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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_612.txt | div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>F.J. </span>Korhonen</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0301926812002938" target="_self"><span class="anchor-text">How long-lived ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1067.txt | italic","_":"P"},{"#name":"__text__","_":") granulite facies retrogression is characterized by Grt-Sil-Kfs-Pl-Bt-Rt-Liq-Qz. Pseudosection approaches were undertaken in the Na"},{"$":{"loc":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_":"O-CaO-K"},{"$":{"loc":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_641.txt | 3 class="title">Cyclicity in Cordilleran orogenic systems</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Nat. Geosci.</h3></div><div class="series">(2009)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>K... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_575.txt | representing a main collisional event between ca. 1030 and 970<!-- --> <!-- -->Ma, followed by a contact metamorphic event at 930<!-- --> <!-- -->Ma. Magmatism has been grouped into a ‘syn-collisional’ suite at 1050–1035<!-- --> <!-- -->Ma, a ‘post-collisional’ suite at 980–930<!-- --> <!-- -->Ma, ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_928.txt | is no consensus as to the large-scale tectonic processes that shaped the orogen (e.g., Möller et al., 2013, Slagstad et al., 2013a, Slagstad et al., 2013b)."}]},{"#name":"para","$":{"id":"par0030","view":"all"},"$$":[{"#name":"__text__","_":"The Sirdal Magmatic Belt (SMB) is a recently discovered granitic batholith in... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_798.txt | 6 May 2015","Publication date":"1 August 2015","Version of Record":"19 June 2015"},"downloadFullIssue":false,"entitlementReason":"unsubscribed","hasBody":true,"has-large-authors":false,"hasScholarlyAbstract":true,"headerConfig":{"contactUrl":"https://service.elsevier.com/app/contact/supporthub/sciencedirect/","userName... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_90.txt | TA Am 207Pb/206Pb 1 916.9 ±1.9 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Veggja, B642, TB Am 207Pb/206Pb 1 917 ±14 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Feda, B114, TC Am 207Pb/206Pb 1 917.5 ±1.8 Bingen & van Breemen, 1998
Rogaland-VA Augen g | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_705.txt | . 980–930 Ma) orogenesis as well as Sveconorwegian migmatization (1050–950 Ma). Newly documented 1050–1020 Ma magmatism and migmatization extend the Sirdal Magmatic Belt to a 300 km-long, NNW-SSE trending crustal domain, with the northern boundary corresponding to the gradual transition from Telemar... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_685.txt | n = 1212), Baltica (NE Europe, n = 1922), Amazonia (central South America, n = 625), Kalahari (southern Africa and Dronning Maud Land in East Antarctica, n = 386), and western Australia (n = 199). Laurentia, Baltica, and Amazonia (and possibly other cratons) most likel... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_618.txt | a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">J. Volcanol. Geotherm. Res.</h3></div><div class="series">(2008)</div></span></li></ul><div class="u-display-none"><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>D. </spa... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_38.txt |
eclogite facies metamorphism in the Sveconorwegian Province of
SW Sweden. Precambrian Research 106, 261-275.
Johansson, Å. 1990: Age of the Önnestad syenite and some gneissic
granites along the southern part of the Protogine Zone, southern
Sweden. In Gower, C.F., Rivers, T. & Ryan, B. (eds.), Mid-Proterozoic
Laurentia... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1293.txt | #name":"surname","_":"Schmidt"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S."},{"#name":"surname","_":"Poli"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Magmatic epidote"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Rev. ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_6.txt | 17 1392 21 93.9
11 0.0929 0.0028 3.41 0.14 0.266 0.008 0.69 1485 57 1522 39 102.5
7 0.0934 0.0010 3.39 0.05 0.264 0.002 0.62 1496 21 1508 12 100.8
13 0.0935 0.0010 3.10 0.05 0.241 0.003 0.71 1497 21 1390 14 92.8
9 0.0936 0.0019 3.40 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_601.txt | "><button type="button" class="button button-anchor" aria-disabled="false"><span class="button-text">Special issue articles</span></button><button type="button" class="button button-anchor" aria-disabled="false"><span class="button-text">Recommended articles</span></button></div><div class="Tail text-s"></div><div id="... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_14.txt |
evaporation dating of complex zircons from a pegmatite in the
high-grade gneisses of southwestern Sweden. Lithos 38, 93-105.
Söderlund, U., Jarl, L.-G., Persson, P.-O., Stephens, M.B. & Wahlgren,
C.-H. 1999: Protolith ages and timing of deformation in the
eastern, marginal part of the Sveconorwegian orogen, southweste... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_3.txt | conorwegian orogen.
