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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_878.txt | ":[{"$$":[{"#name":"__text__","_":"A total of 4344 magmatic U-Pb ages in the range 2300 to 800 Ma have been compiled from the Great Proterozoic Accretionary Orogen along the margin of the Columbia / Nuna supercontinent and from the subsequent Grenvillian collisional orogens forming the core of Rodinia. The age data are... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_26.txt | .003 0.59 1103 53 1045 19 94.7
8 0.0927 0.0021 3.44 0.12 0.269 0.007 0.76 1482 42 1538 36 103.8
5 0.0939 0.0014 3.21 0.07 0.248 0.003 0.66 1506 29 1428 17 94.8
6 0.0944 0.0011 3.22 0.05 0.247 0.003 0.66 1516 22 1424 13 93.9
3 0. | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_48.txt | the Rjukan
group. Along the Åmot-Vardefjell shear zone limiting
the Telemark sector to the NE, the Hallingdal gneiss and
quartzite complex is exposed (Fig. 3). A quartzite sample
from this complex contains detrital zircons ranging
from 3.13 to 1.71 Ga (Bingen et al. 2001a). The data
indicate that this complex was depo... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1148.txt | ":[{"#name":"label","_":"Bingen et al., 2005"},{"#name":"reference","$":{"id":"sbref0040","refId":"8"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"B."},{"#name":"surname","_":"Bingen"}]},{"#name":"author","$$":[{"#name":"given-nam... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_38.txt | 35 19 1704 14 4.0
18p 16215 0.10315 0.8 4.137 1.5 0.2909 1.3 0.86 1646 18 1681 14 2.1
21 19469 0.10490 0.8 4.217 1.6 0.2916 1.4 0.85 1649 20 1713 15 3.7
13 24932 0.10379 0.9 4.176 1.5 0.2918 1.2 0.81 1651 18 1693 16 2.5
08 115 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_22.txt | veconorwegian contractional tectonics: examples from southern Norway. Precambrian Research 133,
207-222.
Hoffman, P.F. 1991: Did the breakout of Laurentia turn Gondwanaland inside-out? Science 252, 1409-1412.
Högdahl, K., Andersson, U.B. & Eklund, O. 2004: The Transcandinavian Igneous Belt (TIB) in Sweden: a review of ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_4.txt | ithologies were assembled during the Gothian accretionary event (Andersen et al. 2004a; Åhäll & Connelly 2008;
Bingen et al. 2008a). The timing of Gothian amphibolitefacies metamorphism is estimated at 1540 Ma (Table 4;
Åhäll & Connelly 2008; Bingen et al. 2008b). The 1660-
1520 Ma lithologies are overlain by the poorl... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_39.txt | 2007b; Fig. 4). Titanite ages
at c. 913 to 901 ±7 Ma in this gneiss complex attest to
late-Sveconorwegian high-grade metamorphism (Fig. 4;
Table 5; Heaman & Smalley 1994; Bingen et al. 1998).
