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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_68.txt | , Skånevik metarhyolite, Fig. 9B 03a (5) 356 44 97 24414 0.09190 0.40 3.062 2.27 0.2416 2.23 0.98 1465 8 1395 28 95.2
15a 165 24 50 5519 0.09212 0.74 3.403 2.35 0.2679 2.23 0.95 1470 14 1530 30 104.1
12a 279 42 86 17376 0.09245 0.37 3.462 2.26 0 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_75.txt | oki et al., 2002
Haglebu granite gneiss, N95-113 T Zrn 1153 ±2 Bingen et al., 2003
Brunkeberg fm, porphyry, 903KLN T Zrn 1155 ±2 Laajoki et al., 2002
Oftefjell gp, Ljosdalsvatnet porphyry, 902KLN T Zrn 1155 ±3 Laajoki et al., 2002
Hidderskog metacharnockite, B308 R Zrn 1159 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_674.txt | ) with limited or no deformation and only weakly metamorphosed, and that the molybdenite-bearing brittle fractures cut folded leucosome in the migmatite xenoliths (Fig. 5D). We therefore consider it highly unlikely that molydenite Re–Os ages from Ørsdalen date high-grade metamorphism, as suggested by Bingen and Stein (... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_47.txt | -align:left;text-decoration:none;text-indent:0;text-shadow:none;text-transform:none;white-space:normal;background:none;overflow:visible;vertical-align:baseline;visibility:visible;z-index:auto;box-shadow:none}#onetrust-banner-sdk label:before,#onetrust-banner-sdk label:after,#onetrust-banner-sdk.checkbox:after,#onetrust... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_648.txt | h3 class="title">Geotectonic evolution of southern Scandinavia in light of a late-Proterozoic plate-collision</h3><span class="host u-clr-grey6 u-font-sans"></span></li><li class="bib-reference u-margin-s-bottom"><span class="author u-font-sans"><span>C. </span>Gower</span><h3 class="title">Correlations between the Gre... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_638.txt | div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>B. </span>Bingen</span><em> et al.</em></span><h3 class="title">U–Pb monazite ages in amphibolite- to granulite-facies orthogneiss reflect hydrous mineral breakdown reactions: Sveconorwegian Prov... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_5.txt | intruded by the 1340-1250 Ma bimodal plutonic
Kungsbacka suite (Austin Hegardt et al. 2007), and 960-
920 Ma post-collisional norite-granite plutons, including
the Flå and Bohus plutons (Fig. 5; Eliasson & Schöberg
1991; Scherstén et al. 2000; Årebäck & Stigh 2000; Hellström et al. 2004; Bingen et al. 2006).
The Idefj... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1207.txt | The high-grade metamorphic Precambrian of the Sirdal-Ørsdal area, Rogaland/Vest-Agder, south-west Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nor. Geol. Unders."}]},{"#name":"volume-nr","_":"318"}]},{"#name":"date","_":"1975"}]},{"#n... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_157.txt | JmZWF0dXJlIjoiV2ViVmlld1hSZXF1ZXN0ZWRXaXRoRGVwcmVjYXRpb24iLCJleHBpcnkiOjE3MTk1MzI3OTksImlzU3ViZG9tYWluIjp0cnVlfQ=="><meta http-equiv="origin-trial" content="A/ERL66fN363FkXxgDc6F1+uc | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_26.txt | 1975), and relic zircon cores at 1.58, 1.51 and 1.50 Ga in
granulites (Möller et al. 2002, 2003).
The Rogaland-Vest Agder sector displays a significant
magmatic suite at 1.18-1.15 Ga and voluminous Sveconorwegian plutonism between 1.05 and 0.92 Ga (Table
10). Late-Sveconorwegian plutonism includes the 0.93
Ga Rogaland ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_715.txt | The structural, metamorphic and magmatic evolution of Mesoproterozoic orogens</span></span></a><div class="part-of-issue-editors u-margin-s-bottom"><span>Edited by </span><div class="authors"><span>Nick</span> <span>Roberts</span>, <span>Trond</span> <span>Slagstad</span>, <span>Giulio</span> <span>Viola</span></div></... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1211.txt | ":{"id":"sbref0145","refId":"29"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"Å."},{"#name":"surname","_":"Johansson"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Baltica, Amazonia and the SAMBA connection –1000 million y... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_61.txt | häll et al., 1995
Horred fm, dacite Zrn 1659 +8/-6 Connelly and Åhäll, 1996
(1) Zrn: zircon, Clm: columbite, Bdl: baddeleyite, Mnz: monazite, Ttn: titanite, Urn: uraninite, Eux: euxenite.
