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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_85.txt | U 206Pb 238U
(Ma) (Ma) (%)
(1) (1) (1) (2) (3
B00-127, Augen gneiss, Røldal, Fig. 10A
2a 0.0924 0.0011 3.53 0.07 0.277 0.004 0.80 1475 22 1576 22 106.8
17b 0.0926 0.0012 2.92 0.06 0.229 0.003 0.74 1479 25 1330 18 89.9 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_34.txt | veconorwegian. Nevertheless, in lowgrade c. 1260 Ma supracrustal rocks of the Suldal Sector
(Langvatn locality in Sæsvatn-Valdal sequence), a molybdenite Re-Os age of 1032 ±2 Ma defines Sveconorwegian
epidote-amphibolite-facies deformation in metabasalt
(Stein & Bingen 2002), while in the underlying basement
a monazite... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_542.txt | href="/journal/precambrian-research/vol/265/suppl/C"><span class="anchor-text"><img class="publication-cover-image" src="https://ars.els-cdn.com/content/image/1-s2.0-S0301926815X00088-cov150h.gif" alt="Precambrian Research"></span></a></div></div><div class="PageDivider"></div><h1 id="screen-reader-main-title" class="... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_69.txt | mer, I.C. 1991: The Proterozoic evolution of the Bamble sector
shear belt, southern Norway: correlations across southern Scandinavia and the Grenvillian controversy. Precambrian Research 49,
107-139.
Stein, H.J., Morgan, J.W. & Scherstén, A. 2000: Re-Os dating of lowlevel highly radiogenic (LLHR) sulfides: the Harnäs g... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_145.txt | k-row{align-items:flex-start;box-sizing:border-box;display:flex;flex-direction:column;justify-content:space-between;margin:auto;max-width:1152px}div#onetrust-banner-sdk.ot-sdk-row:after{display:none}div#onetrust-banner-sdk #onetrust-group-container,div#onetrust-banner-sdk.ot-bnr-flift:not(.ot-iab | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_83.txt | örhandlingar 109, 39-45.
Welin, E. 1994: Isotopic investigations of Proterozoic igneous rocks in
south-western Sweden. GFF 116, 75-86.
Westphal, M., Schumacher, J.C. & Boschert, S. 2003: High-temperature metamorphism and the role of magmatic heat sources at the
Rogaland Anorthosite Complex in Southwestern Norway. Journ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_960.txt | $":{"id":"eadd0005","type":"email"},"_":"kris.kirkland@gmail.com"}]},{"#name":"author","$":{"id":"aut0010"},"$$":[{"#name":"given-name","_":"R.H."},{"#name":"surname","_":"Smithies"},{"#name":"cross-ref","$":{"id":"crf0055","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1046.txt | , Northern Taibai Str. 229, Xi’an 710069, China"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"State Key Laboratory of Continental Dynamics"},{"#name":"organization","_":"Department of Geology"},{"#name":"organization","_":"Northwest University"},{"#name":"address-line","_":"Northern ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_48.txt | 2 0.57 9370 0.09347 7 3.34870 556 0.25984 41 1497.4 1.5 5.8
2 1gr,+75,cl,c,e,s-pr 5 31.9 115 2 0.49 6528 0.09318 8 3.32506 551 0.25880 38 1491.6 1.6 7.2
3 5gr,vpb-c,eq,e,pr 14 30 106 1 0.56 18886 0.09332 6 3.33149 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_843.txt | otectonic unit and the other two areas are located within the Telemark and Rogaland–Vest Agder sectors in the central and southwestern parts of the Telemark lithotectonic unit, respectively. New and existing geochronology data on metamorphism and cooling, combined with detailed rock magnetic analyses indicate that stud... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_736.txt | -Lin</span> <span>Wu</span>, …, <span>Wei</span> <span>Wang</span></div></div><div class="buttons"></div></li><li class="RelatedContentPanelItem u-display-none"><div class="sub-heading u-padding-xs-bottom"><h3 class="related-content-panel-list-entry-outline-padding text-s u-font-serif" id="recommended-articles-article4... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_19.txt | measured by ID-TIMS and
ages ranging from Permian to Archaean are analysed
together with the unknown samples. A summary of
88 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 1. Situation map of SW Scandinavia with lithotectonic domains and shear zones used in this work.