The Rogaland-Vest Agder sector is characterized by
amphibolite- to granulite-facies metamorphism. Four
isograds reflect an incre... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_946.txt | of the belt. Microprobe data on plagioclase and hornblende were acquired on a CAMECA SX100 instrument at the Microsonde Ouest, in Brest, France. The operating conditions were 15"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"kV and 20"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"nA with a... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_285.txt | ,#onetrust-pc-sdk.ot-pli-hdr~.ot-cat-item.ot-cat-header+.ot-tgl{padding-left:28px}#onetrust-pc-sdk.ot-sel-all-hdr,#onetrust-pc-sdk.ot-sel-all-chkbox{display:inline-block;width:100%;position:relative}#onetrust-pc-sdk.ot-sel-all-chkbox{z-index:1}# | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_45.txt | ±7 Söderlund et al., 1999
Brustad augen gneiss, Br9602 Zrn 1674 ±10 Alm et al., 2002
Mårdaklev granitic gneiss Zrn 1676 ±10 Söderlund et al., 2002
Filipstad granite gneiss, 604 Zrn 1676 ±7 Lindth et al., 1994
Gällared N, veined gneiss Zrn 1679 ±13 Söderlund et al., 2002
Hagfors granite gneiss, 602 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_62.txt |
Rogaland Hidra monzonorite, charnockite dyke Zrn U-Pb 931 ±10 Pasteels et al., 1979
Rogaland Helleren anorthosite, 75-65 Zrn U-Pb 932 ±3 Schärer et al., 1996
Rogaland Åna-Sira anorthosite, 92-21 Zrn U-Pb 932 ±3 Schärer et al., 1996
Telemark Vehuskjerringa granite, 072496-1 Zrn U-P | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_672.txt | 26822001395"><span class="anchor-text">Anorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwegian continental back-arc setting</span></a></h3><div class="text-s">2022, Precambrian Research</div><div class="CitedSection u-margin-s-top"><div clas... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1320.txt | "},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Torske"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The South Norway Precambrian region – a Proterozoic coredilleran-type orogenic segment"}]}]}... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_24.txt | Andersson et al., 1999
South Undeformed granite dyke, Högabjär, HB6 Zrn U-Pb 952 ±7 Möller et al., 2007
South Undeformed granite dyke, Gällared Zrn Pb-Pb 956 ±7 Möller & Söderlund, 1997
PZ Görbjörnarp syenite Zrn U-Pb 1204 +14/-8 Hansen & Lindh, 1991
PZ Gumlösa-Glimåkra granite | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1210.txt | title","$$":[{"#name":"maintitle","_":"Contrib. Mineral. Petrol."}]},{"#name":"volume-nr","_":"116"}]},{"#name":"date","_":"1994"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"433"},{"#name":"last-page","_":"447"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0145"},"$$":[{"#name":"label","_":"Johansson, 2009"}... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_9.txt | b-Sr errorchron for protolith formation in the Røldal
valley (Berg 1977).
In the Skånevik area (Fig. 5; Mortensen 1942), a thin
belt of weakly deformed metavolcanic rocks ranges in
composition from basalt to andesite to rhyolite. The
metavolcanic rocks are interlayered with metastandstone,
metatuffite, metaconglomerate... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_55.txt | 0.5-2 cm) subhedral megacrysts of microcline. Rounded mafic enclaves
of medium- to fine-grained diorite occur some 20-30 m
away from the sampling site. Three zircon fractions, collected in a population of prismatic pale-brown zircon,
yield concordant analyses with an average 207Pb/206Pb age
of 928 ±3 Ma (Fig. 5). This... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen5.txt | part5 -------------------
Physical properties[edit]
These changes in composition and microstructure result in changes in the properties of kerogen. For example, the skeletal density of kerogen increases from approximately 1.1 g/ml at low thermal maturity to 1.7 g/ml at high thermal maturity. This evolution is consiste... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_69.txt | (Pb, Sr, Nd, Hf)
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_152.txt |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_51.txt | phenoclasts commonly larger than 1 cm separated by
shear bands rich in fine-grained quartz and biotite. Metamorphic epidote is present in the matrix of the sample
and reflects amphibolite-facies overprint. Zircon is prismatic, with no sign of a metamorphic rim. Twentyfour
analyses of zircon yield a 207Pb/206Pb age of 1... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_392.txt | r.ot-acc-txt,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1158.txt | ":"1998"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"143"},{"#name":"last-page","_":"154"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0055"},"$$":[{"#name":"label","_":"Bingen and van Breemen, 1998b"},{"#name":"reference","$":{"id":"sbref0055","refId":"11"},"$$":[{"#name":"contribution","$":{"langtype":"en... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_33.txt | 13 17 2.4
10 23958 0.10382 0.7 4.271 1.6 0.2984 1.4 0.89 1683 21 1694 13 0.6
20 1755 0.10510 2.0 4.354 2.4 0.3004 1.4 0.57 1694 20 1716 36 1.3
04 14985 0.10382 0.8 4.304 1.5 0.3006 1.3 0.84 1694 19 1694 16 -0.1
12 6966 0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1449.txt | -floating-button__svg-fill" d="M14.588 0l.445.328c1.807 1.303 3.961 2.533 6.461 3.688 2.015.93 4.576 1.746 7.682 2.446 0 14.178-4.73 24.133-14.19 29.864l-.398.236C4.863 30.87 0 20.837 0 6.462c3.107-.7 5.668-1.516 7.682-2. | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_84.txt | en, B., Demaiffe, D., Liégeois, J.P., Hertogen, J., Weis,
D. & Michot, J. 1995: The 1160 Ma old Hidderskog meta-charnockite: implications of this A-type pluton for the Sveconorwegian belt
in Vest Agder (SW Norway). Lithos 36, 51-66.
