grained quartz sandstone and sandstone with quartz sericca microschist.", "triple_list": [ [ "Dongchong Group", "Lithology", "Yellow, white, gray, yellow, light purple, gray calcium-containing fine-grained quartz sandstone" ], [ "Dongchong Group", "Lithology", "sandstone" ], [ "Dongchong Group", "Lithology", "Quartz sericaceous microschist" ], [ "Dongchong Group", "Lithology", "Fine clastic rock" ] ] }, { "text": "Fourth-System Alluvial Alluvial, 24.28m", "triple_list": [ [ "The fourth system of flood alluvial", "thickness", "24.28m" ] ] }, { "text": "The Luodong Group in the survey area was only found in the north of Jinzhu Town, Guangxi. The exposed area was very small, only 2.90m2, accounting for 0.02% of the total area of the survey area, and was distributed in a linear manner in the northeast direction.", "triple_list": [ [ "Luodong Group", "Exposed", "Guangxi Fengzhu Town North" ], [ "Luodong Group", "area", "2.90m2" ], [ "Luodong Group", "Distribution pattern", "Northeastward linear distribution" ] ] }, { "text": "Gray-black thin-medium-layered siliceous rocks intersected with gray-white thin layered mudstone, 32.00m ————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Gray-black thin-medium-layered siliceous rocks with gray-white thin layered mudstones", "thickness", "32.00m" ], [ "Gray-black thin-medium-layered siliceous rocks with gray-white thin layered mudstones", "Integration of contacts", "New factory group" ], [ "New factory group", "Lithology", "Yellow-brown medium-thick layered muddy siltstone" ], [ "New factory group", "Lithology", "Gray-red thick layered mudstone" ] ] }, { "text": "Floating soil, 115.9m", "triple_list": [ [ "surface dust", "thickness", "115.9m" ] ] }, { "text": "Gray-green thick layered fine-grained metamorphic sandstone with gray-dark gray medium-layered thousand rocks and gray-dark gray diaboli veins, 35.44m", "triple_list": [ [ "Gray-green thick layered fine-grained metamorphic sandstone intersected with gray-dark gray medium-layered thousand rocks and gray-dark gray diaboli veins", "thickness", "35.44m" ] ] }, { "text": "Gray-green green curtain stone tremolite quartz schist and magnetite-containing diopterolite garnet skarn 24.0m", "triple_list": [ [ "Gray green green tremolite quartz schist", "thickness", "24.0m" ], [ "Magnetite diopylate garnet skall", "thickness", "24.0m" ] ] }, { "text": "Red-brown quartz mica schist, with mylonite tectonic breccia of about 9m wide, 121.7m", "triple_list": [ [ "Red-brown quartz mica schist", "thickness", "121.7m" ], [ "Mylonite tectonic breccia", "thickness", "About 9m wide" ] ] }, { "text": "Light yellow gray-white thick layer of blocky fine-grained quartz sandstone with muddy fine sandstone amid silt sandstone, 89m", "triple_list": [ [ "Light yellow, gray-white thick layer of blocky fine-grained quartz sandstone with muddy fine sandstone amidst silt sandstone", "thickness", "89m" ] ] }, { "text": "The ancient tomb group in the survey area was found north of Heishi Village in Cenxi and north of Liantan Town in Yunnan County. It was distributed in a northeastern band, about 65.88m2, accounting for 0.39% of the total area of the survey area.", "triple_list": [ [ "Ancient Tomb Group", "Exposed", "North of Cenxi Heishi Village" ], [ "Ancient Tomb Group", "Exposed", "North Liantan Town, Yunnan County" ], [ "Ancient Tomb Group", "Distribution pattern", "Northeastern belt distribution" ], [ "Ancient Tomb Group", "area", "65.88m2" ] ] }, { "text": "The lithologies of Donggangling Formation in the survey area are gray-white-dark gray-thin-middle-thick layered limestone bioclass limestone marl limestone amid limestone and dolomite dolomite, etc., with a small amount of calcified mudstone, mainly biological clastic limestone, and horizontal stratigraphic.", "triple_list": [ [ "Donggangling Group", "Lithology", "Gray-white gray-dark gray-middle-thick layered limestone" ], [ "Donggangling Group", "Lithology", "Bioclastic limestone" ], [ "Donggangling Group", "Lithology", "Marlite" ], [ "Donggangling Group", "Lithology", "Mixed limestone" ], [ "Donggangling Group", "Lithology", "Dolomites limestone" ], [ "Donggangling Group", "Lithology", "Dolomite" ], [ "Donggangling Group", "Lithology", "Calcium mudstone" ], [ "Donggangling Group", "Lithology", "Bioclastic limestone" ], [ "Donggangling Group", "Develop", "Horizontal stratification" ] ] }, { "text": "Yellow-brown mica quartz schist with marble black carbonaceous thousand rock, 53.7m", "triple_list": [ [ "Yellow-brown mica quartz schist marble black carbonaceous thousand rock", "thickness", "53.7m" ] ] }, { "text": "Xinyisi Heshikou uses blue-gray mica quartz schist mica quartzite as the main lens body with oblique elongated amphibole and marble.", "triple_list": [ [ "Xinyisi Heshiwu", "Lithology", "Blue-gray mica quartz schist mica quartzite" ], [ "Blue-gray mica quartz schist mica quartzite", "Contained", "oblique angular amphibole" ], [ "Blue-gray mica quartz schist mica quartzite", "Contained", "Marble lens body" ] ] }, { "text": "The distribution of the Qingbaikou-Cambrian, Devon-Carboniferous, Cretaceous and Quaternary strata in the Yangchun County Survey District is relatively concentrated, while the distribution of the Jixian, Ordovician, Silurian, Permian, Triassic-Jurassic and Paleogene strata is scattered.", "triple_list": [ [ "Yangchun County Survey District", "Stratigraphical zoning", "Qingbaikou period-Cambrian, Devon-Carboniferous, Cretaceous, Quaternary strata" ], [ "Yangchun County Survey District", "Stratigraphical zoning", "Jixian Chronicle, Ordovician, Silurian, Permian, Triassic-Jurassic, Paleogene strata" ] ] }, { "text": "The tiger pond group in the survey area is rich in micropaleophyllum, with a total of 32 genera and 77 species, with choys as the dominant. Their overall characteristics are mainly Leiopsophosphaera, rachysphaerium, Reticulumt, etc., with the size of 15~45m, and with the diameter of 15~30m, accounting for 80%~90% of the total; Laminarites, Taeniatum, Lignum, Polyporata, etc., accounting for 3~5% of the total; Lignum, riangumorpha, Micrhystridium, Quadratimorpha, etc. with more complex decorative patterns also account for 3~7%; Favososphaerium, Ooidium, Ooidium, The emergence of uruchcunica, etc.", "triple_list": [ [ "Tiger Pond Group", "Paleontological", "Leiopsophosphaera" ], [ "Tiger Pond Group", "Paleontological", "rachysphaeridium" ], [ "Tiger Pond Group", "Paleontological", "Reticulumt" ], [ "Tiger Pond Group", "Paleontological", "ynsphaeridium" ], [ "Tiger Pond Group", "Paleontological", "Lophosphaeridium" ], [ "Tiger Pond Group", "Paleontological", "Laminarites" ], [ "Tiger Pond Group", "Paleontological", "Taeniatum" ], [ "Tiger Pond Group", "Paleontological", "Lignum" ], [ "Tiger Pond Group", "Paleontological", "Polyporata" ], [ "Tiger Pond Group", "Paleontological", "Lignum" ], [ "Tiger Pond Group", "Paleontological", "riangumorpha" ], [ "Tiger Pond Group", "Paleontological", "Micrhystridium" ], [ "Tiger Pond Group", "Paleontological", "Quadratimorpha" ], [ "Tiger Pond Group", "Paleontological", "Favosophaeridium" ], [ "Tiger Pond Group", "Paleontological", "Ooidium" ], [ "Tiger Pond Group", "Paleontological", "uruchcunica" ] ] }, { "text": "The Bali Group in the survey area is mainly distributed east of Yangchun-Helang Yun'an Town, and a small area is exposed near the Donghu Reservoir south of Enping, about 233.32m2, accounting for 1.38% of the total area of the survey area.", "triple_list": [ [ "Bali Group", "Located at", "Yangchun—East from the town of Yun'an, Helang" ], [ "Bali Group", "area", "About 233.32m2" ] ] }, { "text": "The Gaozhou crust rock combination is mainly found in Wangsha Town, Xinyi City. There are sporadic exposures near the south and west ceratops of the picture, with an area of about 64.52m2, accounting for 0.38% of the total area of the survey area.", "triple_list": [ [ "Gaozhou Case Rock Combination", "Exposed", "Wangsha Town, Xinyi City" ], [ "Gaozhou Case Rock Combination", "Exposed", "Long Xiu" ], [ "Gaozhou Case Rock Combination", "area", "Area is about 64.52m2" ] ] }, { "text": "The Hepu Group in the survey area was exposed near Guiyi Town, Cenxi City, Guangxi, about 50.77m2, accounting for 0.30% of the total area of the survey area.", "triple_list": [ [ "Hepu Group", "Exposed", "Near Guiyi Town, Cenxi City, Guangxi" ], [ "Hepu Group", "area", "50.77m2" ] ] }, { "text": "The lithological combination of Xinchang Formation is a small amount of fine sandstone interlayer between yellow-brown muddy silt sandstone and light gray-red mudstone.", "triple_list": [ [ "New factory group", "Lithology", "Tawny mud silt sandstone" ], [ "New factory group", "Lithology", "Light gray-red mudstone" ], [ "New factory group", "Lithology", "Fine sandstone" ] ] }, { "text": "The lower part of the lithology of the Xindu Formation is light yellow, light gray-white thick layer of blocky fine-grained quartz sandstone with silt sandstone, partially intersected with gravel sandstone; the middle part is light yellow, gray medium-thick layered silt mudstone mudstone mudstone mudstone mudstone mudstone with fine-grained quartz sandstone; the upper part is gray white medium-thick layered quartz sandstone mudstone, with particle sequence stratigraphic horizontal stratigraphic.", "triple_list": [ [ "Xindu Group", "Lithology", "Light yellow light gray white thick layer of blocky fine-grained quartz sandstone" ], [ "Xindu Group", "Lithology", "Siltstone" ], [ "Xindu Group", "Lithology", "Gravel-containing sandstone" ], [ "Xindu Group", "Lithology", "Light yellow-gray medium-thick layered silty mudstone" ], [ "Xindu Group", "Lithology", "Mud siltstone" ], [ "Xindu Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Xindu Group", "Lithology", "Off-white medium-thick layered quartz sandstone" ], [ "Xindu Group", "Lithology", "Mudstone" ], [ "Xindu Group", "Develop", "Granular Sequence Laminating" ], [ "Xindu Group", "Develop", "Horizontal stratification" ] ] }, { "text": "Yellow-brown mica quartz schist with marble black carbonaceous thousand rock, 53.7m", "triple_list": [ [ "Tawny mica quartz schist", "Contained", "Marble black carbonaceous thousand rock" ], [ "Tawny mica quartz schist", "thickness", "53.7m" ] ] }, { "text": "The top of the first group of Yunkai Group is marked by marble and the second group of the overlying Yunkai Group is in integrated contact with the total thickness >1417m.", "triple_list": [ [ "The first group of Yunkai Group", "Lithology", "Dali Rock" ], [ "The first group of Yunkai Group", "Integration of contacts", "The second group of Yunkai Group" ], [ "The first group of Yunkai Group", "thickness", "1417m" ] ] }, { "text": "Gray thin-medium-layer fine sandstone is mainly mixed with silt sandstone, 55m ———————————————————————————————————————————————————————— Dagangding Formation of the underlying silt sandstone, gray-dark gray thin-layer silt sandstone", "triple_list": [ [ "Gray thin-medium-layer fine sandstone is the main silt sandstone", "thickness", "55m" ], [ "Gray thin-medium-layer fine sandstone is the main silt sandstone", "Integration of contacts", "Dagang Ding Group" ], [ "Dagang Ding Group", "Lithology", "Ash - dark gray thin layered silt sandy mudstone" ] ] }, { "text": "The upper part of the Daganshan Formation is light gray-green mica quartz schist, cross-stone mica quartz schist, gray-black red-columnite dimica schist, gray-black carbonaceous mica schist, carbonaceous sericite thousand rocks interspersed with thin layered cross-stone dolomite schist and a small amount of gray crude acidic tuff.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Light gray-gray green mica quartz schist" ], [ "Dakanshan Group", "Lithology", "Cross stone mica quartz schist" ], [ "Dakanshan Group", "Lithology", "Grey-black redcopylene dimica schist" ], [ "Dakanshan Group", "Lithology", "gray-black carbon mica schist" ], [ "Dakanshan Group", "Lithology", "Carbon sericite thousand rock" ], [ "Dakanshan Group", "Contained", "Thin layered cruciate dolomite schist" ], [ "Dakanshan Group", "Contained", "Gray coarse acidic tuff" ] ] }, { "text": "Rocks are generally affected by shallow metamorphism, and most mudstones have a thousand-shaped structure.", "triple_list": [ [ "Mudstone", "Develop", "Thousand-shaped structure" ] ] }, { "text": "The Lianxian Group of the survey area is distributed in Matang, Anchunwan, Yunfu Gaofeng Town, Yunkai District, and other places with an exposed area of about 74.62m2, accounting for 0.44% of the total area.", "triple_list": [ [ "Lianxian Group", "Exposed", "Matang, Anchunwan, Yunfu Gaofeng Town, Yunkai District" ], [ "Lianxian Group", "area", "74.62m2" ] ] }, { "text": "The Daganshan Formation (Nhd) originated from the Daganshan Formation 728 (1967) of the Guangdong Provincial Geological Bureau Comprehensive Research Brigade, which was named after the Dajiangping section of Yunfu County, to represent the Precambrian strata in the area.", "triple_list": [ [ "Dakanshan Formation (Nhd)", "Located at", "Dajiangping, Yunfu County" ], [ "Dakanshan Formation (Nhd)", "Age", "Precambrian" ] ] }, { "text": "The Qingbaikou-Sindan-Stratigraphic strata are widely distributed in the Yunfu and Luoding-Xinyi-Yangchun areas.", "triple_list": [ [ "Qingbaikou-Shendan formation", "Located at", "Yunfu" ], [ "Qingbaikou-Shendan formation", "Located at", "Luo Ding-Xinyi-Yangchun" ] ] }, { "text": "The brachiopods in the Hepu group are flourishing, and there are also Haifeng Clamella and Metamorphosis.", "triple_list": [ [ "Hepu Group", "Paleontological", "Brachiopod" ], [ "Hepu Group", "Paleontological", "Haifeng clams" ], [ "Hepu Group", "Paleontological", "Algae" ], [ "Hepu Group", "Paleontological", "Aphrodisiac" ] ] }, { "text": "Fossils such as fish Antiarchi, Arthrodira, Asterolepiformes, Placodermi, Euarthrodira and brachiopod Lingula sp. were found in the Lianhuashan Formation. The Nanjing Institute of Paleontology identified its era as Early Devonian-Early Middle Devonian", "triple_list": [ [ "Lotus Mountain Group", "Paleontological", "Antiarchi" ], [ "Lotus Mountain Group", "Paleontological", "Arthrodira" ], [ "Lotus Mountain Group", "Paleontological", "Asterolepiformes" ], [ "Lotus Mountain Group", "Paleontological", "Placodermi" ], [ "Lotus Mountain Group", "Paleontological", "Euarthrodira" ], [ "Lotus Mountain Group", "Paleontological", "Brachiopod Lingula sp." ], [ "Lotus Mountain Group", "Age", "Early Devonian-Early Middle Devonian" ] ] }, { "text": "The Dongchong Group of the survey area is distributed in the Beihekou-Kuidong area of Lidong Town, Yinzhu Town, Guangxi, north of Guangxi, Guangdong, with a total area of only 31.00m2, accounting for 0.18% of the total area of the survey area.", "triple_list": [ [ "Dongchong Group", "Exposed", "Guangxi Jinzhu Town North Guangdong Yunan Lidong Town Beihekou-Kuidong" ], [ "Dongchong Group", "area", "31.00m2" ] ] }, { "text": "Gray-green medium-thick layered calcareous mudstone with gray-black mudstone, 19.01m", "triple_list": [ [ "Gray-green medium-thick layered calcareous mudstone with gray-black mudstone", "thickness", "19.01m" ] ] }, { "text": "The Guidong Southeast Sub-district includes the Donggangling Group of the Xindu Group of the Lianhuashan Group and the Liujiang Group.", "triple_list": [ [ "Guidong Southeast Division", "Outcrop", "Lotus Mountain Group" ], [ "Guidong Southeast Division", "Outcrop", "Xindu Group" ], [ "Guidong Southeast Division", "Outcrop", "Donggangling Group" ], [ "Guidong Southeast Division", "Outcrop", "Liujiang Group" ] ] }, { "text": "Flaky quartzite and mica quartz schist interlayer, 107.8m", "triple_list": [ [ "Flaky quartzite", "thickness", "107.8m" ], [ "Mica quartz schist", "thickness", "107.8m" ] ] }, { "text": "Gray-white gray-green mica quartz schist with flaky quartzite, flat layer, 145.2m", "triple_list": [ [ "Gray white gray green mica quartz schist", "Contained", "Flaky quartzite" ], [ "Gray white gray green mica quartz schist", "thickness", "145.2m" ] ] }, { "text": "————Integration———————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "The first group of Yunkai Group", "thickness", "Total thickness >1417.8m" ] ] }, { "text": "Dark gray medium-layered silty limestone, containing wrist-porous Cytospirfer sp. Cytospirfer sp., 110.4m", "triple_list": [ [ "Dark gray medium-layered silty limestone", "Paleontological", "Cytospirfer sp." ], [ "Dark gray medium-layered silty limestone", "Paleontological", "Cyrtospirfer sp." ], [ "Dark gray medium-layered silty limestone", "thickness", "110.4m" ] ] }, { "text": "The lithology of the Luohong Formation is mainly clotted with grey yellow-white and blue-gray conglomerate quartz sandstone and gravel-containing thousand-metal rocks, and partially clotted limestone lens body.", "triple_list": [ [ "Luo Hong Group", "Lithology", "Gray yellow and white and blue-gray gravel rock" ], [ "Luo Hong Group", "Lithology", "Sandstone" ], [ "Luo Hong Group", "Lithology", "Quartz sandstone" ], [ "Luo Hong Group", "Lithology", "Thousands of gravels" ], [ "Luo Hong Group", "Lithology", "Mud siltstone" ], [ "Luo Hong Group", "Lithology", "Limestone lens body" ] ] }, { "text": "Gray medium-layered sheet physical and chemical metamorphic silt sandstone with thin layered Qianmei rock, 15.50m", "triple_list": [ [ "Gray medium-layered sheet physical and chemical metamorphic silt sandstone interspersed with thin layered thousand rocks", "thickness", "15.50m" ] ] }, { "text": "Lianxian Formation is a gray medium-thick layered fine crystal dolomite dolomite limestone with a small amount of gray-black argillite limestone.", "triple_list": [ [ "Lianxian Group", "Lithology", "Gray medium-thick layered fine crystal dolomite" ], [ "Lianxian Group", "Lithology", "Dolomites limestone" ], [ "Lianxian Group", "Lithology", "Gray-black mud limestone" ] ] }, { "text": "Gray yellow gray-red medium-thick layered metamorphic silt sandstone with light purple-red thin layered Qianmei rock, 89.49m", "triple_list": [ [ "Gray yellow gray-red medium-thick layered metamorphic silt sandstone with light purple-red thin layered Qianmei rock", "thickness", "89.49m" ] ] }, { "text": "Light gray dark gray thick layered metamorphic feldspar quartz sandstone with black mica schist, 37.9m", "triple_list": [ [ "Light gray dark gray thick layered metamorphic feldspar quartz sandstone with black mica schist", "thickness", "37.9m" ] ] }, { "text": "This work was conducted in the actual test section of Kengpingping in Guizi Town, Xinyi, with a relatively complete exposure, which can represent the overall appearance of the Kengping-angle porphyry system in the survey area. Its southern and northern boundaries are in fault contact with the Yunkai group.", "triple_list": [ [ "Kengping Xibi-angle porphyry system", "Fault contact", "Clouds open the group" ] ] }, { "text": "Gray-green shale with green sandstone, with pen stone Pristiographus aff. dubius, 2.0m", "triple_list": [ [ "Gray-green shale with green sandstone", "Paleontological", "Bishi Pristiographus aff. dubius" ], [ "Gray-green shale with green sandstone", "thickness", "2.0m" ] ] }, { "text": "Gray light yellow medium-thin layered punctate black cloud red column horn rocks with a small amount of angular lithification fine medium-grained quartz mixed sandstone, 30m", "triple_list": [ [ "Gray light yellow medium-thin layered punctate black cloud red pillar horn rock with a small amount of horn rock lithified fine medium-grained quartz sandstone", "thickness", "30m" ] ] }, { "text": "The Qingbaikou-Sindan-Stratigraphic strata are widely distributed in the Yunfu and Luoding-Xinyi-Yangchun areas.", "triple_list": [ [ "Qingbaikou-Shendan formation", "Exposed", "Yunfu" ], [ "Qingbaikou-Shendan formation", "Exposed", "Luo Ding-Xinyi-Yangchun" ] ] }, { "text": "Gray-black sheet of physical and chemical mica feldspar quartzite intersected with mica microschist, thin layer and strip shape, single layer thickness 23cm, 46.2m", "triple_list": [ [ "Gray-black sheet physical and chemical mica feldspar quartzite intersecting mica microschips", "Distribution pattern", "Strip shape" ], [ "Gray-black sheet physical and chemical mica feldspar quartzite intersecting mica microschips", "thickness", "46.2m" ] ] }, { "text": "Dark gray medium-thick layered horn lithified sand-containing mud conglomerate, 5m", "triple_list": [ [ "Dark gray medium-thick layered horn lithified sand-containing mud gravel rock", "thickness", "5m" ] ] }, { "text": "Most of the survey area belongs to the Yunkai Dashan Yunwu Mountain Range, which constitutes a low- and medium-mountain terrain that generally runs northwest to southeast, with an average Elevation of about 1,000m.", "triple_list": [ [ "Investigation Area", "Belongs to", "Clouds open up the mountains, clouds and mists, mountains" ], [ "Investigation Area", "Distribution pattern", "Low and medium-mountain terrain in northwest-southeast" ], [ "Investigation Area", "Elevation", "1000m" ] ] }, { "text": "The Tiger Tang Group (Z2lh), the Jiangxi District Test Team (1964), was established in the Tiger Tang Group, Shangxiang, Xiajiang County, Jiangxi Province. It refers to a set of rematerials between the Xiafang Group and the Likeng Group. The group in the survey area was only found in the east of Yangchun City, with an exposed area of about 39.14m2, accounting for 0.23% of the total area of the survey area.", "triple_list": [ [ "Tiger Pond Group (Z2lh)", "Lithology", "Compound quartz" ], [ "Tiger Pond Group (Z2lh)", "area", "About 39.14m2" ], [ "Tiger Pond Group (Z2lh)", "Located at", "East of Yangchun City" ] ] }, { "text": "The second group of the overlying strata cloud group, the upper thick layered horn lithified mica feldspar quartzite quartzite schist", "triple_list": [ [ "The second group of Yunkai Group", "Lithology", "Thick layered horn lithified mica feldspar quartzite" ], [ "The second group of Yunkai Group", "Lithology", "Quartz Mica Schist" ] ] }, { "text": "Gray-white—Gray-green flaky quartzite with mica schist and quartz mica schist, 68.6m", "triple_list": [ [ "Gray-white-grey flaky quartzite with mica schist and quartz mica schist", "thickness", "68.6m" ] ] }, { "text": "The Lianhuashan Group in the survey area was classified as the Xiadivontong.", "triple_list": [ [ "Lotus Mountain Group", "Age", "Lower ditto" ] ] }, { "text": "The rocks in the Kengping Sepia-angle porphyry system have been significantly deformed and metamorphized. The rock combinations of their original rocks mainly include layered gabbles, gabbles (shield), pyroxene porphyry, quartz horn porphyry, siliceous rock, etc.", "triple_list": [ [ "Kengping Xibi-horned porphyry system rocks", "Lithology", "Laminated gabbro" ], [ "Kengping Xibi-horned porphyry system rocks", "Lithology", "Galactic diaquat (seat)" ], [ "Kengping Xibi-horned porphyry system rocks", "Lithology", "Pyroxyl porphyry" ], [ "Kengping Xibi-horned porphyry system rocks", "Lithology", "Quartz horn porphyry" ], [ "Kengping Xibi-horned porphyry system rocks", "Lithology", "Silicone rock" ] ] }, { "text": "The main lithologies of the Daganshan Formation are quartz mica schist mica quartz schist metamorphic quartz sandstone metamorphic feldspar quartz sandstone metamorphic silts quartz rocks and black carbonaceous thousand rocks gray-white siliceous (manganese) limestone tuff and pyrite layer. The bottom is marked by gray-white conglomerate as a sign in parallel and unconformal contact with the second group of the underlying Yunkai Group, and the top is in integrated contact with the overlying Bali Formation, with a thickness of 8901508m.