intercept ages obtained during a period overl... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_20.txt | U-Pb 1614 ±7 Lundqvist & Skiöld, 1993
Delsjön augen gneiss, Landvetter Badplats, DC04202 Zrn U-Pb 1614 ±5 Ahlin et al., 2006
Slemmestad metarhyolite, 01/25 Zrn U-Pb 1615 ±31 Andersen et al., 2004
Åmål granodiorite, 77018 Zrn U-Pb 1616 ±24 Welin et al., 1982
Migmatitic Delsj | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_122.txt |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_42.txt | , P.J., Kennedy, A. & Kröner, A. 2003: Linking growth
episodes of zircon and metamorphic textures to zircon chemistry:
an example from the ultrahigh-temperature granulites of Rogaland (SW Norway). In Vance, D., Müller, W. & Villa, I.M. (eds.),
Geochronology: linking the isotopic record with petrology and textures. Geol... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_19.txt | en et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 1. Situation map of SW Scandinavia showing the main lithotectonic units and shear zones of the Sveconorwegian orogenic belt.
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia 45
Table 1. LA-ICPMS U-Pb data on zircon
206Pb 207Pb 207... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_141.txt | ), f.buffer([he + ce, he + "-done", he + de + ce, he + de + ue], this.featureName), h.buffer(["newURL"], this.featureName), p.buffer([pe], this.featureName), s.buffer(["propagate", ge, le, "executor-err", "resolve" + ce], this.featureName), o.buffer([pe, "no-" + pe], this.featureName), a.buffer(["new-jsonp", "cb-start"... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_100.txt | 1996
Eastern Segment, Protogine Zone, and Sveconorwegian Frontal Deformation Zone
Centre Metagranite, Övre Fryken, W2, TD-TF Am 207Pb/206Pb 3 956 ±6 Söderlund et al., 1999
Centre Metagranite foliated, Karlstad, W1, TE-TG Am 207Pb/206Pb 3 976 ±4 Söderlund et al., 1999
Centre Quartz monzonite, sheared, Lilla Edsvattnet, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_3.txt | ;
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1275.txt | name":"label","_":"Roberts et al., 2011"},{"#name":"reference","$":{"id":"sbref0230","refId":"46"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"N.M.W."},{"#name":"surname","_":"Roberts"}]},{"#name":"author","$$":[{"#name":"given-na... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_26.txt | , P.-O. 1997: Geochronology and
stuctural setting of the 1.38 Ga Torpa granite; implications for
charnockite formation in SW Sweden. GFF 119, 37-43.
Åhäll, K.-I. & Connelly, J. 1998: Intermittent 1.53-1.13 Ga magmatism
in western Baltica; age constraints and correlations within a
postulated supercontinent. Precambrian ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_10.txt | .0941 0.0008 3.49 0.07 0.269 0.005 0.90 1510 17 1534 25 101.6
5d 0.0947 0.0008 3.22 0.06 0.247 0.004 0.89 1522 15 1421 20 93.3
1b 0.0948 0.0013 3.27 0.07 0.250 0.004 0.74 1524 25 1441 19 94.5
4a 0.0951 0.0010 3.64 0.07 0.278 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_64.txt | ,#onetrust-pc-sdk h6,#ot-sdk-cookie-policy h6{font-size:1.5rem;line-height:1.6}@media(min-width: 550px){#onetrust-banner-sdk h1,#onetrust-pc-sdk h1,#ot-sdk-cookie-policy h1{font-size:1.5rem}#onetrust-banner-sdk h2,#onetrust-pc-sdk h2,#ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_162.txt | href="//cdn.plu.mx/summary.css"><script type="text/javascript" src="//ajax.googleapis.com/ajax/libs/jquery/1.10.2/jquery.min.js"></script><script type="text/javascript" src="//cdn.plu.mx/extjs/xss.js"></script><style type="text/css">.MathJax_Hover_Frame {border-radius:.25em; -webkit-border-radius:.25em; | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_52.txt | eastern part of the south Rogaland igneous complex,
southern Norway. Lithos 12, 199-208.