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_475.txt | T2uHq_M1r-XQq8htU6Z3GjHfE" style="white-space: pre-wrap;"></style></head>
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_18.txt | /235U=137.88. The ISOPLOT
program (Ludwig 2001) was used to generate concordia
diagrams and average ages.
Granitoids from the Eastern Segment
Few geochronological data are available in the northernmost Norwegian part of the Eastern Segment, known as
the Solør Complex (Heim et al. 1996; Nordgulen 1999;
Mansfeld 2000; Al... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_39.txt | 81 0.10193 0.8 4.110 1.8 0.2924 1.6 0.88 1654 23 1660 15 0.3
15 39170 0.10422 0.9 4.206 1.7 0.2927 1.4 0.86 1655 21 1701 16 2.7
07 19559 0.10450 0.9 4.228 1.6 0.2934 1.3 0.83 1659 19 1706 16 2.7
10 22466 0.10456 0.8 4.237 1 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_108.txt | ) selected date
(4) n: number of analysed fractions
Table 5. Compilation of titanite U-Pb data in the Sveconorwegian belt.
57
In the northernmost part of the Eastern Segment (Solør
Complex), no significant Sveconorwegian metamorphism has been detected except in the vicinity of the
Mylonite Zone and other local shear zo... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_466.txt | ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy a,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_28.txt |
The Telemarkia Terrane (Fig. 1) is characterized by a
voluminous 1520-1480 Ma magmatic event (Fig. 6;
Table 3; Bingen et al. 2005), referred to as the Telemarkian event by Bingen et al. (2008a). No older magmatic
rocks are positively identified. The 1520-1480 Ma volcanic and plutonic suites have a poorly defined geoch... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_75.txt | .50 0.26074 1.42 0.95 1489 9 1494 19 100.3
13b 475 341 165 109487 0.09319 0.42 3.4349 1.48 0.26733 1.42 0.96 1492 8 1527 19 102.4
12a 135 53 43 22879 0.09361 0.75 3.3406 1.60 0.25882 1.41 0.88 1500 14 1484 19 98.9
06a 257 132 83 29983 0.09370 0.52 3.36 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_47.txt | as evident from the Gothian units of the
Østfold-Akershus sector, SE Norway. Journal of Conference Abstracts
4 (1), 137.
Mansfeld, J. 2000: 200 m.y. of episodic crustal growth in the ØstfoldAkershus sector, SE Norway 24 Nordiske Geologiske Vintermøte, 6-9
Jan 2000, 115. Norwegian Geological Society, Geonytt, Trondheim... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_51.txt | ,t-pr 4 52.5 234 2 0.39 15527 0.09242 6 3.22034 418 0.25190 32 1476.0 1.1 4.3
4 2gr,+75,pb,t-pt 4 66.4 260 3 0.46 5627 0.09222 7 3.06422 464 0.24100 33 1471.8 1.4 9.8
S93-338, Ullensvang group metarhyolite, Fig. 8F
1 3gr,-75, | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_74.txt | , J.L. 1971: Le facies granulite en Norvège méridionale. 1. Les
associations minéralogiques. Lithos 4, 239-249.
