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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1199.txt | ":"pages","$$":[{"#name":"first-page","_":"1"},{"#name":"last-page","_":"20"}]}]},{"#name":"comment","_":"(special paper)"}]}]},{"#name":"bib-reference","$":{"id":"bib0125"},"$$":[{"#name":"label","_":"Harley, 1998"},{"#name":"reference","$":{"id":"sbref0125","refId":"25"},"$$":[{"#name":"contribution","$":{"langtype":... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_844.txt | the Telemark Lithotectonic Unit. Accordingly, the new paleomagnetic poles for the Bamble (P"},{"$":{"loc":"post"},"#name":"inf","_":"lat"},{"#name":"__text__","_":" = -6.6°N, P"},{"$":{"loc":"post"},"#name":"inf","_":"long"},{"#name":"__text__","_":" = 218.4°E, N = 38, A"},{"$":{"loc":"post"},"#name":"inf","_":"95"},{... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1458.txt | class="category-switch-handler" data-optanongroupid="3" checked="" aria-labelledby="ot-header-id-3"> <label class="ot-switch" for="ot-group-id-3"><span class="ot-switch-nob" aria-checked="true" role="switch" aria-label="Functional Cookies"></span> <span class="ot-label-txt">Functional Cookies</span></label> </div></di... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_1.txt | -scale Sveconorwegian
shear zones (Figs. 1, 2; Berthelsen 1980; Park et al. 1991;
Gorbatschev & Bogdanova 1993; Romer 1996; Bingen
et al. 2001a; Andersen et al. 2002b). Progress in the
understanding of the Sveconorwegian orogeny, and
more globally of the Grenvillian orogeny, requires
large-scale evaluation of continent... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_943.txt | of SMB magmatism. Data from 28 of these samples are previously unpublished (see Table 1). Several different techniques have been used to analyze these samples, including Laser-Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) at the Geological Survey of Norway, and at the NERC Isotope Geosciences Labor... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_890.txt | Bjerkreim-Sokndal layered intrusion. Most felsic lithologies show the signature (including high positive Eu anomalies) of anatectic processes in disequilibrium melting conditions and rapid extraction from the source rocks. Flowage differentiation in the emplacement process explains the various compositions, as commonl... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_560.txt | 38 12-12 12zm66-6e1c6.62 0 12 5.38 12 12s-5.38 12-12 12-12-5.38-12-12 5.38-12 12-12zm0 62c-6.56 0-12.44 2.9-16.48 7.48l-28.42-15.28c0.58-1.98 0.9-4.04 0.9-6.2s-0.32-4.22-0.9-6 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_58.txt | Scherstén, A., Larson, S.Å., Cornell, D.H. & Stigh, J. 2004: Ion probe
dating of a migmatite in SW Sweden: the fate of zircon in crustal
processes. Precambrian Research 130, 251-266.
Schiellerup, H., Lambert, D.D., Prestvik, T., Robins, B., McBride, J.S. &
Larsen, R.B. 2000: Re–Os isotopic evidence for a lower crustal ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1089.txt | ","$":{"id":"aut0035"},"$$":[{"#name":"given-name","_":"Matthew S.A."},{"#name":"surname","_":"Horstwood"},{"#name":"cross-ref","$":{"id":"crf0195","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]}]}],"floats":[],"footnotes":[],"attachments":[]},"title":{"content":[{"#name":"title","$":{"id":"tit000... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1486.txt | by OneTrust Opens in a new Tab"><img alt="Powered by Onetrust" src="https://cdn.cookielaw.org/logos/static/powered_by_logo.svg" title="Powered by OneTrust Opens in a new Tab"></a></div></div><!-- Cookie subgroup container --><!-- Vendor list link --><!-- Cookie lost link --><!-- Toggle HTML element --><!-- Checkbox HT... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_53.txt | 1999: Geologisk kart over Norge, berggrunnskart
Hamar, 1:250000. Norges geologiske undersøkelse.
Nordgulen, Ø. & Skår, Ø. 2004: Mesoproterozoic crustal evolution of
the Idefjorden terrane: U-Pb age determination of granitoids using
LA-ICPMS analyses of zircon. GFF 126, 31-32.
O'Nions, R.K. & | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_50.txt | roterozoic and
younger magmatic rocks. These include 1650-1500 Ma
rapakivi granite plutons and related rocks (Haapala et
al. 2005), the 1460 Ma Tuna dolerites (Söderlund et al.