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Quartz mica schist" ], [ "Dakanshan Group", "Lithology", "Mica quartz schist" ], [ "Dakanshan Group", "Lithology", "Metamorphic quartz sandstone" ], [ "Dakanshan Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "Dakanshan Group", "Lithology", "Metamorphic siltstone" ], [ "Dakanshan Group", "Lithology", "Quartzite" ], [ "Dakanshan Group", "Lithology", "Black carbon thousand rock" ], [ "Dakanshan Group", "Lithology", "Off-white siliceous rock" ], [ "Dakanshan Group", "Lithology", "Manganese limestone" ], [ "Dakanshan Group", "Lithology", "Tuff" ], [ "Dakanshan Group", "Lithology", "Pyrite layer" ], [ "Dakanshan Group", "Lithology", "Off-white gravel" ], [ "Dakanshan Group", "Integration of contacts", "The second group of Yunkai Group" ], [ "Dakanshan Group", "Integration of contacts", "Bali Group" ], [ "Dakanshan Group", "thickness", "8901508m" ] ] }, { "text": "A predecessor measured a series of sections in the survey area and measured that the thickness of the Tianziling Group was 787.6m.", "triple_list": [ [ "Tianziling Group", "thickness", "787.6m" ] ] }, { "text": "The lithologies of Gaotan Formation are gray-gray green purple-red metamorphic (quartz) sandstone metamorphic siltstone mica quartz schist thin layered (including carbon) sericite thousand rocks, and horizontal stratigraphics are retained.", "triple_list": [ [ "Gaotan Group", "Lithology", "Gray gray green purple red metamorphic (quartz) sandstone" ], [ "Gaotan Group", "Lithology", "Metamorphic siltstone" ], [ "Gaotan Group", "Lithology", "Mica quartz schist" ], [ "Gaotan Group", "Lithology", "Thin layered (containing carbon) sericite thousand rock" ], [ "Gaotan Group", "Develop", "Horizontal stratification" ] ] }, { "text": "Gray-white—Gray-green flaky quartzite with mica schist and quartz mica schist, 68.6m", "triple_list": [ [ "Gray-white—Gray-green flaky quartzite", "thickness", "68.6m" ], [ "Gray-white—Gray-green flaky quartzite", "Lithology", "Mica quartz schist" ], [ "Gray-white—Gray-green flaky quartzite", "Lithology", "Quartz mica schist" ] ] }, { "text": "Light grayish grayish white thick layered block fine-grained quartz sandstone intersected with thin-layered argilled silt sandstone or fine-grained quartz sandstone, 84m", "triple_list": [ [ "Light grayish grayish white thick layered block fine-grained quartz sandstone intersected with thin-layered argilled silt sandstone or fine-grained quartz sandstone", "thickness", "84m" ] ] }, { "text": "The ancient tomb group developed horizontal layer texture and strip-like structure, with a thickness of 543m.", "triple_list": [ [ "Ancient Tomb Group", "Develop", "Horizontal stratification" ], [ "Ancient Tomb Group", "Develop", "Layer" ], [ "Ancient Tomb Group", "Develop", "Strip structure" ], [ "Ancient Tomb Group", "thickness", "543m" ] ] }, { "text": "Light yellow-white medium-thick layered fine-grained quartz sandstone with medium-thick layered muddy silt sandstone, 69m", "triple_list": [ [ "Light yellow-white medium-thick layered fine-grained quartz sandstone with medium-thick layered argillary silt sandstone", "thickness", "69m" ] ] }, { "text": "Xindu Group, total thickness >330m", "triple_list": [ [ "Xindu Group", "thickness", "330m" ] ] }, { "text": "The Dongchong Formation is mudstone quartz sandstone and marlstone and carbon-containing mudstone. It is thin-medium-layered, horizontal stratigraphic and strip-like structures, indicating that it is deposited in a semi-deep-sea environment with weak hydrodynamics.", "triple_list": [ [ "Dongchong Group", "Lithology", "Mudstone" ], [ "Dongchong Group", "Lithology", "Quartz sandstone" ], [ "Dongchong Group", "Lithology", "Marlite" ], [ "Dongchong Group", "Lithology", "Carbon-containing mudstone" ], [ "Dongchong Group", "Develop", "Horizontal stratification" ], [ "Dongchong Group", "Develop", "Strip structure" ], [ "Dongchong Group", "Belongs to", "Sedimentation in semi-deep sea environment" ] ] }, { "text": "Gray-black and gray-white striped magnesium marble and magnesium calcite quartz mica microschist 2.7m", "triple_list": [ [ "Gray-black and gray-white striped magnesium marble and magnesium calcite quartz mica microschist", "thickness", "2.7m" ] ] }, { "text": "Gray black yellow white quartz mica microschist charcoal sericite thousand rock, 69.1m", "triple_list": [ [ "Gray black yellow white quartz mica microschist", "Contained", "Carbon sericite thousand rock" ], [ "Gray black yellow white quartz mica microschist", "thickness", "69.1m" ] ] }, { "text": "Gray-green thick layered mica quartzite intersecting micro-thin layered quartz mica microschist, 39.3m", "triple_list": [ [ "Gray-green thick layered mica quartzite intersecting micro-thin layered quartz mica microschist", "thickness", "39.3m" ] ] }, { "text": "The survey area is mainly distributed in the areas of Chunguigang-Tanshui, Helang-Yunan Fulin and Cenxi Jinzhu-Yuntongmen, Nafuyangchun City, Taishan, with only 311.00m2, accounting for 1.84% of the total area of the survey area.", "triple_list": [ [ "Investigation Area", "Located at", "Nanyang Chunchun City, Taishan City, Guigang-Tanshui and Helang-Yunan Fulin and Cenxi Jinzhu-Yunnantongmen" ], [ "Investigation Area", "area", "311.00m2" ] ] }, { "text": "Silicate carbonite combination, with off-white striped siliceous rock (particle quartzite) on the upper part, horizontally layered, and carbonite mica quartz schist on the lower part, 51.9m", "triple_list": [ [ "Silicate carbonite combination", "Lithology", "Off-white striped siliceous rock" ], [ "Silicate carbonite combination", "Lithology", "Particular quartzite" ], [ "Silicate carbonite combination", "Develop", "Horizontal stratification" ], [ "Silicate carbonite combination", "Lithology", "Carbon mica quartz schist" ], [ "Silicate carbonite combination", "thickness", "51.9m" ] ] }, { "text": "The lithologies of the Dagangding Formation are gray-white-dark gray medium-thick layered fine-grained quartz mixed sandstone fine-grained quartz sandstone gravel-containing sandstone fine-grained quartz sandstone thin-layered mudstone and silty mudstone with a thickness of >692m.", "triple_list": [ [ "Dagang Ding Group", "Lithology", "Gray-white-dark gray medium-thick layered fine-grained quartz hybrid sandstone" ], [ "Dagang Ding Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Dagang Ding Group", "Lithology", "Gravel-containing sandstone" ], [ "Dagang Ding Group", "Lithology", "Fine-grained rock" ], [ "Dagang Ding Group", "Lithology", "Chop sandstone" ], [ "Dagang Ding Group", "Lithology", "Thin layered mudstone" ], [ "Dagang Ding Group", "Lithology", "Silty mudstone" ], [ "Dagang Ding Group", "thickness", "692m" ] ] }, { "text": "Thin layered quartz mica microschist, 66.4m", "triple_list": [ [ "Thin layered quartz mica microschist", "thickness", "66.4m" ] ] }, { "text": "The Bali Formation is mainly composed of the basic strata of fine sandstone-siltstone-mudstone, and is partially interspersed with siliceous rocks.", "triple_list": [ [ "Bali Group", "Lithology", "Fine sandstone-siltstone-milestone" ], [ "Bali Group", "Contained", "Silicone rock" ] ] }, { "text": "Dark gray medium-thick layered horn lithified silt mudstone, horizontally layered, 5m", "triple_list": [ [ "Dark gray medium-thick layered horn lithified silt mudstone", "Develop", "Horizontal stratification" ], [ "Dark gray medium-thick layered horn lithified silt mudstone", "thickness", "5m" ] ] }, { "text": "The Chunwan Formation in the survey area belongs to shallow marine sedimentation.", "triple_list": [ [ "Chunwan Group", "Belongs to", "shallow ocean sedimentation" ] ] }, { "text": "The exposed area of the Liujiang Formation is about 11.61m2, accounting for 0.07% of the total area. The lithologies of this group in the survey area are gray-blue gray-black-brown thin-layer siliceous rocks, siliceous mudstones containing amily siliceous rocks, etc., locally intersected (phosphorus siliceous) shale mudstones, and horizontally stratigraphic Develop.", "triple_list": [ [ "Liujiang Group", "area", "11.61m2" ], [ "Liujiang Group", "Lithology", "Gray blue gray gray black-brown thin layer of silica rock" ], [ "Liujiang Group", "Lithology", "Strip siliceous rock" ], [ "Liujiang Group", "Lithology", "Silicone mudstone" ], [ "Liujiang Group", "Lithology", "Slurry siliceous rock" ], [ "Liujiang Group", "Lithology", "(phospho-siliceous) shale" ], [ "Liujiang Group", "Lithology", "Mixed limestone" ], [ "Liujiang Group", "Develop", "Horizontal stratification" ] ] }, { "text": "Gray black yellow white mica quartz schist, 56.2m", "triple_list": [ [ "Gray black yellow white mica quartz schist", "thickness", "56.2m" ] ] }, { "text": "Light yellow thin layered thousand-piece fine sandy mudstone, 30m", "triple_list": [ [ "Light yellow thin layered thousand-piece fine sandy mudstone", "thickness", "30m" ] ] }, { "text": "Yellow-brown quartz mica sheets, with floating soil at the bottom, 180.3m", "triple_list": [ [ "Tawny quartz mica tablets", "Contained", "surface dust" ], [ "Tawny quartz mica tablets", "thickness", "180.3m" ] ] }, { "text": "Physical and chemical mica quartzite with black thin layered quartz mica schist and 0.5m thick oblique elongated flasheschist, 131.4m", "triple_list": [ [ "Physical and chemical mica quartzite with black thin layered quartz mica schist", "thickness", "131.4m" ], [ "oblique angular radiuschlid", "thickness", "0.5m thick" ] ] }, { "text": "Iron ore layers are seen in Dadongtian, Yunli and other places. The skarn-type magnetite on the upper part of this group can be used as a contrast mark in the area, and the marble on the top can be used as a division mark.", "triple_list": [ [ "Earth-See iron ore layer", "Located at", "Big winter fields, clouds" ], [ "Earth-See iron ore layer", "Contained", "Skarn magnetite" ], [ "Earth-See iron ore layer", "Contained", "Dali Rock" ] ] }, { "text": "The combined lithologies of Gaozhou surface crust rocks are mainly gray dark gray gray white mica quartz schist quartz mica schist black cloud horns flared rock pomegranate silicon line potassium long grain rock shallow grain rock sandwiched thin layered quartzite and marble lens bodies, which undergo mixed lithification to varying degrees.", "triple_list": [ [ "Gaozhou Case Rock Combination", "Lithology", "Gray dark gray gray white mica quartz schist" ], [ "Gaozhou Case Rock Combination", "Lithology", "Quartz mica schist" ], [ "Gaozhou Case Rock Combination", "Lithology", "Black clouds and grain rock" ], [ "Gaozhou Case Rock Combination", "Lithology", "Angle diffraction granite" ], [ "Gaozhou Case Rock Combination", "Lithology", "Potassium long-granular rock" ], [ "Gaozhou Case Rock Combination", "Lithology", "shallow grain rock" ], [ "Gaozhou Case Rock Combination", "Lithology", "Thin layered quartz rock" ], [ "Gaozhou Case Rock Combination", "Lithology", "Marble lens body" ] ] }, { "text": "Mica Quartz Platyrospar, 9.9m", "triple_list": [ [ "Mica quartz plagioclase horn", "thickness", "9.9m" ] ] }, { "text": "Gray black yellow white quartz mica microschist charcoal sericite thousand rock, 69.1m", "triple_list": [ [ "Gray black yellow white quartz mica microschist charcoal sericite thousand rock", "thickness", "69.1m" ] ] }, { "text": "Gray-black quartz mica schist with feldspar mica quartz schist, 139.3m", "triple_list": [ [ "Gray-black quartz mica schist containing carbon", "Contained", "feldspar mica quartz schist" ], [ "Gray-black quartz mica schist containing carbon", "thickness", "139.3m" ] ] }, { "text": "The Gaotan Group is in fault contact with the Yunkai Group and the upper part is in integrated contact with the Water-Shi Group.", "triple_list": [ [ "Gaotan Group", "Fault contact", "Clouds open the group" ], [ "Gaotan Group", "Integration of contacts", "Water stone group" ] ] }, { "text": "Gray-red-grey yellow sheets of physical and chemical fine-grained metamorphic sandstone with gray-purple-red metamorphic silt sandstone and a small amount of slate, 97.67m", "triple_list": [ [ "Gray-red-grey yellow sheets of physical and chemical fine-grained metamorphic sandstone with gray-purple-red metamorphic silt sandstone and a small amount of slabs", "thickness", "97.67m" ] ] }, { "text": "Light yellow light gray white medium-thick layered medium-fine grain quartz sandstone with a small amount of silt sandstone, including brachiopods, 20m", "triple_list": [ [ "Light yellow light gray white medium-thick layered medium-fine grain quartz sandstone with a small amount of silt sandstone", "Paleontological", "Brachiopod" ], [ "Light yellow light gray white medium-thick layered medium-fine grain quartz sandstone with a small amount of silt sandstone", "thickness", "20m" ] ] }, { "text": "The survey area is found in the east area of Nafu Town, Taishan City. The exposed area is small, only 6.12m2, accounting for 0.04% of the total area of the survey area, and is spread in a north-north and east-west belt.", "triple_list": [ [ "Investigation Area", "Located at", "East of Nafu Town, Taishan City" ], [ "Investigation Area", "area", "6.12m2" ], [ "Investigation Area", "Distribution pattern", "North-north eastward belt-shaped cloth" ] ] }, { "text": "Quartz sodium porphyry, 18.2m", "triple_list": [ [ "Quartz sodium porphyry", "thickness", "18.2m" ] ] }, { "text": "These reflect the sedimentary environment of the Hepu Formation as shallow-semi-deep sea.", "triple_list": [ [ "Hepu Group", "Belongs to", "Shallow sea-semi-deep sea sedimentary environment" ] ] }, { "text": "The Yunkai group in the survey area has not bottomed out. The first and second groups are continuous sedimentation. The geological era of the Leiminuscula minuteta-Leiopsophospaera minor group contained in the microplant fossil combination of the Leiminuscula minuteta-Leiopsophospaera minor group is more likely to Belongs to to the late Proterozoic Qingbaikou period. Judging from the isotope age data, 922~940Ma is generally used as the formation age of metamorphic volcanic rock interlayer, and 872.8±8.6Ma is the sedimentary age of the thin layered siliceous rock sands sandwiched by the gray-black carbonaceous thousand rocks. The possibility of the Qingbaikou period is higher. Therefore, the era of the Yunkai group in the survey area may be the Qingbaikou period, and the corresponding strata are the Qingbaikou system.", "triple_list": [ [ "Clouds open the group", "Paleontological", "Leiominuscula minute-Leiopsophospaera minor combination" ], [ "Clouds open the group", "Lithology", "Gray-black charcoal-containing thousand rocks" ], [ "Clouds open the group", "Contained", "Thin layered siliceous rock" ], [ "Clouds open the group", "Age", "Aobashi's mouth" ] ] }, { "text": "Floating soil, 10m ——————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "surface dust", "thickness", "10m" ], [ "surface dust", "Integration of contacts", "Xindu Group" ], [ "Xindu Group", "Lithology", "Mud siltstone" ], [ "Xindu Group", "Lithology", "Siltstone" ] ] }, { "text": "Off-white striped siliceous rock (particle quartzite), horizontally layered, 17.9m", "triple_list": [ [ "Off-white striped siliceous rock (particle quartzite)", "Develop", "Horizontal stratification" ], [ "Off-white striped siliceous rock (particle quartzite)", "thickness", "17.9m" ] ] }, { "text": "The lithology of the ancient tomb formation is gray light yellow fine-grained quartz sandstone medium-grained quartz mixed sandstone dark gray silty strip mudstone silty mudstone and shale, and the base is medium-grained quartz (milk) sandstone.", "triple_list": [ [ "Ancient Tomb Group", "Lithology", "Gray light yellow fine-grained quartz sandstone" ], [ "Ancient Tomb Group", "Lithology", "Medium-fine-grained quartz hybrid sandstone" ], [ "Ancient Tomb Group", "Lithology", "Dark gray silty sandy strip mudstone" ], [ "Ancient Tomb Group", "Lithology", "Silty mudstone" ], [ "Ancient Tomb Group", "Lithology", "shale" ], [ "Ancient Tomb Group", "Lithology", "Medium-fine-grained quartz (hybrid) sandstone" ] ] }, { "text": "The total change in the first group of Yunkai Group of the upper and lower strata in the area is not large. The lithology is mainly metamorphic siltstone, metamorphic feldspar quartz sandstone, mica quartz schist, quartz mica schist, and sericaceous kilograms. The original rock is a quartz interlayered quartz.", "triple_list": [ [ "The first group of clouds in the upper and lower strata", "Lithology", "Metamorphic siltstone" ], [ "The first group of clouds in the upper and lower strata", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "The first group of clouds in the upper and lower strata", "Lithology", "Mica quartz schist" ], [ "The first group of clouds in the upper and lower strata", "Lithology", "Quartz mica schist" ], [ "The first group of clouds in the upper and lower strata", "Lithology", "Sericite thousand rocks" ] ] }, { "text": "Light yellow medium-thick layered muddy silt sandstone with fine-grained sandstone, 29m", "triple_list": [ [ "Light yellow medium-thick layered muddy silt sandstone with fine-grained sandstone", "thickness", "29m" ] ] }, { "text": "Gray silver-gray mica quartz schist, 87.7m", "triple_list": [ [ "Gray silver grey mica quartz schist", "thickness", "87.7m" ] ] }, { "text": "The lithology of the Hepu Formation is gray, light gray, light yellow siltstone argillary siltstone mudstone shale and a small amount of quartz sandstone feldspar quartz sandstone lithotomy quartz sandstone, with mudstone or lithotomy quartz sandstone at the bottom, and is integrated with the limestone or limestone lens body at the top, with a thickness of 910-941m.", "triple_list": [ [ "Hepu Group", "Lithology", "Gray light gray light yellow siltstone" ], [ "Hepu Group", "Lithology", "Mud siltstone" ], [ "Hepu Group", "Lithology", "Mudstone" ], [ "Hepu Group", "Lithology", "shale" ], [ "Hepu Group", "Lithology", "Quartz sandstone" ], [ "Hepu Group", "Lithology", "Feldspar quartz sandstone" ], [ "Hepu Group", "Lithology", "Rock cutting quartz sandstone" ], [ "Hepu Group", "Lithology", "Mudstone" ], [ "Hepu Group", "Lithology", "Rock cutting quartz sandstone" ], [ "Hepu Group", "Integration of contacts", "Limestone" ], [ "Hepu Group", "Integration of contacts", "Limestone lens body" ], [ "Hepu Group", "thickness", "910-941m" ] ] }, { "text": "Gray thin-medium-layered metamorphic fine sandstone with gray thin-layered Qianmei rock, 30.14m", "triple_list": [ [ "Gray thin-medium-layer metamorphic fine sandstone with gray thin-layered thousand-four rock", "thickness", "30.14m" ] ] }, { "text": "Gray-green-light gray-red metamorphic silt sandstone with gray-red Qianmei rock, 90.33m", "triple_list": [ [ "Gray-green-light gray-red metamorphic silt sandstone with gray-red thousand rocks", "thickness", "90.33m" ] ] }, { "text": "Quartz mica microschist with green stone dioprene horn rock and thin layered mica feldspar quartzite 89.5m", "triple_list": [ [ "Quartz mica microschist with green stone dioprene horn rock", "thickness", "89.5m" ], [ "Thin layered mica feldspar quartzite", "thickness", "89.5m" ] ] }, { "text": "Black shale, with pilostone Demirastrites involutus Streptographus crispus S. exiguousS. sp., 8.0m", "triple_list": [ [ "Black shale", "Paleontological", "Bistone Demirastrites involutus Streptographus crispusS. exiguousS. sp." ], [ "Black shale", "thickness", "8.0m" ] ] }, { "text": "Gray light gray medium-thin layered silty thousand rocks containing Molongia sp. M.cf.uniplicata (Grubaw), 68m", "triple_list": [ [ "Gray light gray medium-thin layered silt thousand rocks", "Paleontological", "Molongia sp. M.cf.uniplicata(Grubaw)" ], [ "Gray light gray medium-thin layered silt thousand rocks", "thickness", "68m" ] ] }, { "text": "Floating soil, 25m", "triple_list": [ [ "surface dust", "thickness", "25m" ] ] }, { "text": "Fossils such as plants Psilophyton sp., brachiopod Lingula sulcatifera Gr., L.ex.gr. sulcatifera Gr., and flap gills Posidonia sp. were found in gray shale.", "triple_list": [ [ "Gray shale", "Paleontological", "Plant Psilophyton sp." ], [ "Gray shale", "Paleontological", "Brachiopod Lingula sulcatifera Gr." ], [ "Gray shale", "Paleontological", "L.ex.gr. sulcatifera Gr." ], [ "Gray shale", "Paleontological", "Posidonia sp." ] ] }, { "text": "The second group of Yunkai Group measured: Tandong-Fengdongkou section, Shimiao-Looudou section, Sanjiacun-Daipai section, Huanghuajiang section, Hongguanyan-Daipai section, etc.", "triple_list": [ [ "The second group of Yunkai Group", "Contained", "Tandong-Fengdongkou section" ], [ "The second group of Yunkai Group", "Contained", "Shimiao-Lounge section" ], [ "The second group of Yunkai Group", "Contained", "Sanjia Village - Dapi Section" ], [ "The second group of Yunkai Group", "Contained", "Huanghuajiang section" ], [ "The second group of Yunkai Group", "Contained", "Hong Guanyan Gu - Da Pi Section" ] ] }, { "text": "The Cambrian-Silurian strata are widely distributed, mainly seen in Kaitaishanyangchun Luoding and Yunan and Cenxi.", "triple_list": [ [ "Cambrian-Silurian strata", "Exposed", "Opening platform Shanyangchun Luoding Yunan and Cenxi" ] ] }, { "text": "Mica Quartz Platyrospar, 9.9m", "triple_list": [ [ "Mica quartz plagioclase horn", "thickness", "9.9m" ] ] }, { "text": "The Xindu group contains fossils such as brachiopods Stringocephalus sp., Desquamatia sp., Alveolitell sp., Syningopora sp., Amphipor sp., Paramphipora sp., and gastropod bivalves.", "triple_list": [ [ "Xindu Group", "Paleontological", "Brachiopod Stringocephalus sp." ], [ "Xindu Group", "Paleontological", "Desquamatia sp." ], [ "Xindu Group", "Paleontological", "Coral Alveolitell sp." ], [ "Xindu Group", "Paleontological", "Syringopora sp." ], [ "Xindu Group", "Paleontological", "Foraminifera Amphipor sp." ], [ "Xindu Group", "Paleontological", "Paraamphipora sp." ], [ "Xindu Group", "Paleontological", "Gastropod" ], [ "Xindu Group", "Paleontological", "Bivalves" ] ] }, { "text": "The lithologies of Dongchong Formation are thin-medium-layered gray-gray yellow medium-fine-grained quartz mixed sandstone, and locally they are quartz sericite thousand rock sericite thousand rock and carbon-containing mudstone, and the bottom is quartz mixed sandstone, and the top is quartz mixed sandstone.", "triple_list": [ [ "Dongchong Group", "Lithology", "Thin-medium-layered gray-gray yellow medium-fine-grained quartz hybrid sandstone" ], [ "Dongchong Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Dongchong Group", "Lithology", "Mudstone" ], [ "Dongchong Group", "Lithology", "Quartz sericite thousand rock" ], [ "Dongchong Group", "Lithology", "Serous Quartz Thousand Rocks" ], [ "Dongchong Group", "Lithology", "Marlite" ], [ "Dongchong Group", "Lithology", "Carbon-containing mudstone" ], [ "Dongchong Group", "Lithology", "Medium-layered quartz sandstone" ], [ "Dongchong Group", "Lithology", "Miscellaneous sandstone" ], [ "Dongchong Group", "Lithology", "Mudstone" ] ] }, { "text": "The Carboniferous strata are widely distributed, and Yunfu En Ping Kaiping Luoding Yangchun and other places are distributed. They can be divided into Lianxian Group or Dasaiba Group Shitangzi Group and Hutian Group.", "triple_list": [ [ "Carboniferous strata", "Exposed", "Yunfu En Pingping Yangchun" ], [ "Carboniferous strata", "Outcrop", "Lianxian Group" ], [ "Carboniferous strata", "Outcrop", "Dashengba Group" ], [ "Carboniferous strata", "Outcrop", "Shizhuzi Group" ], [ "Carboniferous strata", "Outcrop", "Water measurement group" ], [ "Carboniferous strata", "Outcrop", "Hutian Group" ] ] }, { "text": "Anti-granular stratigraphy in gravel-containing sandstone", "triple_list": [ [ "Gravel-containing sandstone", "Develop", "Antigranulation sequence stratigraphy" ] ] }, { "text": "Gray-black thin-layer siliceous rock, 2.80m", "triple_list": [ [ "Gray-black thin-layer siliceous rock", "thickness", "2.80m" ] ] }, { "text": "Overlapping Hushan Formation, gray-black thin-medium-layered siliceous rocks with gray-white extremely thin layered mudstone ———————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Hushan Group", "Lithology", "Gray-black thin-medium-layered siliceous rock" ], [ "Hushan Group", "Lithology", "Off-white extremely thin layered mudstone" ], [ "Hushan Group", "Integration of contacts", "New factory group" ], [ "New factory group", "thickness", "132.31m" ] ] }, { "text": "Luohong Formation and the underlying water stone Formation were in parallel and unconformed contact, and in integrated contact with the overlying Luodong Formation, with a thickness of 2518m, horizontal laminar Develop, and bottom erosion can be seen at the bottom of the conglomerate.", "triple_list": [ [ "Luo Hong Group", "Integration of contacts", "Water stone group" ], [ "Luo Hong Group", "Integration of contacts", "Luodong Group" ], [ "Luo Hong Group", "thickness", "2518m" ], [ "Luo Hong Group", "Develop", "Horizontal stratification" ] ] }, { "text": "The lithological combination of Gaozhou surface crust rock combination in Changpo Longxiu is the gravel granite-calcium silicate-granule rock-transparent marble combination, and its metamorphism reaches the high-angle amphibole-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-piloschist, etc., and its metamorphism reaches the horn amphibole rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granule rock-granu", "triple_list": [ [ "Gaozhou Case Rock Combination", "Lithology", "Pomegranate-calcium silicate-emegranate-transparent marble combination" ], [ "Gaozhou Case Rock Combination", "Lithology", "Mixed rock-sized pomegranate rock-serratic black cloud-serratic rock-serratic schist" ] ] }, { "text": "Ash-gray-green medium-thick layered mudstone with gray silt sandstone and gray-black carbon-containing mudstone, 28.91m", "triple_list": [ [ "Ash-gray-green medium-thick layered mudstone with gray silt sandstone and gray-black carbon-containing mudstone", "thickness", "28.91m" ] ] }, { "text": "Dimica quartz schist with off-white sheet mica quartzite, 137.6m", "triple_list": [ [ "Dimica quartz schist", "Contained", "Off-white sheet mica quartzite" ], [ "Dimica quartz schist", "thickness", "137.6m" ] ] }, { "text": "Chunwan Formation is a set of gray, green, gray, red, yellow, and gray and other variegated sand mud or calcified clastic rocks.", "triple_list": [ [ "Chunwan Group", "Lithology", "Gray green, gray, red, yellow, gray and other variegated sand mud or calcified clastic rock" ] ] }, { "text": "The Dongjiang Division of Yunkai District includes the Tianziling Group of the Chunwan Group of Guitou Qun and the Maozifeng Group.", "triple_list": [ [ "Yunkai District Dongjiang District", "Outcrop", "Guitou Group" ], [ "Yunkai District Dongjiang District", "Outcrop", "Chunwan Group" ], [ "Yunkai District Dongjiang District", "Outcrop", "Tianziling Group" ], [ "Yunkai District Dongjiang District", "Outcrop", "Hat Peak Group" ] ] }, { "text": "The lithologies of the Laohutang Formation are metamorphic (feldspar) quartz sandstone, quartzite sandy rocks with carbonaceous serous rocks and sandy silty slates, etc., with a thickness of 950m.", "triple_list": [ [ "Tiger Pond Group", "Lithology", "Metamorphic (feldspar) quartz sandstone" ], [ "Tiger Pond Group", "Lithology", "Quartzite" ], [ "Tiger Pond Group", "Contained", "Carbon-containing sericinous rock" ], [ "Tiger Pond Group", "Contained", "Sandy silty slab" ], [ "Tiger Pond Group", "thickness", "950m thick" ] ] }, { "text": "Gray-black medium-thin layered siliceous rocks with gray-white thin-layered mudstone, 11.23m", "triple_list": [ [ "Gray-black medium-thin layered siliceous rocks with gray-white thin-layered mudstones", "thickness", "11.23m" ] ] }, { "text": "The Xindu Group is distributed in Zhangmu Town, Guiyi Town, Guangxi and other places, with an exposed area of about 12.01m2, accounting for 0.07% of the total area.", "triple_list": [ [ "Xindu Group", "Exposed", "Zhangmu Town, Guiyi Town, Guangxi" ], [ "Xindu Group", "area", "12.01m2" ] ] }, { "text": "The rocks in Yunkai Group are generally metamorphic and mixed lithification. The original rocks are composed of fine sand-silt-silt-silt sediments, and the basic volcanic carbonate siliceous rock thin layer or lens body with marine facies. They are characterized by the Develop of horizontal stratum with strip-like structures. The sedimentary minerals mainly include phosphothiote layer and manganese-containing limestone in deep water reduction environment, indicating that the Yunkai Group in the survey area belongs to semi-deep-deep sea-deep sea sedimentation.", "triple_list": [ [ "Clouds open the group", "Lithology", "Common metamorphosis and mixed lithification" ], [ "Clouds open the group", "Distribution pattern", "Strip structure" ], [ "Clouds open the group", "Develop", "Horizontal streak layer" ], [ "Clouds open the group", "Lithology", "Semi-deep sea-deep sea phase sedimentation" ] ] }, { "text": "Gray-black thin-layer siliceous rock with gray-white extremely thin layer of mudstone, 44.62m", "triple_list": [ [ "Gray-black thin-layer siliceous rock with gray-white extremely thin layer of mudstone", "thickness", "44.62m" ] ] }, { "text": "The Lanweng Formation should Belongs to to semi-deep-deep sea phase sedimentation.", "triple_list": [ [ "Orchid group", "Belongs to", "Semi-deep sea-deep sea phase sedimentation" ] ] }, { "text": "Daganshan Formation, total thickness >1021m", "triple_list": [ [ "Dakanshan Group", "thickness", "1021m" ] ] }, { "text": "The second group of Yunkai Group showed parallel and unconformal contact with the conglomerates of Daganshan Formation, and the lower part was in integrated contact with the marble or calcareous siltstone at the top of the first group of Yunkai Group, with a total thickness of >1343m.", "triple_list": [ [ "The second group of Yunkai Group", "Integration of contacts", "Daganshan Formation" ], [ "The second group of Yunkai Group", "Lithology", "The marble rock at the top of the first group of Yunkai Group" ], [ "The second group of Yunkai Group", "Lithology", "Calcium siltstone" ], [ "The second group of Yunkai Group", "thickness", "1343m" ] ] }, { "text": "The top of the first group of Yunkai Group is marked by marble and the second group of the overlying Yunkai Group is in integrated contact.", "triple_list": [ [ "Top of the first group of Yunkai Group", "Integration of contacts", "The second group of overturned clouds" ] ] }, { "text": "Gray-brown gray-red medium-thick layered fine-grained sheet physical and chemical metamorphic sandstone intersected with ash-gray-yellow thin-layered thousand-focus rock, 42.82m", "triple_list": [ [ "Gray-brown gray-red medium-thick layered fine-grained sheet physical and chemical metamorphic sandstone intersected with ash-gray yellow thin-layered thousand rocks", "thickness", "42.82m" ] ] }, { "text": "The Dongchong Formation of the overlying formation is transformed into ploxial black cloud red column horn rock, with fine-grained quartz sandstone at the bottom. ——————————————————————————————————————————— Luodong Formation, total thickness of 19.0m", "triple_list": [ [ "Dongchong Group", "Lithology", "Spotted black clouds and red pillars rock" ], [ "Dongchong Group", "Lithology", "Fine-grained quartz hybrid sandstone in horn lithification" ], [ "Dongchong Group", "Integration of contacts", "Luodong Group" ], [ "Luodong Group", "thickness", "19.0m" ] ] }, { "text": "The interlayers have changed in different places: Xinyifengdongkou, Luodingdumen Ganzhu and other places are interspersed with multiple gray-black carbon-like thousand-member rocks, while Xinyiloudong areas are interspersed with carbon-like thousand-member rocks and thin-layer strip-like siliceous rocks.", "triple_list": [ [ "Xinyifengdongkou, Luodingdumen Ganzhu and other places", "Lithology", "Multi-layer gray-black carbonaceous thousand rocks" ], [ "Xinyi Building", "Lithology", "Carbon-containing thousand rocks" ], [ "Xinyi Building", "Lithology", "Thin-layer striped siliceous rock" ] ] }, { "text": "Brown and yellow shale fragments, 3.0m", "triple_list": [ [ "Brown and yellow shale fragments", "thickness", "3.0m" ] ] }, { "text": "Floating soil, 244.4m", "triple_list": [ [ "surface dust", "thickness", "244.4m" ] ] }, { "text": "The Silurian strata are distributed in the Yunkai strata zone in the southeastern Guizhou strata zone, and from bottom to top are the Liantan strata group and the Fangcheng group.", "triple_list": [ [ "Silurian strata", "Stratigraphical zoning", "Southeast Guizhou stratigraphic division" ], [ "Silurian strata", "Stratigraphical zoning", "Yunkai stratigraphic partition" ], [ "Silurian strata", "Outcrop", "Dagang Ding Group" ], [ "Silurian strata", "Outcrop", "Ancient Tomb Group" ], [ "Silurian strata", "Outcrop", "Liantan Group" ], [ "Silurian strata", "Outcrop", "Hepu Group" ], [ "Silurian strata", "Outcrop", "Fangcheng Group" ] ] }, { "text": "Light yellow, green, brown, red, medium-thick layered silty serous slate, horizontally layered, 15m", "triple_list": [ [ "Light yellow, green, brown, red, medium-thick layered silty serous slab", "Develop", "Horizontal stratification" ], [ "Light yellow, green, brown, red, medium-thick layered silty serous slab", "thickness", "15m" ] ] }, { "text": "Gray-green thin-medium-thick layered sheets of physical and chemical mica quartzite with yellow-brown, purple-red micro-thin layered quartz schist, >266.1m, no bottom is seen", "triple_list": [ [ "Gray-green thin-medium-thick layered sheets of physicochemical mica quartzite", "thickness", ">266.1m" ], [ "Gray-green thin-medium-thick layered sheets of physicochemical mica quartzite", "Contained", "Yellow-brown, purple-red micro-thin layered quartz schist" ] ] }, { "text": "Tawny quartz mica schist, 87.2m", "triple_list": [ [ "Tawny quartz mica schist", "thickness", "87.2m" ] ] }, { "text": "The Gaozhou crust rock combination is mainly found in Wangsha Town, Xinyi City. There are sporadic exposures near the south and west ceratops of the picture, with an area of about 64.52m2, accounting for 0.38% of the total area of the survey area.", "triple_list": [ [ "Gaozhou Case Rock Combination", "Exposed", "Wangsha Town, Xinyi City" ], [ "Gaozhou Case Rock Combination", "Exposed", "Picture of the picture is near the south and west ceratops cultivation" ], [ "Gaozhou Case Rock Combination", "area", "64.52m2" ] ] }, { "text": "The strata of Yangchun County survey area is widely distributed, and all strata of the strata have been developed since the Jixian period.", "triple_list": [ [ "Yangchun County Survey District", "Develop", "All strata have developed since the Jixian Chronicle" ] ] }, { "text": "Rhythmic Develop of horizontal stratification quartile in Dagangding Formation", "triple_list": [ [ "Dagang Ding Group", "Develop", "Horizontal stratification" ], [ "Dagang Ding Group", "Develop", "Reprocessing" ], [ "Dagang Ding Group", "Develop", "Stone rhyme" ] ] }, { "text": "Dimica quartz schist with off-white sheet mica quartzite, 137.6m", "triple_list": [ [ "Dimica quartz schist with off-white sheet mica quartzite", "thickness", "137.6m" ] ] }, { "text": "The lithology of the Dagangding Formation is dark gray silty mudstone containing silty mudstone, with a small amount of thin-layered fine sandstone, with a slight increase from bottom to top, and the top is thin-layered mudstone.", "triple_list": [ [ "Dagang Ding Group", "Lithology", "Dark gray silty mudstone" ], [ "Dagang Ding Group", "Lithology", "Silty sand mud rock" ], [ "Dagang Ding Group", "Lithology", "Thin-microlayer fine sandstone" ], [ "Dagang Ding Group", "Lithology", "sandstone" ], [ "Dagang Ding Group", "Lithology", "Thin layered mudstone" ] ] }, { "text": "Gray-green medium-thick layered metamorphic silt sandstone with a small amount of gray medium-layered fine-grained metamorphic sandstone, 116.44m", "triple_list": [ [ "Gray-green medium-thick layered metamorphic silt sandstone with a small amount of gray medium-layered fine-grained metamorphic sandstone", "thickness", "116.44m" ] ] }, { "text": "In the Hushan Group in the survey area, major elements such as Isographus virusie Harris, Cardinographus sp., and etragraphus bigsby were found. The era belongs to the Early Ordovician Red Garden Period-Great Bay Period.", "triple_list": [ [ "Hushan Group", "Paleontological", "Isographus virusie virusie Harris" ], [ "Hushan Group", "Paleontological", "Cardinographus sp." ], [ "Hushan Group", "Paleontological", "etragraphus bigsby" ], [ "Hushan Group", "Age", "Early Ordovician Red Garden Period-Greater Bay Period" ] ] }, { "text": "Floating soil, 115.9m", "triple_list": [ [ "surface dust", "thickness", "115.9m" ] ] }, { "text": "The survey area is mainly distributed in Dongwei, Zhangmu Town, Guiyi Town, Guangxi, and other places. The exposed area is about 19.78m2, accounting for 0.12% of the total area. The lithology is medium-thick layered medium-fine-grained quartz sandstone, gravel-containing quartz mixed sandstone, and thin-layered argillite silty sandstone.", "triple_list": [ [ "Investigation Area", "Located at", "Dongwei, Zhangmu Town, Guiyi Town, Guangxi" ], [ "Investigation Area", "area", "19.78m2" ], [ "Investigation Area", "Lithology", "Medium-thick layered medium-fine grain quartz sandstone" ], [ "Investigation Area", "Lithology", "Gravel-containing quartz sandstone" ], [ "Investigation Area", "Lithology", "Thin layered muddy siltstone" ], [ "Investigation Area", "Lithology", "Silty mudstone" ] ] }, { "text": "Brown-gray striped shale, 6.0m", "triple_list": [ [ "Brown-gray striped shale", "thickness", "6.0m" ] ] }, { "text": "The Bali Formation (Z1b), Jiangxi District Survey Team (1969), was named after the Bali profile of Xiaoxi Township, Yudu County, Jiangxi Province. It refers to a set of shallow marine terrestrial pyroclastic siliceous rocks integrated between Shaba Huang Formation and Niujiao River Group.", "triple_list": [ [ "Bali Formation (Z1b)", "Located at", "Bali, Xiaoxi Township, Yudu County, Jiangxi" ], [ "Bali Formation (Z1b)", "Lithology", "Shallow marine terrestrial pyroclastic siliceous rock" ] ] }, { "text": "The survey area is mainly produced in the Daganshan Group and the Tiger Tang Group in the Nanhua-Sinian period. The most species were obtained in the Tiger Tang Group, mainly containing Leiominuscula (Glossy Chlorella), Leiopsophosphaera (Chlorella), rachysphaera (Clossy Chlorella), rachysphaera (Clossy Chlorella).", "triple_list": [ [ "Dakanshan Group", "Age", "Nanhua-Zhendanji" ], [ "Tiger Pond Group", "Age", "Nanhua-Zhendanji" ], [ "Tiger Pond Group", "Paleontological", "Leiominuscula (Chlorella glossy)" ], [ "Tiger Pond Group", "Paleontological", "Leiopsophosphaera (Chlorophylla)" ], [ "Tiger Pond Group", "Paleontological", "rachysphaeridium (Rhodge Sphereus)" ] ] }, { "text": "Luodong Formation, Lower Voluhong Formation and Overly Overhead Dongchong Formation both showed integrated contact, and developed horizontal stratification and strip-like structure.", "triple_list": [ [ "Luodong Group", "Integration of contacts", "Luo Hong Group" ], [ "Luodong Group", "Integration of contacts", "Dongchong Group" ], [ "Luodong Group", "Develop", "Horizontal stratification" ], [ "Luodong Group", "Develop", "Strip structure" ] ] }, { "text": "Overly covered formation water stone formation, gray-purple-red metamorphic silt sandstone sandstone intersected with Qianmeiyan----------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------", "triple_list": [ [ "Water stone group", "Lithology", "Gray purple-red metamorphic siltstone" ], [ "Water stone group", "Lithology", "Qianmeiyan" ], [ "Water stone group", "Fault contact", "Gaotan Group" ], [ "Gaotan Group", "thickness", "1766.33m" ] ] }, { "text": "The lithology of Chunwan Formation is fine-grained quartz sandstone feldspar quartz sandstone mixed with silty mudstone calcified mudstone and thin layer of biolimestone, and horizontal stratigraphic Develop.", "triple_list": [ [ "Chunwan Group", "Lithology", "Fine-grained quartz sandstone" ], [ "Chunwan Group", "Lithology", "Feldspar quartz sandstone" ], [ "Chunwan Group", "Lithology", "Silty mudstone" ], [ "Chunwan Group", "Lithology", "Calcium mud siltstone" ], [ "Chunwan Group", "Lithology", "Thin layer of biolimestone" ], [ "Chunwan Group", "Develop", "Horizontal stratification" ] ] }, { "text": "The lithologies of the Bali Formation are metamorphic (feldspar) quartz sandstone, metamorphic siltstone, mica quartz schist, and kilogram rocks, which are mainly thin-layered carbonaceous kilogram rocks, thin-layer quartzite (siliceous rocks) and quartz mica schist.", "triple_list": [ [ "Bali Group", "Lithology", "Metamorphic (feldspar) quartz sandstone" ], [ "Bali Group", "Lithology", "Metamorphic siltstone" ], [ "Bali Group", "Lithology", "Mica quartz schist" ], [ "Bali Group", "Lithology", "Qianmeiyan" ], [ "Bali Group", "Contained", "Thin layered carbonaceous rock" ], [ "Bali Group", "Contained", "Thin layer of quartzite (siliceous rock)" ], [ "Bali Group", "Contained", "Quartz mica schist" ] ] }, { "text": "Gray striped shale, 2.0m", "triple_list": [ [ "Gray striped shale", "thickness", "2.0m" ] ] }, { "text": "The original Dakanshan group refers to a set of strata composed of ground trough type complex quartz construction, volcanic siliceous iron-manganese construction and muddy shale construction.", "triple_list": [ [ "Original Dakan Mountain Group", "Lithology", "Groove type quartz" ], [ "Original Dakan Mountain Group", "Lithology", "Volcanic siliceous ferromanganese" ], [ "Original Dakan Mountain Group", "Lithology", "Mud shale" ] ] }, { "text": "Gray thin-layered thousand rocks with thin-layered fine-grained metamorphic sandstone, 122.32m", "triple_list": [ [ "Gray thin-layered Qianmei rocks with thin-layered fine-grained metamorphic sandstone", "thickness", "122.32m" ] ] }, { "text": "Physical and chemical fine-grained metamorphic sandstone and silty slate interlayers, 23.2m", "triple_list": [ [ "Physical and chemical fine-grained metamorphic sandstone and silty slate interlayers with gray-grey-green middle-layered flakes", "thickness", "23.2m" ] ] }, { "text": "The mudstone is covered with rolling layering, but it has not been seen bottoming out, and it is in integrated contact with the overlying ancient tomb group.", "triple_list": [ [ "Mudstone", "Develop", "Cover lamination" ], [ "Mudstone", "Integration of contacts", "Ancient Tomb Group" ] ] }, { "text": "Light gray quartz silty sandy sericite thousand rocks with black carbonaceous thousand rocks, 33.6m", "triple_list": [ [ "Light gray quartz silty sandy sericite thousand rocks with black carbonaceous thousand rocks", "thickness", "33.6m" ] ] }, { "text": "Gray white light gray sheet physical and chemical black cloud oblique length crystalline rock with thin layer of quartz mica schist, 80.8m", "triple_list": [ [ "Gray white light gray sheets of physical and chemical black clouds with oblique lengths of grain rock", "Contained", "Thin layer of quartz mica schist" ], [ "Gray white light gray sheets of physical and chemical black clouds with oblique lengths of grain rock", "thickness", "80.8m" ] ] }, { "text": "Yellow-brown mica schist with thin layered mica quartz schist, 86.6m", "triple_list": [ [ "Tawny mica schist", "thickness", "86.6m" ], [ "Tawny mica schist", "Contained", "Thin layered mica quartz schist" ] ] }, { "text": "Gaozhou crust rock assembly rock is invaded by flaky granite.", "triple_list": [ [ "Gaozhou Case Rock Combination Rock", "Invade", "Hemp granite" ] ] }, { "text": "The lithology of the Hepu Formation is gray light yellow mixed sandstone silt sandy mudstone and a small amount of manganese-containing calcium silica mudstone, with quartz rhythm characteristics.", "triple_list": [ [ "Hepu Group", "Lithology", "Grey light yellow mixed sandstone" ], [ "Hepu Group", "Lithology", "Silty mudstone" ], [ "Hepu Group", "Lithology", "Manganese-containing calcium silicate" ], [ "Hepu Group", "Develop", "Rhythmic characteristics of fume" ] ] }, { "text": "Daganshan Formation, total thickness >1021m", "triple_list": [ [ "Dakanshan Group", "thickness", ">1021m" ] ] }, { "text": "The Chunwan Formation is relatively developed in the survey area and is mainly distributed in Chunshuangyue Village, Xiyang Hengbei, Enping - Luodingliantan, Luoguo, Weiguo, and other places. The exposed area is about 254.83m2, accounting for 1.51% of the total area.", "triple_list": [ [ "Chunwan Group", "Exposed", "Enping Hengpi West Yangchun Shuangyue Village - Luodingliantan, Weiguo" ], [ "Chunwan Group", "area", "254.83m2" ] ] }, { "text": "Both the Tianziling group and the Chunwan group and the Maozifeng group were in integrated contact, and the contact relationship was clear.", "triple_list": [ [ "Tianziling Group", "Integration of contacts", "Chunwan Group" ], [ "Tianziling Group", "Integration of contacts", "Hat Peak Group" ] ] }, { "text": "The second group of Yunkai Group, thick layered horned lithomorphized mica feldspar quartzite with quartz black mica schist at the upper part, gray-green flake green curtain at the lower part", "triple_list": [ [ "The second group of Yunkai Group", "Lithology", "Thick layered horn lithified mica feldspar quartzite quartz-millica schist" ], [ "The second group of Yunkai Group", "Lithology", "Gray green flake green curtain" ] ] }, { "text": "Purple-red Thousand Rocks (Physical and Chemical Mudstone) with red metamorphic silt sandstone, 28.35m", "triple_list": [ [ "Purple-red Qianmei Rock (Physical and Chemical Mudstone) with red metamorphic silt", "thickness", "28.35m" ] ] }, { "text": "The lower part of the Daganshan Formation, the gray-banded quartz dimica schist, the dark gray-green striped cross-silt dimica schist, the gray-black carbonaceous mica schist, the silt sandstone, the carbonaceous mica quartz schist, the granule rock, the gray-blocked black mica plagiarite, the dioplastic plagiarite and the gray-black thin-layered crystalline limestone, the volcanic tuff material is concentrated in Pengshi, >243m", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray striped quartz dimica schist" ], [ "Dakanshan Group", "Lithology", "Dark gray-green striped cross stone dimica schist" ], [ "Dakanshan Group", "Lithology", "gray-black carbon mica schist" ], [ "Dakanshan Group", "Contained", "Siltstone" ], [ "Dakanshan Group", "Contained", "Carbon mica quartz schist" ], [ "Dakanshan Group", "Contained", "Granular rock" ], [ "Dakanshan Group", "Contained", "Gray blocky mica plagioclalis" ], [ "Dakanshan Group", "Contained", "diopylate plagioclase" ], [ "Dakanshan Group", "Contained", "Gray-black thin layer of fine particle crystalline limestone" ], [ "Dakanshan Group", "Contained", "Volcanic tuff material" ], [ "Gray striped quartz dimica schist", "thickness", ">243m" ], [ "Dark gray-green striped cross stone dimica schist", "thickness", ">243m" ], [ "gray-black carbon mica schist", "thickness", ">243m" ], [ "Volcanic tuff material", "Located