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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1388.txt | ":{"id":"sect0090"},"_":"Garnet-bearing paragneiss"}]}]},{"#name":"entry","$":{"id":"sec0080","depth":"2"},"$$":[{"#name":"label","_":"4.6"},{"#name":"title","$":{"id":"sect0095"},"_":"Metamorphosed and deformed SMB granites (metaSMB)"}]}]},{"#name":"entry","$":{"id":"sec0085","type":"sections","depth":"1"},"$$":[{"#na... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_87.txt | 0.004 0.76 1491 27 1460 21 97.9
| |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_69.txt | nz 1093±6 Am Nodular gneiss, Snarum, B0030 U-Pb SIMS 9 Bingen et al., 2008
Kongsberg Mnz 1095±12 Am Nodular gneiss, Snarum, B0030 U-Pb LA-ICPMS 10 Bingen et al., 2008
Kongsberg Zrn 1102±28 Am Quartzite, Snarum, N95129 U-Pb SIMS 1 Bingen et al., 2001
Kongsberg Moly 1112±4 Am S | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_8.txt | zircon from 10 samples.
from a highly deformed section (strong lineation and
foliation parallel to regional NW-SE structural pattern,
occurrence of 1-10 m layers of amphibolite parallel to
foliation) in the Røldal valley yields an age of 1495 ± 13
Ma for magmatic activity in this gneiss complex (sample
B00-127; Tables... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_52.txt | granite pluton
The Idefjorden Terrane hosts two large post-collisional
granite plutons (Fig. 4), the Bohus-Iddefjorden pluton to
the east of the Oslo rift (Eliasson & Schöberg 1991; Eliasson et al. 2003) and the Flå pluton to the west of the Oslo
rift (Smithson 1963; Nordgulen 1999). The Flå pluton
(c. 70 x20 km in si... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_25.txt | 85 1608 23 1665 18 3.4
12 9093 0.10224 1.0 4.029 1.8 0.2858 1.5 0.83 1621 21 1665 19 2.7
08 16105 0.10464 0.9 4.128 1.7 0.2861 1.4 0.85 1622 21 1708 17 5.0
21 15508 0.10388 1.1 4.124 1.7 0.2879 1.4 0.80 1631 20 1695 19 3.7
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_0.txt | Introduction
The Sveconorwegian orogen of SW Scandinavia
represents a truncated and comparatively small segment of the global Grenvillian belt. The Sveconorwegian orogen results from a collision between
Fennoscandia and an unknown craton at the end of the
Mesoproterozoic (1.1-1.0 Ga). It consists of latePalaeoproterozo... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_80.txt | t granite gneiss H Zrn 1649 +33/-19 Ragnhildstveit et al., 1994
(1) T: Telemark sector, H: Hardangervidda sector, S: Suldal sector, R: Rogaland-Vest Agder sector
| |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_27.txt | 191 2.0 0.2978 1.6 0.78 1680 23 1662 24 -1.1
FUN26, granite
01p,x 4681 0.09507 1.1 2.197 3.4 0.1676 3.2 0.94 999 30 1529 21 35
15p,x 10359 0.10472 0.9 2.706 2.3 0.1874 2.1 0.92 1107 22 1709 17 35
06p 10227 0.10282 0.8 3.327 2.1 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_581.txt | class="Introduction u-font-serif text-s u-margin-l-ver"><h2 class="u-h4 u-margin-s-bottom">Introduction</h2><section id="sec0005"><p id="par0025">The Late Mesoproterozoic features widespread orogenesis across many continents that is generally ascribed to the formation of a supercontinent named Rodinia (e.g. Li et al.,... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_9.txt | 32.
Skår, Ø. 2002: U-Pb geochronology and geochemistry of early-Proterozoic rocks of the tectonic basement windows in central
Nordland, Caledonides of north-central Norway. Precambrian
Research 116, 265-283.