2005), 1460-1440 Ma granite plutons (Cecys & Benn
2007), the 1270-1250 Ma Central Scandinavian Dolerite Group (Söderlund et al. 2006), and the ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_754.txt | ollow"><span class="anchor-text">Remote access</span></a></li><li><a class="anchor u-display-block u-clr-grey8 u-margin-s-bottom u-margin-0-bottom-from-sm u-margin-m-right-from-sm u-margin-l-right-from-md anchor-default" href="https://sd-cart.elsevier.com/?" target="_blank" id="els-footer-shopping-cart" rel="nofollow">... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_117.txt | Release", "addPageAction", "setCurrentRouteName", "setPageViewName", "setCustomAttribute", "interaction", "noticeError", "setUserId", "setApplicationVersion"].forEach(t => {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1263.txt | ":"2012"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"443"},{"#name":"last-page","_":"469"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0210"},"$$":[{"#name":"label","_":"Paterson et al., 2008"},{"#name":"reference","$":{"id":"sbref0210","refId":"42"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_44.txt | ite (sample S93-305; Tables 1, 2; Figs. 3, 8D). The
Rjukan group is spatially associated with plutonic rocks
(commonly gradual change in grain size between the
two types of rocks). Two foliated plutons yield intrusion ages of 1509 +19/-3 Ma (Table 10; Grotte suite;
Ragnhildstveit et al. 1994) and 1476 ± 13 Ma (Tinn gra... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_768.txt | ":{"view":"all","id":"par0005"},"#name":"para"}],"$":{"id":"lsti0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0010"},"#name":"para","_":"The SMB host rocks were metamorphosed regionally during or prior to granite emplacement."}],"$":{"id":"lsti0010"},"#name":"list-item"},{"$$"... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_5.txt | somewhere to the northwest of their present
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
A four-phase model for the Sveconorwegian orogeny,
SW Scandinavia
Bernard Bingen, Øystein Nordgulen & Giulio Viola
Bingen, B., Nordgulen, Ø. & Viola, G.; A four-phase model for the... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1416.txt | ');
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_885.txt | Duchesne J.-C., Grard A.","doi":"10.1016/j.lithos.2021.106267","externalArticle":false,"issn":"00244937","openAccess":0,"pii":"S0024493721003030","publicationDate":"2021-10-01","publicationTitle":"Lithos","publicationYear":"2021","scopusArticleUrl":"http://www.scopus.com/scopus/inward/record.url?partnerID=10&rel=3 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_945.txt | SMB granites"},{"#name":"para","$":{"id":"par0305","view":"all"},"$$":[{"#name":"__text__","_":"Mineral composition data, acquired by microprobe, were obtained from different parts of the SMB (black triangles in Fig. 1a) in order to determine the pressure and temperature ("},{"#name":"italic","_":"P"},{"#name":"__text... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1290.txt | volume-nr","_":"15"}]},{"#name":"date","_":"2013"}]}]},{"#name":"comment","_":"EGU2013-13958"}]}]},{"#name":"bib-reference","$":{"id":"bib0255"},"$$":[{"#name":"label","_":"Sawyer, 2008"},{"#name":"reference","$":{"id":"sbref0255","refId":"51"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_12.txt | ennoscandia based on deep
seismic and gravity data. Terra Nova 8, 558-566.
Andersson, U.B., Sjöström, H., Högdahl, K. & Eklund, O. 2004:
Transscandinavian Igneous Belt; evolutionary models. In Högdahl,
K., Andersson, U.B. & Eklund, O. (eds.), The Transscandinavian
Igneous Belt (TIB) in Sweden; a review of its | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_99.txt | , B99143 Am 207Pb/206Pb 3 1043 ±8 Bingen et al., 2008
Bäckefors granite 207Pb/206Pb 2 1554 ±2 Åhäll et al., 2008
Rönnäng tonalite, T2light 207Pb/206Pb 1 1565 c. Connelly & Åhäll, 1996
Rönnäng tonalite, T1dark 207Pb/206Pb 1 1573 c. Connelly & Åhäll, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_731.txt | span>Wilson</span> <span>Teixeira</span>, …, <span>Richard E.</span> <span>Ernst</span></div></div><div class="buttons"></div></li><li class="RelatedContentPanelItem u-display-block"><div class="sub-heading u-padding-xs-bottom"><h3 class="related-content-panel-list-entry-outline-padding text-s u-font-serif" id="recomme... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_825.txt | 687","thirdParty":false,"volume":"Volume 384","abstract":{"$$":[{"$$":[{"$":{"id":"st005"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0005"},"#name":"para","_":"Sveconorwegian pegmatites form two age groups: (1) 1100–1030 Ma and (2) 930–890 ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_44.txt | U-Pb and Th-Pb data define overlapping age ranges,