at", "Pengshi" ] ] }, { "text": "Light gray granular rock, 42.2m", "triple_list": [ [ "Light grey granular rock", "thickness", "42.2m" ] ] }, { "text": "Tawny metamorphic feldspar quartz sandstone flash gray black quartz mica schist, 52.4m", "triple_list": [ [ "Tawny metamorphic feldspar quartz sandstone flash gray black quartz mica schist", "thickness", "52.4m" ] ] }, { "text": "Gray fine-grained metamorphic sandstone with silt sandstone and gray-green medium-thick layered slate, 35.15m", "triple_list": [ [ "Gray fine-grained metamorphic sandstone with silt sandstone and gray-green medium-thick layered slabs", "thickness", "35.15m" ] ] }, { "text": "Gray-yellow medium-thin layered sheet physical and chemical fine-grained metamorphic sandstone and gray-dark gray thousand rocks, 50.93m", "triple_list": [ [ "Gray-yellow Medium-Thin-Layered Plate Physical and Chemical Fine-Grade Metamorphic Sandstone and Gray-Dark Gray Thousand Rocks", "thickness", "50.93m" ] ] }, { "text": "Physical and chemical mica feldspar quartzite with weathered purple-red layered quartz mica schist, 132.0m", "triple_list": [ [ "Physical and chemical mica feldspar quartzite", "thickness", "132.0m" ] ] }, { "text": "Gray silver-gray mica quartz schist, 87.7m", "triple_list": [ [ "Gray silver grey mica quartz schist", "thickness", "87.7m" ] ] }, { "text": "The Ordovician strata in the Yunkai strata zone is the Lanwen Group of the Luodong Group of Luohong Group, Luodong Group, and Dongchong Group.", "triple_list": [ [ "Yunkai stratigraphic partition", "Outcrop", "Ordovician strata" ], [ "Ordovician strata", "Outcrop", "Luo Hong Group" ], [ "Ordovician strata", "Outcrop", "Luodong Group" ], [ "Ordovician strata", "Outcrop", "Dongchong Group" ], [ "Ordovician strata", "Outcrop", "Orchid group" ] ] }, { "text": "The Bali Group in the survey area is mainly distributed east of Yangchun-Helang Yun'an Town, and a small area is exposed near the Donghu Reservoir south of Enping, about 233.32m2, accounting for 1.38% of the total area of the survey area.", "triple_list": [ [ "Bali Group", "Exposed", "Yangchun—East from the town of Yun'an, Helang" ], [ "Bali Group", "Exposed", "Near East Lake Reservoir south of Enping" ], [ "Bali Group", "area", "233.32m2" ] ] }, { "text": "Silica carbonite combination, with an off-white striped siliceous rock (particle quartzite) on the upper part, with horizontal stratigraphic texture and sericite distribution along the layer; the lower part is carbonite quartz schist, 51.9m", "triple_list": [ [ "Silicate carbonite combination", "Contained", "Off-white striped siliceous rock (particle quartzite)" ], [ "Silicate carbonite combination", "Contained", "Serimoto" ], [ "Silicate carbonite combination", "Contained", "Carbon mica quartz schist" ], [ "Silicate carbonite combination", "thickness", "51.9m" ], [ "Off-white striped siliceous rock (particle quartzite)", "Develop", "Horizontal stratification" ] ] }, { "text": "Gray medium-thick layered horn lithified fine sandstone, 4m", "triple_list": [ [ "Gray medium-thick layered horn lithified fine sandstone", "thickness", "4m" ] ] }, { "text": "The Tianziling Formation in the survey area is a shallow sea and is a carbonate platform phase deposited.", "triple_list": [ [ "Tianziling Group", "Belongs to", "The shallow sea area is partially deposition of carbonate terraces" ] ] }, { "text": "The lithologies of Chunwan Formation are gray-light grey fine-grain feldspar quartz sandstone calcium alene silt silt silt silt shale silt shale silt silt shale silt silt shale silt silt shale silt silt silt shale silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt", "triple_list": [ [ "Chunwan Group", "Lithology", "Ash - Light grey fine-grained feldspar quartz sandstone" ], [ "Chunwan Group", "Lithology", "Calcium silt sandstone" ], [ "Chunwan Group", "Lithology", "Feldspar quartz siltstone" ], [ "Chunwan Group", "Lithology", "Feldspar quartz sandstone" ], [ "Chunwan Group", "Lithology", "Mud shale" ], [ "Chunwan Group", "Lithology", "Silty shale" ], [ "Chunwan Group", "Lithology", "Slate" ], [ "Chunwan Group", "Lithology", "Calcium silt sandstone" ], [ "Chunwan Group", "Lithology", "Calcium or silt mudstone" ], [ "Chunwan Group", "Lithology", "Siltstone" ], [ "Chunwan Group", "Contained", "Iron mud nodules" ], [ "Chunwan Group", "Develop", "Horizontal stratification" ] ] }, { "text": "Gray-white light gray sheets of physical and chemical black cloud oblique length-grained rocks intersected with thin layer of quartz black mica schist, 80.8m —————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Gray white light gray sheet physical and chemical black cloud oblique length variable grain rock with thin layer of quartz black mica schist", "thickness", "80.8m" ], [ "Gray white light gray sheet physical and chemical black cloud oblique length variable grain rock with thin layer of quartz black mica schist", "Integration of contacts", "The first group of Yunkai Group" ], [ "The first group of Yunkai Group", "Lithology", "Gray-green quartz mica tablets" ] ] }, { "text": "The upper part of the Daganshan Formation is mainly gray-black striped mica quartz schist, white and gray-black striped carbonaceous quartzite and sheet-shaped particulate quartzite. The lower gray-black carbon sericite thousand rocks and the strip-shaped pyrite layer were interlayered (the upper part was mainly pyrite and particulate quartzite), and a small amount of volcanic tuff material was found in the Pengshi-Benggang area, >216m", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray-black striped mica quartz schist" ], [ "Dakanshan Group", "Lithology", "White and gray-black striped carbonaceous particles quartzite" ], [ "Dakanshan Group", "Lithology", "Flake-like quartzite" ], [ "Dakanshan Group", "Contained", "Off-white siliceous rock" ], [ "Dakanshan Group", "Lithology", "Gray-black charcoal sericite thousand rock" ], [ "Dakanshan Group", "Lithology", "Striped pyrite layer" ], [ "Dakanshan Group", "Lithology", "Pyrite" ], [ "Gray-black charcoal sericite thousand rock", "thickness", ">216m" ], [ "Striped pyrite layer", "thickness", ">216m" ], [ "Pyrite", "Contained", "Particular quartzite" ], [ "Volcanic tuff material", "Located at", "Pengshi-Benggang area" ] ] }, { "text": "The lithology of the Shuishi Formation is layered metamorphic sandstone metamorphic siltstone Qianmei Rocks Siltstone silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt silt", "triple_list": [ [ "Water stone group", "Lithology", "Laminated metamorphic sandstone" ], [ "Water stone group", "Lithology", "Metamorphic siltstone" ], [ "Water stone group", "Lithology", "Qianmeiyan" ], [ "Water stone group", "Lithology", "Silty slab" ], [ "Water stone group", "Lithology", "Slate" ], [ "Water stone group", "Lithology", "Carbon-containing thousand rocks" ], [ "Water stone group", "Develop", "Horizontal stratification" ] ] }, { "text": "The second group of Yunkai Group was in parallel and unconformal contact with the conglomerate at the bottom of Daganshan Formation, and the lower part was in integrated contact with the marble or calcareous siltstone at the top of the first group of Yunkai Group, with a total thickness of >1343m.", "triple_list": [ [ "The second group of Yunkai Group", "Unconformity contact", "The gravel at the bottom of the Daganshan Formation" ], [ "The second group of Yunkai Group", "thickness", "Total thickness >1343m" ], [ "The second group of Yunkai Group", "Integration of contacts", "Top of the first group of Yunkai Group" ], [ "Top of the first group of Yunkai Group", "Lithology", "Dali Rock" ], [ "Top of the first group of Yunkai Group", "Lithology", "Calcium siltstone" ] ] }, { "text": "1:25 million Yangchun County Survey Area is located in the hinterland of Yunkai Mountain in western Guangdong, with the West River to the north, Guangxi to the west, the Pearl River Delta to the east, and the Yangjiang City to the south.", "triple_list": [ [ "Yangchun County Survey Area", "Located at", "The mountains are blooming in western Guangdong" ], [ "Yangchun County Survey Area", "Located at", "Xijiang" ], [ "Yangchun County Survey Area", "Located at", "Guangxi" ], [ "Yangchun County Survey Area", "Located at", "Pearl River Delta" ], [ "Yangchun County Survey Area", "Located at", "Yangjiang City" ] ] }, { "text": "Hepu Group, not seen its peak, with a thickness of 343m.", "triple_list": [ [ "Hepu Group", "thickness", "343m" ] ] }, { "text": "Based on this, the era of the Kengping Xibi-horn porphyry system was placed in the Sinian period. The Leiominuscula minute-Leiopsophospaera minor group of biological strata was built by Nanyi (1993). Currently, 37 genera and 93 species of micro-params have been collected in the Yunkai Group strata.", "triple_list": [ [ "Kengping Xibi-angle porphyry system", "Age", "Zhendan" ], [ "Kengping Xibi-angle porphyry system", "Paleontological", "Leiominuscula minuteta — Leiopsphospaera minor combination" ] ] }, { "text": "The Shangbali Formation in the area is mainly composed of gray, gray-green medium-thick layered metamorphic (feldspar) quartz sandstone and metamorphic siltstone in the Zhen'an area of Yunfu. The metamorphic sandstone in the south to Yangchun has significantly decreased, with the lithology of gray-green mica quartz schist and Qianmei rock interlayered with metamorphic sandstone; while the lithology of the Enping-Yangjiang Xinzhou area of Dongjiang Stratigraphic Zone is gray metamorphic siltstone and Qianmei rock interlayered with metamorphic sandstone, thin layers of quartzite, quartz mica schist and gray-black carbon-containing thousand rocks.", "triple_list": [ [ "Bali Group", "Located at", "Yunfu Zhen'an area" ], [ "Bali Group", "Lithology", "Ash, gray-green medium-thick layered metamorphic (feldspar) quartz sandstone" ], [ "Bali Group", "Lithology", "Metamorphic siltstone" ], [ "Bali Group", "Contained", "Mica quartz schist" ], [ "Bali Group", "Contained", "Qianmeiyan" ], [ "Bali Group", "Contained", "Silicone rock" ], [ "Bali Group", "Located at", "spring" ], [ "Bali Group", "Lithology", "Ash, gray-green mica quartz schist" ], [ "Bali Group", "Lithology", "Qianmeiyan" ], [ "Bali Group", "Contained", "Metamorphic Sandstone" ], [ "Bali Group", "Stratigraphical zoning", "Dongjiang" ], [ "Bali Group", "Located at", "Enping-Yangjiang Xinzhou Area" ], [ "Bali Group", "Lithology", "Gray metamorphic siltstone" ], [ "Bali Group", "Lithology", "Qianmeiyan" ], [ "Bali Group", "Contained", "Metamorphic Sandstone" ], [ "Bali Group", "Contained", "Thin layer of quartzite" ], [ "Bali Group", "Contained", "Quartz mica schist" ], [ "Bali Group", "Contained", "Gray-black charcoal-containing thousand rocks" ] ] }, { "text": "The horizontal stratigraphic micro-stratigraphic Develop of Dagangding Formation, and mudstone generally contains 12% carbon.", "triple_list": [ [ "Dagang Ding Group", "Develop", "Horizontal stratification" ], [ "Dagang Ding Group", "Develop", "Microstructure" ], [ "Dagang Ding Group", "Lithology", "Mudstone" ] ] }, { "text": "Lianxian Formation is a set of carbonate rocks mainly deposited by dolomite, with huge thickness, paleontology in the rocks are less developed, only some coral fossils appear, and the sedimentary structure is not developed, and only a small number of bird's eye structures are seen.", "triple_list": [ [ "Lianxian Group", "Belongs to", "Carbonate sedimentation mainly in dolomite" ], [ "Lianxian Group", "Paleontological", "Corals" ], [ "Lianxian Group", "Develop", "Bird's eye structure" ] ] }, { "text": "Metamorphic coarse basal rock with variable residual pores and almond structure, 0.8m", "triple_list": [ [ "Metamorphic coarse basal rock", "Develop", "Change residual air hole" ], [ "Metamorphic coarse basal rock", "Develop", "Almond structure" ], [ "Metamorphic coarse basal rock", "thickness", "0.8m" ] ] }, { "text": "The lower part of the Daganshan Formation is characterized by gray-black strip mica thousand rocks with volcanic rock pyrite layer and limestone lens body siliceous rock. The middle part is a rhythmic layer composed of quartzite mica quartz schist and quartz mica schist, with a top of which is a dolomite lens body containing phosphorus.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray-black striped mica thousand rock" ], [ "Dakanshan Group", "Contained", "Volcanic pyrite strata" ], [ "Dakanshan Group", "Contained", "Limestone lens body siliceous rock" ], [ "Dakanshan Group", "Lithology", "Quartzite Mica Quartz Schist" ], [ "Dakanshan Group", "Lithology", "Quartz mica schist" ], [ "Dakanshan Group", "Contained", "Phosphorus-containing dolomite lens body" ] ] }, { "text": "Yellow-brown thin-layer mica feldspar quartzite and black mica schist interlayer, grey-green-gray black magnetite Yangqi petrified garnet skarn, 76.6m", "triple_list": [ [ "Yellow-brown thin layered mica feldspar quartzite", "thickness", "76.6m" ], [ "Mica schist", "thickness", "76.6m" ], [ "Grey-green-grey black magnetite Yangqi petrified garnet skarn", "thickness", "2.7m" ] ] }, { "text": "Liujiang Group, total thickness >547m", "triple_list": [ [ "Liujiang Group", "thickness", "547m" ] ] }, { "text": "Gray light yellow black clouds with red columns, 19.0m —————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Gray light yellow with black clouds and red columns oblique curtain stone horn rock", "thickness", "19.0m" ], [ "Gray light yellow with black clouds and red columns oblique curtain stone horn rock", "Integration of contacts", "Luo Hong Group" ], [ "Luo Hong Group", "Lithology", "Light gray spotted black cloud red pillar stone horn rock" ], [ "Luo Hong Group", "Lithology", "Horned lithified sandstone" ] ] }, { "text": "The Luohong Group in the survey area is mainly distributed in the northwest of Yangchun Basin and the north of Jinzhu Town in Guangxi, with an exposed area of 257.46m2, accounting for 1.52% of the total area of the survey area.", "triple_list": [ [ "Luo Hong Group", "Exposed", "Northwest Yangchun Basin" ], [ "Luo Hong Group", "Exposed", "Guangxi Fengzhu Town North" ], [ "Luo Hong Group", "area", "257.46m2" ] ] }, { "text": "Gray-white gray-green thin-layer mica quartzite with mica schist, horizontal stratigraphic Develop, 502.2m", "triple_list": [ [ "Gray white gray-green thin layered mica quartzite", "Contained", "Mica schist" ], [ "Gray white gray-green thin layered mica quartzite", "Develop", "Horizontal stratification" ], [ "Gray white gray-green thin layered mica quartzite", "thickness", "502.2m" ] ] }, { "text": "Gray black yellow white mica quartz schist, 56.2m", "triple_list": [ [ "Gray black yellow white mica quartz schist", "thickness", "56.2m" ] ] }, { "text": "Yellow-white giant thick layer—medium-thick layered fine-grained sandstone and gray thin-layered mudstone interlayered with gray black thin-layered siliceous rock, 134.63m", "triple_list": [ [ "Yellow-white giant thick layer—medium-thick layered fine-grained sandstone and gray thin-layered mudstone interlayered with gray black thin-layered siliceous rock", "thickness", "134.63m" ] ] }, { "text": "Gray medium-thin layered fine-grained metamorphic sandstone interspersed with thin-layered Qianmei rock, 63.47m", "triple_list": [ [ "Gray medium-thin layered fine-grained metamorphic sandstone interspersed with thin-layered thousand rocks", "thickness", "63.47m" ] ] }, { "text": "Dongchong Formation was in fault contact with the Lanwen Formation in Kuidong area in Yunan, Guangdong, while Guangxi Fengzhu was in integrated contact with the Lower Fuluodong Formation and the Overly Overlapping Orchid Formation, with a thickness of 241m.", "triple_list": [ [ "Dongchong Group", "Exposed", "Kui Cave, Yunan, Guangdong" ], [ "Dongchong Group", "Fault contact", "Orchid group" ], [ "Dongchong Group", "Exposed", "Guangxi glutinous rice dumplings" ], [ "Dongchong Group", "Integration of contacts", "Luodong Group" ], [ "Dongchong Group", "Integration of contacts", "Orchid group" ], [ "Dongchong Group", "thickness", "241m" ] ] }, { "text": "The second group of Yunkai Group is widely distributed in the Luoding-Xinyi-Yangchun area, about 697.28m2, accounting for 4.12% of the total area of the survey area. The lithologies are gray, gray-black, gray-green metamorphic siltstone, metamorphic feldspar quartz sandstone, mica quartz schist, quartz mica schist, serous schist, and serous thousand rock, intersecting with multiple layers of gray-black carbon quartz serous kilogram, siliceous rock, and manganese-containing quartz schist.", "triple_list": [ [ "The second group of Yunkai Group", "Located at", "Luoding-Xinyi-Yangchun Area" ], [ "The second group of Yunkai Group", "thickness", "About 697.28m2" ], [ "The second group of Yunkai Group", "Lithology", "Ash, gray-black, gray-green metamorphic siltstone" ], [ "The second group of Yunkai Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "The second group of Yunkai Group", "Lithology", "Mica quartz schist" ], [ "The second group of Yunkai Group", "Lithology", "Quartz mica schist" ], [ "The second group of Yunkai Group", "Lithology", "Thousands of silky rocks" ], [ "The second group of Yunkai Group", "Contained", "Multi-layer gray-black carbon quartz sericite thousand rock" ], [ "The second group of Yunkai Group", "Contained", "Silicone rock" ], [ "The second group of Yunkai Group", "Contained", "Manganese-containing quartz schist" ] ] }, { "text": "Gray white dark gray metamorphic feldspar quartz sandstone, thick layered, horizontally layered, 152.7m", "triple_list": [ [ "Gray white dark gray metamorphic feldspar quartz sandstone", "Develop", "Horizontal stratification" ], [ "Gray white dark gray metamorphic feldspar quartz sandstone", "thickness", "152.7m" ] ] }, { "text": "Gray medium-thick layered fine-grained metamorphic sandstone with Qianmei rock, 111.60m", "triple_list": [ [ "Gray medium-thick layered fine-grained metamorphic sandstone intersects Qianmei rock", "thickness", "111.60m" ] ] }, { "text": "Lianxian Formation is a set of gray, dark, gray, gray, black medium and thick layers - thick layered dolomite limestone and dolomite, intersecting gray, black argillite limestone.", "triple_list": [ [ "Lianxian Group", "Lithology", "Gray dark gray gray black medium-thick layer-thick layer dolomite limestone" ], [ "Lianxian Group", "Lithology", "Dolomite" ], [ "Lianxian Group", "Lithology", "Gray-black mud limestone" ] ] }, { "text": "The basic stratigraphy sequence of the Hepu Formation consists of fine sandstone siltstone and mudstone, and develops horizontal stratigraphy, and there are common obvious erosion surfaces between the basic stratigraphy sequences.", "triple_list": [ [ "Hepu Group", "Lithology", "Fine sandstone" ], [ "Hepu Group", "Lithology", "Siltstone" ], [ "Hepu Group", "Lithology", "Mudstone" ] ] }, { "text": "The section of the Luoyi-Tongguping in the Yunkai Group is seen in the second group of the Yunkai Group, Jiayangqi stone and Ying'an porphyry.", "triple_list": [ [ "The second group of Yunkai Group", "Contained", "Yangqi stone green curtain stone rock" ], [ "The second group of Yunkai Group", "Contained", "Ying'an Porphyry" ] ] }, { "text": "The Daganshan Formation contains a large number of micropaleophyte fossils, with a total of 34 genera and 80 species. The main ones are Leiopsophosphaera, rachysphaeradium, Asperotopsophosphaera, Pseudozonosphaera and Leiofusa have significantly increased, and new species such as Orygmatosphaera, Arctacellularia, Hubeiisphaera have appeared. The geological era is more likely to Belongs to to the South China Age. The age value of sedimentary zircon in this group of variogranular feldspar quartzite was 778267828 Ma. Therefore, the era of this group in the investigation area should Belongs to to the South China Age, and its strata is the South China Age.", "triple_list": [ [ "Dakanshan Group", "Paleontological", "Leiopsophosphaera" ], [ "Dakanshan Group", "Paleontological", "rachysphaeridium" ], [ "Dakanshan Group", "Paleontological", "Asperatopsophosphaera" ], [ "Dakanshan Group", "Paleontological", "Pseudozonosphaeridium" ], [ "Dakanshan Group", "Paleontological", "Orygmatosphaeridium" ], [ "Dakanshan Group", "Paleontological", "Arctacialularia" ], [ "Dakanshan Group", "Paleontological", "Hubeisphaera" ], [ "Dakanshan Group", "Age", "Nanhuaji" ] ] }, { "text": "Thin layered quartz mica microschist, 66.4m", "triple_list": [ [ "Thin layered quartz mica microschist", "thickness", "66.4m" ] ] }, { "text": "Light yellowish gray-green medium-thin layered horn lithologized silty sandy mudstone, 32m", "triple_list": [ [ "Light yellowish gray-green medium-thin layered horn lithologized silt sandy mudstone", "thickness", "32m" ] ] }, { "text": "Water stone group refers to a set of complex quartz composed of sandstone slate", "triple_list": [ [ "Water stone group", "Belongs to", "Sandstone slate" ] ] }, { "text": "Flaky quartzite and mica quartz schist interlayer, 107.8m", "triple_list": [ [ "Flaky quartzite and mica quartz schist interlayer", "thickness", "107.8m" ] ] }, { "text": "Depositional structures such as the granule sequence stratigraphic stratigraphic stratigraphic mini-interleaved stratigraphic stratigraphic bottom erosion structure of Lianhuashan Formation.", "triple_list": [ [ "Lotus Mountain Group", "Develop", "Granular Sequence Laminating" ], [ "Lotus Mountain Group", "Develop", "Inclined layering" ], [ "Lotus Mountain Group", "Develop", "Mini-interleaved hierarchy" ], [ "Lotus Mountain Group", "Develop", "Wedge-shaped stratigraphy" ], [ "Lotus Mountain Group", "Develop", "Bottom erosion structure" ] ] }, { "text": "Gray-white gray-green mica quartz schist with flaky quartzite, flat layer, 145.2m", "triple_list": [ [ "Gray-white gray-green mica quartz schist slit quartz rock", "thickness", "145.2m" ] ] }, { "text": "Hepu Formation (S2h) refers to a set of strata integrated between Fangcheng Formation and the ancient tomb Formation. It has relatively single lithologies and is a set of fine clastic rock combinations such as muddy siltstone mudstone and quartz sandstone. It has the characteristics of quartet or quartetite. It is found in the north of Guiyi Town, with an exposed area of 35.99m2, accounting for 0.21% of the total area of the survey area.", "triple_list": [ [ "Hepu Group", "Integration of contacts", "Fangcheng Group" ], [ "Hepu Group", "Integration of contacts", "Ancient Tomb Group" ], [ "Hepu Group", "Lithology", "Mud siltstone" ], [ "Hepu Group", "Lithology", "Mudstone" ], [ "Hepu Group", "Lithology", "Quartz sandstone" ], [ "Hepu Group", "Lithology", "Fine clastic rock" ], [ "Hepu Group", "Develop", "Resolution" ], [ "Hepu Group", "Develop", "Compound quartz" ], [ "Hepu Group", "Exposed", "Guiyi Town North" ], [ "Hepu Group", "area", "35.99m2" ] ] }, { "text": "The above shows that the Daganshan Formation in the survey area is a semi-deep sea sedimentary environment with a relatively warm climate.", "triple_list": [ [ "Dakanshan Group", "Belongs to", "Semi-deep oceanic sedimentary environment" ] ] }, { "text": "The survey area is distributed in the areas of Yangchun Guigang River mouth-Tangping Xinxing Jinzhu-Dajiang Luoding Chuanbu Nanjiayi and Cenxi Jinzhu-Yunnantongmen to Pingjinjiang Reservoir, west of Kaiping Longsheng En, Kaiping. The exposed area is relatively large, about 1020.04m2, accounting for 6.03% of the total area of the survey area.", "triple_list": [ [ "Investigation Area", "Located at", "Kaiping Longshengen Pingjinjiang Reservoir west of Yangchun Guigang River Estuary-Tangping Xinxing