Skår, Ø. & Pedersen, R.B. 2003: Relations between granitoid magmatism and migmatization: U-Pb geochronological e... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1160.txt | of SW Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Contrib. Mineral. Petrol."}]},{"#name":"volume-nr","_":"132"}]},{"#name":"date","_":"1998"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"336"},{"#name":"last-page","_":"353"}]... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_998.txt | ":"0.25"}},{"#name":"__text__","_":"Ma) for the Rincón del Tigre–Huanchaca large igneous province (LIP) of the Amazonian Craton: Implications for the Rodinia supercontinent"}]}],"floats":[],"footnotes":[],"attachments":[]},"openArchive":false,"openAccess":false,"document-subtype":"fla","content-family":"serial","conten... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_95.txt | ble Nelaug granitic gneiss, t beige Am 207Pb/206Pb 1 994 ±30 de Haas et al., 2002
Bamble Nelaug granitic gneiss, t orange-red Am 207Pb/206Pb 1 1090.9 ±1.9 de Haas et al., 2002
Bamble Calc-silicate gneiss, Kragerø, 92-1, Sph921 Am 207Pb/206Pb 1 1105 ±2 Cosca et al., 1998
Bamble Peg | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_82.txt | 3.3509 1.64 0.25654 1.44 0.88 1523 15 1472 19 96.7
08b 155 48 52 66310 0.09496 0.84 3.6934 1.33 0.28210 1.04 0.78 1527 16 1602 15 104.9
23a 151 42 46 16452 0.09517 0.80 3.3558 1.66 0.25573 1.45 0.88 1531 15 1468 19 95.9
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_70.txt | ogaerts, M., Scaillet, B. & Vander Auwera, J. 2006: Phase equilibria
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Bogdanova, S., Bingen, B., Gorbatschev, R., Kheraskova, T., Kozlov, V.,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_548.txt | email or social media contact details icon" width="20" height="20" class="icon icon-envelope react-xocs-author-icon"><path d="m55.8 57.2c-1.78 1.31-5.14 1.31-6.9 0l-31.32-23.2h69.54l-31.32 23.19zm-55.8-24.78l42.94 32.62c2.64 1.95 6.02 2.93 9.4 2. | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_55.txt | ; eu: euhedral; f: faceted; i: inclusion present; l-pr: long prismatic; pb: pale brown; pr: prismatic; s-pr: short prismatic; t-pr: tips from prism. (2) Concentrations are known to ±30% for sample weights of 30 µg and ±50% for samples <3µg. (3) Corrected for 0.0215 mole fraction common-Pb in the 205Pb-235U spike. (4) C... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_3.txt |
Ragnhildstveit, J., Naterstad, J., Jorde, K. & Egeland, B. 1998: Geologisk
kart over Norge, berggrunnskart Haugesund, 1:250000. Norges
geologiske undersøkelse, Trondheim.
Romer, R.L. 1996: Contiguous Laurentia and Baltica before the
Grenvillian-Sveconorwegian orogeny? Terra Nova 8, 173-181.
Romer, R. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_69.txt | , S Norway: U-Pb, Th-Pb and ReOs data. Norwegian Journal of Geology 88, 13-42.
Bogaerts, M., Scaillet, B., Liégeois, J.P. & Vander Auwera, J. 2003: Petrology and geochemistry of the Lyngdal granodiorite (Southern Norway) and the role of fractional crystallization in the genesis of Proterozoic ferro-potassic A-type gran... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_643.txt | class="series">(2013)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>M.N. </span>Ducea</span><em> et al.</em></span><h3 class="title">Igniting flare-up events in Cordilleran arcs</h3><span class="host u-clr-grey6 u-font-sans"><div class="se... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_933.txt | references therein). This orogenic event – the Sveconorwegian orogeny – is commonly interpreted to reflect a continent–continent collision between Baltica–Laurentia on one side and a third continent,"}]}]}]},{"#name":"section","$$":[{"#name":"section","$":{"xmlns:ce":true,"xmlns:mml":true,"xmlns:xs":true,"xmlns:xlink"... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_27.txt | 0956 0.0089 3.20 0.33 0.243 0.011 0.43 1540 177 1401 56 90.9
B00-144, augen gneiss, Suldal, Fig. 10J
7 0.0699 0.0027 1.74 0.07 0.180 0.002 0.29 927 80 1068 12 115.3
11 0.0713 0.0026 1.66 0.07 0.169 0.003 0.40 966 74 1004 15 103.9
10 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_48.txt | ic floor below the Idefjorden
terrane. The 1.19-1.13 Ga association of continental
bimodal magmatism and sediments in Telemarkia
indicates that Telemarkia was affected by continental
100 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
extension (Basin and Range-type extension; Bingen et
al. 2003) before the collision eve... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_167.txt | rust-pc-sdk.ot-pc-footer button{margin:8px 0;background-color:#fff}div#onetrust-pc-sdk.ot-pc-footer-logo{background-color:#fff}div#onetrust-pc-sdk #ot-lst-title span{font-size:24px;font-weight:400;line-height:32px}div#onetrust-pc-sdk #ot-host-lst.ot-host-desc,div#onetrust-pc | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_669.txt | ;12.0, K = 19.4) were assigned 1090 Ma, 1000 Ma, and 900 Ma ages, respectively. The new Bamble paleomagnetic pole reconstructs Baltica at ∼ 1090 Ma with noticeable latitudinal gap from the eastern Laurentian margin and thus does not support classical Baltica-Laurentia configurati... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen3.txt | part3 -------------------
Composition[edit]
Structure of a vanadium porphyrin compound (left) extracted from petroleum by Alfred E. Treibs, father of organic geochemistry. The close structural similarity of this molecule and chlorophyll a (right) helped establish that petroleum was derived from plants.