from 1032 ±5 to 970 ±5 Ma for M1, and from 930 ±2 to
922 ±5 Ma for M2 (Bingen & van Breemen 1998b; Bingen et al. 2008b). Molybdenite associated with generally
deformed quartz veins, pegmatites or leucosomes from
several localities yields Re-Os crystallization ages rang... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1267.txt | .T."},{"#name":"surname","_":"Pidgeon"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.A."},{"#name":"surname","_":"Nemchin"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.D."},{"#name":"surname","_":"Kinny"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Fir-tree and nebulously zoned zircons | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_78.txt | al., 1999 South Moly 957±4, 949±4 Am Felsic vein cutting eclogite boudin, Viared VR3 Re-Os ID-NTIMS 2 Austin Hegardt et al., 2005 South Zrn 961±13 Am Late-kinematic “pinch-and-swell” pegmatite, Gällared N U-Pb SIMS 8 Söderlund et al., 2002 South Zrn 963±22 Ecl Deformed granite dyke in eclogite boudin | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_91.txt | ongsberg Metadacite gneiss, Bingen, 01/19 Zrn U-Pb 1529 ±7 Andersen et al., 2004
Kongsberg Granodiorite, Snarum, HFG Zrn U-Pb 1534 +9/-8 Andersen et al., 2004
Bamble Charnockite gneiss, Flosta Zrn U-Pb 1542 ±8 Kullerud & Machado, 1991
Bamble Justøy tonalite, Justøy, 5/97JUS Zrn U- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_481.txt | .43 4.65 1.32l0.13-2.64c-1.42-0.63-2.97-0.96-4.78-0.96 -4.62 0-6.6 2.44-6.6 5.45 0 5.61 8.78 6.14 8.78 9.93 0 1.48-1.15 3.04-3.86 3.04 -1.72 0-3.4-0.56-4.72-1.39l-0.36 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_476.txt | smetrics.elsevier.com/b/ss/elsevier-sd-prod/1/G.4--NS/1711418025477?pageName=sd%3Aproduct%3Ajournal%3Aarticle&c16=els%3Arp%3Ast&c2=sd&v185=img&v33=ae%3AANON_GUEST&c1=ae%3A228598&c12=ae%3A12975512 />
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_311.txt | -pc-sdk #ot-lst-cnt.ot-vnd-info.ot-vnd-lbl{font-weight:bold;font-size:.85em;margin-bottom:.5rem}#onetrust-pc-sdk #ot-lst-cnt.ot-vnd-info.ot-vnd-cnt{margin-left:.5rem;font-weight:500;font-size:.85rem}#onetrust-pc-sdk.ot-vs-list, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_619.txt | is</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0024493714000048" target="_self"><span class="anchor-text">Tectono-metamorphic evolution of the Jomolhari massif: variations in timing of syn-collisional metamorphism across western Bhutan</span></a></h3><span class="... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_79.txt | slice(3), U + Z), t.on(F + q, function (e, t, n) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1251.txt | 0190","refId":"38"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"C.M."},{"#name":"surname","_":"Mottram"}]},{"#name":"author","$$":[{"#name":"given-name","_":"C.J."},{"#name":"surname","_":"Warren"}]},{"#name":"author","$$":[{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_467.txt | #ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy #cookie-policy-description {
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_74.txt | Zrn 1134 ±21 Andersen et al., 2002
Heddal gp, Skogsåa porphyry, TA992 T Zrn 1145 ±4 Laajoki et al., 2002
Eiddal granite gneiss, N95-65 T Zrn 1146 +/-5 Bingen et al., 2003
Hesjåbutind gabbro T Zrn 1146 ±2 Dahlgren et al., 1990 a
Høydalsmo gp, Dalaå porphyry, 830KLN T Zrn 1150 ±4 Laaj | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_35.txt | -0.6 18 Nov 03 1799 ±38 8 0.1 01 Dec 03 1786 ±17 8 -0.6 04 Dec 03 1793 ±24 11 -0.2 Mean 1794 -0.2 2691 -0.4 963 -0.3 293 -0.3 (1) ØS-99-14, Sjona granite from Nordland, N Norway, ID-TIMS age by Skår (2002). (2) n: number of analyses on distinct crystals (3) Deviation in % relative to reference ID | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_59.txt | U-Pb data on magmatic zircon from the Flå granite
pluton.
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia 49
Table 3. Compilation of geochronological data on magmatic events in the Sveconorwegian belt
Location Lithology, sample Min System Age ±2s Reference
(1) (2) (Ma)
Te... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_24.txt | .