Jinzhu-Dajiang Luoding Chuanbu Nanjiayi and Cenxi Jinzhu-Yunnantongmen" ], [ "Investigation Area", "area", "1020.04m2" ] ] }, { "text": "The era of Luodong Group was tentatively set to be the Central Ordovician.", "triple_list": [ [ "Luodong Group", "Age", "Central Ordovician" ] ] }, { "text": "Gray metamorphic silt sandstone with purple-red thousand rocks and green sheets of physical, chemical metamorphic fine sandstone, 191.32m", "triple_list": [ [ "Gray metamorphic silt sandstone intersected with purple-red thousand rocks and green sheets of physical and chemical metamorphic fine sandstone", "thickness", "191.32m" ] ] }, { "text": "The Bali Formation in the survey area is mainly fine sandstone, mixed with silt sandstone mudstone, partially mixed with silty rocks and carbon-containing layers, with horizontal lamellar texture and rich in pyrite microcrystals. The above indicates that the Bali in the survey area should be deep-sea sedimentation.", "triple_list": [ [ "Bali Group", "Lithology", "Fine sandstone" ], [ "Bali Group", "Lithology", "Siltstone" ], [ "Bali Group", "Lithology", "Mudstone" ], [ "Bali Group", "Lithology", "Silicone rock" ], [ "Bali Group", "Lithology", "Carbon-containing layer" ], [ "Bali Group", "Develop", "Horizontal stratification" ], [ "Bali Group", "Develop", "Laminating" ], [ "Bali Group", "Contained", "Pyrite crystal" ], [ "Bali Group", "Belongs to", "Deep-sea phase sedimentation" ] ] }, { "text": "Gray-green thin layer of calcareous mudstone and gray-black thin layer of carbonaceous mudstone, 45.16m", "triple_list": [ [ "Gray-green thin layer of calcareous mudstone and gray-black thin layer of carbonaceous mudstone interlayer", "thickness", "45.16m" ] ] }, { "text": "Overlapping strata Liantan Formation, containing mud powder-fine sandstone intersected with thin layered mudstone, locally intersected with unequal grained sandstone —————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Liantan Group", "Lithology", "Mud powder - fine sandstone" ], [ "Liantan Group", "Lithology", "Thin layered mudstone" ], [ "Liantan Group", "Lithology", "Unequal sandstone" ], [ "Liantan Group", "Integration of contacts", "Ancient Tomb Group" ], [ "Liantan Group", "thickness", "543m" ] ] }, { "text": "Liantan Group, thickness >224.30m", "triple_list": [ [ "Liantan Group", "thickness", "224.30m" ] ] }, { "text": "The second group of Yunkai Group, not seen the peak, the total thickness is >2703.3m", "triple_list": [ [ "The second group of Yunkai Group", "thickness", "2703.3m" ] ] }, { "text": "The Yangchun County Survey Zone can be roughly divided into three stratigraphic zones. The northwest part of the Luoding-Guangning Fault Zone (i.e. the northeast corner of the survey area) is the southeast part of the Guizhou stratigraphic zone, and the southeast part of the newly emerging duplex rock foundation is the Dongjiang stratigraphic zone, and the range between them is classified as the Yunkai stratigraphic zone.", "triple_list": [ [ "Yangchun County Survey District", "Stratigraphical zoning", "Three strata partitions" ] ] }, { "text": "The most species were obtained in the Tiger Tang Group, mainly containing Leiominuscula (Glossy Chlorella), Leiopsophosphaera (Chlorella), rachysphaera (Closy Chlorella), rachysphaera (Closy Chlorella).", "triple_list": [ [ "Tiger Pond Group", "Paleontological", "Leiominuscula (Chlorella glossy)" ], [ "Tiger Pond Group", "Paleontological", "Leiopsophosphaera (Chlorophylla)" ], [ "Tiger Pond Group", "Paleontological", "rachysphaeridium (Rhodge Sphereus)" ], [ "Tiger Pond Group", "Paleontological", "rachysphaeridium (Groups)" ] ] }, { "text": "Acid tuff found in Jingwei-Benggang area, >282m", "triple_list": [ [ "Acid tuff", "thickness", ">282m" ], [ "Acid tuff", "Located at", "Shiwei-Benggang area" ] ] }, { "text": "The main lithologies of the Daganshan Formation are quartz mica schist, mica quartz schist, metamorphic quartz sandstone, metamorphic feldspar quartz sandstone, metamorphic siltstone, quartzite with black carbonaceous kilogram, off-white siliceous rock, (manganese) limestone, tuff and pyrite layers. The bottom is marked by the gray-white conglomerate, which is in parallel and unconformal contact with the second group of the underlying Yunkai Group, and the top is in integrated contact with the overlying Bali Formation, with a thickness of 890~1508m.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Quartz mica schist" ], [ "Dakanshan Group", "Lithology", "Mica quartz schist" ], [ "Dakanshan Group", "Lithology", "Metamorphic quartz sandstone" ], [ "Dakanshan Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "Dakanshan Group", "Lithology", "Metamorphic siltstone" ], [ "Dakanshan Group", "Lithology", "Quartzite" ], [ "Dakanshan Group", "Lithology", "Off-white siliceous rock" ], [ "Dakanshan Group", "Lithology", "(Manganese) Limestone" ], [ "Dakanshan Group", "Lithology", "Tuff" ], [ "Dakanshan Group", "Lithology", "Pyrite layer" ], [ "Dakanshan Group", "Lithology", "Off-white gravel" ], [ "Dakanshan Group", "Unconformity contact", "The second group of the underworld clouds" ], [ "Dakanshan Group", "Integration of contacts", "Overlapping Bali Group" ], [ "Dakanshan Group", "thickness", "890~1508m" ], [ "Quartzite", "Contained", "Black carbon thousand rock" ] ] }, { "text": "The second group of Yunkai Group is a thin layered cross-shaped quartz schist in the Gaodong area of Wangsha.", "triple_list": [ [ "The second group of Yunkai Group", "Located at", "Wangsha Gaodong area" ], [ "The second group of Yunkai Group", "Lithology", "feldspar mica quartz schist" ], [ "feldspar mica quartz schist", "Contained", "Medium-thin layered cruciate mica quartz schist" ] ] }, { "text": "The first group of Yunkai Group is mainly composed of metamorphic feldspar quartz sandstone mica quartz schist and quartz mica schist garnet quartz schist quartz schist quartzite (siliceous rock), interlayer, translucent dioprene rock, metamorphic matrix volcanic rock, magnetite skarn strip magnetite layer, pyrite lens body phosphate layer and dolomite marble (manganite) marble, etc.", "triple_list": [ [ "The first group of Yunkai Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "The first group of Yunkai Group", "Lithology", "Mica quartz schist" ], [ "The first group of Yunkai Group", "Lithology", "Quartz mica schist" ], [ "The first group of Yunkai Group", "Lithology", "Garnet Quartz Mica Schist" ], [ "The first group of Yunkai Group", "Lithology", "Quartzite" ], [ "The first group of Yunkai Group", "Lithology", "Silicone rock" ], [ "The first group of Yunkai Group", "Lithology", "Yangqishishishishishidilucent rock" ], [ "The first group of Yunkai Group", "Lithology", "Yangqi stone green curtain stone rock" ], [ "The first group of Yunkai Group", "Lithology", "Metamorphic material volcanic rocks" ], [ "The first group of Yunkai Group", "Lithology", "Magnetite skarn" ], [ "The first group of Yunkai Group", "Lithology", "Strip magnetite layer" ], [ "The first group of Yunkai Group", "Lithology", "Pyrite lens body phosphate layer" ], [ "The first group of Yunkai Group", "Lithology", "Baiyun marble" ], [ "The first group of Yunkai Group", "Lithology", "(Contains manganese) Marble" ] ] }, { "text": "Yellow-brown medium-thick layered muddy siltstone and light gray-red thick layered mudstone (bottom not seen), 132.31m", "triple_list": [ [ "Yellow-brown medium-thick layered muddy siltstone and light gray-red thick layered mudstone", "thickness", "132.31m" ] ] }, { "text": "The Dagangding Group has a horizontal layered intertwined layered texture layered structure.", "triple_list": [ [ "Dagang Ding Group", "Develop", "Horizontal stratification" ], [ "Dagang Ding Group", "Develop", "Interleaved hierarchy" ], [ "Dagang Ding Group", "Develop", "Laminated structure" ] ] }, { "text": "The Liantan Group in the survey area should Belongs to to the Early Silurian system.", "triple_list": [ [ "Liantan Group", "Age", "Early Shiliu system" ] ] }, { "text": "The upper part of the Daganshan Formation is composed of feldspar quartz sandstone and sericaceous shale. The top of it is limestone lens body or calcare siltstone. The basic stratigraphic sequence is rhythmic deposition composed of sand-silt-silt-silt.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Feldspar quartz sandstone" ], [ "Dakanshan Group", "Lithology", "sericaceous shale" ], [ "Dakanshan Group", "Lithology", "Limestone lens body" ], [ "Dakanshan Group", "Lithology", "Calcium siltstone" ], [ "Dakanshan Group", "Lithology", "Sand-silt-mill" ] ] }, { "text": "The upper part of the Daganshan Formation: brown-yellow, light gray-green, gray-white quartzite intersected with blue-gray, gray-white, gray-black thin-layered sericite kilograms, and gray-green, gray-black striped quartzite intersected with gray-green, gray-black striped quartzite intersected with gray-green and gray-black striped quartzite.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Brown yellow, light gray green, off-white quartz rock" ], [ "Dakanshan Group", "Contained", "Blue-gray, gray-white, gray-black thin-layer sericite thousand rocks" ], [ "Dakanshan Group", "Contained", "Gray-green, gray-black striped quartz rock" ] ] }, { "text": "The Lanwen Formation and the upper Devonian strata and the Cretaceous red pot of the Lower Fu Dongchong Formation are both in fault contact, with a thickness of about 1096m.", "triple_list": [ [ "Orchid group", "Fault contact", "Dongchong Group" ], [ "Orchid group", "Fault contact", "Devonian strata" ], [ "Orchid group", "Fault contact", "Cretaceous Red Basin" ], [ "Orchid group", "thickness", "1096m" ] ] }, { "text": "Overlapping Xindu Formation, light yellow white thick layer of blocky fine-grained quartz sandstone and silt sandstone——————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Xindu Group", "Lithology", "Light yellow white thick layer of blocky fine-grained quartz sandstone with silt sandstone" ], [ "Xindu Group", "Integration of contacts", "Lotus Mountain Group" ], [ "Lotus Mountain Group", "thickness", "542m" ] ] }, { "text": "From the above lithophagocytic characteristics analysis, the sedimentary environment of Lianxian Formation is the tidal environment of the carbonate platform.", "triple_list": [ [ "Lianxian Group", "Belongs to", "Carbonate platform tide environment" ] ] }, { "text": "Local sandstones show horizontal strata and staggered strata Develop.", "triple_list": [ [ "sandstone", "Develop", "Horizontal stratification" ], [ "sandstone", "Develop", "Inclined layering" ], [ "sandstone", "Develop", "Interleaved hierarchy" ] ] }, { "text": "The lower part is blue-gray gray-white light gray-thin-medium-thick layered quartzite and dolomite quartzite and blue-gray sericite kilogram rock, 90m————parallel and unconsolidation————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "The lower part of the blue-gray gray-white light gray-thin color-medium-thick layered quartzite and dolomite quartzite interlayered ceratops and ceratops of the blue-gray sericite thousand rocks", "thickness", "90m" ], [ "The lower part of the blue-gray gray-white light gray-thin color-medium-thick layered quartzite and dolomite quartzite interlayered ceratops and ceratops of the blue-gray sericite thousand rocks", "Integration of contacts", "The second group of Yunkai Group" ], [ "The second group of Yunkai Group", "Lithology", "Cross stone" ], [ "The second group of Yunkai Group", "Lithology", "Garnet" ], [ "The second group of Yunkai Group", "Lithology", "Quartz dimica schist" ], [ "The second group of Yunkai Group", "Lithology", "Garnet" ], [ "The second group of Yunkai Group", "Lithology", "Mica granular rock" ], [ "The second group of Yunkai Group", "Lithology", "Mica granule rock" ] ] }, { "text": "The sedimentary environment of the Xindu Formation is shallow sea and land sheds.", "triple_list": [ [ "Xindu Group", "Belongs to", "Shallow sea and land sheds" ] ] }, { "text": "Off-white striped siliceous rock (particle quartzite), horizontally layered, 17.9m", "triple_list": [ [ "Off-white striped siliceous rock (particle quartzite)", "Develop", "Horizontal stratification" ], [ "Off-white striped siliceous rock (particle quartzite)", "thickness", "17.9m" ] ] }, { "text": "Gray medium-thick layered, porphyry black cloud red column horn rocks included in the angle lithified fine medium-grained quartz mixed sandstone, with horizontal stratigraphic micro-layering, 201m", "triple_list": [ [ "Gray medium-thick layered porphyry black cloud red pillar horn rocks in the angle lithified fine medium-grained quartz sandstone", "Develop", "Horizontal stratification" ], [ "Gray medium-thick layered porphyry black cloud red pillar horn rocks in the angle lithified fine medium-grained quartz sandstone", "Develop", "Microstructure" ], [ "Gray medium-thick layered porphyry black cloud red pillar horn rocks in the angle lithified fine medium-grained quartz sandstone", "thickness", "201m" ] ] }, { "text": "The lower part of the Daganshan Formation is blue-gray, gray-white, light gray-thin colored thin-medium-thick layered quartzite and dolomite quartzite with blue-gray sericite thousand rocks, local interlayer conglomerate, 90m", "triple_list": [ [ "Dakanshan Group", "Lithology", "Blue-gray, gray-white, light gray-thick layered quartzite" ], [ "Dakanshan Group", "Lithology", "Mica Quartzite" ], [ "Dakanshan Group", "Contained", "Blue-gray sericite thousand rocks" ], [ "Dakanshan Group", "Contained", "Interlayer gravel" ], [ "Blue-gray, gray-white, light gray-thick layered quartzite", "thickness", "90m" ] ] }, { "text": "The Laohutang Formation is mainly composed of the basic strata of fine sandstone-siltstone-milestone-milestone, which are interspersed with siliceous rocks and carbonaceous layers. They are mostly thin-layered and horizontally layered. The siliceous rocks are light in color, thin-layered or striped sandwiched in mudstone, and are rich in pyrite microcrystals. The above indicates that the Laohutang Formation in the investigation area should Belongs to to deep-sea current sedimentation.", "triple_list": [ [ "Tiger Pond Group", "Lithology", "Fine sandstone-siltstone-milestone" ], [ "Tiger Pond Group", "Lithology", "Silicone rock" ], [ "Tiger Pond Group", "Contained", "Carbon layer" ], [ "Tiger Pond Group", "Distribution pattern", "Thin layered" ], [ "Tiger Pond Group", "Develop", "Horizontal layering" ], [ "Silicone rock", "Distribution pattern", "Thin layered or striped" ], [ "Silicone rock", "Lithology", "Pyrite crystal" ], [ "Mudstone", "Contained", "Silicone rock" ], [ "Tiger Pond Group", "Belongs to", "Deep sea-current sedimentation" ] ] }, { "text": "Gray medium-thick layered fine-grained sandstone with light gray medium-thin layered mudstone, 20.51m", "triple_list": [ [ "Gray medium-thick layered fine-grained sandstone with light gray medium-thin layered mudstone", "thickness", "20.51m" ] ] }, { "text": "Gray-green green curtain stone tremolite quartz schist and magnetite-containing diopterolite garnet skarn 24.0m", "triple_list": [ [ "Gray-green green tremolite quartz schist and magnetite-containing diopterolite garnet skall", "thickness", "24.0m" ] ] }, { "text": "Magnetite containing Yangqi Petrochemical Dioplastic and Dioplastic Garnet Sikarn, 18.0m", "triple_list": [ [ "Magnetite containing Yangqi Petrochemical Dioplastic and Dioplastic Garnet Sika", "thickness", "18.0m" ] ] }, { "text": "It is more likely that the era belongs to the late Sedan period, and the isochronous age value was obtained in the top siliceous rocks of this group, which is 6123Ma. Therefore, the era of the Laohutang Formation in the investigation area should be the late Sedan period, and the corresponding strata is the upper Sedan period.", "triple_list": [ [ "Tiger Pond Group", "Age", "Late Zhendan" ] ] }, { "text": "Gray-green thin-layer sheet physical and chemical mica microschist with tremolite green curtain stone horn rock, 135.3m", "triple_list": [ [ "Physical and chemical mica microschist with gray-green thin-layer flakes", "thickness", "135.3m" ] ] }, { "text": "Gray thin layered metamorphic silt sandstone with gray-black thin layered Qianmei rock, 82.07m", "triple_list": [ [ "Gray thin layered metamorphic silt sandstone with gray black thin layered Qianmei rock", "thickness", "82.07m" ] ] }, { "text": "Dark gray micro-thin layered silty strip mudstone with silty mudstone, horizontal stratigraphic and strip-like tectonic Develop, Petalolihus hispanicus (Haberfelmer), Spiroptus sp., S. minor Bouce, Streptograptus sp., 488m", "triple_list": [ [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Develop", "Horizontal stratification" ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Develop", "Strip structure" ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Paleontological", "Bishi Petalolihus hispanicus (Haberfelmer)" ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Paleontological", "spirographus sp." ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Paleontological", "S. minor Bouce" ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "Paleontological", "Streptographus sp." ], [ "Dark gray micro-thin layered silty sandy strip mudstone with silty sandy mudstone", "thickness", "488m" ] ] }, { "text": "The middle part of the Daganshan Formation is gray-green, gray-black thin-layered quartz dimica schist, dimica quartz schist and sericca quartz schist.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray-green, gray-black thin-layered quartz dimica schist" ], [ "Dakanshan Group", "Lithology", "Dimica quartz schist" ], [ "Dakanshan Group", "Lithology", "sericca quartz schist" ], [ "Dakanshan Group", "Contained", "Off-white thin layered mica flake quartzite" ] ] }, { "text": "Most of the Yangchun County Survey District belongs to the Yunkai Dashan and Yunwushan Mountains. They form a medium and low mountain terrain that generally runs northwest to southeast, with an average Elevation of about 1,000m. The highest peak is called Datianding and an elevation of 1,704m.", "triple_list": [ [ "Yangchun County Survey District", "Belongs to", "Clouds open up the mountains, clouds and mist mountains" ], [ "Yangchun County Survey District", "Distribution pattern", "Low and medium-mountain terrain in northwest-southeast" ], [ "Yangchun County Survey District", "Elevation", "Average Elevation of 1000m" ], [ "Datianding", "Elevation", "Elevation 1704m" ] ] }, { "text": "The Hutang Formation has a Shizui-Mashan measured profile control in the investigation area. The lower part is a layer of gray-white quartzite and a gray-black thin layer of carbonaceous thousand rocks; the upper part is a quartzite sandwiched thousand rocks, and the bottom is marked by the appearance of a large set of quartzite, which is integrated and in contact with the lower Fubali Formation, but has not been seen.", "triple_list": [ [ "Tiger Pond Group", "Located at", "Shizui-Mashan" ], [ "Tiger Pond Group", "Lithology", "Off-white quartz rock" ], [ "Tiger Pond Group", "Lithology", "Gray-black thin layer contains 1,000 carbonaceous rocks" ], [ "Tiger Pond Group", "Lithology", "Quartzite" ], [ "Tiger Pond Group", "Contained", "Qianmeiyan" ], [ "Tiger Pond Group", "Lithology", "Large set of quartz rock" ], [ "Tiger Pond Group", "Integration of contacts", "Xiafubali Formation" ] ] }, { "text": "The Devonian strata are distributed in Yangchun Xinxing Luoding, Enping, Guangdong and Guiyi Town, Guangxi, etc., and are divided into Yunkai District and Dongjiang District of the Southeast Guizhou District.", "triple_list": [ [ "Devonian strata", "Exposed", "Guangdong Enping Yangchun emerging Luoding" ], [ "Devonian strata", "Exposed", "Guiyi Town, Guangxi" ], [ "Devonian strata", "Stratigraphical zoning", "Guangxi District Yunkai District" ], [ "Devonian strata", "Stratigraphical zoning", "Dongjiang Branch" ] ] }, { "text": "The second group of Yunkai Group is widely distributed in the Luoding-Xinyi-Yangchun area, about 697.28m2, accounting for 4.12% of the total area of the survey area. The lithology is gray-gray-black, gray-green metamorphic siltstone metamorphic feldspar quartz sandstone mica quartz schist quartz schist quartz schist quartz schist schist schist schist schist schist schist schist schist schist schist schist.", "triple_list": [ [ "The second group of Yunkai Group", "Exposed", "Luo Ding-Xinyi-Yangchun" ], [ "The second group of Yunkai Group", "area", "697.28m2" ], [ "The second group of Yunkai Group", "Lithology", "Gray gray black gray green metamorphic siltstone" ], [ "The second group of Yunkai Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "The second group of Yunkai Group", "Lithology", "Mica quartz schist" ], [ "The second group of Yunkai Group", "Lithology", "Quartz mica schist" ], [ "The second group of Yunkai Group", "Lithology", "Thousands of silky rocks" ], [ "The second group of Yunkai Group", "Lithology", "Multi-layer gray-black carbon quartz sericite thousand rock" ], [ "The second group of Yunkai Group", "Lithology", "Silicone rock" ], [ "The second group of Yunkai Group", "Lithology", "Manganese-containing quartz schist" ] ] }, { "text": "The lower part of the Daganshan Formation is gray-brown-yellow flake quartzite, gray-white mica quartzite and blue-gray thin layer of sericite kilograms, and the upper part of the gray cross-schist dimica schist and mica quartz schist. Lower light gray pyrite dioplastic mica potassium feldspar (protolithium contains calcium), metaplaque plagioclase dimica schist, >75m", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray brown yellow flake quartzite" ], [ "Dakanshan Group", "Lithology", "Off-white mica quartzite" ], [ "Dakanshan Group", "Lithology", "Blue-gray thin layer of sericite thousand rock" ], [ "Dakanshan Group", "thickness", ">115m" ], [ "Dakanshan Group", "Lithology", "Gray cross stone dimica schist" ], [ "Dakanshan Group", "Lithology", "Mica quartz schist" ], [ "Dakanshan Group", "Lithology", "Light gray pyrite diopylene mica potassium feldspar rock (protolithium contains calcium)" ], [ "Dakanshan Group", "Lithology", "Dimitral mica schist" ], [ "Dakanshan Group", "thickness", ">75m" ] ] }, { "text": "Tawny metamorphic feldspar quartz sandstone flash gray black quartz mica schist, 52.4m", "triple_list": [ [ "Tawny metamorphic feldspar quartz sandstone flash gray black quartz mica schist", "thickness", "52.4m" ] ] }, { "text": "Physical and chemical mica feldspar quartzite with weathered purple-red layered quartz mica schist, 132.0m", "triple_list": [ [ "Physical and chemical mica feldspar quartzite with weathered purple-red stratified layered quartz mica schist", "thickness", "132.0m" ] ] }, { "text": "Gray yellow-grey-red fine-grained metamorphic sandstone with a small amount of gray-green slate, 16.24m", "triple_list": [ [ "Gray yellow-grey-red fine-grained metamorphic sandstone intersects a small amount of gray-green slate", "thickness", "16.24m" ] ] }, { "text": "The sedimentary environment of the Ordovician period is different, and the Ordovician period in the Dongjiang strata zone is called the Xinchang Formation Hushan Formation.", "triple_list": [ [ "New Factory Group Hushan Group", "Belongs to", "Ordovician strata" ] ] }, { "text": "Gray-white gray-green thin-layer mica quartzite with mica schist, horizontal stratigraphic Develop, 502.2m", "triple_list": [ [ "Gray white gray-green thin layered mica quartzite intersected mica schist", "Develop", "Horizontal stratification" ], [ "Gray white gray-green thin layered mica quartzite