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 115
Table 9. Selection | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_68.txt | , B99114 U-Pb SIMS 7 Bingen et al., 2008
Vardefjell SZ Zrn 1012±7 Am Banded gneiss tonalitic, mylonitic, Flå, B99111 U-Pb SIMS 15 Bingen et al., 2008
Bamble-Kongsberg Terranes
Kongsberg Mnz 1092±1 Am Nodular gneiss, Snarum, B0030 U-Pb ID-TIMS 2 Bingen et al., 2008
Kongsberg M | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen9.txt | part9 -------------------
Extra-terrestrial[edit]
Carbonaceous chondrite meteorites contain kerogen-like components. Such material is thought to have formed the terrestrial planets. Kerogenous materials have been detected also in interstellar clouds and dust around stars.
The Curiosity rover has detected organic deposi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_582.txt | correlated to the Sveconorwegian orogen of southwest Fennoscandia (Gower et al., 1990, Romer, 1996, Karlstrom et al., 2001, Johansson, 2009). Recent work in the eastern Grenville Province by Gower et al. (2008) has, however, shown that this region was characterized by dextral, strike-slip movements, in contrast to the... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_49.txt | & Baadsgaard, H. 1971: A radiometric study of polymetamorphism in the Bamble region, Norway. Contributions to Mineralogy and Petrology 34, 1-21.
Page, L.M., Möller, C. & Johansson, L. 1996a: 40Ar/39Ar geochronology
across the Mylonite Zone and the Southwestern Granulite Province
in the Sveconorwegian Orogen of S Swede... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1485.txt | section></section><div class="ot-pc-footer ot-pc-scrollbar"><div class="ot-btn-container"> <button class="save-preference-btn-handler onetrust-close-btn-handler">Confirm my choices</button></div><!-- Footer logo --><div class="ot-pc-footer-logo"><a href="https://www.onetrust.com/products/cookie-consent/" target="_blank... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_849.txt | broadly similar latitudes between 1000 and 900 Ma, there is no geologic and paleomagnetic evidence for placing them next to each other."}],"$":{"view":"all","id":"sp0015"},"#name":"simple-para"}],"$":{"view":"all","id":"as015"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab015","lang":"en","class":"author"},"#nam... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_37.txt | Möller et al., 2007
South Migmatitic gneiss, locally charnockitic, 3 samples Zrn U-Pb 1671 ±4 Rimsa et al., 2007
PZ Hagshult granite, 83114 Zrn U-Pb 1673 ±19 Jarl, 2002
SFDZ Trysil “tricolor” granite gneiss, Tr4 Zrn U-Pb 1673 ±8 Heim et al., 1996
Centre Grey granite gneiss, Forshaga, SWS2 Zrn U- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_39.txt | , Br9602 Zrn U-Pb 1674 ±10 Alm et al., 2002
South Stenberget red gneiss, Romeleåsen, 85015 Zrn U-Pb 1675 ±25 Johansson et al., 1993
South Veined granitic gneiss, Mårdaklev Zrn U-Pb 1676 ±10 Söderlund et al., 2002
Centre Filipstad gneissic granite Zrn U-Pb 1676 ±7 Lindh et al., 1994
South Veined granitic gne | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1246.txt | ures to Zircon Chemistry: An Example from the Ultrahigh-Temperature Granulites of Rogaland (SW Norway)"}]},{"#name":"volume-nr","_":"vol. 220"}]}]},{"#name":"date","_":"2003"},{"#name":"publisher","$$":[{"#name":"name","_":"Geological Society"},{"#name":"location","_":"London"}]}]},{"#name":"pages","$$":[{"#name":"firs... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_554.txt | -text"><span class="react-xocs-alternative-link"><span class="given-name">T.</span> <span class="text surname">Røhr</span> </span><span class="author-ref" id="baff0005"><sup>a</sup></span></span></button>, <button class="button-link button-link-primary" type="button" data-sd-ui-side-panel-opener="true" data-xocs-conten... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_69.txt | U-Pb 1046 ±12 Möller et al., 2003
Rogaland Feda granodiorite suite, Mandal augen gneiss, B206 Zrn U-Pb 1049 +2/-8 Bingen & van Breemen, 1998
Rogaland Feda granodiorite suite, Veggja augen gneiss, B642 Zrn U-Pb 1051 +2/-8 Bingen & van Breemen, 1998
Rogaland Feda granodiorite suite, Feda augen gneiss, B | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_68.txt | .