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
Jansen, J.B.H., Blok, R.J., Bos, A. & Scheelings, M. 1985: Geothermometry and geobarometry in Rogaland and preliminary results from
the Bamble area, S Norway. In Tobi, A.C. & Touret, J.L. (eds.), The
deep Proterozoic crust ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_41.txt | exotic craton is
nevertheless permissible.
The Bamble-Kongsberg sector contains lithologies
characteristic of both Telemarkia and the Idefjorden
terrane (Figs. 2, 7; Tables 1, 9-10). The Bamble-Kongsberg
sector shares with the Idefjorden terrane the 1.57-1.52 Ga
calc-alkaline suite associated with greywacke metasedime... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_42.txt | of 0.5 GPa (Fig. 8f). Petrological
evidence suggests that superposition of three metamorphic phases took place. High-temperature granulitefacies assemblages (M2) commonly include relicts of
older, high-grade medium-pressure assemblages (M1,
0.6-0.8 GPa), and they are themselves commonly surrounded by post-peak corona ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_346.txt | ot-acc-hdr.ot-chkbox{position:relative;margin:0.5rem}#onetrust-pc-sdk.ot-vs-config.ot-acc-hdr.ot-chkbox label,#onetrust-pc-sdk ul.ot-subgrps.ot-acc-hdr.ot-chkbox label,#onetrust-pc-sdk.ot-subgrp-cntr ul.ot-subgrps.ot-acc-hdr.ot-chk | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_507.txt | 57 8c-14.7 0-28.5 5.72-38.9 16.1-10.38 10.4-16.1 24.22-16.1 38.9 0 30.32 24.68 55 55 55 14.68 0 28.5-5.72 38.88-16.1 10.4-10.4 16.12-24.2 16.12-38.9 0-30.32-24.68-55-55-55zm0 1e1c24.82 0 45 20 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_129.txt | Z=(H-(H%4))/4;d=(H%4)*8;aa[Z]=aa[Z]|(128<<d);aa[I-2]=F<<3;aa[I-1]=F>>>29;return aa}function B(x){var k="",F="",G,d;for(d=0;d<=3;d++){G=(x>>>(d*8))&255;F="0"+G.toString(16);k=k+F.substr( | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_773.txt | 0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma, followed by a contact metamorphic event at 930"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma. Magmatism has been grouped into a ‘syn-collisional’ suite at 1050–1035"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma, a ‘post-collisional’ ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1026.txt | 0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0020"},"#name":"para","_":"Kinematic analysis shows an east-directed transport of the nappe."}],"$":{"id":"lsti0020"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0025"},"#name":"para","_":"Tran... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_161.txt | eVar15 : 'Event - Search Results Click Position'
,eVar19 : 'Search - Advanced Criteria'
,eVar21 : 'Promo - Clicked ID'
,eVar22 : 'Page - Test ID'
,eVar27 : 'Event - Auto | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_61.txt | ough, P.W.L. 1983: Rare earth,
Th, Hf, Ta, and large-ion lithophile element variations in metabasites from the Proterozoic amphibolite-granulite transition zone
at Arendal, South Norway. Earth and Planetary Science Letters 63,
446-458.
Smithson, S.B. 1963: Granite studies: II. The Precambrian Flå granite, a
geological ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_158.txt | -hdr{padding:8px 0;width:100%}div#onetrust-pc-sdk.ot-plus-minus{transform:translateY(2px)}div#onetrust-pc-sdk.ot-accordion-layout.ot-cat-item>button{background:0 0!important;border:0!important;height:44px!important;max-width:none!important;width:calc(100% - 48px)!important}div#onetrust-consent-sdk #onetrust | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_892.txt | to intrude at a lower temperature below the ductile-brittle transition."}],"$":{"view":"all","id":"as0005"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab0005","lang":"en","class":"author"},"#name":"abstract"},{"$$":[{"$":{"id":"st0010"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{"$$":[{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_60.txt | ||!i) return null;
var a = (0, _.M)(),
s = (0, _.Ht)(),
c = Date.now(),
u = {
spanId: a,
traceId: | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_30.txt | ot-ven-hdr>p a{position:relative;z-index:2;pointer-events:initial}#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-vnd-info a,#onetrust-pc-sdk.ot-vs-list.ot-vnd-item.ot-vnd-info a{margin-right:auto}#onetrust-pc-sdk.ot-pc-footer-logo img{width:136px;height: | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_42.txt | yd dolerite dyke, RA412 Zrn 1565 ±5 Ask, 1996
Metadolerite dyke, CHW670-OK450 Bdl 1568 +30/-8 Wahlgren et al., 1996
Visbergen, aplitic dyke, S6 Zrn 1612 ±8 Connelly et al., 1996
Vägasked grey gneiss, 85017 Zrn 1640 ±16 Johansson et al., 1993
granodiorite Ammesjön 79112 Zrn 1645 ±9 Welin, 1994
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_10.txt | & O’Nions, R.K. 1994: A re-examination of the influence
of composition on argon retentivity in metamorphic calcic amphiboles. Chemical Geology 112, 39-56.
