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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_28.txt | ) (2) (Ma)
South Migmatitic Torpa granite, TA1 Zrn U-Pb 1359 ±26 Andersson et al., 2002
South Tjärnesjö granite, isotropic facies, Björshult Zrn U-Pb 1368 ±4 Andersson et al., 1999
South Torpa granite Zrn U-Pb 1380 ±6 Åhäll et al., 1997
South Tjärnesjö granite, veined facies, TJ25D Zrn U-Pb | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_27.txt | large-scale gneiss dome (Corti et al. 2003), progressively exhumed after 970 Ma (Bingen et al. 2006). The
extent of this gneiss dome is not well defined, but it may
include high-grade gneisses in the southern part of the
Telemark sector (South Telemark Gneisses). Two stages
of doming can be inferred. (1) A first stage... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_7.txt | },
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1456.txt | ><div class="ot-hlst-cntr"><button class="ot-link-btn category-host-list-handler" aria-label="Cookie Details List" data-parent-id="1">Cookie Details List</button></div></div></div><div class="ot-accordion-layout ot-cat-item ot-vs-config" data-optanongroupid="3"><button aria-expanded="false" ot-accordion="true" aria-co... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_707.txt | remelting of older crust. The Hf–O isotopic patterns show that Sveconorwegian magmas differ from typical arc magmas by lower involvement of sedimentary components and juvenile material. This makes the 1050–930 Ma magmatism incompatible with a long-term subduction setting. The ca. 1650–1500 Ma samples, in con... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_658.txt | regimes after peak metamorphism, whereas Group 2 pegmatites formed in an extensional regime and the required heat for partial melting was provided by mafic magma underplating.</p><p id="sp0015">Differences in the rheological behavior of amphibolite and granitic gneiss during extensional tectonics are the major reason ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_896.txt | stract-sec"}],"$":{"view":"all","id":"ab0010","lang":"en","class":"author-highlights"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstracts"},"pdf":{"urlType":"download","url":"/science/article/pii/S0024493721003030/pdfft?md5=9c1e6d5cd3205522b92514a596186105&pid=1-s2 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_29.txt | ll et al. 1995; Brewer et al. 1998;
Andersen et al. 2004). Metaplutonic suites range in age
from 1.62 to 1.52 Ga (Table 8; Fig. 7B; Connelly & Åhäll
90 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 3. Geological sketchmap of S Norway with a summary of sampling and results.
1996; Brewer et al. 1998; Åhäll et al. 20... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_85.txt | b 1506 ±2 Bingen et al., 2005
Suldal Granodiorite, Sand, B00139 Zrn U-Pb 1506 ±13 Bingen et al., 2005
Vardefjell SZ Flå, granodioritic banded gneiss, B99114 Zrn U-Pb 1507 ±14 Bingen et al., 2008
Telemark Grotte suite, tonalite gneiss Zrn U-Pb 1509 +19/-3 Ragnhildstveit et al., 1994
Tele | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_83.txt | Zrn 1419±12 Am Reddish veined orthogneiss, Dagsås U-Pb SIMS 4 Söderlund et al., 2002 South Zrn 1425±7 Am Migmatite granitic gneiss, Högabjär, leucosome HB2 U-Pb SIMS 18 Möller et al., 2007 South Zrn 1426±18 Am Interboudin granite pegmatite, Viared, EAH0207 U-Pb SIMS 9 Austin Hegardt et al., 2005 South | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_35.txt | .10284 0.9 3.932 1.6 0.2773 1.3 0.84 1578 19 1676 16 5.9
16p 6373 0.10415 1.0 4.020 1.6 0.2799 1.3 0.80 1591 18 1699 18 6.4
23p 5777 0.10236 0.7 3.982 1.2 0.2821 1.0 0.83 1602 14 1667 13 3.9
