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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_845.txt | text__","_":" = 6.1°, K = 15.6), central Telemark (P"},{"$":{"loc":"post"},"#name":"inf","_":"lat"},{"#name":"__text__","_":" = -17.4° N, P"},{"$":{"loc":"post"},"#name":"inf","_":"long"},{"#name":"__text__","_":" = 229.8° E, N = 23. A"},{"$":{"loc":"post"},"#name":"inf","_":"95"},{"# | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_10.txt | ,
N.J. 2004: Mid-Proterozoic magmatic arc evolution at the
southwest margin of the Baltic shield. Lithos 73, 289-318.
Andersson, J., Söderlund, U., Cornell, D., Johansson, L. & Möller, C.
1999: Sveconorwegian (-Grenvillian) deformation, metamorphism
and leucosome formation in SW Sweden, SW Baltic Shield:
constraints fr... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_8.txt | 96.2
5 0.0949 0.0016 3.17 0.06 0.243 0.003 0.53 1525 33 1401 14 91.8
B00-140, granodiorite gneiss, Suldal, Fig. 10D
5b (4) 0.0915 0.0009 3.30 0.06 0.262 0.004 0.83 1457 19 1499 20 102.9
2a 0.0937 0.0008 4.06 0.08 0.314 0.005 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1019.txt | ller"},{"#name":"cross-ref","$":{"id":"crf0115","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"affiliation","$":{"id":"aff0005"},"$$":[{"#name":"label","_":"a"},{"#name":"textfn","_":"Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden"},{"#name":"affiliation... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_57.txt | a suture zone represented by the Mylonite
Zone at around 980 Ma. This model provides an elegant
explanation for 972 ±14 Ma eclogite-facies metamorphism in the Eastern Segment, but lacks independent
lithological evidence.
The Sveconorwegian belt lacks known exposure of
Sveconorwegian ultramafic rocks that could represe... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1102.txt | 9268"},{"pii":"S0301926814001946","doi":"10.1016/j.precamres.2014.06.003","journalTitle":"Precambrian Research","publicationYear":"2014","publicationDate":"2014-09-01","volumeSupText":"Volume 251","articleNumber":"","pageRange":"141-163","trace-token":"AAAAQBmEilysDXkD7OK1VKES7UWiA9gDew_6uZ2wtPLYIO0JPVH7plophYQy | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_36.txt | geotectonic setting of 1.52-1.48 Ga continental building is
uncertain. In the Suldal sector, preliminary geochemical
data on abundant andesite-dacite and granodiorite
lithologies suggest an active continental margin setting.
In the Telemark sector, the bimodal character of volcanism (Tuddal fm vs. Vemork fm) and the A... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_824.txt | -01-01","publicationTitle":"Precambrian Research","publicationYear":"2023","scopusArticleUrl":"http://www.scopus.com/scopus/inward/record.url?partnerID=10&rel=3.0.0&view=basic&eid=2-s2.0-85144414687&md5=ca25dc2c3f4512b95eb834e79ea2aa4","scopusEid":"2-s2.0-85144414 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_787.txt | 26815001424","price":{"currency":"USD","totalPrice":27.95},"purchaseNonDiscounted":{"linkUrl":"/getaccess/pii/S0301926815001424?corporate=true","price":{"currency":"USD","totalPrice":37.95}}},"analyticsMetadata":{"accountId":"228598","accountName":"ScienceDirect Guests","loginStatus":"anonymous","userId":"12975512","is... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1280.txt | name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"Ga accretionary orogeny in SW Fennoscandia"}]}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Int, Geol. Rev."}]}]},{"#name":"date","_":"2015"}]},{"#name":"pages","$$":[{"#name":"first-page... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_44.txt | rication of the terranes exposed in the orogen
between 1.13 and 0.97 Ga. Telemarkia is the westernmost coherent continental domain exposed in the orogen
(Figs. 1, 2). Two distinct assembly models are sketched
in Fig. 12. One sketch features Telemarkia at the margin
of Fennoscandia before the Sveconorwegian orogeny
(ind... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_77.txt | gren et al., 1990 b
Gjerstad augen gneiss, M5 T Zrn 1187 ±2 Heaman and Smalley, 1994
Drivheia granite gneiss, M200 T Zrn 1205 ±9 Heaman and Smalley, 1994
Trossovdal fm, Nyastøl metarhyolite S Zrn 1259 ±2 Brewer et al., 2004
Trossovdal fm, Nyastøl metarhyolite, B9817 S Zrn 1260 ±8 Bingen et | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1355.txt | 15,"scopusHubEid":"2-s2.0-67649548414","crossRefDoi":"10.1038/ngeo469"},{"refId":16,"scopusHubEid":"2-s2.0-84872812236","crossRefDoi":"10.1093/petrology/egs070"},{"refId":17,"scopusHubEid":"2-s2.0-37449022608"},{"refId":20,"scopusHubEid":"2-s2.0-00 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_21.txt | : Zircon dating of
polymetamorphic rocks in southwestern Sweden. Sveriges
Geologiska Undersökning C797, 1-34.