Cosca, M.A., Mezger, K. & Essene, E.J. 1998: The Baltica-Laurentia
connection: Sveconorwegian (Grenvillian) metamorphism, cooling, and unroofing in the Bamble Secto... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_95.txt | merch.push('evar104=' + this.stripProductDelimiters(prodList[i].details.toLowerCase()));
}
if (prodList[i].position) {
merch.push('evar | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_46.txt | Kullerud & Dahlgren
1993; Cosca et al. 1998; de Haas et al. 2002). (2) The
Bamble-Kongsberg sector contains the youngest recorded
undisputable Mesoproterozoic volcanic arc magmatic
suite, namely, the 1.20-1.18 Ga tholeiitic gabbro to
tonalite Tromøy suite (Knudsen & Andersen 1999;
Andersen et al. 2004). This suite atte... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_605.txt | onism</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Precambrian Res.</h3></div><div class="series">(2004)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>G.M. </span>Bybee</span><em> et al.</e... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1291.txt | $$":[{"#name":"given-name","_":"E.W."},{"#name":"surname","_":"Sawyer"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Atlas of Migmatites. Canadian Mineralogist Special Publication 9"}]}]},{"#name":"host","$$":[{"#name":"book","$$":[{"#name":"date","_":"2008"},{"#name":"publisher","$$":[{"#name":"name","_":"NRC ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1375.txt | /S0024493714000048/pdfft?md5=1c6e54685591c2d1010a68165b0e096e&pid=1-s2.0-S0024493714000048-main.pdf"}},{"refId":58,"pii":"0301926895000976","filesize":"2MB","pdf":{"urlType":"download","url":"/science/article/pii/0301926895000976/pdf?md5=84d3507ea72 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_47.txt | .32 6017 0.09357 5 3.30349 491 0.25655 38 1499.5 1.0 2.6
4 4gr,+75,pb,tu,t-pr 8 100 389 2 0.28 21579 0.09335 4 3.27935 426 0.25479 33 1495.0 0.9 3.4
S93-305, Rjukan group metarhyolite, Fig. 8D
1 2gr,+75,cl,c,s-pr 8 31.4 111 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_0.txt | (d) Falkenberg phase: 980-970 Ma.
(e, f): Dalane phase: 970-900 Ma.
References quoted in text and in Tables
3, 4, 5.
59
northernmost part of the Eastern Segment (Solør Complex), the Protogine Zone and the Sveconorwegian Frontal Deformation Zone are poorly documented, as little
Sveconorwegian deformation has been identi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_78.txt | hover,#onetrust-banner-sdk.ot-sdk-button.ot-sdk-button-primary:focus,#onetrust-banner-sdk button.ot-sdk-button-primary:focus,#onetrust-banner-sdk input[type=submit].ot-sdk-button-primary:focus,#onetrust-banner-sdk input[type=reset].ot-sdk-button-primary:focus,#onetrust-banner-sdk input[type=button].ot | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_72.txt | ome, NR16A R Zrn 1039 ±11 Möller et al., 2003
Augen gneiss, NR2B R Zrn 1039 ±7 Möller et al., 2002
Grt migmatite gneiss, NR12E R Zrn 1046 ±12 Möller et al., 2003
Feda augen gneiss suite, Mandal, B206 R Zrn 1049 +2/-8 Bingen and van Breemen, 1998 a
Feda augen gneiss suite, Veggja, B642 R Z | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1139.txt | O."},{"#name":"surname","_":"Sigmond"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H."},{"#name":"surname","_":"Stein"}]}]},{"#name":"title","$$":[{"#name":"maintitle","$$":[{"#name":"__text__","_":"Baltica-Laurentia link during the Mesoproterozoic: 1.27"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__",... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_36.txt |
Larsson, D. & Söderlund, U. 2005: Lu-Hf apatite geochronology of
mafic cumulates: an example from a Fe-Ti mineralization at Smålands Taberg, southern Sweden. Chemical Geology 224, 201-211.
Lindh, A., Schöberg, H. & Annertz, K. 1994: Disturbed radiometric
ages and their bearing on interregional correlations in the SW B... | |
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