Bingen, B., Andersson, J., Söderlund, U. & Möller, C. 2008a: The Mesoproterozoic in the Nordic countries. Episodes 31 (1), 6 p.p.
Bingen, B., Davis, W.J., Hamilton, M.A., Engvik, A., Stein, H.J., Skår, Ø.
& Nordgulen, Ø. 2008b: Geochronology of high-grade metamorphism in the Sveconorwegian belt | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_76.txt | 66 1.50 0.26059 1.41 0.94 1502 10 1493 19 99.4
17a 345 70 97 32951 0.09373 0.47 3.1645 1.50 0.24487 1.42 0.95 1503 9 1412 18 94.0
03a 245 127 80 23416 0.09394 0.50 3.4114 1.49 0.26339 1.41 0.94 1507 9 1507 19 100.0
09a 297 44 91 33579 0.09422 0.42 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_15.txt | et al., 2004
Migmatitic banded orthogneiss, Bua, TK1+TK2 Zrn U-Pb 1585 ±11 Andersson et al., 2002
Rönnäng tonalite Zrn U-Pb 1587 ±3 Connelly & Åhäll, 1996
Uddevalla granodiorite, 76267 Zrn U-Pb 1587 ±36 Welin et al., 1982
Stenkyrka granite Zrn U-Pb 1588 ±5 Connelly & Å | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_29.txt | in the Baltic Shield; a review addressing the tectonic
characteristics of Svecofennian, TIB 1 -related, and Gothian events.
GFF 122, 193-206.
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 105
106 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY Table 1. Summary of sampling and z... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_345.txt | nd-item.ot-acc-hdr.ot-chkbox,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-acc-hdr.ot-chkbox,#onetrust-pc-sdk #ot-pc-lst.ot-vs-list.ot-vnd-item.ot-acc-hdr.ot-chkbox,#onetrust-pc-sdk.ot-accordion-layout.ot-checkbox-consent. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_39.txt | Precambrian Research 159,
133-154.
Lundmark, A.M. & Corfu, F. 2008: Late-orogenic Sveconorwegian
massif anorthosite in the Jotun Nappe Complex, SW Norway, and
causes of repeated AMCG magmatism along the Baltoscandian
margin. Contributions to Mineralogy and Petrology 155, 147-163.
Lundqvist, I. & Skiöld, T. 1992: Preli... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1051.txt | },{"#name":"correspondence","$":{"id":"cor1"},"$$":[{"#name":"label","_":"⁎"},{"#name":"text","_":"Corresponding authors."}]}]}],"floats":[],"footnotes":[],"attachments":[]},"lastAuthor":{"content":[{"#name":"author","$":{"id":"au050","author-id":"S0301926816300146-344918f813a6d27170094e691af1bf4f"},"$$":[{"#name":"giv... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_677.txt | ic massif-type anorthosites and the significance of typically associated ultrahigh-temperature (UHT) host rocks have been debated for decades. This is particularly true of the Rogaland Anorthosite Province (RAP) in the SW Sveconorwegian Orogen. Earlier studies suggest that the RAP was emplaced over 1–3 Myr around 930&n... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_449.txt | policy.ot-sdk-cookie-policy-title{margin-bottom:1.2em}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy>section{margin-bottom:1em}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy th{min-width:75px}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy a,#ot-sdk-cookie-policy-v2.ot | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_106.txt | . intercept 17 1470 ±25 Connelly et al., 1996
PZ Gumlösa-Glimåkra gneissic granite, Vanås Gods, 86010 Am 207Pb/206Pb 3 942 c. Johansson, 1990
PZ-SFDZ Monzonite, Broby, E1, TA 207Pb/206Pb 1 1657 c. Söderlund et al., 1999
PZ-SFDZ Metagranite, Åserud, W3, TA Am 207Pb/ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_317.txt | border-bottom:none}#onetrust-pc-sdk.ot-vs-list.ot-vnd-item.ot-vnd-info-cntr,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-vnd-info-cntr{border:1px solid #d8d8d8;padding:.75rem 1.75rem;padding-bottom:0;width:auto;margin-top:.5rem}#onetrust-pc- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_22.txt | -Os geochronology records granulitefacies melting at 970 Ma, interpreted as evidence for
regional decompression following regional M1 medium
pressure metamorphism (Bingen & Stein 2003).