intersected mica schist", "thickness", "502.2m" ] ] }, { "text": "Gray-green sheet physical and chemical metamorphic silt sandstone with light purple-red thousand-colored rocks, 77.25m", "triple_list": [ [ "Physical and chemical metamorphic silt sandstone with light purple-red thousand rocks", "thickness", "77.25m" ] ] }, { "text": "Yellow-white, yellow-brown, silver-gray wrinkled mica quartz schist quartz schist quartz schist black mica schist interlayer, 146.3m", "triple_list": [ [ "Yellow-white, yellow-brown, silver-gray wrinkled mica quartz schist quartz schist schist schist interlayer", "thickness", "146.3m" ] ] }, { "text": "The Bali Formation is mainly composed of the basic strata of fine sandstone-siltstone-mudstone, and is partially interspersed with siliceous rocks.", "triple_list": [ [ "Bali Group", "Lithology", "Fine sandstone" ], [ "Bali Group", "Lithology", "Siltstone" ], [ "Bali Group", "Lithology", "Mudstone" ], [ "Bali Group", "Lithology", "Silicone rock" ] ] }, { "text": "Ash-white slate with gray-purple sheets of physical and chemical metamorphic silt sandstone and metamorphic fine sandstone, 41.57m", "triple_list": [ [ "Ash-white slate with gray-purple sheets of physical and chemical metamorphic silt sandstone and metamorphic fine sandstone", "thickness", "41.57m" ] ] }, { "text": "Thick layered sheet of physicochemical mica quartzite, 70.4m thick in the middle, purple-red altered green curtain stone tremolite with a thickness of 156.7m", "triple_list": [ [ "Thick layered sheets of physicochemical mica quartzite", "thickness", "156.7m" ], [ "purple-red altered green curtain stone tremolite", "thickness", "Thickness 70.4m" ] ] }, { "text": "Black shale, 1.0m", "triple_list": [ [ "Black shale", "thickness", "1.0m" ] ] }, { "text": "The first group of Yunkai Group is mainly composed of metamorphic feldspar quartz sandstone, mica quartz schist and quartz mica schist, garnet quartz mica schist, quartzite (siliceous rock), quartzite (siliceous rock), intersecting radialite, yangqi leverite, yangqi leverite, metamorphic matrix volcanic rock, magnetite skarn, strip magnetite layer, pyrite lens body phosphate layer, dolomite marble (manganite) marble, etc.", "triple_list": [ [ "The first group of Yunkai Group", "Lithology", "Metamorphic feldspar quartz sandstone" ], [ "The first group of Yunkai Group", "Lithology", "Mica quartz schist" ], [ "The first group of Yunkai Group", "Lithology", "Quartz mica schist" ], [ "The first group of Yunkai Group", "Lithology", "Garnet Quartz Mica Schist" ], [ "The first group of Yunkai Group", "Lithology", "Quartzite (siliceous rock) interlayers with different thicknesses" ], [ "The first group of Yunkai Group", "Lithology", "Jiayang rock translucent rock" ], [ "The first group of Yunkai Group", "Lithology", "Yangqi stone green curtain stone rock" ], [ "The first group of Yunkai Group", "Lithology", "Metamorphic material volcanic rocks" ], [ "The first group of Yunkai Group", "Lithology", "Magnetite skarn" ], [ "The first group of Yunkai Group", "Lithology", "Strip magnetite layer" ], [ "The first group of Yunkai Group", "Lithology", "Pyrite lens body phosphate layer" ], [ "The first group of Yunkai Group", "Lithology", "Baiyun marble (including manganese) marble" ] ] }, { "text": "Gray-black quartz mica schist with feldspar mica quartz schist, 139.3m", "triple_list": [ [ "Gray-black quartz schist containing carbonaceous quartz schist with feldspar mica quartz schist", "thickness", "139.3m" ] ] }, { "text": "In the Luodingfuhe-Xiangdong area, quartz sericite, quartz mica schist, metamorphic siltstone is mainly mixed with chlorite quartzite, garnet rock, iron manganese layer and ferro-containing chlorite rock.", "triple_list": [ [ "Luo Ding Fuhe-Xiangdong Belt", "Lithology", "Quartz serita" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Lithology", "Quartz mica schist" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Lithology", "Metamorphic siltstone" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Contained", "Green Quartz Rock" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Contained", "Garnet Rock" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Contained", "Iron-manganese layer" ], [ "Luo Ding Fuhe-Xiangdong Belt", "Contained", "Iron-containing chlorite rock" ] ] }, { "text": "The Liantan Group in the survey area was exposed in Huangpo, north of Lantian Chongyu Nanliantan in Guiyi Town, Cenxi, and other places, 21.48m2, accounting for 0.13% of the total area of the survey area.", "triple_list": [ [ "Liantan Group", "Exposed", "North of Guiyi Town, Cenxi" ], [ "Liantan Group", "Exposed", "Huangpo-North of Lantian Chongyu Nanliantan" ], [ "Liantan Group", "area", "21.48m2" ] ] }, { "text": "The gray metamorphic sandstone of the Shuishi Formation in the Dongjiang Formation Zone is the main sandy thousand-metal rock with a thickness of >910m, and it is in integrated contact with the Gaotan Formation.", "triple_list": [ [ "Dongjiang Stratigraphic Zone", "Outcrop", "Water stone group" ], [ "Water stone group", "Lithology", "Gray metamorphic sandstone" ], [ "Water stone group", "Lithology", "Striped sandy rock" ], [ "Water stone group", "thickness", "910m" ], [ "Water stone group", "Integration of contacts", "Gaotan Group" ] ] }, { "text": "Coral fossils were found in the dolomite of Pseudourinia cf. tangpaouensis Yü, Cystophrentis sp., Syningopora gracilis, Keyserlingophyllum, Hapsiphyllumsp.", "triple_list": [ [ "Flying the Dolomites", "Paleontological", "Coral fossils Pseudouralinia cf. tangpaouensis Yü" ], [ "Flying the Dolomites", "Paleontological", "Cystophrentis sp." ], [ "Flying the Dolomites", "Paleontological", "Syringopora gracilis" ], [ "Flying the Dolomites", "Paleontological", "Keyserlingophyllum" ], [ "Flying the Dolomites", "Paleontological", "Hapsiphyllumsp." ] ] }, { "text": "The Donggangling Group is mainly distributed in Luyun Kongjie in Guangxi and Xinrong Town, Luojing Town, Fenjie Town, Luoding City, etc., with an exposed area of about 26.54m2, accounting for 0.16% of the total area.", "triple_list": [ [ "Donggangling Group", "Exposed", "Green Cloud Kongjie in Guangxi" ], [ "Donggangling Group", "Exposed", "Luojing Town in Luoding City - Xinrong Town, Fenjie Town" ], [ "Donggangling Group", "area", "26.54m2" ] ] }, { "text": "The Hepu Formation contains pyrite with manganese and crystals intact, and is rich in marine fossils such as Bisilia and Brachiopods.", "triple_list": [ [ "Hepu Group", "Contained", "Pyrite" ], [ "Hepu Group", "Paleontological", "Bishi" ], [ "Hepu Group", "Paleontological", "sea lily" ], [ "Hepu Group", "Paleontological", "Brachiopod" ] ] }, { "text": "The Cambrian-Silurian strata are widely distributed, mainly seen in Kaiping, Taishan, Yangchun, Luoding, Yunan and Cenxi.", "triple_list": [ [ "Cambrian-Silurian strata", "Located at", "Kaiping, Taishan, Yangchun, Luoding, Yunan and Cenxi places" ] ] }, { "text": "The Dagangding Formation is a dark silty sandstone combination with fine sandstone, with micro-thin layered, horizontal stratigraphic structure, etc., and there are locally seen intact pyrite, and the plankton-containing pyrite fauna, reflecting the construction characteristics of semi-deep sea-phase remite.", "triple_list": [ [ "Dagang Ding Group", "Lithology", "Silty mudstone" ], [ "Dagang Ding Group", "Lithology", "Fine sandstone" ], [ "Dagang Ding Group", "Develop", "Horizontal stratification" ], [ "Dagang Ding Group", "Develop", "Strip structure" ], [ "Dagang Ding Group", "Develop", "Layer structure" ], [ "Dagang Ding Group", "Contained", "Pyrite" ], [ "Dagang Ding Group", "Paleontological", "Bistone fauna" ], [ "Dagang Ding Group", "Belongs to", "Semi-deep sea rematerial construction" ] ] }, { "text": "Light gray granular rock, 42.2m", "triple_list": [ [ "Light grey granular rock", "thickness", "42.2m" ] ] }, { "text": "Metamorphic coarse basal rock with variable residual pores and almond structure, 0.8m", "triple_list": [ [ "Metamorphic coarse basal rock", "thickness", "0.8m" ] ] }, { "text": "Light gray quartz silty sandy sericite thousand rocks with black carbonaceous thousand rocks, 33.6m", "triple_list": [ [ "Light gray quartz silty sericite thousand rock", "Contained", "Black charcoal-containing thousand rocks" ], [ "Light gray quartz silty sericite thousand rock", "thickness", "33.6m" ] ] }, { "text": "Floating soil, 244.4m", "triple_list": [ [ "surface dust", "thickness", "244.4m" ] ] }, { "text": "The Chunwan Formation is distributed in the east of the Weiguo Heshui-Chunwan, Nafuen Pingsha Lake, Taishan, and Xinxing Paradise on the west side of Shijiao-tanshui. The exposed area is about 301.06m2, accounting for 1.78% of the total area.", "triple_list": [ [ "Chunwan Group", "Exposed", "Taishan Fuen Pingsha Lake Yangchun Weiguo Heshui-East to Chunwan" ], [ "Chunwan Group", "Exposed", "Shiliu - The emerging paradise on the west side of Tanshui" ], [ "Chunwan Group", "area", "301.06m2" ] ] }, { "text": "Overly covered strata, gray-white-grey-red giant thick complex conglomerate, unconsolidated, Hushan Formation, total thickness 645.22m", "triple_list": [ [ "Guitou Group", "Lithology", "Gray-white-grey-red giant thick complex gravel rock" ], [ "Guitou Group", "Unconformity contact", "Hushan Group" ], [ "Guitou Group", "thickness", "645.22m" ] ] }, { "text": "Luodong Formation (O2l) refers to a set of gray-white thick layered dolomite fine crystalline limestone sand chip limestone integrated on the Luohong Formation.", "triple_list": [ [ "Luodong Group", "Integration of contacts", "Luo Hong Group" ], [ "Luodong Group", "Lithology", "Off-white thick layered dolomite fine crystal limestone" ], [ "Luodong Group", "Lithology", "Sand chip limestone" ] ] }, { "text": "The Hepu Formation, the Lower Fuliantan Formation and the Overlying Fangcheng Formation are in integrated contact, and the appearance of quartz (miscellaneous) sandstone or siliceous mudstone carbonate or mudstone-sanded limestone lens bodies are used as the boundary marker at the bottom top, with a thickness of >343m.", "triple_list": [ [ "Hepu Group", "Integration of contacts", "Liantan Group" ], [ "Hepu Group", "Integration of contacts", "Fangcheng Group" ], [ "Hepu Group", "Lithology", "Quartz (mixed) sandstone" ], [ "Hepu Group", "Lithology", "Silicone mudstone" ], [ "Hepu Group", "Lithology", "Carbonate rock" ], [ "Hepu Group", "Lithology", "Mudstone" ], [ "Hepu Group", "Lithology", "Limestone lens body" ], [ "Hepu Group", "thickness", "343m" ] ] }, { "text": "The Daganshan Formation in the survey area is mainly fine sandstone, siltstone, mudstone, and mudstone, with black carbonaceous layers, marine volcanic rocks, pyrite layers, siliceous rocks and (phosphorus-containing) carbonate lenses. The strip-like structure and horizontal stratum are developed. The micro-paleophytes contained in the survey area are absolutely dominant with chorizos with simple patterns. The above shows that the Daganshan Formation in the survey area is a semi-deep marine sedimentary environment with a relatively warm climate.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Fine sandstone" ], [ "Dakanshan Group", "Lithology", "Siltstone" ], [ "Dakanshan Group", "Lithology", "Mudstone" ], [ "Dakanshan Group", "Contained", "Black carbon layer" ], [ "Dakanshan Group", "Contained", "Maritime volcanic rocks" ], [ "Dakanshan Group", "Contained", "Pyrite layer" ], [ "Dakanshan Group", "Contained", "Silicite and (phosphorus-containing) carbonate lens body" ], [ "Dakanshan Group", "Distribution pattern", "Strip structure" ], [ "Dakanshan Group", "Develop", "Horizontal streak layer" ], [ "Dakanshan Group", "Paleontological", "Chlorella" ], [ "Dakanshan Group", "Belongs to", "Semi-deep oceanic sedimentary environment" ] ] }, { "text": "The first group of Yunkai Group (QnY1) refers to a group at the lower part of Yunkai Group, which is widely distributed in the Luoding-Xinyi-Yangchun area, with a large exposed area of about 924.27m2, accounting for 5.46% of the total area of the survey area.", "triple_list": [ [ "Yunkai Group First Group (QnY1)", "area", "924.27m2" ] ] }, { "text": "Dark gray thin layered biosiliceous rocks, containing bamboo entaculita, 46m.", "triple_list": [ [ "Dark gray thin layered biosiliceous rock", "Paleontological", "Bamboo joint stone entaculita" ], [ "Dark gray thin layered biosiliceous rock", "thickness", "46m" ] ] }, { "text": "Bali Formation (Z1b) refers to a set of shallow marine terrestrial pyroclastic siliceous rocks integrated between Shabahuang Formation and Niujiao River Formation.", "triple_list": [ [ "Bali Group", "Integration of contacts", "Shaba Huang Group" ], [ "Bali Group", "Integration of contacts", "Niujiao River Group" ], [ "Bali Group", "Belongs to", "Construction of shallow marine terrestrial pyroclastic siliceous rock" ] ] }, { "text": "According to a 1:200,000-year-old district report, the foraminifera Amphipora sp., a limestone-containing foramen in Xinbanyan.", "triple_list": [ [ "New Banyan limestone", "Paleontological", "Foraminifera Ammphipora sp." ] ] }, { "text": "Quartz mica microschist with green stone dioprene horn rock and thin layered mica feldspar quartzite 89.5m", "triple_list": [ [ "Quartz mica microschist with chlorophyllite diopyllite and thin-layer mica feldspar quartzite", "thickness", "89.5m" ] ] }, { "text": "The fourth system flood alluvial, 121.56m", "triple_list": [ [ "The fourth system of flood alluvial", "thickness", "121.56m" ] ] }, { "text": "The Bali Group and the Laohutang Group in the survey area are continuous sedimentation, so it is more appropriate to classify the era of the Bali Group as the Early Sedan period, and the corresponding strata are the Lower Sedan period.", "triple_list": [ [ "Bali Group", "Age", "Early Shining" ], [ "Tiger Pond Group", "Age", "Early Shining" ] ] }, { "text": "Quartz sodium porphyry, 18.2m", "triple_list": [ [ "Quartz sodium porphyry", "thickness", "18.2m" ] ] }, { "text": "Stone mica quartz schist with quartz black mica schist———————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Quartz schist with quartz black mica schist", "Integration of contacts", "The first group of Yunkai Group" ], [ "The first group of Yunkai Group", "thickness", "1417.8m" ] ] }, { "text": "The Kengping Xibi-horn porphyry system (Z1Ksp) is surrounded by faults, and is exposed in the Kengping-Xianjingwei in Guizi Town, Xinyi, and the Longhugang Huodao-Yaogu area of Chashan Town, only 124.91m2, accounting for 0.74% of the total area of the survey area.", "triple_list": [ [ "Kengping Xibi-angle porphyry system (Z1Ksp)", "Distribution pattern", "Remains" ], [ "Kengping Xibi-angle porphyry system (Z1Ksp)", "Located at", "Kengping in Guizi Town, Xinyi - Xianjingwei and Longhugang Huodao in Chashan Town - Yaogu" ], [ "Kengping Xibi-angle porphyry system (Z1Ksp)", "area", "124.91m2" ] ] }, { "text": "The Lanweng Formation in the survey area is distributed in the north of Hekou Town, Yunan, north of Gaocun, Yun'an. The distribution range is small, only 14.51m2, accounting for 0.09% of the total area of the survey area. The lithology is purple-red, gray-white gravel-containing fine-grained quartz sandstone amidst silt sandstone mudstone and quartz sericite thousand rocks.", "triple_list": [ [ "Orchid group", "Exposed", "North of Yun'an Gaocun North of Yunan Hekou Town" ], [ "Orchid group", "area", "14.51m2" ], [ "Orchid group", "Lithology", "Purple red gray off-white gravel fine-grained quartz sandstone" ], [ "Orchid group", "Lithology", "Mud siltstone" ], [ "Orchid group", "Lithology", "Mudstone" ], [ "Orchid group", "Lithology", "Quartz sericite thousand rock" ] ] }, { "text": "The Daganshan Formation in the survey area is mainly fine sandstone silt sandstone mudstone, with black carbonaceous layer marine volcanic rock pyrite layer siliceous rock and (phosphorus-containing) carbonate lens body. The strip-like structure horizontal stratum is developed. The micro-paleophytes contained in it have absolute advantages for chalia with simple patterns and structures.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Fine sandstone" ], [ "Dakanshan Group", "Lithology", "Siltstone" ], [ "Dakanshan Group", "Lithology", "Mudstone" ], [ "Dakanshan Group", "Lithology", "Black carbonaceous marine volcanic rock" ], [ "Dakanshan Group", "Lithology", "Pyrite layer siliceous rock" ], [ "Dakanshan Group", "Lithology", "(Phos containing) Carbonate rock lens body" ], [ "Dakanshan Group", "Develop", "Strip structure" ], [ "Dakanshan Group", "Develop", "Horizontal streak layer" ], [ "Dakanshan Group", "Paleontological", "Chlorella" ] ] }, { "text": "The Luohong Formation of the overlying formation, the fossil quartz conglomerate and the medium-coarse-grained metamorphic sandstone splint are parallel and unconformed. The total thickness of the water stone form is 2662.88m", "triple_list": [ [ "Luo Hong Group", "Lithology", "Physical and chemical quartz gravel" ], [ "Luo Hong Group", "Lithology", "Medium-coarse-metamorphic sandstone" ], [ "Luo Hong Group", "Lithology", "Slate" ], [ "Luo Hong Group", "Integration of contacts", "Water stone group" ], [ "Water stone group", "thickness", "2662.88m" ] ] }, { "text": "The Chunwan Group in the survey area is mainly distributed in Taishan, including Fuyang, Chunwei, Weiguo, Heshui, Dongmashuixi Xinxing Paradise, etc., and is also distributed fragmentally in Shijiao-Tanshuiyangchun and other places, with an exposed area of about 133.75m2, accounting for 0.79% of the total area.", "triple_list": [ [ "Chunwan Group", "Exposed", "Taishan's Fuyang and Chun Weiguo Heshui East and West Emerging Paradise" ], [ "Chunwan Group", "Exposed", "Shiliu-tanshuiyangchun" ], [ "Chunwan Group", "area", "133.75m2" ] ] }, { "text": "The upper part of the Daganshan Formation is mainly composed of manganese-containing sericite thousand rocks, quartz weaving mica thousand rocks, sericite thousand rocks and striped particle quartzite. The lower part is mainly composed of carbon sericite quartzite and quartz sericite kilograms and thin-layer siliceous rocks.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Manganese-containing sericite thousand rocks" ], [ "Dakanshan Group", "Contained", "Quartz mica kilogram" ], [ "Dakanshan Group", "Contained", "Sericite thousand rocks" ], [ "Dakanshan Group", "Contained", "Striped microparticle quartzite" ], [ "Dakanshan Group", "Lithology", "Carbon sericite thousand rock" ], [ "Dakanshan Group", "Lithology", "Quartz sericite thousand rock" ], [ "Dakanshan Group", "Contained", "Flake-like particles carbon sericite quartzite" ], [ "Dakanshan Group", "Contained", "Thin layered siliceous rock" ] ] }, { "text": "The Dagan Mountain group in the survey area is distributed in Luodingweidi-Yun'an County Zhen'an-Yunfuyaoguyangchun-Helang and other places, with wide exposure, about 772.46m2, accounting for 4.57% of the total area of the survey area.", "triple_list": [ [ "Dakanshan Group", "Exposed", "Luodingweidi-Zhen'an County-Yunfuyaoguyangchun-Helang" ], [ "Dakanshan Group", "area", "772.46m" ] ] }, { "text": "The Cambrian strata is called the Gaotan Formation Water Stone Formation.", "triple_list": [ [ "Cambrian strata", "Outcrop", "Gaotan Group" ], [ "Cambrian strata", "Outcrop", "Water stone group" ] ] }, { "text": "Yellow-brown mica schist with thin layered mica quartz schist, 86.6m", "triple_list": [ [ "Yellow-brown mica schist with thin layered mica quartz schist", "thickness", "86.6m" ] ] }, { "text": "The Hushan Formation in the survey area is distributed in the east area of Nafu Town, Taishan City. The exposed area is small, only 12.23m2, accounting for 0.07% of the total area of the survey area. The lithology is mainly siliceous rocks and shale. It is in integrated contact with the lower Fu Xinchang Formation. The top is covered by the unconforming contact of the Guitou Group with a thickness of 645m.", "triple_list": [ [ "Hushan Group", "Exposed", "East of Nafu Town, Taishan City" ], [ "Hushan Group", "area", "12.23m2" ], [ "Hushan Group", "Lithology", "Silicone rock" ], [ "Hushan Group", "Lithology", "shale" ], [ "Hushan Group", "Integration of contacts", "New factory group" ], [ "Hushan Group", "Integration of contacts", "Guitou Group" ], [ "Hushan Group", "thickness", "645m" ] ] }, { "text": "The Dagangding Group of the survey area was found in the area of Lidong Town, Yunnan County and the northwest of Heishi Village, Guiyi Town, Cenxi City, Guangxi City, with an exposed area of only 18.95m2, accounting for 0.11% of the total area of the survey area.", "triple_list": [ [ "Dagang Ding Group", "Exposed", "Lidong Town, Yunnan County" ], [ "Dagang Ding Group", "Exposed", "Northwest of Heishi Village, Guiyi Town, Cenxi City, Guangxi" ], [ "Dagang Ding Group", "area", "18.95m2" ] ] }, { "text": "Gaozhou crust rock assembly is invaded by flaky granite, and partly produced huge xenophobia.", "triple_list": [ [ "Hemp granite", "Invade", "Gaozhou Case Rock Combination Rock" ] ] }, { "text": "Gray-green thin-layer sheet physical and chemical mica microschist with tremolite green curtain stone horn rock, 135.3m", "triple_list": [ [ "Physical and chemical mica microschist with tremolite green curtain stone horn rock", "thickness", "135.3m" ] ] }, { "text": "Magnetite containing Yangqi Petrochemical Dioplastic and Dioplastic Garnet Sikarn, 18.0m", "triple_list": [ [ "Magnetorite containing Yangqi Petrochemical Tremolite", "thickness", "18.0m" ], [ "Diopylate garnet skarn", "thickness", "18.0m" ] ] }, { "text": "The Bali Formation in the survey area is mainly fine sandstone, which is sandstone and mudstone, and partially siliceous rocks and carbon-containing layers. It has horizontal layered textures and is rich in pyrite microcrystals. The above indicates that the Bali in the survey area should be deep-sea sedimentation.", "triple_list": [ [ "Bali Group", "Lithology", "Fine sandstone" ], [ "Bali Group", "Contained", "Siltstone" ], [ "Bali Group", "Contained", "Mudstone" ], [ "Bali Group", "Contained", "Silicone rock" ], [ "Bali Group", "Contained", "Carbon-containing layer" ], [ "Bali Group", "Develop", "Horizontal stratification" ], [ "Bali Group", "Lithology", "Pyrite crystal" ], [ "Bali Group", "Lithology", "Deep-sea phase sedimentation" ] ] }, { "text": "Yellow-white, yellow-brown, silver-gray wrinkled mica quartz schist, quartz mica schist, and black mica schist interlayer, 146.3m", "triple_list": [ [ "Yellow-white, yellow-brown, silver-gray wrinkled mica quartz schist", "thickness", "146.3m" ], [ "Quartz mica schist", "thickness", "146.3m" ], [ "Mica schist", "thickness", "146.3m" ] ] }, { "text": "Gray light gray medium-thick layered porphyry black cloud red column horn rock and horn lithified fine medium-grained quartz mixed sandstone, 49m", "triple_list": [ [ "Gray light gray medium-thick layered porphyry black cloud red column horn rock and horn rocky fine medium-grained quartz sandstone interlayer", "thickness", "49m" ] ] }, { "text": "Gray-red thin plate-like calcareous silt sandstone and gray-red mudstone interlayer, 2.1 m", "triple_list": [ [ "Gray-red thin plate-like calcareous silt sandstone and gray-red mudstone interlayer", "thickness", "2.1 m" ] ] }, { "text": "The carbonate sedimentation combination in the subtidal zone is represented by the second section of Langshan Formation. The main lithologies are dark gray thin-middle round cylindrical crystal limestone biological clastic mud crystal limestone dark gray middle layer round cylindrical limestone light gray thick layer containing biological clastic microcrystalline limestone.", "triple_list": [ [ "Carbonate deposition combination in subtidal zone", "Contained", "Section 2 of Langshan Group" ], [ "Section 2 of Langshan Group", "Lithology", "Dark gray thin-middle round worm mud crystal limestone" ], [ "Section 2 of Langshan Group", "Lithology", "Bioclass mud crystal limestone" ], [ "Section 2 of Langshan Group", "Lithology", "Dark gray middle layer round worm limestone" ], [ "Section 2 of Langshan Group", "Lithology", "Light gray thick layer of bioclad microcrystalline limestone" ] ] }, { "text": "According to the paleobiological characteristics of the rock combination and the contact relationship between strata, the Jurassic system in the area is divided from bottom to top into the Central Orthodox Ormonla Formation and the Upper Jurass-Lower Cretaceous Shamuluo Formation.", "triple_list": [ [ "Jurassic", "Outcrop", "Xiatongmugagang Day Group" ], [ "Jurassic", "Outcrop", "The Russian-Monle Group of the Central Government" ], [ "Jurassic", "Outcrop", "Upper Jurass-Lower Cretaceous Sharmuro Formation" ] ] }, { "text": "The quadrup of the coral Grypophyllum-Disphyllum group was exposed to the Berbagowaqiu and other places. The corresponding rock formation was the Chagoroma group.", "triple_list": [ [ "Grypophyllum-Disphyllum combination belt", "Exposed", "Beerbaguwa Poor Fruit" ], [ "Grypophyllum-Disphyllum combination belt", "Exposed", "Chago Roma Group" ] ] }, { "text": "The era of the Nongqun was mainly the Early Cretaceous.", "triple_list": [ [ "Let's make a group", "Age", "Early Cretaceous" ] ] }, { "text": "Gray thin-middle-grained quartz sandstone and gray-black mudstone are interlayered, and the two form the basic layer sequence (12 in total, each of which is 35 m thick), 63.8 m", "triple_list": [ [ "Gray thin-middle-fine-grained quartz sandstone and gray-black mudstone interlayer", "thickness", "63.8 m" ] ] }, { "text": "The middle part of the Daganshan Formation is gray-green, gray-black thin-layered quartz dimica schist, dimica quartz schist and sericca quartz schist.