Welin, E. & Samuelsson, L. 1987: Rb-Sr and U-Pb isotope studies of
granitoid plutons in the Göteborg region, southwestern Sweden.
Geologiska Föreningens i Stockholm Förhandlingar 109, 39-45.
Welin, E. 1994: Iso... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1172.txt | author","$$":[{"#name":"given-name","_":"M.N."},{"#name":"surname","_":"Ducea"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P."},{"#name":"surname","_":"Kapp"}]},{"#name":"author","$$":[{"#name":"given-name","_":"G."},{"#name":"surname","_":"Zandt"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Cyclicit... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_196.txt | ftr-stacked.ot-pc-refuse-all-handler{margin-bottom:0px}#onetrust-pc-sdk.ot-ftr-stacked #ot-pc-content{bottom:160px}#onetrust-pc-sdk.ot-ftr-stacked.ot-pc-footer button{width:100%;max-width:none}#onetrust-pc-sdk.ot-ftr-stacked.ot-btn-container{margin:0 30px;width:calc | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_24.txt | inen et al (2001).
sector is interpreted in this paper as an early-Sveconorwegian collision zone between Telemarkia and the
Idefjorden terrane (Fig. 1) and is described separately.
Eastern Segment
The easternmost continental domain of the Sveconorwegian orogen is historically called the Eastern Segment and is bounded t... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_135.txt | fP: () => a,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_699.txt | ronological and isotopic studies on magmatism and migmatization</span></a></h3><div class="text-s">2021, Precambrian Research</div><div class="CitedSection u-margin-s-top"><div class="u-margin-s-left"><div class="cite-header text-s u-text-italic u-font-sans">Citation Excerpt :</div><p class="u-font-serif text-xs">Consi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_863.txt | ii/S0301926822001395/pdfft?md5=799b7c2fb451acfa427b271c056cf741&pid=1-s2.0-S0301926822001395-main.pdf"}},{"articleTitle":"A geochronological review of magmatism along the external margin of Columbia and in the Grenville-age orogens forming the core of Rodinia","authors":"Johansson Å., Bingen B., Huhma H., Waight T., Ve... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_61.txt | van Breemen, 1998
Rogaland-VA Zrn 1032±5, 1020±7, 1011±7, 1002±7, 980±7 Am Augen gneiss, Osen, NR2B U-Pb SIMS 5 Möller et al., 2002
Rogaland-VA Mnz 904±8 Gr Augen gneiss, Sira, B198 U-Pb ID-TIMS 1 Bingen & van Breemen, 1998
Rogaland-VA Mnz 971±2, 951 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_8.txt | t {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_23.txt | 02 4998 0.10228 1.1 3.580 2.4 0.2539 2.2 0.90 1458 29 1666 20 12
16p 7609 0.10379 1.0 3.676 1.9 0.2568 1.6 0.86 1474 21 1693 18 13
11 6971 0.10265 1.1 3.829 2.3 0.2706 2.0 0.87 1544 28 1673 21 7.7
03 12247 0.10493 1.1 3.926 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1107.txt | author","$":{"id":"aut0025"},"$$":[{"#name":"given-name","_":"Jean-Louis"},{"#name":"surname","_":"Paquette"},{"#name":"cross-ref","$":{"id":"crf0865","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]}]},{"#name":"author","$":{"id":"aut0030","orcid":"0000-0003-1898-221X"},"$$":[{"#name":"given-name",... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1212.txt | host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Precambrian Res."