Dalane phase, 970-900 Ma
At and after 970 Ma (Figs. 8e, f), the Sveconorwegian belt
entered a period of relaxation or gravitational co... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_57.txt | 0.025% 1
σ). U blank
= 0.2 pg; Pb blank < 10 pg. Absolute uncertainties (1
σ) in the Pb/U and 207Pb/206Pb ratios calculated following Ludwig (1980). (7) λ 238U = 1.55125 10-10 y-1, λ 235U = 9.8485 10-10 y-1, 238U/235
U
= 137.88. (8) Percent discordance along the discordia line shown in the corresponding concordia diagr... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_253.txt | -cat-item>button[aria-expanded=false]~.ot-acc-txt,#onetrust-pc-sdk.ot-acc-cntr>button[aria-expanded=false]~.ot-acc-txt,#onetrust-pc-sdk li>button[aria-expanded=false]~.ot-acc-txt{margin-top:0;max-height:0;opacity:0;overflow:hidden;width:100%;transition:.25s ease-out;display | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_11.txt | of the southern part of the Eastern Segment as a core complex, and exhumation of the Rogaland-Vest
Agder sector in the Telemarkia Terrane as a wide gneiss dome. Formation of the gneiss dome peaked at 930-920 Ma with low-pressure high-temperature granulite-facies metamorphism and intrusion of an anorthosite-mangerite-c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_541.txt | text">Precambrian Research</span></a></h2><div class="text-xs"><a class="anchor anchor-default" href="/journal/precambrian-research/vol/265/suppl/C" title="Go to table of contents for this volume/issue"><span class="anchor-text">Volume 265</span></a>, <!-- -->August 2015<!-- -->, Pages 57-77</div></div><div class="publ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1393.txt | name":"title","$":{"id":"sect0145"},"_":"Large migmatitic screen within the SE part of the SMB, near Konsmo"}]},{"#name":"entry","$":{"id":"sec0135","depth":"3"},"$$":[{"#name":"label","_":"6.3.2"},{"#name":"title","$":{"id":"sect0150"},"_":"Garnet-bearing, migmatitic paragneiss in Oltedal"}]}]}]},{"#name":"entry","$":... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_17.txt | 05 0.237 0.003 0.84 1518 17 1371 17 90.4
7 0.0948 0.0009 3.57 0.06 0.273 0.004 0.82 1524 18 1555 20 102.0
18a 0.0949 0.0007 3.42 0.06 0.261 0.004 0.90 1525 14 1496 20 98.1
9b 0.0951 0.0008 3.21 0.06 0.245 0.004 0.87 1530 17 1413 20 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1364.txt | 15"},{"refId":63,"scopusHubEid":"2-s2.0-0038170355"},{"refId":64,"scopusHubEid":"2-s2.0-79960697234"},{"refId":65,"scopusHubEid":"2-s2.0-84903900360"},{"refId":66,"scopusHubEid":"2-s2.0-60949113681","crossRefDoi":"10.1017/S0263593300001516"},{"refId":67,"sc | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1122.txt | __text__","_":"Ma for the charnockitic facies and 926"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"±"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"4"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma for the granitic facies. Both facies display similar extent of differentiati... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_49.txt | is made up of Paleoproterozoic crust of the
Svecofennian belt and the Transcandinavian Igneous
Belt (TIB; Gorbatschev & Bogdanova 1993; Högdahl
et al. 2004; Korja et al. 2006). The TIB consists of little
deformed granitoids and porphyries formed between
1850 and 1660 Ma, with a general alkali-calcic signature. This Pa... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_187.txt | 63px)}#onetrust-pc-sdk.ot-vs-list.ot-always-active,#onetrust-pc-sdk.ot-cat-grp.ot-always-active{float:right;clear:none;color:#3860be;margin:0;font-size:.813em;line-height:1.3}#onetrust-pc-sdk.ot-pc-scrollbar::-webkit-scrollbar-track{margin-right:20px}#onetrust-pc-sdk | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_119.txt | stn: [a.D.sessionTrace],