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Gray-green, gray-black thin-layered quartz dimica schist" ], [ "Dakanshan Group", "Lithology", "Dimica quartz schist" ], [ "Dakanshan Group", "Lithology", "sericca quartz schist" ], [ "Dakanshan Group", "Contained", "Off-white thin layered mica flake quartzite" ] ] }, { "text": "The Tibet Geology and Mineral Resources Bureau (1997) divided the Carbonite System into the Laga Formation of the Middle Carbonite System and the Angjie Formation of the Upper Carbonite System-Lower Permian.", "triple_list": [ [ "Carbonite", "Outcrop", "Carboniferous Organism Yongzhu Group" ], [ "Carbonite", "Outcrop", "Laga Formation of Carboniferous Systems" ], [ "Carbonite", "Outcrop", "Upper Carboniferous Order - Lower Permian Angjie Group" ] ] }, { "text": "The main lithologies in the lower part are andesite breccia andesite, a small amount of pyroclastic rocks, and the main lithologies in the upper part are Andesite lava, (permeable)pyroxene andesite and a small amount of pyroclastic rocks.", "triple_list": [ [ "Lower part", "Lithology", "Andanyan" ], [ "Lower part", "Lithology", "breccia andes" ], [ "Lower part", "Lithology", "Pyroclastic rock" ], [ "Lower part", "Lithology", "Andan quasi-collection lava" ], [ "Lower part", "Lithology", "pyroxene andshan rock" ], [ "Lower part", "Lithology", "Ying'an Rock" ], [ "Lower part", "Lithology", "Pyroclastic rock" ] ] }, { "text": "The devon system is integrated on the Silurian system and is also covered by Carboniferous clastic rocks. Its era should be later than the Silurian period and earlier than the Carboniferous period.", "triple_list": [ [ "Mud pot system", "Integration of contacts", "Shiliu Department" ], [ "Mud pot system", "Integration of contacts", "Carboniferous clastic rock" ], [ "Mud pot system", "Age", "Shiliji" ], [ "Mud pot system", "Age", "Carboniferous period" ] ] }, { "text": "Gray-red and maroon middle-layer conglomerate with a small amount of thin layer of fine-grained rock sandstone, 20.9 m", "triple_list": [ [ "Gray-red and maroon middle-layer conglomerate with a small amount of thin-layer fine-grained sandstone", "thickness", "20.9 m" ] ] }, { "text": "The rock fragment composition in the Shen'anshan crystalline crystal tuff is Andesite, subangular-angular-subround, with a size of 0.05 mm, a content of 70%, 8.4 m", "triple_list": [ [ "The rock fragment composition of Shen'anshan crystalline crystalline tuff is Andesan", "thickness", "8.4 m" ] ] }, { "text": "The actual test profile of the Songwoji-Chinese Jurassic-Chinese Jurassic-Shenla Formation in Shuanghu District is located at Songwoji, about 22 m east of Nancuozhe Township, Shuanghu District. The starting coordinates are N31°53′43.9″, E88°07′10.7″, the end coordinates are N31°54′22.8″, E88°07′10.8″, and the cross section is about 1 m long.", "triple_list": [ [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "Located at", "Song Wori, about 22 m east of Nancuozhe Township, Shuanghu District" ], [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "Coordinates", "N31°53′43.9″" ], [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "Coordinates", "E88°07'10.7″" ], [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "Coordinates", "N31°54'22.8″" ], [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "Coordinates", "E88°07'10.8″" ], [ "Shuanghu District Song and Chinese Jurassics Group Test Profile", "length", "1 m" ] ] }, { "text": "A brown-yellow muddy silty sandstone lens body with gray-black silty mudstone containing more grey-black mudstone, see horizontal insect hole 1.5 m", "triple_list": [ [ "Brown-yellow muddy silt sandstone lens body with gray-black silt sandstone containing more sandstones", "Develop", "Horizontal insect hole" ], [ "Brown-yellow muddy silt sandstone lens body with gray-black silt sandstone containing more sandstones", "thickness", "1.5 m" ] ] }, { "text": "Rock has a patchy structure, almond-like structure, 10.2 m", "triple_list": [ [ "rock", "Distribution pattern", "Spotted structure" ], [ "rock", "Develop", "Almond-like structure" ], [ "rock", "thickness", "10.2 m" ] ] }, { "text": "The Laga group was integrated on the Yongzhu group and was integrated and covered by the Lower Permian Angjie group. The era should have been later than the Devonian period and earlier than the Early Permian.", "triple_list": [ [ "Laga Group", "Integration of contacts", "Yongzhu Group" ], [ "Laga Group", "Integration of contacts", "Lower Permian Angjie Group" ], [ "Laga Group", "Age", "Devonian" ], [ "Laga Group", "Age", "Early Permian" ] ] }, { "text": "Gray thick - huge thick layer of glossy oasis limestone, occasionally containing flint clumps, 17.3 m", "triple_list": [ [ "Thick gray - huge thick layer of glossy oasis limestone", "Contained", "Flint clumps" ], [ "Thick gray - huge thick layer of glossy oasis limestone", "thickness", "17.3 m" ] ] }, { "text": "Gray yellow medium-layer fine-grained quartz sandstone, developing trough-like staggered stratigraphic, upward thinning, 4.9 m", "triple_list": [ [ "Gray yellow medium-layer fine-grained quartz sandstone", "Develop", "Grooved interlaced stratigraphic" ], [ "Gray yellow medium-layer fine-grained quartz sandstone", "thickness", "4.9 m" ] ] }, { "text": "Light gray-green thin layer of muddy silt sandstone and gray-thin-middle-fine-grained quartz sandstone, the two form the basic layer sequence (11 in total), 81.4 m", "triple_list": [ [ "Light gray-green thin layer of muddy silt sandstone and gray-thin-middle-fine-grained quartz sandstone", "thickness", "81.4 m" ] ] }, { "text": "Gray thin plate-shaped sedimentary crystalline crystalline tuff and gray-purple mudstone interlayer, 12.5 m", "triple_list": [ [ "Gray thin plate-shaped sandy Anshan crystalline crystalline tuff and gray-purple mudstone interlayer", "thickness", "12.5 m" ] ] }, { "text": "Yellow-brown thin-middle medium-fine-grained quartz sandstone with gray-black mudstone, the sandstone has parallel stratigraphic and small plate-like interlaced stratigraphic thickness 2526.9 m", "triple_list": [ [ "Yellow-brown thin-middle-middle-fine-grained quartz sandstone with gray-black mudstone", "thickness", "2526.9 m" ], [ "sandstone", "Develop", "Parallel layering" ], [ "sandstone", "Develop", "Small plate-like staggered stratigraphy" ] ] }, { "text": "The Central Jurassic Dingshenla group was named by the Tibet Regional Transfer Team (1986). The location was in Dongcuo North of Gaize County. The main lithologies were basalt and Andyro tuff, etc., which were not integrated into the Jurassic Mugagang Ri group, and the era returned to the early Cretaceous.", "triple_list": [ [ "Central Jurassic to Shenra Group", "Exposed", "Go to Shenla in Dongcuo North of Gaize County" ], [ "Central Jurassic to Shenra Group", "Lithology", "Basalt" ], [ "Central Jurassic to Shenra Group", "Lithology", "Andanyan" ], [ "Central Jurassic to Shenra Group", "Lithology", "Tuff" ], [ "Central Jurassic to Shenra Group", "Unconformity contact", "Jurassic Mugagang Day Group" ], [ "Central Jurassic to Shenra Group", "Age", "Early Cretaceous" ] ] }, { "text": "Bivalves Lopha sp., Ostreamea gen. et sp. ind, etc. are captured in Kolannan.", "triple_list": [ [ "Kelannan", "Paleontological", "Bivalve Lopha sp." ], [ "Kelannan", "Paleontological", "Ostreacea gen. et sp. ind" ] ] }, { "text": "Gray-green calcareous mudstone, 4.1 m", "triple_list": [ [ "Gray-green calcareous mudstone", "thickness", "4.1 m" ] ] }, { "text": "The C layer is mainly siltstone and develops horizontal stratigraphics.", "triple_list": [ [ "Layer C", "Lithology", "Siltstone" ], [ "Layer C", "Develop", "Horizontal stratification" ] ] }, { "text": "Gray long-elastic supermylonite, developmental mylon and tensile threads, with eyeball texture structure, fissure and crack Develop, 118m", "triple_list": [ [ "Gray long-ebony supermylon", "Develop", "Myrgonal facial" ], [ "Gray long-ebony supermylon", "Develop", "Tensile threading" ], [ "Gray long-ebony supermylon", "Develop", "Eye texture structure" ], [ "Gray long-ebony supermylon", "Develop", "Spot-breaking twigs" ], [ "Gray long-ebony supermylon", "thickness", "118m" ] ] }, { "text": "The rhyolite subclass is exposed in the upper part of the Deshenla Formation and is distributed in the Qukangbale area. The rocks are grayish white and light red, with spotty structures.", "triple_list": [ [ "Rhyolite subcategory", "Exposed", "Go to Shenla Group" ], [ "Rhyolite subcategory", "Exposed", "Qukangbal" ], [ "Rhyolite subcategory", "Distribution pattern", "Spotted structure" ], [ "Rhyolite subcategory", "Develop", "Flow pattern structure" ] ] }, { "text": "Physical and chemical mica quartzite with black thin layered quartz mica schist and 0.5m thick oblique elongated flasheschist, 131.4m", "triple_list": [ [ "Physical and chemical mica quartzite with black thin layered quartz mica schist", "thickness", "131.4m" ], [ "oblique angular radiuschlid", "thickness", "0.5m thick" ] ] }, { "text": "The sedimentary combination of clastic rocks in the subtidal zone is represented by the lower part of the Angjie Formation. The main lithologies are gray-black silty mudstone containing silty mudstone mudstone mudstone mudstone mudstone mudstone mudstone mudstone mudstone and fine sandstone lenses, and Contained relatively abundant foraminiferous corals, sea lilies, etc.", "triple_list": [ [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Contained", "The lower part of Angjie group" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Lithology", "Gray-black silt mudstone" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Lithology", "Silty sandy rock" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Lithology", "Mud siltstone" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Lithology", "Gray-black middle layer containing bioclastic mud crystal limestone" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Lithology", "Fine sandstone lens body" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Develop", "Foraminifera" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Develop", "coral" ], [ "Subtidal clastic rock sedimentation combination in subtidal zone", "Develop", "sea lily" ] ] }, { "text": "The lower part of the Dewuka lower group in Yongzhu area is black calcareous shale and dark gray thin layer of limestone, and the upper part is earthy yellow-gray calcareous shale and dark gray thin layer of limestone, which contains rich serolis and a small amount of brachiopods, with a thickness of 183 m.", "triple_list": [ [ "Yongzhu", "Outcrop", "Dewu Card's second group" ], [ "Dewu Card's second group", "Lithology", "Black calcium shale" ], [ "Dewu Card's second group", "Lithology", "Dark gray thin layer of limestone" ], [ "Dewu Card's second group", "Lithology", "Yellowish yellowish gray calcium shale" ], [ "Dewu Card's second group", "Lithology", "Dark gray thin layer of limestone" ], [ "Dewu Card's second group", "Paleontological", "Bishi" ], [ "Dewu Card's second group", "Paleontological", "Brachiopod" ], [ "Dewu Card's second group", "thickness", "183 m" ] ] }, { "text": "The sedimentary combination of Hekou Bay is represented by the lower part of the Omonle Formation. The main lithologies are gray-gray-green-gray-yellow mudstone silty mudstone yellow-brown thin layer fine-grained quartz sandstone, with the lower part interstices silty sandstone lens body and the upper part interstices silty oasis limestone lens body.", "triple_list": [ [ "Hekou Bay Sedimentary Combination", "Contained", "The lower part of the Russian Monle Group" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Gray gray-green gray-yellow mudstone" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Silty mudstone" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Yellow-brown thin layer of fine-grained quartz sandstone" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Mud siltstone lens body" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Sand mud oximeters" ], [ "Hekou Bay Sedimentary Combination", "Lithology", "Limestone lens body" ] ] }, { "text": "The shallow sea shelter sedimentary combination is represented by the middle and upper part of the Dewuka Lower Formation. The main lithology is blue-gray thin plate-thin layer of mud crystal limestone gray thin plate-shaped silty microcrystalline limestone, gray-black carbon-containing calcium slate, and Nautilus fossils. The horizontal texture is extremely developed and no shallow water sedimentary marks are seen.", "triple_list": [ [ "Shallow sea shed sedimentary combination", "Contained", "Dewuka's lower group middle and upper part" ], [ "Shallow sea shed sedimentary combination", "Lithology", "Blue-gray thin plate-thin layer of mud crystal limestone" ], [ "Shallow sea shed sedimentary combination", "Lithology", "Gray thin plate-shaped silty microcrystalline limestone" ], [ "Shallow sea shed sedimentary combination", "Lithology", "Gray-black calcareous slabs containing carbon" ], [ "Shallow sea shed sedimentary combination", "Paleontological", "Nautilus fossil" ], [ "Shallow sea shed sedimentary combination", "Develop", "Horizontal texture" ] ] }, { "text": "The Cretaceous region extends eastward to the Bangor area and westward to the Gejigar area.", "triple_list": [ [ "Cretaceous", "Exposed", "Bangor" ], [ "Cretaceous", "Exposed", "Gejigar" ] ] }, { "text": "Light blue-gray silty mudstone, horizontal insect hole 62.5 m", "triple_list": [ [ "Light blue-gray silty mudstone", "Develop", "Horizontal insect hole" ], [ "Light blue-gray silty mudstone", "thickness", "62.5 m" ] ] }, { "text": "Grey-green mudstone is rich in sporestone Cyachidites australis Yu, Varirugosisporites tolmanensis Srivastava, 156.6 m", "triple_list": [ [ "Gray-green mudstone", "Paleontological", "Spore Powder Cyachidites australis Yu" ], [ "Gray-green mudstone", "Paleontological", "Varirugosisportes tolmanensis Srivastava" ], [ "Gray-green mudstone", "thickness", "156.6 m" ] ] }, { "text": "The total thickness of the Russian kills and supplementary group is about 2902 m.", "triple_list": [ [ "Russia kills and regroups", "thickness", "2902 m" ] ] }, { "text": "Gray-red, maroon-red thin layer of fine medium-grained rock-cut sandstone, with gravel at the bottom, with parallel stratigraphic and wedge-shaped interlaced stratigraphic, 17.2 m", "triple_list": [ [ "Gray reddish-brown thin layer of fine medium-grained crystal sandstone", "Develop", "Parallel layering" ], [ "Gray reddish-brown thin layer of fine medium-grained crystal sandstone", "Develop", "Wedge-shaped interlaced layering" ] ] }, { "text": "The strata of Yangchun County survey area is widely distributed, and all strata of the strata have been developed since the Jixian period.", "triple_list": [ [ "Yangchun County Survey District", "Develop", "All strata have developed since the Jixian Chronicle" ] ] }, { "text": "Sericite slate is mainly distributed in the Yongzhu Group, with a granular scale crystal structure and a plate-like structure, and a silky luster can be seen along the plate surface.", "triple_list": [ [ "sericite slate", "Exposed", "Yongzhu Group" ], [ "sericite slate", "Distribution pattern", "Granular scale crystal structure" ], [ "sericite slate", "Develop", "Plate-like structure" ] ] }, { "text": "The Yongzhu Group in the Yongzhu area of Shenzha Yongzhu collected a large number of brachiopod corals, which were in the late Carboniferous period.", "triple_list": [ [ "Shinza Yongzhu", "Outcrop", "Yongzhu Group" ], [ "Yongzhu Group", "Paleontological", "Brachiopod" ], [ "Yongzhu Group", "Paleontological", "coral" ], [ "Yongzhu Group", "Age", "Late Carboniferous" ] ] }, { "text": "Profile of the Eugene Pana Group of the Anzicuonan Allied by Anzicuonan Township, Shenzha County. Eugene Pana Group (E2p), thickness >1803.05 m", "triple_list": [ [ "Profile of the Pana Group of Angzicuonan Alley of the Xintong in Zhuoni Township, Shenzha County", "Contained", "The Pana Group of the Innovative Universe" ], [ "The Pana Group of the Innovative Universe", "thickness", "1803.05 m" ] ] }, { "text": "The Carboniferous System was integrated with the Chagoroma Group of the middle and upper devon system, but it was not seen above.", "triple_list": [ [ "Carbonite", "Integration of contacts", "Middle and upper devons Chagoroma Group" ] ] }, { "text": "Gray-black silty mud slate, 4.6 m", "triple_list": [ [ "Gray-black silty mud slab rock", "thickness", "4.6 m" ] ] }, { "text": "The Angjie Formation is mainly sandstone sandstone and silty mudstone. The sandstone has a high maturity, good sorting, and the particle size is mainly 0.03-0.06 mm.", "triple_list": [ [ "Ang Jie Group", "Lithology", "Siltstone" ], [ "Ang Jie Group", "Lithology", "Silty mudstone" ], [ "Ang Jie Group", "Lithology", "sandstone" ] ] }, { "text": "The top of the Zalonoma Formation is represented by the top of the Zalonoma Formation, which is mainly black thin plate-shaped mud crystal limestone, containing fossils such as nautilus and apriculi.", "triple_list": [ [ "Under-tidal sedimentation combination in platform", "Contained", "Zanon Oma Group Top" ], [ "Under-tidal sedimentation combination in platform", "Lithology", "Black thin plate-shaped mud crystal limestone" ], [ "Under-tidal sedimentation combination in platform", "Lithology", "Nautilus" ], [ "Under-tidal sedimentation combination in platform", "Lithology", "Acanthus" ] ] }, { "text": "Gray-black sandy silty mudstone, containing sporadic gravel 1.6 m", "triple_list": [ [ "Gray-black sandy silt mudstone", "Contained", "gravel" ], [ "Gray-black sandy silt mudstone", "thickness", "1.6 m" ] ] }, { "text": "Gray-black mudstone with gray-yellow thin-medium fine-grained feldspar quartz sandstone and fine-grained quartz sandstone, containing spores. Leiotriletes rombodeus Bolchovitina, Pterisporites medirhaptes Li, Classopollis sp., Dicheiropollis sp.", "triple_list": [ [ "Gray-black mudstone with gray-yellow thin-middle fine-grained feldspar quartz sandstone and fine-grained quartz sandstone", "Paleontological", "Leiotriletes rombodeus Bolchovitina" ], [ "Gray-black mudstone with gray-yellow thin-middle fine-grained feldspar quartz sandstone and fine-grained quartz sandstone", "Paleontological", "Pterisisporites medirhaptes Li" ], [ "Gray-black mudstone with gray-yellow thin-middle fine-grained feldspar quartz sandstone and fine-grained quartz sandstone", "Paleontological", "Classopollis sp." ], [ "Gray-black mudstone with gray-yellow thin-middle fine-grained feldspar quartz sandstone and fine-grained quartz sandstone", "Paleontological", "Dicheiropollis sp." ] ] }, { "text": "Light gray thin-middle-layer mud wafer limestone, round elliptical, size is 1.8-7.5 mm, content 55%, bivalve content 2% —————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————————", "triple_list": [ [ "Light gray thin-middle mud wafer limestone", "Paleontological", "Round worm" ], [ "Light gray thin-middle mud wafer limestone", "Paleontological", "Bivalves" ], [ "Light gray thin-middle mud wafer limestone", "Integration of contacts", "A paragraph" ], [ "A paragraph", "thickness", "714.3 m" ] ] }, { "text": "Light blue-gray silty mudstone, horizontal insect hole 78.6 m", "triple_list": [ [ "Light blue-gray silty mudstone", "Develop", "Horizontal insect hole" ], [ "Light blue-gray silty mudstone", "thickness", "78.6 m" ] ] }, { "text": "The high water level system domain (HS) is found in the 1519 layer of the Yushaheli section, with a thickness of 342 m, and the bottom interface is the largest sea surface.", "triple_list": [ [ "High water level system domain", "Located at", "Russian killing and complementary profile 1519 floor" ], [ "High water level system domain", "thickness", "342 m" ] ] }, { "text": "The Jurassic system is not integrated and covered by the Langshan Formation of the Lower Cretaceous in the Salt Lake District of Geji County, and its era should be the Jurassic-Early Cretaceous.", "triple_list": [ [ "Jurassic", "Exposed", "Geji County Salt Lake District" ], [ "Jurassic", "Unconformity contact", "Lower Cretaceous Langshan Formation" ], [ "Jurassic", "Age", "Jurassic-Early Cretaceous" ] ] }, { "text": "Gray black yellow white quartz mica microschist charcoal sericite thousand rock, 69.1m", "triple_list": [ [ "Gray black yellow white quartz mica microschist", "Contained", "Carbon sericite thousand rock" ], [ "Gray black yellow white quartz mica microschist", "thickness", "69.1m" ] ] }, { "text": "The lower part of the eastern part is gray-brown medium-layer fine gravel medium-grain quartz sandstone medium-grain quartz sandstone.", "triple_list": [ [ "Lower Eastern", "Lithology", "Gray-brown medium gravel rock" ], [ "Lower Eastern", "Lithology", "Fine-grained quartz sandstone" ], [ "Lower Eastern", "Lithology", "Medium-grained quartz sandstone" ] ] }, { "text": "Iron ore layers are seen in Dadongtian, Yunli and other places. The skarn-type magnetite on the upper part of this group can be used as a contrast mark in the area, and the marble on the top can be used as a division mark.", "triple_list": [ [ "Earth-See iron ore layer", "Located at", "Big winter fields, clouds" ], [ "Earth-See iron ore layer", "Contained", "Skarn magnetite" ], [ "Earth-See iron ore layer", "Contained", "Dali Rock" ] ] }, { "text": "Light gray medium-layer fine-grained quartz sandstone, 200.8 m", "triple_list": [ [ "Light gray medium-layer fine-grained