Pedersen, S. & Konnerup-Madsen, J. 2000: Geology of the Setesdalen
area, South Norway: implications for the Sveconorwegian evolution of South Norway. Bulletin of the Geological Society of Denmark
46, 181-201.
Persson, A.I. 1999: A... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_719.txt | list-entry-outline-padding text-s u-font-serif" id="special-issue-articles-article1-title"><a class="anchor u-clamp-2-lines anchor-default" href="/science/article/pii/S0301926815001618" title="Detrital zircon signatures of the Baltoscandian margin along the Arctic Circle Caledonides in Sweden: The Sveconorwegian connec... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_trap3.txt | part3 -------------------
Stratigraphic trap[edit]
Stratigraphic trapStratigraphic trap under an unconformity.Stratigraphic trap in a coral reef (reservoir rock) sealed in mudstones (caprock).Stratigraphic trap associated with an evaporite diapir (pink).blue: source rock; yellow: reservoir rock; green: cap rock; red: ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_156.txt | delete e[r], s.parentNode && s.parentNode.removeChild(s), i && i.forEach(e => e(n)), t) return t(n);
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_111.txt | Andersson et
al. 1999; 2002a; Söderlund et al. 2002; Möller et al. 2007).
Zircon inclusions in eclogite-facies garnet provide a maximum age of 972 ±14 Ma for the ecolgite-facies overprint
(Ullared locality; Fig. 8d; Johansson et al. 2001). Titanite
U-Pb data range from 956 ±4 to 923 ±3 Ma (Fig. 4, Table
5; Connelly et... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1349.txt | },{"#name":"volume-nr","_":"95"}]},{"#name":"date","_":"2010"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"185"},{"#name":"last-page","_":"187"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0355"},"$$":[{"#name":"label","_":"Zen and Hammarstrom, 1984"},{"#name":"reference","$":{"id":"sbref0355","refId":"71"},... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_734.txt | bottom"><h3 class="related-content-panel-list-entry-outline-padding text-s u-font-serif" id="recommended-articles-article3-title"><a class="anchor u-clamp-2-lines anchor-default" href="/science/article/pii/S0301926816300146" title="Discovery of pelitic high-pressure granulite from Manjinggou of the Huai’an Complex, Nor... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1260.txt | _":"S.R."},{"#name":"surname","_":"Paterson"}]},{"#name":"author","$$":[{"#name":"given-name","_":"V."},{"#name":"surname","_":"Memeti"}]},{"#name":"author","$$":[{"#name":"given-name","_":"G."},{"#name":"surname","_":"Pignotta"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S."},{"#name":"surname","_":"Erdmann | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_611.txt | 26801001541" target="_self"><span class="anchor-text">Long-lived (1.8–1.0<!-- --> <!-- -->Ga) convergent orogen in southern Laurentia, its extensions to Australia and Baltica, and implications for refining Rodinia</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Preca... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_55.txt | 125.
Andréasson, P.G. & Rodhe, A. 1994: Ductile and brittle deformation
within the Protogine Zone, southern Sweden: a discussion. Geologiska Föreningens i Stockholm Förhandlingar 116, 115-117.