Kerogen is a com... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1192.txt | $$":[{"#name":"first-page","_":"247"},{"#name":"last-page","_":"257"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0115"},"$$":[{"#name":"label","_":"Gower et al., 2008"},{"#name":"reference","$":{"id":"sbref0115","refId":"23"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1342.txt | Nelson"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H.K."},{"#name":"surname","_":"Brueckner"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.P."},{"#name":"surname","_":"LeHuray"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Patagonian batholith at 48°S, Chile; geochemical and isotopic va... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_488.txt | .29-0.4 2.08-0.4 2.28 0 2.48 1.15 2.54 3.43 0.03 1.19 0.03 3.17 0.03 3.17 0.03 3-0.1 6.47-0.1 6.47h2.54c0 0 0.07-4.49 0.07-6.96 0-1.48 0.03-2.97-0.1-4.46C63.31 7.43 61.49 6.57 58 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_41.txt | 11 Andersson et al., 2002
South Migmatite granitic gneiss, Högabjär, mesosome HB1 Zrn U-Pb 1686 ±12 Möller et al., 2007
North Rhyolite, Hukusjøen, FUN33 Zrn U-Pb 1687 ±11 Bingen et al., this work
Centre Quartz-monzonite gneiss, Zachrisdal, AL84030 Zrn U-Pb 1688 ±10 Persson et al., 1995
North Tors | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_496.txt | 6.6M145.87 14.13c0-5.18-1.42-7.56-6.01-7.56 -3.86 0-6.67 2.77-6.67 7.92 0 4.92 2.97 7.82 6.73 7.82 2.81 0 4.36-0.63 5.68-1.42l-0.2-2.31c-0.89 0.79-2.94 1.55-4.69 1.55 -3.14 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1030.txt | folds are commonly S-vergent, but symmetric folds with different degrees of tightness are also present. Melt was present at all stages of deformation and the structural relations demonstrate mutual feedback between melt localization and fold formation. F2 folds have shallowly E-plunging fold axis parallel to a stretch... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_909.txt | generally have juvenile Hf isotopic compositions associated with varying δ"},{"$":{"loc":"post"},"#name":"sup","_":"18"},{"#name":"__text__","_":"O values of 4.5–9‰, consistent with subduction-accretion processes involving significant sedimentary recycling. This accretionary margin was most likely transformed into the... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1462.txt | -2"> <label class="ot-switch" for="ot-group-id-2"><span class="ot-switch-nob" aria-checked="true" role="switch" aria-label="Performance Cookies"></span> <span class="ot-label-txt">Performance Cookies</span></label> </div></div><!-- accordion detail --><div class="ot-acc-grpcntr ot-acc-txt"><p class="ot-acc-grpdesc ot-c... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen10_0.txt | part10 -------------------
See also[edit]
Asphaltene – Heavy organic molecular substances that are found in crude oil
Oil shale geology – Branch of geology
Petroleum geology – Study of the origin, occurrence, movement, accumulation, and exploration of hydrocarbon fuels
Tholin – Class of molecules formed by ultraviolet ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_645.txt | "><h3 class="title">Nor. Geol. Unders.</h3></div><div class="series">(1982)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="author u-font-sans"><span>T. </span>Falkum</span><h3 class="title">The Sveconorwegian magmatic and tectonometamorphic evolution of the high grade Proterozoic Flekkefjord ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_922.txt | \"><span class=\"anchor-text\">Publishing Ethics Policies</span></a> page. View our <a class=\"anchor u-display-inline anchor-alternative\" href=\"https://www.elsevier.com/researcher/author/submit-your-paper\" target=\"_blank\"><span class=\"anchor-text\">Publishing with Elsevier: step-by-step</span></a> page to learn ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_47.txt | rsdalen district demonstrates granulite-facies conditions at 973 ±4 Ma, probably related to decompression biotite dehydration-melting
following M1 metamorphism (0.55 GPa-800 °C; Bingen
& Stein 2003). (3) Zircon included in cordierite coronas
around garnet dates regional decompression at 955 ±8
Ma following M1 metamorph... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_118.txt |
Fig. 7. Sketchmap showing the distribution of magmatic rocks and sedimentary basins between 1220 and 1140 Ma shortly before the
Sveconorwegian orogeny.