Tucker, R.D., Krogh, T.E. & Råheim, A. 1990: Proterozoic evolution and
age - province boundaries in the central part of the Western Gneiss
Region, Norway: results of U–Pb dating of accessory minerals from
Tro... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_28.txt | return!(e && e instanceof Function && e.apply &&!e[o]);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1018.txt | ":{"id":"aut0010"},"$$":[{"#name":"given-name","_":"Aránzazu"},{"#name":"surname","_":"Piñán-Llamas"},{"#name":"cross-ref","$":{"id":"crf0110","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]}]},{"#name":"author","$":{"id":"aut0015"},"$$":[{"#name":"given-name","_":"Charlotte"},{"#name":"surname","_... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_686.txt | 10<!-- --> <!-- -->000-km-long external active continental margin of Columbia from its assembly at ca. 1800 Ma until its dispersal at ca. 1260 Ma, after which all cratons studied were involved in the Rodinia-forming Grenvillian orogeny. However, the magmatic record is not smooth and even but highly irre... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_48.txt | (window.pageData && pageData.search && pageData.search.facets) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_913.txt | word","$":{"id":"kw0010"},"$$":[{"#name":"text","_":"SW Norway"}]},{"#name":"keyword","$":{"id":"kw0015"},"$$":[{"#name":"text","_":"Granitic batholith"}]},{"#name":"keyword","$":{"id":"kw0020"},"$$":[{"#name":"text","_":"Geochronology"}]},{"#name":"keyword","$":{"id":"kw0025"},"$$":[{"#name":"text","_":"Petrography"}]... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1017.txt | "}]},{"#name":"cross-ref","$":{"id":"crf0105","refid":"cor0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"⁎"}]},{"#name":"e-address","$":{"id":"eadd0005","type":"email"},"_":"lorraine.tual@geol.lu.se"},{"#name":"e-address","$":{"id":"eadd0010","type":"email"},"_":"lorraine.tual@gmail.com"}]},{"#name":"author","$ | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_2.txt | reconstructions, involve an
oblique collision between a common Laurentia-Baltica
margin and the Amazonia indenter.
This paper reviews available geochronological data on
magmatic and metamorphic events in the Sveconorwegian Belt. New zircon U-Pb data are also reported on a
few samples to complete this information. The ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_87.txt | , granodioritic gneiss, B00140 Zrn U-Pb 1519 ±12 Bingen et al., 2005
Vardefjell SZ Flå, tonalitic banded gneiss, B99111 Zrn U-Pb 1528 ±16 Bingen et al., 2008
Bamble and Kongsberg Terranes
Bamble Herefoss granite Zrn U-Pb 920 +16/-27 Andersen et al., 2002
Bamble Herefoss granite, 107 Ttn U-Pb 926 ± | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1133.txt | "}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"A summary of the critical relations in the central part of the Sierra Nevada Batholith, California, U.S.A."}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Geol. Soc. Am. Mem."}]},{"#name":... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_111.txt | y = n.Yu.ST,
w = "-start",
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x = "-body",
E = "cb" + A,
T = "jsTime",
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1062.txt | o0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$$":[{"#name":"__text__","_":"Peak metamorphic conditions of the pelitic granulite estimated at 11.5–15"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"kbar, 810–860"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"°C."}],"$":{"vie... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_47.txt | charnockitic Zrn U-Pb 1796 ±7 Stephens, in Söderlund et al., 1999
(1) Telemarkia Terrane: Vardefjell SZ: Vardefjell Shear Zone, Rogaland: Rogaland Vest Agder Sector
Eastern Segment: North: Solør transect, Centre: Lake Vänern transect, South: South of Vårgårda, PZ: Protogine Zone
SFDZ: Sveconorwegian Frontal Deformatio... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_99.txt | if (prodList[i].referenceModuleTitle) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_38.txt | 405.