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_534.txt | .61-7.15 8.68-15.9 8.68-25.13 0-10.91-4.25-21.17-11.96-28.88-7.72-7.71-17.97-11.96-28.88-11.96s-21.17 4.25-28.88 11.96c-7.72 7.71-11.97 17.97-11.97 28.88s4.25 21.17 11.97 28.88c7.71 7 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_870.txt | _":"sml"},{"#name":"filesize","_":"10393"},{"#name":"pixel-height","_":"164"},{"#name":"pixel-width","_":"83"},{"#name":"attachment-type","_":"IMAGE-THUMBNAIL"}],"$":{"xmlns:xocs":true},"#name":"attachment"},{"$$":[{"#name":"attachment-eid","_":"1-s2.0-S0301926821003910-ga1_lrg.jpg"},{"#name":"ucs-locator"," | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_3.txt | result suggests that these sectors are
genetically linked and part of the same continent at the
onset of the Sveconorwegian orogeny. The name
Telemarkia is proposed for this piece of continent. The
Sveconorwegian orogeny can be pictured as polyphase
imbrication of crust at the margin of Fennoscandia
between 1.13 and 0... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_35.txt | F. 2007: Lithostratigraphy of the Mesoproterozoic
Vemork formation, central Telemark, Norway. Bulletin of the Geological Society of Finland 79, 41-67.
Larson, S.Å., Cornell, D.H. & Armstrong, R.A. 1999: Emplacement
ages and metamorphic overprinting of granitoids in the Sveconorwegian Province in Värmland, Sweden - an ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_242.txt | -sdk #ot-fltr-modal.ot-label-txt{display:inline-block;font-size:.85em;color:dimgray}#onetrust-pc-sdk #ot-fltr-cnt{z-index:2147483646;background-color:#fff;position:absolute;height:90%;max-height:300px;width:325px;left:210px;margin-top:10px;margin-bottom:20px;padding-right:10px;border-radius: | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_89.txt | v(t) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_777.txt | ":"__text__","_":"Ma precedes and overlaps the main Sveconorwegian metamorphic event(s) that affected the region."}],"$":{"view":"all","id":"spar0015"},"#name":"simple-para"},{"$$":[{"#name":"__text__","_":"Our observations of cross-cutting relationships between previously metamorphosed gneisses and SMB rocks indicate ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_144.txt | ent-sdk p:hover{opacity:1!important}div#onetrust-consent-sdk a:focus,div#onetrust-consent-sdk button:focus,div#onetrust-consent-sdk input:focus{outline:2px solid #eb6500!important;outline-offset:1px!important}div#onetrust-banner-sdk.ot-sdk-container{padding:0;width:auto}div#onetrust-banner-sdk.ot-sd | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_681.txt | ></li><li class="ListArticleItem u-margin-l-bottom"><div class="sub-heading u-margin-xs-bottom"><h3 class="u-font-serif" id="citing-articles-article-3-title"><a class="anchor anchor-default" href="/science/article/pii/S0301926821003910"><span class="anchor-text">A geochronological review of magmatism along the external... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_483.txt | 0.03-1.09 -0.23-1.98-2.15-2.67-4.88-2.67 -3 0-6.7 2.31-6.7 7.76 0 5.22 2.77 7.99 6.63 7.99 1.68 0 3.47-0.36 4.95-1.39l-0.2-2.31c-0.99 0.82-2.84 1.52-4.06 1.52 -2.14 0-4 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_956.txt | for the editing, Federico Farina and an anonymous reviewer for comments that helped improve the manuscript. We also thank the "},{"#name":"grant-sponsor","$":{"id":"gs1","type":"simple","role":"http://www.elsevier.com/xml/linking-roles/grant-sponsor"}}]}]}]}],"floats":[],"footnotes":[],"attachments":[]},"questionsAndA... |
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