06p 14472 0.10407 0.8 4 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1472.txt | 0-10.085-3.518-18.746-10.567-25.978
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_991.txt | de San Andrés, Calle 27, Pabellón Geologia, Campus Universitario Cota Cota, La Paz, Bolivia"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Instituto de Investigaciones Geológicas y del Medio Ambiente, Universidad Mayor de San Andrés"},{"#name":"address-line","_":"Calle 27, Pabellón G... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1478.txt | c-3.234,7.801-1.903,14.467,3.999,19.985l140.757,140.753v138.755c0,4.955,1.809,9.232,5.424,12.854l73.085,73.083
c3.429,3.614,7.71,5.428,12.851,5.428c2.282,0,4.66-0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1150.txt | name":"given-name","_":"J."},{"#name":"surname","_":"Ragnhildstveit"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J."},{"#name":"surname","_":"Mansfeld"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R.D."},{"#name":"surname","_":"Tucker"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J.P."},{" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_37.txt | 2870 1.3 0.83 1626 18 1721 16 5.5
17 110354 0.10538 1.0 4.171 1.7 0.2871 1.4 0.81 1627 20 1721 19 5.5
02p 42032 0.10340 0.8 4.098 1.5 0.2874 1.2 0.83 1629 18 1686 16 3.4
09p 55522 0.10439 0.8 4.156 1.5 0.2888 1.3 0.86 16 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_33.txt | 33 intrusion 10J
1 1494 33 relic
Sauda Vanvik granite gneiss medium B00-147 348978 6604031 Bt, Ms, Grt, Ep LA-ICPMS 7 3 1.0 1065 74 intrusion 10I
4 0.19 1508 32 relic
Ullensvang Ullensvang gp metarhyolite weak S93-338 369900 6695100 Bt, Ms, Ep ID-TIMS 3 3 0.49 1489 1 extrusion 8F
Skånevik | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_127.txt | onetrust-button-group-parent{padding-left:3%;padding-right:4%;margin-left:0}#onetrust-banner-sdk.ot-buttons-fw:not(.ot-iab-2) #onetrust-button-group{margin-right:0;margin-top:1.25em;width:100%}#onetrust-banner-sdk.ot-buttons-fw:not(.ot-iab-2) #onetrust-button-group button{width: | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_53.txt | i complex, central Sweden.
Precambrian Research 95, 109-127.
Persson, P.O., Wahlgren, C.H. & Hansen, B.T. 1983: U-Pb ages of Proterozoic metaplutonics in the gneiss complex of southern Värmland, south-western Sweden. Geologiska Föreningens i Stockholm
Förhandlingar 105, 1-8.
Persson, P.O., Lindh, A., Schöberg, H., Hans... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_9.txt | 1090-1080 Ma. (2) At
1050-980 Ma, the Agder phase corresponds to the main Sveconorwegian oblique (?) continent-continent collision. It resulted in underthrusing and
burial of the Idefjorden Terrane to high-pressure conditions at 1050 Ma, followed by exhumation. Crustal thickening in the Telemarkia Terrane led
to protr... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_867.txt | d-ucs-content-store-eu-west/content/pii:S0301926821003910/ga1/DOWNSAMPLED/image/jpeg/b71e57349052edc40737f7818f6c8c24/ga1.jpg"},{"#name":"file-basename","_":"ga1"},{"#name":"abstract-attachment","_":"true"},{"#name":"filename","_":"ga1.jpg"},{"#name":"extension","_":"jpg"},{"#name":"filesize | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_664.txt | 7-45 45z"></path></svg></button></div><div class="u-display-none" aria-hidden="true"><div class="abstract u-margin-xs-top u-margin-m-bottom u-font-serif text-s" id="reference-abstract"><div class="u-margin-ver-m"><p id="sp0015">Here we present new <sup>40</sup>Ar/<sup>39</sup>Ar geochronology, rock magnetic, and paleo... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_19.txt | ic: 1.27 Ga development
of continental basins in the Sveconorwegian Orogen, southern
Norway. Canadian Journal of Earth Sciences 39, 1425-1440.