Sampling and analytical methods
Samples were collected along a broad E-W transect
across the western part of the Sveconorwegian orogen
in S Norway. These include metavolcanic, metaigneous
and metasedimentary rocks from pre-Sveconorwegian
supracrustal complexes and their possible basement
(Figs. 3, 4... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_976.txt | ,"xmlns:sb":true},"#name":"abstracts"},"pdf":{"urlType":null},"iss-first":"","vol-first":"265","isThirdParty":false,"language":"en","issn-primary-unformatted":"03019268","issn-primary-formatted":"0301-9268"},{"pii":"S0301926814002514","doi":"10.1016/j.precamres.2014.07.006","journalTitle":"Precambrian Research","public... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_15.txt | a characteristic assemblage of quartzite, mica gneiss, sillimanite-rich gneiss and
minor orthoamphibole-cordierite rocks. The Kongsberg
Terrane hosts a suite of c. 1200 Ma mafic plutons (Munz
et al. 1994). The Bamble Terrane hosts the 1200-1180 Ma
gabbro-tonalite Tromøy complex, 1170-1150 Ma granitecharnockite metaplu... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_173.txt | Identity User'
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_602.txt | header><h2 class="u-h4 u-margin-l-ver"><span>References</span><span> (71)</span></h2></header><ul><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><a class="anchor title anchor-default" href="/science/article/p... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_539.txt | 16 pad-left pad-right" lang="en"><div class="Publication" id="publication"><div class="publication-brand u-show-from-sm"><a class="anchor anchor-default" href="/journal/precambrian-research" title="Go to Precambrian Research on ScienceDirect"><span class="anchor-text"><img class="publication-brand-image" src="https://s... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_68.txt | avatnet, NR17C Zrn U-Pb 1037 ±16 Möller et al., 2002
Rogaland Pegmatite leucosome, Gyavatnet, NR16A Zrn U-Pb 1039 ±11 Möller et al., 2003
Rogaland Granodiorite augen gneiss, Osen, NR2B Zrn U-Pb 1039 ±7 Möller et al., 2002
Rogaland Garnet migmatite gneiss, Gyadalen, NR12E Zrn | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_40.txt | .6 0.2939 1.3 0.84 1661 19 1707 15 2.7
19 49621 0.10375 0.8 4.231 1.7 0.2957 1.4 0.87 1670 21 1692 15 1.3
11 23029 0.10360 0.7 4.236 1.5 0.2965 1.2 0.86 1674 18 1690 14 0.9
22 67947 0.10366 1.0 4.243 2.0 0.2968 1.8 0 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1095.txt | oproterozoic Bandak succession in southern Norway consists of interlayered quartzites and meta-volcanic rocks with well preserved depositional and structural relations, which when combined provide important information on the late Mesoproterozoic continental margin of Baltica prior to the assembly of the supercontinent... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_851.txt | agstad T., Henderson I.H.C., Roberts N.M.W., Kulakov E.V., Ganerød M., Kirkland C.L., Dalslåen B., Creaser R.A., Coint N.","doi":"10.1016/j.precamres.2022.106695","externalArticle":false,"issn":"03019268","openAccess":1,"pii":"S0301926822001395","publicationDate":"2022-07-15","publicationTitle":"Precambrian Research | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_13.txt | character and evolution,
37, 103-110. Geological Survey of Finland, Special Paper 37, Espoo.
Ask, R. 1996: Single zircon evaporation Pb-Pb ages from the Vaggeryd
syenite and dolerites in the SE part of the Sveconorwegian orogen,
Småland, S Sweden. GFF 118, A8.
Berg, Ø. 1977: En geokronologisk analyse av prekambrisk ba... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_650.txt | its geological evolution and a summary of the contributions made by this volume</h3><span class="host u-clr-grey6 u-font-sans"></span></li></div><button class="button-alternative button-alternative-secondary text-m u-font-sans u-margin-l-bottom button-alternative-icon-left" type="button" id="show-more-refs-btn"><span ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_973.txt | ritus was derived from non-Yilgarn Archean sources, and reworked Archean sources, which were added to sedimentary basins developed over the Musgrave Province basement during and after c. 1400"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma. To the south of the Musgrave Province, the Madura Province has ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_525.txt | .04-4.99-14.24l-89.37-64.09 c-4.63-3.2-10.68-3.2-14.95,0L30.11,74.61c-3.2,2.49-5.34,6.05-5.34,10.33C24.77,92.06,30.46,97.76,37.58,97.76z M126.95,36.87 l49.49,35.25H77.46 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_421.txt | ion-layout.ot-cat-item{border-width:0 0 2px}div#onetrust-pc-sdk.ot-accordion-layout.ot-cat-item:first-of-type{border-width:2px 0}div#onetrust-pc-sdk.ot-accordion-layout.ot-acc-hdr{padding:8px 0;width:100%}div#onetrust-pc-sdk.ot-plus-minus{transform:translateY(2px)}div# | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1171.txt | ]}]},{"#name":"bib-reference","$":{"id":"bib0075"},"$$":[{"#name":"label","_":"DeCelles et al., 2009"},{"#name":"reference","$":{"id":"sbref0075","refId":"15"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"P.G."},{"#name":"surname",... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_65.txt | .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, Sveco... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1518.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_45.txt | 02 ±11 Lundqvist & Persson, 1999