58 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 8. Sketchmaps showing the distribution of metamorphism, magmatic
rocks and sedimentary basins during
the Svecono... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_60.txt | Sm-Nd 855 ±59 Walderhaug et al, 1999
Rogaland Rymteland pegmatite Urn U-Pb 914 ±6 Pasteels et al., 1979
Rogaland Egersund-Ogna anorthosite, margin 75-32 Bdl U-Pb 915 ±4 Schärer et al., 1996
Telemark Tørdal granite, 082996-1 Zrn U-Pb 918 ±7 Andersen et al., 2007
Rogaland Tellnes dyke, ilmenite | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_742.txt | "></path></svg></button></div></section><section class="RelatedContentPanel u-margin-s-bottom"><header id="metrics-header" class="related-content-panel-header u-margin-s-bottom"><button class="button-link related-content-panel-toggle is-up button-link-primary button-link-icon-right" type="button" aria-expanded="true"><... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen2.txt | part2 -------------------
Formation[edit]
Kerogen is formed during sedimentary diagenesis from the degradation of living matter. The original organic matter can comprise lacustrine and marine algae and plankton and terrestrial higher-order plants. During diagenesis, large biopolymers from, e.g., proteins, lipids, and c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_53.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_16.txt | Masses 202Hg, 204(Hg + Pb),
206Pb, 207Pb, 208Pb, 232Th and 238U are measured. The
interference between 204Pb and 204Hg contained in the
Ar gas is corrected by monitoring 202Hg and assuming
a 204Hg/202Hg ratio of 0.2293. A 60 sec gas blank analysis
is performed between each zircon analysis. The measured
isotope ratios ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_22.txt | uge, J.F., Storey, C.D. & Parrish, R.R.
2004: Mesoproterozoic bimodal volcanism in SW Norway,
evidence for recurring pre-Sveconorwegian continental margin
tectonism. Precambrian Research 134, 249-273.
Baadsgaard, H., Chaplin, C. & Griffin, W.L. 1984: Geochronology of
the Gloserheia pegmatite, Froland, southern Norway. ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_972.txt | __text__","_":"Ma event, which saw the convergence and final amalgamation of those combined cratons with the South Australian Craton. Well-defined Nd- and Hf-isotopic evolution arrays for the Musgrave Province reflect a juvenile basement with distinct 1950–1900, 1600–1550"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"_... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_6.txt | NAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 87
Timing of continental building in the Sveconorwegian
orogen, SW Scandinavia
Bernard Bingen, Øyvind Skår, Mogens Marker, Ellen M. O. Sigmond, Øystein
Nordgulen, Jomar Ragnhildstveit, Joakim Mansfeld, Robert D. Tucker &
Jean-Paul Liégeois
Binge... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_45.txt | Berkley.
Lundqvist, I. & Skiöld, T. 1993: U-Pb zircon dating of volcanic rocks of
the Åmål Group, western Sweden. In Lundqvist, T. (ed.), Radiometric dating results, C823, 24-30. Sveriges Geologiska Undersökning,
Uppsala.
Lundqvist, T. & Persson, P.-O. 1999: Geochronology of porphyries and
related rocks in northern an... |
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