}]},{"#name":"volume-nr","_":"175"}]},{"#name":"date","_":"2009"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"221"},{"#name":"last-page","_":"234"}]}]}]}]},{"#name":"bib-reference","$":{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_860.txt | leucosome in extensional pull-aparts associated with the RED yields ages of 950–935 Ma, consistent with Re–Os molybdenite ages from brittle extensional structures in the hanging-wall block that range between 980 and 930 Ma. A metapelite in the immediate vicinity of the RAP yields a 950 Ma U–Pb age of matrix-hosted mon... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_237.txt | 1.3}#onetrust-pc-sdk.ot-host-name a{font-size:1em}#onetrust-pc-sdk.ot-host-expand{margin-top:3px;margin-bottom:3px;clear:both;display:block;color:#3860be;font-size:.72em;font-weight:normal}#onetrust-pc-sdk.ot-host-expand *{font-size:inherit}#onetrust-pc-sdk.ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_904.txt | f–O isotopic compositions."}],"$":{"id":"o0020"},"#name":"list-item"}],"$":{"id":"l0005"},"#name":"list"}],"$":{"view":"all","id":"sp0005"},"#name":"simple-para"}],"$":{"view":"all","id":"as005"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab005","lang":"en","class":"author-highlights"},"#name":"abstract"},{"$$":[... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen1.txt | part1 -------------------
Kerogen is solid, insoluble organic matter in sedimentary rocks. It consists of a variety of organic materials, including dead plants, algae, and other microorganisms, that have been compressed and heated by geological processes. All the kerogen on earth is estimated to contain 10 tons of car... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_48.txt | elongate metarhyolite body (>50 km long) situated some 25 km east of the Mylonite Zone (Fig. 2). The
sample shows small quartz and feldspar phenocrysts (<3
mm) in a fine-grained (<50 µm) volcanic matrix with
centimetre-scale flow banding preserved. Nineteen analyses of prismatic zircon spread along a concordia line
wi... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_1.txt | Agder sectors merged into one terrane called Telemarkia. The
curves are based on dates from Tables 1, 7-10.
94 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 8. Concordia diagrams presenting IDTIMS U-Pb data on zircon from 7 samples.
Hardangervidda sector
The Hardangervidda sector is exposed on the Hardangervidda ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1213.txt | #name":"label","_":"Karlstrom et al., 2001"},{"#name":"reference","$":{"id":"sbref0150","refId":"30"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"K.E."},{"#name":"surname","_":"Karlstrom"}]},{"#name":"author","$$":[{"#name":"given... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_74.txt | 27365 1.53 0.96 1465 9 1559 21 106.4
01a 138 56 44 12612 0.09248 0.73 3.3821 1.59 0.26522 1.41 0.89 1477 14 1517 19 102.7
12b 137 54 44 61958 0.09280 0.63 3.3609 1.54 0.26266 1.41 0.91 1484 12 1503 19 101.3
15a 457 279 151 48745 0.09308 0.47 3.3462 1 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_628.txt | -reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>J.M. </span>Bartley</span><em> et al.</em></span><h3 class="title">Incremental pluton emplacement by magmatic crack-seal</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Trans. R. Soc. Edin... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_23.txt | ogenic Sveconorwegian foreland basins on Fennoscandia suggests that