Bingen, B., Nordgulen, Ø., Sigmond, E.M.O., Tucker, R.D., Mansfeld, J.
& Högdahl, K. 2003: Relations between 1.19-1.13 Ga continental
magmatism, sedimentation and metamorphism, ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_1.txt | itation_journal_title" content="Precambrian Research">
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1459.txt | grpcntr ot-acc-txt"><p class="ot-acc-grpdesc ot-category-desc" id="ot-desc-id-3">These cookies enable the website to provide enhanced functionality and personalisation. They may be set by us or by third party providers whose services we have added to our pages. If you do not allow these cookies then some or all of thes... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_613.txt | HT) metamorphism? Constraints from zircon and monazite geochronology in the Eastern Ghats orogenic belt, India</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">(2013)</div></span></li><li class="bib-reference u-margin-s-bottom... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_8.txt | ndal phase represents the collision between the Idefjorden and
Telemarkia Terranes, which produced the Bamble and Kongsberg tectonic wedges. This phase involved closure of an oceanic basin, possibly marginal to Fennoscandia, accretion of a volcanic arc, high-grade metamorphism and deformation in the Bamble and Kongsber... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_143.txt | ,V,C[P+0],U,4096336452);V=t(V,Y,X,W,C[P+7],T,1126891415);W=t(W,V,Y,X,C[P+14],R,2878612391);X=t(X,W,V,Y,C[P+5],O,4237533241);Y=t(Y,X,W,V,C[P+12],U,1700485571);V=t | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_80.txt | .96 0.26612 1.75 0.89 1496 17 1521 24 101.7
10a 83 35 27 12815 0.09352 1.23 3.4474 3.31 0.26736 3.07 0.93 1498 23 1527 42 101.9
11a 378 109 113 30453 0.09359 0.69 3.2757 1.57 0.25384 1.41 0.90 1500 13 1458 18 97.2
08a 161 46 51 30722 0.09374 0.79 3.50 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1286.txt | },{"#name":"title","$$":[{"#name":"maintitle","_":"Contiguous Laurentia and Baltica before the Grenvillian-Sveconorwegian orogeny?"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Terra Nova"}]},{"#name":"volume-nr","_":"8"}]},{"#name":"date","_... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_17.txt | eds.), Mid-Proterozoic Laurentia-Baltica, 38, 1-20. Geological Association of Canada, Special Paper 38.
Haapala, I., Rämö, O.T. & Frindt, S. 2005: Comparison of Proterozoic
and Phanerozoic rift-related basaltic-granitic magmatism. Lithos
80, 1-32.
Hageskov, B. 1985: Constrictional deformation of the Koster dyke
swarm i... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1360.txt | -84861184886"},{"refId":42,"scopusHubEid":"2-s2.0-54049110965"},{"refId":44,"scopusHubEid":"2-s2.0-33747689115"},{"refId":45,"scopusHubEid":"2-s2.0-84893167165"},{"refId":46,"scopusHubEid":"2-s2.0-84863579514"},{"refId":48,"scopusHubEid":"2-s2.0- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_661.txt | ListArticleItem u-margin-l-bottom"><div class="sub-heading u-margin-xs-bottom"><h3 class="u-font-serif" id="citing-articles-article-1-title"><a class="anchor anchor-default" href="/science/article/pii/S0301926822002303"><span class="anchor-text">Paleomagnetism and <sup>40</sup>Ar/<sup>39</ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_555.txt | content-id="aut0030"><span class="button-link-text"><span class="react-xocs-alternative-link"><span class="given-name">Bjørn E.</span> <span class="text surname">Sørensen</span> </span><span class="author-ref" id="baff0015"><sup>c</sup></span></span></button></div></div></div><button class="button-link button-link-seco... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1222.txt | W.D."},{"#name":"surname","_":"Birch"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M.C."},{"#name":"surname","_":"Gilbert"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J.D."},{"#name":"surname","_":"Grice"}]},{"#name":"author","$$":[{"#name":"given-name","_":"F.C."},{"#name":"surname","_":"Haw | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_14.txt | NAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 97
Fig. 10. cont.