PZ Alvesta granite gneiss, 86011 Zrn U-Pb 1713 ±3 Johansson, 1990
North Tonalite, Mo Zrn U-Pb 1731 ±7 Mansfeld, 2000
Centre Meta granite Zrn U-Pb 1777 +38/-22 Welin, in Söderlund et al., 1999
PZ-SFDZ Filipstad granite, 82051 Zrn U-Pb 1783 ±10 Jarl & Johansson, 1988
SF | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_576.txt | charnockite–granite (AMCG) suite at 930<!-- --> <!-- -->Ma. New detailed mapping and geochronology in the area reveal a very different and much more complex evolution, and require re-evaluation of previously presented models. In this paper, we focus on the introduction and description of a newly discovered, ca. 20... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_598.txt | 2 class="section-title u-h4 u-margin-l-top u-margin-xs-bottom">Conclusions</h2><p id="par0460">A major conclusion of this work is that magmatic activity was a much more voluminous and intergral part of the orogenic evolution than hitherto known (cf., Bingen et al., 2008a), and that the metamorphic evolution in SW Norwa... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_584.txt | shaped the orogen (e.g., Möller et al., 2013, Slagstad et al., 2013a, Slagstad et al., 2013b).</p><p id="par0030">The Sirdal Magmatic Belt (SMB) is a recently discovered granitic batholith in the southwestern part of the orogen (Fig. 1a), emplaced between ca. 1060 and 1020<!-- --> <!-- -->Ma (Slagstad et al., 201... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1004.txt | 3853"},{"#name":"pixel-height","_":"100"},{"#name":"pixel-width","_":"219"},{"#name":"attachment-type","_":"IMAGE-THUMBNAIL"}],"$":{"xmlns:xocs":true},"#name":"attachment"}],"#name":"attachments"},{"$$":[{"$":{"id":"sect0005"},"#name":"section-title","_":"Graphical abstract"},{"$$":[{"$":{"view":"all","id":"spar0095"},... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1027.txt | mainly induced by flow."}],"$":{"id":"lsti0025"},"#name":"list-item"}],"$":{"id":"lis0020"},"#name":"list"}],"$":{"view":"all","id":"spar0085"},"#name":"simple-para"}],"$":{"view":"all","id":"abst0005"},"#name":"abstract-sec"}],"$":{"view":"all","id":"abs0005","class":"author-highlights"},"#name":"abstract"},{"$$":[{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_903.txt | ":{"view":"all","id":"p0015"},"#name":"para","_":"The recognition of 1050–1020 Ma magmatism and migmatization in the study area delineates the northern extension of the Sirdal Magmatic Belt."}],"$":{"id":"o0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0020"},"#name":"para","_":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1103.txt | ZDlQulARozDA9MQh7YO1z9TIOXBSfqEWmKFlvh4MWzTbPnyKhzTocQTdPw","authors":{"content":[{"#name":"author-group","$":{"id":"aug0005"},"$$":[{"#name":"author","$":{"id":"aut0005"},"$$":[{"#name":"given-name","_":"Jacqueline"},{"#name":"surname","_":"Vander Auwera"},{"#name":"cross-ref","$":{"id | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_58.txt | . 8.
108 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY Table 3. SIMS U-Pb data on detrital zircons from a metasandstone sample Concentrations Atomic ratios Ages Sample/ U Th Pb 206Pb 207Pb ±σ 207Pb ±σ 206Pb ±σ rho 207Pb ±σ 206Pb ±σ Disc. analysis 204Pb 206Pb 235U 238U 206Pb 238U (ppm) (ppm) (ppm) (%) (%) | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_10.txt | and magmatism in the Idefjorden and Telemarkia Terranes.
At 1050 Ma (Fig. 8b), the Idefjorden Terrane was underthrust and buried to a depth of at least 35 km and possibly more than 50 km, resulting in high-pressure amphibolite- to granulite-facies metamorphism (1.0-1.5 GPa;
Bingen et al. 2008b; Söderlund et al. 2008).... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1155.txt | ","$$":[{"#name":"maintitle","_":"Lithos"}]},{"#name":"volume-nr","_":"87"}]},{"#name":"date","_":"2006"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"328"},{"#name":"last-page","_":"346"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0050"},"$$":[{"#name":"label","_":"Bingen and Van Breemen, 1998a"},{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_50.txt | basin related to formation of the BambleKongsberg collision zone.
After 1.10 Ga, Sveconorwegian deformation propagated
towards the foreland and hinterland to accommodate
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_772.txt | id":"spar0010"},"#name":"simple-para","_":"The Late Mesoproterozoic Sveconorwegian Province is commonly correlated with the continent-collision related Grenville Province in eastern Canada. Recently, however, the evolution of the Sveconorwegian Province in SW Norway has been strongly debated, casting doubt on a direct ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1272.txt | is et al., 2014"},{"#name":"reference","$":{"id":"sbref0225","refId":"45"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"D."},{"#name":"surname","_":"Regis"}]},{"#name":"author","$$":[{"#name":"given-name","_":"C.J."},{"#name":"surn... | |
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