thinning of the orogen was driven more by extension
than erosion. Two high-grade domains, the southern part
of the Eastern Segment and the Rogaland-Vest Agder
sector in the Telemarkia Terrane, were exhumed to upper
crustal levels after 970 Ma (Fig. 4),... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1336.txt | ":"S.R."},{"#name":"surname","_":"Paterson"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Mesoscopic structures resulting from crystal accumulation and melt movement in granites"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Trans. R. ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_899.txt | 109438101&md5=1911444b5f45223bfd3678812dd8665","scopusEid":"2-s2.0-85109438101","snippets":["Considering the limited sampling area in this study, we suggest that more combined Hf–O isotopic studies, especially on the samples from South Norway, are probably required (as one granite sample with high δ18O values of 11–12‰... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_2.txt | Figs. 1, 2). It consists of
an amphibolite-facies gneiss domain with a generally
E-W structural pattern (Sigmond 1998). Orthogneisses
are interlayered with metasedimentary rocks. The
geochronology of these rocks is poorly established. One
granite gneiss yields a poor upper intercept age of 1649
+33/-19 Ma (Mårsbrot gra... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_43.txt | Steninge mafic dyke, Steninge, S2 Zrn 1654 ±9 Christoffel et al., 1999
Visbergen, paleosome, S4 Zrn 1660 ±5 Connelly et al., 1996
Karlstad metagranite, W1 Zrn 1661 ±27 Söderlund et al., 1999
Särdal orthogneiss, paleosome, S1 Zrn 1664 ±7 Christoffel et al., 1999
Hagshult granite, 83114 Zrn 1673 ±19 J | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_461.txt | policy-v2.ot-sdk-cookie-policy td,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy tr{display:block}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table.ot-host,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table.ot-cookies-type{width:auto}#ot-sdk-cookie-policy-v2.ot-sdk | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_30.txt | Y Minerals Method n tot n sel MSWD Age ± 2
σ Fig.
(1) (2) (3) (3) (4) (5) (5) (6) (Ma) (7) (8)
Magmatic rocks
Idefjorden terrane
Hønefoss Follum tonalite gneiss medium N95-130 568300 6673000 Amp, Bt, Ttn ID-TIMS 4 4 U.I. 1555 3 intrusion 8B
Østre Toten | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_367.txt | width: 896px)and (max-height: 425px)and (orientation: landscape){#onetrust-pc-sdk.otPcCenter{left:0;top:0;min-width:100%;height:100%;border-radius:0}#onetrust-pc-sdk.ot-pc-header{height:auto;min-height:20px}#onetrust-pc-sdk.ot-pc-header.ot-pc-logo{max-height:30px}#onetrust-pc | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_58.txt | Uddevalla granodiorite, 76267 Zrn 1587 ±36 Welin et al., 1982
Stenkyrka granite Zrn 1588 ±5 Connelly and Åhäll, 1996
Racken red syeno-granite gneiss, DC972 Zrn 1590 ±14 Larson et al., 1999
Harnäs gneiss, Hn96093 Zrn 1595 +24/-17 Alm et al., 2002
Racken quartz monzodiorite gneiss, DC9413 Zrn 15 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_20.txt | the Morkheia
Complex and associated gneisses, south Norway: implications for
disturbed Rb–Sr systems and for the temporal evolution of Mesoproterozoic magmatism in Laurentia. Geochimica et Cosmochimica
Acta 58, 1899-1911.