quartz sandstone", "thickness", "200.8 m" ] ] }, { "text": "In the Zhashan area of Bangor County, it is composed of purple-red, gray-green tuff conglomerate containing gravel sandstone and a small amount of silt sandstone and limestone, containing Orbitolina concave, with a thickness of 1800 m.", "triple_list": [ [ "Zhashan area, Bangor County", "Lithology", "Purple red gray green tuff conglomerate" ], [ "Zhashan area, Bangor County", "Lithology", "Gravel-containing sandstone" ], [ "Zhashan area, Bangor County", "Lithology", "sandstone" ], [ "Zhashan area, Bangor County", "Lithology", "Siltstone" ], [ "Zhashan area, Bangor County", "Lithology", "Limestone" ], [ "Zhashan area, Bangor County", "Paleontological", "Orbitolina concave" ], [ "Zhashan area, Bangor County", "thickness", "1800 m" ] ] }, { "text": "The Dhoni group contains bivalves of the round worm, and the time was determined as the Early Cretaceous Barrem-Aputt period", "triple_list": [ [ "Doni Group", "Paleontological", "Round worm" ], [ "Doni Group", "Paleontological", "Bivalves" ], [ "Doni Group", "Paleontological", "Gastropod" ], [ "Doni Group", "Age", "Barem Period of the Early Cretaceous Period-Apute Period" ] ] }, { "text": "The 1-layer sequence is located in the lower section of the Quehala group, consisting of the marine invasion system and the high-water level system domain, with a thickness of 94-117 m.", "triple_list": [ [ "1 layer sequence", "Located at", "The second section of Quehara group" ], [ "1 layer sequence", "Contained", "Low water level system area sea invasion system area" ], [ "1 layer sequence", "Contained", "High water level system domain" ], [ "1 layer sequence", "thickness", "94-117 m" ] ] }, { "text": "Gray-green silty mudstone 11.5 m", "triple_list": [ [ "Gray-green silty mudstone", "thickness", "11.5 m" ] ] }, { "text": "Gray-black mudstone with horizontal streak 99.8 m", "triple_list": [ [ "Grey-black mudstone", "Develop", "Horizontal streak layer" ], [ "Grey-black mudstone", "thickness", "99.8 m" ] ] }, { "text": "The thick gray layer contains bioclass mud crystal limestone, with a biological debris content of 1%, mainly cypress worms and a small number of bivalves", "triple_list": [ [ "Gray thick layer of bioclastic mud crystal limestone", "Paleontological", "Bio-shatter" ], [ "Gray thick layer of bioclastic mud crystal limestone", "Paleontological", "Round worm" ], [ "Gray thick layer of bioclastic mud crystal limestone", "Paleontological", "Bivalves" ] ] }, { "text": "The lithologic changes in the area are not much, mainly andesite, with more volcanic clastic rocks in the west and more volcanic lava in the east.", "triple_list": [ [ "Go to Shenla Group", "Lithology", "Andanyan" ], [ "Go to Shenla Group", "Lithology", "Pyroclastic rock" ], [ "Go to Shenla Group", "Lithology", "Volcanic lava" ] ] }, { "text": "The river-alloxis fan sedimentation combination, represented by the Jingzhushan Formation, is mainly lithologic: variegated thick layer conglomerate medium-grained rock-cut sandstone fine-grained rock-cut sandstone.", "triple_list": [ [ "River-alluvial fan sedimentation combination", "Contained", "Jingzhushan Group" ], [ "Jingzhushan Group", "Lithology", "Variegated thick layer of gravel" ], [ "Jingzhushan Group", "Lithology", "Gravel-containing medium rock" ], [ "Jingzhushan Group", "Lithology", "Chop sandstone" ], [ "Jingzhushan Group", "Lithology", "Fine-grained rock" ], [ "Jingzhushan Group", "Lithology", "Chop sandstone" ] ] }, { "text": "Brown-gray longinite mylonite, developmental mylonite and tensile threads, with eyeball texture structure, 5m", "triple_list": [ [ "brown grey longiel mylonite", "Develop", "Myrgonal facial" ], [ "brown grey longiel mylonite", "Develop", "Tensile threading" ], [ "brown grey longiel mylonite", "Develop", "Eye texture structure" ], [ "brown grey longiel mylonite", "thickness", "5m" ] ] }, { "text": "The upper part of the Daganshan Formation is composed of feldspar quartz sandstone and sericaceous shale. The top of it is limestone lens body or calcare siltstone. The basic stratigraphic sequence is rhythmic deposition composed of sand-silt-silt-silt.", "triple_list": [ [ "Dakanshan Group", "Lithology", "Feldspar quartz sandstone" ], [ "Dakanshan Group", "Lithology", "sericaceous shale" ], [ "Dakanshan Group", "Lithology", "Limestone lens body" ], [ "Dakanshan Group", "Lithology", "Calcium siltstone" ], [ "Dakanshan Group", "Lithology", "Sand-silt-mill" ] ] }, { "text": "Gray-red thin layer of calcium quartz silt sandstone, with small oblique stratigraphic, 4.1 m", "triple_list": [ [ "Gray-red thin layer of calcium quartz silts", "Develop", "Inclined layering" ], [ "Gray-red thin layer of calcium quartz silts", "thickness", "4.1 m" ] ] }, { "text": "Light blue-gray silty mudstone 29.2 m", "triple_list": [ [ "Light blue-gray silty mudstone", "thickness", "29.2 m" ] ] }, { "text": "Grey-red almond-shaped angamite, 1.0 m", "triple_list": [ [ "Grey-red almond-shaped yinganite", "thickness", "1.0 m" ] ] }, { "text": "Gray-black thin-middle silty sandstone with silty mudstone, 56.9 m", "triple_list": [ [ "Gray-black thin-middle silty sandstone interspersed with silty mudstone", "thickness", "56.9 m" ] ] }, { "text": "Classopollis-Dicheiroplis combination belt era was the early Cretaceous period.", "triple_list": [ [ "Classopollis-Dicheiroplis combination belt", "Age", "Early Cretaceous" ] ] }, { "text": "The profile is in an angle-inconsistent contact with the lower Cretaceous Doni Formation, and it is not topped.", "triple_list": [ [ "profile", "Unconformity contact", "Lower Cretaceous Doni Formation" ] ] }, { "text": "Gray thin layer of muddy silt sandstone and calcified coarse silt sandstone, 28.5 m", "triple_list": [ [ "Gray thin layer of muddy siltstone and calcified coarse siltstone", "thickness", "28.5 m" ] ] }, { "text": "The range of Nima is 87°00′88°30′English longitude, 31°00′32°00′North latitude, and an area of 15803.5 m2.", "triple_list": [ [ "Damn area", "Coordinates", "87°00′88°30′" ], [ "Damn area", "Coordinates", "31°00′32°00′" ], [ "Damn area", "area", "15803.5 m2" ] ] }, { "text": "Gray mudstone with thin layer of fine-grained quartz sandstone bioclass limestone, 90.7 m", "triple_list": [ [ "Gray mudstone with thin layer of fine-grained quartz sandstone bioclad limestone", "thickness", "90.7 m" ] ] }, { "text": "The Qingbaikou-Sindan-Stratigraphic strata are widely distributed in the Yunfu and Luoding-Xinyi-Yangchun areas.", "triple_list": [ [ "Qingbaikou-Shendan formation", "Located at", "Yunfu" ], [ "Qingbaikou-Shendan formation", "Located at", "Luo Ding-Xinyi-Yangchun" ] ] }, { "text": "Gray-green muddy silt sandstone Develop horizontal stratum 37.4 m", "triple_list": [ [ "Gray-green muddy siltstone", "Develop", "Horizontal streak layer" ], [ "Gray-green muddy siltstone", "thickness", "37.4 m" ] ] }, { "text": "The Downi Formation is shallow-marine clastic rock with volcanic rock", "triple_list": [ [ "Doni Group", "Lithology", "shallow-Coastal Clastite" ], [ "Doni Group", "Lithology", "Volcanic rocks" ] ] }, { "text": "Gray-green thin-medium-thick layered sheets of physical and chemical mica quartzite with yellow-brown, purple-red micro-thin layered quartz schist, >266.1m, no bottom is seen", "triple_list": [ [ "Gray-green thin-medium-thick layered sheets of physicochemical mica quartzite", "thickness", ">266.1m" ], [ "Gray-green thin-medium-thick layered sheets of physicochemical mica quartzite", "Contained", "Yellow-brown, purple-red micro-thin layered quartz schist" ] ] }, { "text": "Rock Develop horizontal stratigraphy and lenticular structure, limestone contains fossil fragments such as bivalve apriculi, and has strong biological disturbances and contains relatively abundant biological remains. Palaeophycus tubularis, Solithos verticalis, Cruziana sp.", "triple_list": [ [ "rock", "Develop", "Horizontal stratification" ], [ "rock", "Develop", "Lens condition" ], [ "rock", "Paleontological", "Bivalves" ], [ "rock", "Paleontological", "Acanthus" ], [ "rock", "Paleontological", "Biological relics Palaeophycus tubularis" ], [ "rock", "Paleontological", "Solithos verticalis" ], [ "rock", "Paleontological", "Cruziana sp." ] ] }, { "text": "The survey area is mainly produced in the Daganshan Group and the Tiger Tang Group in the Nanhua-Sinian period. The most species were obtained in the Tiger Tang Group, mainly containing Leiominuscula (Glossy Chlorella), Leiopsophosphaera (Chlorella), rachysphaera (Clossy Chlorella), rachysphaera (Clossy Chlorella).", "triple_list": [ [ "Dakanshan Group", "Age", "Nanhua-Zhendanji" ], [ "Tiger Pond Group", "Age", "Nanhua-Zhendanji" ], [ "Tiger Pond Group", "Paleontological", "Leiominuscula (Chlorella glossy)" ], [ "Tiger Pond Group", "Paleontological", "Leiopsophosphaera (Chlorophylla)" ], [ "Tiger Pond Group", "Paleontological", "rachysphaeridium (Rhodge Sphereus)" ] ] }, { "text": "Gray-white—Gray-green flaky quartzite with mica schist and quartz mica schist, 68.6m", "triple_list": [ [ "Gray-white—Gray-green flaky quartzite", "thickness", "68.6m" ], [ "Gray-white—Gray-green flaky quartzite", "Lithology", "Mica quartz schist" ], [ "Gray-white—Gray-green flaky quartzite", "Lithology", "Quartz mica schist" ] ] }, { "text": "The Carboniferous and Lower Permian system are mainly terrestrial clastic rocks.", "triple_list": [ [ "Carbonite", "Lithology", "Luyuan clastic rock" ], [ "Lower Permian", "Lithology", "Luyuan clastic rock" ] ] }, { "text": "Mudstone is rich in sporopollum Varirugosisporites tolmanensis Srivastava, 25.0 m", "triple_list": [ [ "Mudstone", "Paleontological", "Spore Varirugosisportes tolmanensis Srivastava" ], [ "Mudstone", "thickness", "25.0 m" ] ] }, { "text": "Gray thin plate-like fine-grained quartz sandstone and gray-black mudstone are interlayered, and they form a rhythmic layer, 510cm thick, 54.7m", "triple_list": [ [ "Gray thin plate-like fine-grained quartz sandstone and gray-black mudstone interlayer", "thickness", "54.7 m" ] ] }, { "text": "Dark gray almond-like andesite, the rock has a patchy structure and an almond-like structure.", "triple_list": [ [ "Dark gray almond-shaped andes", "Distribution pattern", "Spotted structure" ], [ "Dark gray almond-shaped andes", "Develop", "Almond-like structure" ] ] }, { "text": "Gray-black sheet mud slate with gray fine-grained quartz sandstone and gray-black mud crystal limestone lens body, 23.2 m", "triple_list": [ [ "Gray-black sheet-shaped mud slate with grey fine-grained quartz sandstone and gray-black mud crystal limestone lens", "thickness", "23.2 m" ] ] }, { "text": "Purple-red, gray-green, iron-containing mud crystal limestone 10.8 m", "triple_list": [ [ "Purple-red, gray-green, iron-containing mud crystal limestone", "thickness", "10.8 m" ] ] }, { "text": "The actual measured profile of the Samulu Formation of the upper Jurass-lower Cretaceous in Nima County is located at the Samulu Formation of the Riria Lu about 20 m northwest of Nima County. The starting coordinates are N31°57′16.4″, E87°07′55.5″, the end coordinates are N31°58′51.4″, E87°07′12.2″, and the section is about 3.5 m long. It is integrated and contacted with the lower Jurassic Ormonle Formation, and has not been seen above.", "triple_list": [ [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Located at", "Nima County about 20 m northwest of Riri Alu" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Coordinates", "N31°57'16.4″" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Coordinates", "E87°07'55.5″" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Coordinates", "N31°58′51.4″" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Coordinates", "E87°07'12.2″" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "length", "3.5 m" ], [ "The actual test profile of the Samulu Formation of the Riria Lu Upper Jurass-Lower Cretaceous in Nima County", "Integration of contacts", "Central Jurassic Russian Monle Group" ] ] }, { "text": "Gray-black silty mud silty silty sandstone and gray-black middle-layer silty microcrystalline limestone, 267.3 m", "triple_list": [ [ "Gray-black silty mud silty silty silty sandstone and gray-black middle-layer silty microcrystalline limestone", "thickness", "267.3 m" ] ] }, { "text": "The mudstone is rich in spores. Leiotriletes sp., Annulispora sp., Apicularisporites sp., Kluisporites sp., Classopollis sp., Pseudopicea sp., Cyathididites minor Couper, Baculatisporites sp., Stereisporites sp., etc.", "triple_list": [ [ "Mudstone", "Paleontological", "spore Leiotriletes sp." ], [ "Mudstone", "Paleontological", "Annulispora sp." ], [ "Mudstone", "Paleontological", "Apicularisporites sp." ], [ "Mudstone", "Paleontological", "Kluisporites sp." ], [ "Mudstone", "Paleontological", "Classopollis sp." ], [ "Mudstone", "Paleontological", "Pseudopicea sp." ], [ "Mudstone", "Paleontological", "Cyathididites minor Couper" ], [ "Mudstone", "Paleontological", "Baculatisporites sp." ], [ "Mudstone", "Paleontological", "Stereisporites sp." ] ] }, { "text": "In the western part of the upper section, the gray thin layer of fine-grained quartz sandstone fine-grained quartz sandstone and gray-black mud slate interlayer, with a small amount of silt sandstone. The sandstone contains insect traces Planolites montanus, and the mud slate contains sporesp. Classopollis sp., Annuispora sp., the basic layer sequence is sandstone → mud slate, with a thickness of 520.4 m.", "triple_list": [ [ "The upper western part", "Lithology", "Gray thin layer of fine-grained rock" ], [ "The upper western part", "Lithology", "quartz sandstone" ], [ "The upper western part", "Lithology", "Fine-grained quartz sandstone" ], [ "The upper western part", "Lithology", "Gray-black mud slate rock" ], [ "The upper western part", "Lithology", "Siltstone" ], [ "The upper western part", "thickness", "520.4 m" ], [ "sandstone", "Paleontological", "Planolites montanus" ], [ "Mud slate rock", "Paleontological", "Classopollis sp." ], [ "Mud slate rock", "Paleontological", "Annuispora sp." ] ] }, { "text": "Based on this, the era of the Kengping Xibi-horn porphyry system was placed in the Sinian period. The Leiominuscula minute-Leiopsophospaera minor group of biological strata was built by Nanyi (1993). Currently, 37 genera and 93 species of micro-params have been collected in the Yunkai Group strata.", "triple_list": [ [ "Kengping Xibi-angle porphyry system", "Age", "Zhendan" ], [ "Kengping Xibi-angle porphyry system", "Paleontological", "Leiominuscula minuteta — Leiopsphospaera minor combination" ] ] }, { "text": "Gray thin layer - thin plate-shaped quartz coarse silt sandstone with a small amount of gray-black sheet mud slate, 10.5 m", "triple_list": [ [ "Gray thin layer - thin plate-shaped quartz coarse silt sandstone with a small amount of gray-black sheet-shaped mud slate", "thickness", "10.5 m" ] ] }, { "text": "In the Aruo area, the main lithologies are gray-green silty mudstone and bioclastic limestone medium-grained quartz sandstone, containing bryozoosin Stenopora sp., and the thickness is greater than 263 m.", "triple_list": [ [ "Aruo", "Lithology", "Gray-green silty mudstone" ], [ "Aruo", "Lithology", "Bioclastic limestone" ], [ "Aruo", "Lithology", "Medium-fine grain quartz sandstone" ], [ "Aruo", "Lithology", "Bryomyces Stenopora sp." ], [ "Aruo", "thickness", "263 m" ] ] }, { "text": "Light gray thin layer of carbonaceous mud slate with light gray calcium slate 21.0 m2", "triple_list": [ [ "Light gray thin layer of carbonaceous mud slate with light gray calcium slate", "area", "21.0 m2" ] ] }, { "text": "The Pana Group era begins in the Eocene.", "triple_list": [ [ "Pana Group", "Age", "An Eternal World" ] ] }, { "text": "Light gray thick layer contains bioclass mud crystal limestone. The biological debris is mainly bivalve, with a size of 0.57 mm, a content of 5%, 10.5 m", "triple_list": [ [ "Light gray thick layer of bioclastic mud crystal limestone", "Paleontological", "Bio-shatter" ], [ "Light gray thick layer of bioclastic mud crystal limestone", "Paleontological", "Bivalves" ], [ "Light gray thick layer of bioclastic mud crystal limestone", "thickness", "10.5 m" ] ] }, { "text": "Dark gray-black feldspar quartz silt sandstone 24.9 m", "triple_list": [ [ "Dark gray-black feldspar quartz siltstone", "thickness", "24.9 m" ] ] }, { "text": "Light blue-gray medium-layer fine-grained feldspar quartz sandstone, developing parallel stratigraphic 53.8 m", "triple_list": [ [ "Light blue-gray medium-layer fine-grained feldspar quartz sandstone", "Develop", "Parallel layering" ], [ "Light blue-gray medium-layer fine-grained feldspar quartz sandstone", "thickness", "53.8 m" ] ] }, { "text": "Gray-green thin plate-shaped mud crystal limestone, layer mask mud crack insect hole, 2.5 m", "triple_list": [ [ "Gray-green thin plate-shaped mud crystal limestone", "Develop", "Mud cracks" ], [ "Gray-green thin plate-shaped mud crystal limestone", "Develop", "Insect hole" ], [ "Gray-green thin plate-shaped mud crystal limestone", "thickness", "2.5 m" ] ] }, { "text": "Gray medium-thin layer of calcified quartz silt sandstone, with wedge-shaped interlaced stratigraphic, 0.4 m", "triple_list": [ [ "Gray medium-thin layer of calcium quartz silt", "Develop", "Wedge-shaped interlaced layering" ], [ "Gray medium-thin layer of calcium quartz silt", "thickness", "0.4 m" ] ] }, { "text": "Light gray huge thick layer contains flint clumps and bioclass mud crystal limestone. The biological debris is mainly round worms and sponge bone needles, with a content of 5%.", "triple_list": [ [ "Light gray huge thick layer containing flint clumps containing biological debris mud crystal limestone", "Paleontological", "Bio-shatter" ], [ "Light gray huge thick layer containing flint clumps containing biological debris mud crystal limestone", "Paleontological", "Round worm" ], [ "Light gray huge thick layer containing flint clumps containing biological debris mud crystal limestone", "Paleontological", "Sponge bone needle" ] ] }, { "text": "Yellow-brown mica quartz schist with marble black carbonaceous thousand rock, 53.7m", "triple_list": [ [ "Tawny mica quartz schist", "Contained", "Marble black carbonaceous thousand rock" ], [ "Tawny mica quartz schist", "thickness", "53.7m" ] ] }, { "text": "Take the Dingrengabu profile in Shenya Township, Nima County as an example. The lithologies of this profile are mainly composed of crystalline tuff lava fusion crystalline tuff crystalline tuff crystalline tuff tuff crystalline tuff tuff tuff tuff crystalline tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff tuff", "triple_list": [ [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Crystal tuff lava" ], [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Melted crystalline tuff" ], [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Crystal tuff" ], [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Ying'an Rock" ], [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Rhyolite" ], [ "Dingrengabu profile in Shenya Township, Nima County", "Lithology", "Sedimentary rock" ] ] }, { "text": "There is a volcanic rock system in the area, with a thickness of about 930 m.", "triple_list": [ [ "Volcanic rock system", "thickness", "930 m" ] ] }, { "text": "Gray-red muddy siltstone, 2.5 m", "triple_list": [ [ "Gray-red muddy siltstone", "thickness", "2.5 m" ] ] }, { "text": "Soil gray silty mud slate, 77 m", "triple_list": [ [ "Soil gray silty mud slab", "thickness", "77 m" ] ] }, { "text": "In the area of Gaizedonbacuo, the Jingzhushan Formation is purple sandstone conglomerate with a thickness of 600-1650 m.", "triple_list": [ [ "If you change it, you will be wrong", "Outcrop", "Jingzhushan Group" ], [ "Jingzhushan Group", "Lithology", "Purple Sandstone" ], [ "Jingzhushan Group", "Lithology", "Polygon" ], [ "Jingzhushan Group", "thickness", "600-1650 m." ] ] }, { "text": "Gray-green thin-layer sheet physical and chemical mica microschist with tremolite green curtain stone horn rock, 135.3m", "triple_list": [ [ "Physical and chemical mica microschist with gray-green thin-layer flakes", "thickness", "135.3m" ] ] }, { "text": "The Doni Formation consists of three lithologic sections of limestone-clad rocks and volcanic rocks, with a thickness of about 3160 m.", "triple_list": [ [ "Doni Group", "Lithology", "Limestone" ], [ "Doni Group", "Lithology", "Clastite" ], [ "Doni Group", "Lithology", "Volcanic rocks" ], [ "Doni Group", "thickness", "3160 m" ] ] }, { "text": "The Upper Cretaceous system is exposed in the Mugagangri strata area of the Pangong Lake-Nujiang strata area and the Wurucuo strata area of the Gangdes-Tengchong strata area of the Bangor-Basu strata area. It is spread in an east-west belt-shaped manner on both sides of the Raja-Kangru fault, with an exposed area of about 370 m2.", "triple_list": [ [ "Upper Cretaceous", "Stratigraphical zoning", "Pangong Lake-Nujiang Stratigraphic Area Mugagangri Stratigraphic Area" ], [ "Upper Cretaceous", "Stratigraphical zoning", "Wurucuo strata community in Bangor-Basu strata area, Gangdise-Tengchong strata area" ], [ "Upper Cretaceous", "Exposed", "Raja-Kangru breaks both sides" ], [ "Upper Cretaceous", "Distribution pattern", "East-west belt-shaped cloth" ], [ "Upper Cretaceous", "area", "370 m2" ] ] }, { "text": "Gray-black fluid-brocytic tuff lava, 20.3 m", "triple_list": [ [ "Gray-black flow-grained breccia crystal tuff lava", "thickness", "20.3 m" ] ] }, { "text": "Xinyisi Heshikou uses blue-gray mica quartz schist mica quartzite as the main lens body with oblique elongated amphibole and marble.", "triple_list": [ [ "Xinyisi Heshiwu", "Lithology", "Blue-gray mica quartz schist mica quartzite" ], [ "Blue-gray mica quartz schist mica quartzite", "Contained", "oblique angular amphibole" ], [ "Blue-gray mica quartz schist mica quartzite", "Contained", "Marble lens body" ] ] }, { "text": "The 3-layer sequence is located in the middle of the pull-down group (59th floor of the 59th section of the juvenile section), consisting of the marine invasion system domain and the high water level system domain, with a thickness of about 185 m.", "triple_list": [ [ "3-layer sequence", "Located at", "Pull down group center" ], [ "3-layer sequence", "Contained", "Maritime invasion system" ], [ "3-layer sequence", "Contained", "High water level system domain" ], [ "3-layer sequence", "thickness", "185 m" ] ] }, { "text": "The sedimentary combination of subtidal-intertidal zones is represented by the lower part of the Oshar-Bo Formation. The main lithologies are gray-gray yellow thin-thick-layer fine-grained quartz sandstone conglomerates, gravel-containing fine-grained rock sandstone feldspar sandstone, and gray-black silty mudstone intersected silty sandstone lens body.", "triple_list": [ [ "Subtidal-intertidal debris deposition combination", "Contained", "Russia kills and reorganizes the lower part" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Gray-gray yellow thin-thick layer of fine-grained quartz sandstone" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Polygon" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Gravel-containing fine rock" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Chop sandstone" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Feldspar rock" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Chop sandstone" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Gray-black silt mudstone" ], [ "Russia kills and reorganizes the lower part", "Lithology", "Siltystone lens body" ] ] } ]