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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_32.txt | ). The voluminous
Stora Le-Marstrand formation and correlative formations
in Norway are made up of metagreywacke associated
with mafic metavolcanic and plutonic rocks deposited
at or after 1.58 Ga (Fig. 2; Åhäll et al. 1998; Bingen et al.
2001a). Two types of detrital zircon age distribution are
recorded in the greywac... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_829.txt | from granites. We test this hypothesis by providing new age data for thirteen pegmatites and one granite. Based on these new age data, we distinguish two age groups of Sveconorwegian pegmatites (>1,000 m"},{"$":{"loc":"post"},"#name":"sup","_":"3"},{"#name":"__text__","_":" in size); Group 1: 1100–1030 Ma and Group 2:... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1094.txt | id":"lis0005"},"#name":"list"}],"$":{"view":"all","id":"spar0005"},"#name":"simple-para"}],"$":{"view":"all","id":"abst0005"},"#name":"abstract-sec"}],"$":{"view":"all","id":"abs0005","class":"author-highlights"},"#name":"abstract"},{"$$":[{"$":{"id":"sect0010"},"#name":"section-title","_":"Abstract"},{"$$":[{"$$":[{"#... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_37.txt | by divergence. (4) Between 970 and 900 Ma, the
Dalane phase is one of gravitational collapse of the belt,
characterized by voluminous post-collisional magmatism, gneiss dome and core complex formation and low
pressure, high temperature metamorphism.
Acknowledgements
R.D. Tucker provided the ID-TIMS analyses of zircon ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_0.txt | oblique (sinistral) convergence (Hageskov 1985; Park et
al. 1991; Stephens et al. 1996). Telemarkia was affected
by major deformation during this period. A detailed
account of Sveconorwegian tectonics is beyond the
scope of this paper. The last undisputable evidence for
convergence in the orogen is provided by 972 ± 14... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_879.txt | = 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 likely formed a ca. 10"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"000-km-long external active continental margin o... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_91.txt | neiss, Sirdal, B179, TA Am 207Pb/206Pb 1 918.6 ±2.4 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Mandal, B204, TB Am 207Pb/206Pb 2 918.7 ±3.9 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Mandal, B630, TC Am 207Pb/206Pb 2 918.9 ±4.4 Bingen & van Breemen | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_41.txt | crust. Journal of Petrology
40, 909-933.
Koistinen, T., Stephens, M.B., Bogatchev, V., Nordgulen, Ø., Wennerström, M. & Korhonen, J. 2001: Geological map of the Fennoscandian shield, Scale 1:2000000. Geological Surveys of Finland,
Norway and Sweden and the North-West Department of Natural
Resources of Russia.
Kullerud... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_680.txt | wall. Field and geochronologic data suggest that the RAP formed and was emplaced over a long period of time, up to 100 Myr, with different emplacement mechanisms reflecting an evolving regional stress regime. The distribution of UHT rocks around the RAP reflects differential extensional exhumation between 980 and 930&... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_13.txt | 1563 ±2 Åhäll et al., 2000
Hisingen suite, Lane granite Zrn U-Pb 1566 ±3 Åhäll & Connelly, 2008
Midtskog tonalite, TA116 Zrn U-Pb 1567 ±8 Andersen et al., 2004
Hisingen suite, Ytterby granodiorite Zrn U-Pb 1570 ±7 Åhäll & Connelly, 2008
Feiring quartz diorite, Ø3 Zrn U-Pb 1574 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_735.txt | class="anchor-text"><span>Discovery of pelitic high-pressure granulite from Manjinggou of the Huai’an Complex, North China Craton: Metamorphic <em>P</em>–<em>T</em> evolution and geological implications</span></span></a></h3><div class="article-source u-clr-grey6"><div class="source">Precambrian Research, Volume 278, ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_2.txt | N. & Åhäll, K.-I. 1998: 1.3 Ga anorogenic
magmatism in Southwest Sweden. Abstracts with programs.
Geological Society of America 30:7, 293.
Ragnhildstveit, J., Sigmond, E.M.O. & Tucker, R.D. 1994: Early Proterozoic supracrustal rocks west of the Mandal-Ustaoset fault zone,
Hardangervidda, South Norway. Terra Nova Abstra... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_61.txt | norite, T2 Zrn U-Pb 920 ±3 Schärer et al., 1996
Rogaland Egersund-Ogna anorthosite, EO1 Zrn U-Pb 929 ±2 Schärer et al., 1996
Rogaland Farsund charnockite, PA70A Zrn U-Pb 930 c. Pasteels et al., 1979
Rogaland Tellnes dyke, quartz mangerite, 849 Zrn U-Pb 931 ±5 Schärer et al., 1996 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_24.txt | afic
rocks and rheomorphic dykes. GFF 121, 25-31.