Heim, M., Skiöld, T. & Wolff, F.C. 1996: Geology, geochemistry and age
of the ‘Tricolor’ granite ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_43.txt | Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Table 2. ID-TIMS zircon U-Pb data on the Flå granite pluton
Fraction Concentrations Atomic ratios Age
ID Nb. Wt. Pb U Pb Th/U 206Pb 207Pb ±s 207Pb ±s 206Pb ±s 207Pb ±s
rad com 204Pb 206Pb 235U 238U 206Pb
(µg) (ppm) (ppm) (pg) | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_632.txt | h3 class="title">Baltica-Laurentia link during the Mesoproterozoic: 1.27<!-- --> <!-- -->Ga development of continental basins in the Sveconorwegian Orogen, southern Norway</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Can. J. Earth Sci.</h3></div><div class="series">(2002)</d... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_823.txt | 391","articles":[{"articleTitle":"Geochronological constraints for a two-stage history of the Sveconorwegian rare-element pegmatite province formation","authors":"Rosing-Schow N., Romer R.L., Müller A., Corfu F., Škoda R., Friis H.","doi":"10.1016/j.precamres.2022.106944","externalArticle":false,"issn":"03019268","open... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1195.txt | ]},{"#name":"issue-nr","_":"1/2"},{"#name":"date","_":"2008"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"61"},{"#name":"last-page","_":"95"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0120"},"$$":[{"#name":"label","_":"Gower et al., 1990"},{"#name":"reference","$":{"id":"sbref0120","refId":"24"},"$$":[{"#n... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_92.txt | Pb 1557 ±24 Andersen et al., 2004
Bamble Justøy tonalite, Homborsund, 9/97HOM Zrn U-Pb 1569 ±23 Andersen et al., 2004
Bamble Gjerstadvatn tonalite, 10/97NES Zrn U-Pb 1572 ±20 Andersen et al., 2004
Idefjorden Terrane
Blomskog granite, pegmatite BM1 Moly Re-Os 915 ±3 Bingen et al., 2006
Hakefj | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_865.txt | .106463","externalArticle":false,"issn":"03019268","openAccess":1,"pii":"S0301926821003910","publicationDate":"2022-04-01","publicationTitle":"Precambrian Research","publicationYear":"2022","scopusArticleUrl":"http://www.scopus.com/scopus/inward/record.url?partnerID=10&rel=3.0.0&view=basic&eid=2-s2.0-85123866786& | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_503.txt | .32 0.45 0.62 0.73 0.91H174.17zM173.56 3.22l-0.22 0.01v0.63h0.22c0.26 0 0.43-0.05 0.43-0.34C174 3.28 173.83 3.21 173.56 3.22z"></path></g></svg></a><div class="gh-nav-cnt u-hide-from-print"><div class="gh-nav-links-container gh-nav- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_47.txt | .51 Ga and consequently are either a
part of the Rjukan group or are younger. They possibly
correlate with the Heddersvatnet formation situated in
the lower part of the overlying Vindeggen group. In the
Gol area, the Rjukan group grades into a gneiss complex. A sample of orthogneiss from this complex yields
an intrusio... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_818.txt | "},"$$":[{"#name":"label","_":"a"},{"#name":"textfn","_":"Geological Survey of Norway, 7491 Trondheim, Norway"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Geological Survey of Norway"},{"#name":"city","_":"Trondheim"},{"#name":"postal-code","_":"7491"},{"#name":"country","_":"Norway... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_842.txt | __","_":"Here we present new "},{"$":{"loc":"post"},"#name":"sup","_":"40"},{"#name":"__text__","_":"Ar/"},{"$":{"loc":"post"},"#name":"sup","_":"39"},{"#name":"__text__","_":"Ar geochronology, rock magnetic, and paleomagnetic data obtained from rocks from three distinct domains of the Precambrian Sveconorwegian orogen... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_637.txt | span><em> et al.</em></span><h3 class="title">Tectonic regimes and terrane boundaries in the high-grade Sveconorwegian belt of SW Norway, inferred from U–Pb zircon geochronology and geochemical signature of augen gneiss suites</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">J. Geol.... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1467.txt | If you do not allow these cookies, you will experience less targeted advertising.</p><div class="ot-hlst-cntr"><button class="ot-link-btn category-host-list-handler" aria-label="Cookie Details List" data-parent-id="4">Cookie Details List</button></div></div></div><!-- Groups sections starts --><!-- Group section ends... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1066.txt | ":"__text__","_":" granulites in Manjinggou area of the Huai’an Complex to provide direct evidence that both pelitic and mafic H"},{"#name":"italic","_":"P"},{"#name":"__text__","_":" granulites suffered similar metamorphic history. The metamorphic peak mineral assemblage of the pelitic granulites is characterized by G... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_70.txt | 0.2844 2.27 0.99 1484 6 1613 33 108.7
16a 344 49 110 20272 0.09280 0.43 3.610 2.27 0.2821 2.23 0.98 1484 8 1602 32 108.0
06a 107 42 36 26824 0.09281 0.48 3.562 2.31 0.2784 2.26 0.98 1484 9 1583 32 106.7
04a 420 72 119 20585 0.09297 0.44 3.166 2.27 | |
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