Andréasson, P.G. & Dallmeyer, R.D. 1995: Tectonothermal evolution
of high-alumina rocks within the Protogine Zone, southern Swe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1348.txt | urname","_":"Whitney"}]},{"#name":"author","$$":[{"#name":"given-name","_":"B.W."},{"#name":"surname","_":"Evans"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Abbreviations for names of rock-forming minerals"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#na... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_634.txt | "><h3 class="title">Nor. J. Geol.</h3></div><div class="series">(2008)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>B. </span>Bingen</span><em> et al.</em></span><h3 class="title">A four-phase model for the Sveconorwegian orogeny, SW Scand... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_75.txt | 17 U-Pb SIMS 2 Åhäll et al., 1998 Zrn 1043±11 Am Kärra granite, pegmatite, DC200020 U-Pb SIMS 8 Austin Hegardt et al., 2007 Zrn 1026±5 Gr Metadolerite dyke, Trollhättan, Haregården U-Pb ID-TIMS 3 Söderlund et al., 2008 Zrn 1046 ±6 Gr Metadolerite dyke, Trollhättan, Lunden U-P | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1116.txt | roan Farsund intrusion (SW Norway)"}],"floats":[],"footnotes":[],"attachments":[]},"openArchive":false,"openAccess":false,"document-subtype":"fla","content-family":"serial","contentType":"JL","abstract":{"$$":[{"$$":[{"$":{"id":"sect0005"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{"$$":[{"#name":"... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_31.txt | & Kramers 1975)
(2) Coefficient of error correlation
(3) Discordance along a discordia line to the origin: 100 *(206Pb/238U age)/(207Pb/206Pb age)
(4) Analysis discarded for mean age calculation
112 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY Table 6. Monitoring of the accuracy of the LA-ICPMS U-Pb analytical method... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_86.txt |
8 0.0927 0.0008 3.29 0.05 0.257 0.004 0.87 1481 15 1476 19 99.6
12 0.0929 0.0011 3.42 0.07 0.267 0.004 0.79 1487 23 1526 22 102.6
9 0.0931 0.0010 2.89 0.05 0.226 0.003 0.80 1489 21 1311 18 88.1
5 0.0932 0.0013 3.26 0.07 0.254 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_136.txt | (X,W,V,Y,C[P+15],M,1236535329);Y=f(Y,X,W,V,C[P+1],A,4129170786);V=f(V,Y,X,W,C[P+6],z,3225465664);W=f(W,V,Y,X,C[P+11],y,643717713);X=f(X,W,V,Y,C[P+0],w,392106 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_604.txt | "><span class="u-font-sans"><span class="author u-font-sans"><span>T.S. </span>Brewer</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0301926804001664" target="_self"><span class="anchor-text">Mesoproterozoic bimodal volcanism in SW Norway, evidence for recurring pre-... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_35.txt | PMS 11 11 0.30 1496 11 intrusion 10B
Sauda Sauda supra granodiorite gneiss weak B00-145 356486 6615548 Bt, Amp, Ttn, Ep LA-ICPMS 12 12 0.41 1497 12 intrusion 10C
Bykle Botsvatn granodiorite gneiss strong B02-022 401532 6584563 Bt, Amp, Ttn SIMS 11 9 1.3 1498 8 intrusion 9C
Bykle Botsvatn granite g | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_2.txt |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_34.txt | 1. The Eastern Segment is not pictured in the model as it developed at the end of the Sveconorwegian
orogeny by underthrusting of the Fennoscandia basement.
on Fennoscandia during the Sveconorwegian orogeny.
In the western part of the orogen, in the Telemark, Hardangervidda, Suldal and Rogaland-Vest Agder sectors,
the... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_56.txt | characteristics. Contributions to Mineralogy and
Petrology 154, 357-369.
B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
71
Romer, R.L. & Smeds, S.A. 1996: U–Pb columbite ages of pegmatites
from Sveconorwegian terranes in southwestern Sweden. Precambrian Research 76, 15-30.
Schärer, U., Wilmart, E. & Duchesne, J.-C. 199... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_13.txt | thonous
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1999). The other lithotectonic units have suffered significant Sveconorwegian transport relative to Fennoscandia
and are referred to as terranes. These are the Idefjorden,
Kongsberg, Bamble and Telemar... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_38.txt | Pb 1674 +24/-19 Persson et al., 1995
PZ-SFDZ Metagranite, Övre Fryken, W2 Zrn U-Pb 1674 ±7 Söderlund et al., 1999
Centre Monzonite, Broby, E1 Zrn U-Pb 1674 ±7 Söderlund et al., 1999
South Borås tonalite, AA9637 Zrn U-Pb 1674 ±8 Scherstén et al., 2000