Connelly, J.N., Berglund, J. & Larson, S.Å. 1996: Thermotectonic evolution of the Eastern Segment of southwestern Sweden: tectonic
constraints from U-Pb geochronology. In Brewer, T.S. (ed.),
Precambrian crustal evolution in the North Atlantic Region, 112,
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_1.txt | 256 0.004 0.74 1512 27 1467 20 97.1
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_7.txt | Berglund, J. & Larson, S.Å. 1996: Thermotectonic evolution of the Eastern Segment of southwestern Sweden: tectonic
constraints from U-Pb geochronology. In Brewer, T.S. (ed.), Precambrian crustal evolution in the North Atlantic Region. Geological
Society, London, Special Publications 112, 297-313.
Corfu, F. & Andersen,... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_67.txt | VA Mnz 1032±5, 990±8 Gr Felsic granulite, Øvstabø, B00158 U-Pb SIMS 13 Bingen et al., 2008
Rogaland-VA Zrn 1035±9, 989 ±11, 955±8 Gr Metapelitic gneiss, Byrkjedal, 122B U-Pb SIMS 30 Tomkins et al., 2005
Vardefjell SZ Zrn 1008±14 Am Banded gneiss granodioritic, Flå | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1112.txt | #name":"textfn","_":"Laboratoire de Géologie, Université Blaise Pascal, 5 Rue Kessler, 63038 Clermont-Ferrand, France"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Laboratoire de Géologie, Université Blaise Pascal"},{"#name":"address-line","_":"5 Rue Kessler"},{"#name":"city","_":"Cl... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_617.txt | font-sans"><span class="author u-font-sans"><span>S.R. </span>Paterson</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S037702730800348X" target="_self"><span class="anchor-text">Growth of complex sheeted zones during recycling of older magmatic units into younger: Saw... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_4.txt | L. & Smeds, S.-A. 1996: U-Pb columbite ages of pegmatites
from Sveconorwegian terranes in southwestern Sweden.
Precambrian Research 76, 15-30.
Scherstén, A., Årebäck, H., Cornell, D., Hoskin, P., Åberg, A. &
Armstrong, R. 2000: Dating mafic-ultramafic intrusions by ionmicroprobing contact-melt zircon: examples from SW ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_714.txt | down"><path d="m1 51l7-7 38 38 38-38 7 7-45 45z"></path></svg></button></header><div class="" aria-hidden="false" aria-describedby="special-issue-articles-header"><div class="u-margin-l-bottom"><div class="u-margin-s-bottom text-xs"><a class="anchor text-m anchor-default" href="/science/journal/03019268/265/supp/C"><sp... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_574.txt | h4 u-margin-l-top u-margin-xs-bottom">Abstract</h2><div id="abst0010"><p id="spar0010">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 ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_499.txt | -0.2-2.31c-0.99 0.82-2.84 1.52-4.06 1.52 -2.15 0-4.55-1.71-4.55-5.91C150.89 10.2 152.97 9.18 153.23 9.01M170 19.44c-0.92 0.36-1.72 0.69-2.51 0.69 -1.16 0-1.58-0.66-1.58-2.34V8 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_676.txt | -down"><path d="m1 51l7-7 38 38 38-38 7 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="sp0010">The tectonic setting and mechanisms and duration of ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_139.txt | X,W,C[P+2],z,4243563512);W=f(W,V,Y,X,C[P+7],y,1735328473);X=f(X,W,V,Y,C[P+12],w,2368359562);Y=D(Y,X,W,V,C[P+5],o,4294588738);V=D(V,Y,X,W,C[P+8],m,2272392833);W= | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_36.txt | -TIMS value (4) Z4510, rhyolite from the Northwest Territories, Canada, ID-TIMS age by Davis & Peterson (1998). (5) ØS-99-316, porphyritic quartz syenite from Jølster pluton, W Norway, ID-TIMS age by Skår & Pedersen (2003). (6) Pegmatite from the Larvik district, S Norway, ID-TIMS age by S. Dahlgren, unpublished data. ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1284.txt | Hf–O constraints on the Mesoproterozoic Suldal Arc, SW Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Contrib. Mineral. Petrol."}]},{"#name":"volume-nr","_":"165"}]},{"#name":"date","_":"2013"}]},{"#name":"pages","$$":[{"#name":"first-p... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_55.txt | 40 Ma
overlapping with magmatism in the TIB. In the Idefjorden Terrane, it took place between c. 1660 and 1520 Ma
during the Gothian accretionary event. In the Telemarkia
Terrane, it took place at 1520-1480 Ma. These three main
lithotectonic units have thus independent ancestries. The
Bamble and Kongsberg Terranes shar... | |
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