of 1501 ± 11 Ma, 1516 ± 11 Ma and 1506 ± 13 Ma
(Tables 1, 5; Fig. 10E-G). A sample from a more than 5
km-wide unit of weakly deformed to massive granite,
showing a gradual contact to the gneiss complex (increasing fabric toward... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_54.txt | 62 0.26170 37 1505.3 1.1
3 10gr,cl-pb,c,pr 5 60.7 2929 5 0.26 4358 0.09393 7 3.40270 499 0.26273 38 1506.7 1.4
(1) Cardinal number indicates the number of crystals analysed; all grains were selected from non-paramagnetic separates at 0˚ tilt at full magnetic field in Frantz Magnetic Separator; +75: size in
mm; c: colou... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1253.txt | ]},{"#name":"author","$$":[{"#name":"given-name","_":"R.R."},{"#name":"surname","_":"Parrish"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Developing an inverted Barrovian sequence; insights from monazite petrochronology"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_12.txt | rn U-Pb 1558 ±2 Åhäll et al., 2000
Biskopsgården granodiorite Zrn U-Pb 1559 ±2 Åhäll et al., 2000
Bäckefors granite Zrn U-Pb 1561 ±2 Åhäll et al., 2000
Gösta granite, SWS7 Zrn U-Pb 1563 +32/-21 Persson et al., 1983
Hisingen granite, Rya granodiorite Zrn U-Pb | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_261.txt | onetrust-pc-sdk.ot-addtl-vendors #ot-lst-cnt:not(.ot-host-cnt).ot-sel-all{padding-right:34px}#onetrust-pc-sdk.ot-addtl-vendors #ot-lst-cnt:not(.ot-host-cnt).ot-sel-all-chkbox{width:auto}#onetrust-pc-sdk.ot-addtl-vendors #ot- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_837.txt | record.url?partnerID=10&rel=3.0.0&view=basic&eid=2-s2.0-85134304048&md5=6e630629ee8735b13c1198cbd21ebf","scopusEid":"2-s2.0-85134304048","thirdParty":false,"volume":"Volume 379","abstract":{"$$":[{"$$":[{"$":{"id":"st010"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{" | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_955.txt | name":"para","$":{"id":"par0480","view":"all"},"$$":[{"#name":"__text__","_":"We would like to thank Benjamin Berge, Bengt Johansen and Brit Inger Vongraven for preparing the samples, Øyvind Skår and Martin Whitehouse for their help acquiring geochronological data, and Jessica Langlade for the microprobe analyses. We w... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_5.txt | 25 2.94 0.09 0.230 0.003 0.39 1475 51 1337 14 90.6
2 0.0926 0.0009 3.15 0.04 0.247 0.002 0.65 1479 18 1421 11 96.1
3 0.0927 0.0009 3.08 0.06 0.241 0.004 0.87 1482 19 1392 22 93.9
15 0.0927 0.0008 3.08 0.06 0.241 0.004 0.88 1483 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_54.txt | orden granite Zrn 1334 +7/-3 Piontek et al., 1998
Askim granite, 78170 Zrn 1362 ±9 Welin and Samuelsson, 1987
Orust dyke swarm, Islandsberg dyke Zrn 1457 ±6 Åhäll and Connelly, 1998
Brevik gabbro Zrn 1502 ±2 Åhäll and Connelly, 1998
Stigfjorden granite Zrn 1503 +3/-2 Åhäll and Connelly, 1998
Norstrand-Sø | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_693.txt | along the margin of the Proterozoic Sveconorwegian Egersund-Ogna (EGOG) anorthosite pluton. They permit the observation of the effects of a diapiric intrusion of anorthosite on its envelope of gneisses. The rocks are mylonitic and result from a strong deformation in UHT granulite facies conditions due to contact metam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1482.txt | sel-all-hdr"><span class="ot-consent-hdr">Consent</span> <span class="ot-li-hdr">Leg.Interest</span></div><div class="ot-sel-all-chkbox"><div class="ot-chkbox" id="ot-selall-hostcntr"><input id="select-all-hosts-groups-handler" type="checkbox"> <label for="select-all-hosts-groups-handler"><span class="ot-label-txt">che... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1334.txt | Norway)"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Precambrian Res."}]},{"#name":"volume-nr","_":"251"}]},{"#name":"date","_":"2014"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"141"},{"#name":"last-page","_":"163"}]}]}]}]},{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_117.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_232.txt | ot-ven-dets h4{padding-top:5px}#onetrust-pc-sdk.ot-ven-dets span{color:dimgray;padding:0;vertical-align:baseline}#onetrust-pc-sdk.ot-ven-dets.ot-ven-pur h4{border-top:1px solid #e9e9e9;border-bottom:1px solid #e9e9e9;padding-bottom:5px;margin-bottom:5px;font- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_102.txt | 2 Am 207Pb/206Pb 1 923 c. Connelly et al., 1996