North Brustad augen gneiss | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1180.txt | Id":"18"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Falkum"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Geologisk kart over Norge, berggrunnskart MANDAL, 1:250,000"}]}]},{"#name":"host","$$... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_652.txt | -articles-header"><h2 class="u-h4 u-margin-l-ver u-font-serif">Cited by (44)</h2></header><div aria-describedby="citing-articles-header"><div class="citing-articles u-margin-l-bottom"><ul><li class="ListArticleItem u-margin-l-bottom"><div class="sub-heading u-margin-xs-bottom"><h3 class="u-font-serif" id="citing-articl... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_524.txt | 24" aria-label="Access through your institution"><svg focusable="false" viewBox="0 0 253.88 253.99" aria-label="Seamless access" width="10" height="20" role="img" class="icon icon-seamless-access inst-icon"><g><path d="M37.58,97.76h178.73c5.7,0,10.68-3.56,12.46-8.9c1.42-5.34-0.36-11 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_60.txt | se porphyry Zrn 1614 ±7 Lundqvist and Skiöld, 1993
Slemmestad metarhyolite, 01/25 Zrn 1615 ±31 Andersen et al., 2004
Åmål granodiorite, 77018 Zrn 1616 ±24 Welin et al., 1982
Olstorp ultramafic intrusion, contact melt OD16 Zrn 1624 ±6 Scherstén et al., 2000
Horred fm, Mjösjö dacite Zrn 1643 ±29 Å | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_51.txt | (Fig. 1). In
its northern part, it forms a ductile shear zone and a
brittle normal fault system recording downthrow of the
Telemark Sector relative to the Hardangervidda Sector
(Sigmond 1985). The fault system displaces rocks of the
Kalhovd formation, deposited after 1065 ±11 Ma (Bingen et al. 2003). Southwards, the M... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_898.txt | camres.2021.106301","externalArticle":false,"issn":"03019268","openAccess":1,"pii":"S0301926821002291","publicationDate":"2021-08-15","publicationTitle":"Precambrian Research","publicationYear":"2021","scopusArticleUrl":"http://www.scopus.com/scopus/inward/record.url?partnerID=10&rel=3.0.0&view=basic&eid=2-s2.0-85 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1268.txt | from granulite facies rocks: evidence for growth and interaction with metamorphic fluids"}]}]},{"#name":"host","$$":[{"#name":"edited-book","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Goldschmidt 2000"}]},{"#name":"date","_":"2000"},{"#name":"publisher","$$":[{"#name":"name","_":"Cambridge Publications"},{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_11.txt | 9567);
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_66.txt | 57 23057 0.12160 0.72 5.978 2.35 0.3566 2.24 0.95 1980 13 1966 38 99.3 (1) Measured ratio (2) Ratio after correction for common Pb, using present-day average terrestrial isotopic composition following Stacey & Kramers (1975) (3) Coefficient of error correlation (4) Discordance along a discordia line to the origin: 100... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_512.txt | .01 9.05-21.85c5.84-5.83 13.59-9.05 21.85-9.05 8.25 0 16.01 3.22 21.84 9.05 5.84 5.84 9.05 13.6 9.05 21.85s-3.21 16.01-9.05 21.85c-5.83 5.83-13.59 9.05-21.84 9.05-8.26 0-16.01-3.22-21.85- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_915.txt | :ja":true,"xmlns":true},"$$":[{"#name":"title","_":"The structural, metamorphic and magmatic evolution of Mesoproterozoic orogens"},{"#name":"editors","$$":[{"#name":"author-group","$$":[{"#name":"author","$$":[{"#name":"degrees","_":"Dr."},{"#name":"given-name","_":"Nick"},{"#name":"surname","_":"Roberts"}]}]},{"#name... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_712.txt | V. All rights reserved.</span></div></article><div class="u-show-from-md col-lg-6 col-md-8 pad-right u-padding-s-top"><aside class="RelatedContent u-clr-grey8" aria-label="Related content"><section class="SpecialIssueArticles" id="special-issue"><section class="RelatedContentPanel u-margin-s-bottom"><header id="special... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_61.txt | sdk-cookie-policy h1,#ot-sdk-cookie-policy h2,#ot-sdk-cookie-policy h3,#ot-sdk-cookie-policy h4,#ot-sdk-cookie-policy h5,#ot-sdk-cookie-policy h6{margin-top:0;font-weight:600;font-family:inherit}#onetrust-banner-sdk h1,#onetrust-pc-sdk h1,#ot-sdk-cookie- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_37.txt | uge & Brewer
1996; Sigmond et al. 1997). Differences in the style of
magmatic suites thus suggest that continental building
and reworking took place in different settings around 1.5
Ga in the different sectors and that the sectors were affected by relative motion after 1.5 Ga. The tight 1.52-1.48 Ga
time interval for c... |
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