Ludwig, K.R. 2001: Users manual for Isoplot/Ex version 2.49, a
geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center, Special Pubication No. 1a, Berkley.
Lundmark, A.M., Corfu, F., Spürgin, S. & Selbekk, R. 2007: Proterozoic
evolution and provenance of the high-grade Jotun Nappe Complex, SW N... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_462.txt | -cookie-policy tr{margin:0 0 1em 0}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy td:before{height:100%;width:40%;padding-right:10px}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy td:before{content:attr(data-label);font-weight:bold}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy li{word-break: | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_145.txt | " href="https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/103/images/favSD.ico" type="image/x-icon">
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_546.txt | 9.38h10.04l-0.93-10.34c-2.15-20.43-20.14-31.66-51.03-31.66s-48.89 11.22-51.05 31.73l-0.91 10.27h10.03m41.93-102.29c-9.72 0-18.24 8.69-18.24 18.59 0 13.67 7.84 23.98 18.24 23.98s18.24-10.31 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_9.txt | belt.
Agder phase, 1050-980 Ma
The main Sveconorwegian orogenic event, here called
the Agder phase, took place between 1050 and 980 Ma
(Figs. 8 b, c). It probably resulted from an oblique (?)
continent-continent collision between Fennoscandia and
another large continent, possibly Amazonia (Fig. 9). This
phase correspo... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_32.txt | ØS9914 Z4510 ØS99316 Larvik Date of Age ±2σ n dev Age ±2σ n dev Age ±2σ n dev Age ±2σ n dev analysis (Ma) (%) (Ma) (%) (Ma) (%) (Ma) (%) (1) (2) (3) (4) (2) (3) (5) (2) (3) (6) (2) (3) ID-TIMS 1797 ±3 2700 ±1 966 ±3 294 ±1 LA-ICPMS 27 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_10.txt | ained (50-100
µm) metarhyolite flow in the centre of the belt provides
an extrusion age of 1491 ± 5 Ma (sample J-482A; Tables
1, 4; Fig. 9B). Along strike, in the Sauda-Suldal area
(Fig. 4), a supracrustal belt is made up of intensely
deformed, fine-grained rocks interpreted as metavolcanic
rocks interlayered with subo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1234.txt | _":"Li et al., 2008"},{"#name":"reference","$":{"id":"sbref0170","refId":"34"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"Z.X."},{"#name":"surname","_":"Li"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S.V."},{"#name":"s... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1475.txt | 0.593,1.339,0.92,2.162,0.92
c0.779,0,1.518-0.297,2.079-0.837C56.255,54.982,56.293,53.08,55.146,51.887z M23.984,6c9.374,0,17,7.626,17,17s-7.626,17-17,17
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_140.txt | v), a.on(ge, v), this.ee.on(me, b), s.on(le, b), a.on(le, b), this.ee.buffer([pe, me, "xhr-resolved"], this.featureName), l.buffer([pe], this.featureName), c.buffer(["setTimeout" + ue, "clearTimeout" + ce, pe], this.featureName), d.buffer([pe, "new-xhr", "send-xhr" + ce], this.featureName | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_969.txt | ":"Basement Hf and Nd signature of Musgrave is different to AFO but similar to Madura."}],"$":{"id":"lsti0020"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0025"},"#name":"para","_":"Musgrave is not the strike equivalent of the AFO."}],"$":{"id":"lsti0025"},"#name":"list-item"}],"$... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_8.txt | on the correlation of allochthonous
crystalline segments of the Scandinavian Caledonides. International Journal of Earth Sciences 91, 955-963.
Corfu, F. & Laajoki, K. 2008: An uncommon episode of mafic magmatism at 1347 Ma in the Mesoproterozoic Telemark supracrustals,
Sveconorwegian orogen - Implications for stratigr... | |
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