South Garnet amphibolite, 9015 Am 206Pb/238U 3 923 ±3 Wang et al., 1998
South Vägasked grey gneiss, 85017 Am 207Pb/206Pb 2 929 ±22 Johansson et al., 1993
South Paleosome in orthogneiss, South Härene, 1 Am Low. intercept 5 932 ±10 Connelly et al., 1996
South Särdal orthog | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_608.txt | self"><span class="anchor-text">Proterozoic southward accretion and Grenvillian orogenesis in the interior Grenville Province in eastern Labrador: evidence from U–Pb geochronological investigations</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Precambrian Res.</h3></div... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_133.txt | 0360);V=u(V,Y,X,W,C[P+1],Q,3905402710);W=u(W,V,Y,X,C[P+2],N,606105819);X=u(X,W,V,Y,C[P+3],M,3250441966);Y=u(Y,X,W,V,C[P+4],S,4118548399);V=u(V,Y,X,W,C[P+ | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_63.txt |
setting (Drivheia gneiss; Heaman & Smalley 1994). The
younger 1170-1140 Ma bimodal magmatism and associated sediment basins, and the 1130 Ma alkaline magmatism suggest an extensional or transtensional tectonic
regime. This rock assemblage has been variably interpreted in a context of continental rifting (Laajoki et al... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_65.txt | +17A U-Pb SIMS 12 Möller et al., 2002
Rogaland-VA Mnz 1013±5, 980±5 Gr Charnockitic gneiss, Gyadalen, B649 Th-Pb ID-TIMS 2 Bingen et al., 2008
Rogaland-VA Mnz 1019±1, 1005±1, 1004±1, 1001±1 Gr Charnockitic gneiss, Gyadalen, B649 U-Pb ID-TIMS 4 Bingen & van | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_726.txt | ="" aria-hidden="false" aria-describedby="recommended-articles-header"><div id="recommended-articles" class="text-xs"><ul><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="recommended-arti... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1369.txt | },{"refId":23,"pii":"S0301926808001319","filesize":"4MB","pdf":{"urlType":"download","url":"/science/article/pii/S0301926808001319/pdfft?md5=97d9eaad112484fce72ce9a2468051b1&pid=1-s2.0-S0301926808001319-main.pdf"}},{"refId":29,"pii":"S0301926809002010","filesize":"3MB"," | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_71.txt | ersen and Konnerup-Madsen, 2000
Charnockite, NR19A R Zrn 1035 ±6 Möller et al., 2002
Fennefoss augen gneiss, B613 T Zrn 1035 +2/-3 Bingen and van Breemen, 1998 a
Rosskreppfjord granite R Zrn 1036 +23/-22 Andersen et al., 2002 a
Charnockite, NR17C R Zrn 1037 ±16 Möller et al., 2002
Pegmatite leucos | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_988.txt | ":"Programa de Pós-Graduação em Geologia e Geoquímica, Universidade Federal do Pará, Belém, PA 66075-110, Brazil"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Programa de Pós-Graduação em Geologia e Geoquímica, Universidade Federal do Pará"},{"#name":"city","_":"Belém"},{"#name":"sta... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_732.txt | or u-clamp-2-lines anchor-default" href="/science/article/pii/S0301926815001473" title="High-temperature deformation in the basal shear zone of an eclogite-bearing fold nappe, Sveconorwegian orogen, Sweden"><span class="anchor-text"><span>High-temperature deformation in the basal shear zone of an eclogite-bearing fold ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_572.txt | class="list-label">•</span><span><p id="par0015">Post-SMB metamorphism was highly localized, and unlikely to result from <a href="/topics/earth-and-planetary-sciences/crustal-thickening" title="Learn more about crustal thickening from ScienceDirect's AI-generated Topic Pages" class="topic-link">crustal thickening</a>.... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_55.txt | Geochronologic investigation of the
metamorphic terrain of southwestern Norway. Norsk Geologisk
Tidsskrift 55, 111-134.
Pasteels, P., Demaiffe, D. & Michot, J. 1979: U-Pb and Rb-Sr geochronology of the eastern part of the south Rogaland igneous complex,
southern Norway. Lithos 12, 199-208.
Pedersen, S. & Konnerup-Mads... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1225.txt | ame","_":"Maresch"}]},{"#name":"author","$$":[{"#name":"given-name","_":"E.H."},{"#name":"surname","_":"Nickel"}]},{"#name":"author","$$":[{"#name":"given-name","_":"N.M.S."},{"#name":"surname","_":"Rock"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J.C."},{"#name":"surname","_":"Schumacher"}]},{"#name":" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_29.txt | Precambrian Research 102, 135-154.
Karlstrom, K.E., Åhäll, K.I., Harlan, S.S., Williams, M.L., McLelland, J.
& Geissman, J.W. 2001: Long lived (1.8-1.0 Ga) convergent orogen
in southern Laurentia, its extensions to Australia and Baltica, and
implications for refining Rodinia. Precambrian Research 111, 5-30.
Kiel, H.M.... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_6.txt | ; implications for primary versus inherited zircon in mafic
rocks and rheomorphic dykes. GFF 121, 25-31.
Connelly, J.N. & Åhäll, K.I. 1996: The Mesoproterozoic cratonization
of Baltica – new age constraints from SW Sweden. In Brewer, T.S.
(ed.), Precambrian crustal evolution in the North Atlantic Region.
Geological Soc... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_72.txt | aland-Vest
Agder, SW Norway. In Tobi, A.C. & Touret, J.L. (eds.), The deep Proterozoic crust in the north Atlantic provinces, NATO-ASI C158, 477-
497. Reidel, Dordrecht.
Tomkins, H.S., Williams, I.S. & Ellis, D.J. 2005: In situ U-Pb dating of
zircon formed from retrograde garnet breakdown during decompression in Rogala... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_536.txt | class="preview-sidebar u-show-from-lg col-lg-6"><div class="PreviewTableOfContents text-s"><h2 class="u-h4 preview-table-of-contents-title">Article preview</h2><ul class="preview-table-of-contents-list"><li id="preview-section-abstract-item" class=""><a class="anchor anchor-default" href="#preview-section-abstract"><s... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_62.txt | AL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
68
inferred from U–Pb zircon geochronology and geochemical signature of augen gneiss suites. Journal of the Geological Society, London
155, 143-154.
Bingen, B. & van Breemen, O. 1998b: U-Pb monazite ages in amphibolite- to granulite-facies ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_479.txt | Direct home page" data-aa-region="header" data-aa-name="ScienceDirect"><img class="gh-logo" src="https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/24/images/elsevier-non-solus-new-grey.svg" alt="Elsevier logo" height="48" width="54"><svg xmlns="http://www.w3.org/2000/svg" version="1.1" height="15... |
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