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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_13.txt | utons in the Telemarkia Terrane (Feda
and Fennefoss augen gneiss suites; Table 3; Bingen et al.
1993; Bingen & van Breemen 1998a). Geotectonic interpretation of these “orogenic” granodiorite suites remains
ambiguous. They can reflect either the final stage of an
active continental margin setting in the belt, or melting... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_1.txt | 3 Hellström et al., 2004
Vinga porphyry Zrn U-Pb 963 ±17 Åhäll & Schöberg, 1999
Skuleboda rare-mineral pegmatite Clm U-Pb 984 ±6 Romer & Smeds, 1996
Högsbo rare-mineral pegmatite Clm U-Pb 1030 ±1 Romer & Smeds, 1996
Timmerhult rare-mineral pegmatite Clm U-Pb 1039 ±3 Rom | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_591.txt | and the data in Electronic Supplement 2.</p><p id="par0085">The geographic extent of the SMB, as shown in Fig. 1a, is based on mapping by the Geological Survey </p></section></section><section><section id="sec0085"><h2 class="section-title u-h4 u-margin-l-top u-margin-xs-bottom">Host rock characteristics and relations... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1346.txt | ":"High-temperature metamorphism and the role of magmatic heat sources at the Rogaland anorthosite complex in Southwestern Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"J. Petrol."}]},{"#name":"volume-nr","_":"44"}]},{"#name":"date","_... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1117.txt | The Farsund intrusion is made of two intermingled coeval facies."}],"$":{"id":"lsti0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0010"},"#name":"para","_":"The two facies belong to the two Sveconorwegian late-orogenic magmatic suites."}],"$":{"id":"lsti0010"},"#name":"list-ite... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1072.txt | 1.88–1.80"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ga). This finding changes previous views that the pelitic rocks and associated mafic granulites are different slabs with individual metamorphic history. The khondalite series from the Huai’an Complex and adjacent Ji’ning Complex were probably experi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_655.txt | 1 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">Most pegmatites of southern Norway seem to be derived from anatectic ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_39.txt | al
4 1801 12 detrital
2 1834 11 detrital
1 1980 25 detrital
(1) gp: group; supra: supracrustals.
(2) Qualitative evaluation of the deformation of the rock following field and petrographic data.
(3) UTM WGS84 coordinates, zone 32.
(4) Diagnostic minerals: Amp: amphibole; Bt: biotite; Ms: muscovite; Ttn: titanite; Ep: ep... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_44.txt | Follum tonalite gneiss, Fig. 8B
1 8gr,+75,cl,c,s-pr 19 18.2 59 2 0.74 10877 0.09617 6 3.59361 566 0.27102 41 1551.1 1.2 0.8
2 6gr,+75,cl,c,s-pr 16 21.7 71 7 0.68 2717 0.09627 13 3.60478 771 0.27158 63 1553.0 2.6 0.5
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_17.txt | West Norway) relatable to forceful emplacement of
expanding plutons. Geologische Rundschau 71, 104-119.
Tucker, R.D., Krogh, T.E. & Råheim, A. 1990: Proterozoic evolution
and age - province boundaries in the central part of the Western
Gneiss Region, Norway: results of U-Pb dating of accessory minerals from Trondheimsf... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_586.txt | wegian orogen, with several geographically overlapping events of different character and timing, that need to be understood in detail, to gain insight into the processes that shaped the orogen.</p></section></div></div><div id="preview-section-snippets"><div class="PageDivider"></div><div class="Snippets u-font-serif t... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_45.txt | ic Geology 25, 727-750.
Mulch, A., Cosca, M.A., Andresen, A. & Fiebig, J. 2005: Time scales of
deformation and exhumation in extensional detachment systems
determined by high-spatial resolution in situ UV-laser 40Ar/39Ar
dating. Earth and Planetary Science Letters 233, 375-390.
Munz, I.A. 1990: Whiteschists and orthoam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_552.txt | W.</span> <span class="text surname">Roberts</span> </span><span class="author-ref" id="baff0010"><sup>b</sup></span></span></button>, <button class="button-link button-link-primary" type="button" data-sd-ui-side-panel-opener="true" data-xocs-content-type="author" data-xocs-content-id="aut0020"><span class="button-link... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_47.txt | , source and REE mobility. Contributions to Mineralogy and
Petrology 116, 32-46.
Nijland, T.G. & Maijer, C. 1993: The regional amphibolite to granulite
facies transition at Arendal, Norway: evidence for a thermal dome.
Neues Jahrbuch für Mineralogie, Abhandlungen 165, 191-221.
Nijland, T.G., Maijer, C., Senior, A. & Ve... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_86.txt | mark Rjukan Gp, Runhellohovet metarhyolite Zrn U-Pb 1510 c. Dahlgren et al., 1990
Telemark Rjukan Gp, metarhyolite, Uvdal, S93-305 Zrn U-Pb 1512 +10/-8 Bingen et al., 2005
Suldal Augen gneiss, Vanvik, B00112 Zrn U-Pb 1516 ±11 Bingen et al., 2005
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_0.txt | area, South Norway: implications for the Sveconorwegian
evolution of South Norway. Bulletin of the Geological Society of
Denmark 46, 181-201.
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 Föreninge... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_29.txt |
et al. 1999, 2002).
In the Idefjorden terrane, continental building is recorded
between 1.66 and 1.52 Ga (Figs. 2, 7; Table 8). The
geochemical and isotopic signatures of magmatic suites
are typical for active margin settings (Brewer et al.
1998; Hageskov & Mørch 2000; Andersen et al. 2004).
Magmatic rocks with a juve... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_587.txt | 4 u-margin-l-top u-margin-xs-bottom">Regional geology</h2><p id="par0035">The study area is located in the southwesternmost part of the Sveconorwegian Province and has previously been interpreted to consist of high-grade ortho- and lesser amounts of para- and banded gneisses that were deformed and metamorphosed between... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_24.txt | Roddick, J.C. & Spiegel, W. 1995: Three natural
zircon standards for U-Th-Pb, Lu-Hf, trace element and REE
analyses. Geostandards Newsletter 19, 1-23.
Zhou, X.Q., Bingen, B., Demaiffe, D., Liégeois, J.-P., Hertogen, J., Weis,
D. & Michot, J. 1995: The 1160 Ma old Hidderskog meta-charnockite: implications | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_624.txt | ><a class="anchor title anchor-default" href="/science/article/pii/S0301926814001946" target="_self"><span class="anchor-text">Source-derived heterogeneities in the composite (charnockite-granite) ferroan Farsund intrusion (SW Norway)</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 cla... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_603.txt | 493705001647" target="_self"><span class="anchor-text">Molybdenite re-os dating constrains gravitational collapse of the Sveconorwegian orogen, SW Scandinavia</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Lithos</h3></div><div class="series">(2006)</div></span></li><li ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_67.txt | , 0724061 T Ttn 918 ±7 Andersen et al., 2002 a
Tellnes dyke, ilmenite norite, T2 R Zrn 920 ±3 Schärer et al., 1996
Egersund-Ogna anorthosite, EO1 R Zrn 929 ±2 Schärer et al., 1996
Farsund charnockite, PA70A R Zrn 930 ca. Pasteels et al., 1979
Tellnes dyke, quartz mangerite, 849 R Zrn 931 ±5 Sch | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_28.txt |
Åhäll, K.-I., Connelly, J.N. & Brewer, T.S. 2000: Episodic rapakivi
magmatism due to distal orogenesis? Correlation of 1.69-1.50 Ga
orogenic and inboard, "anorogenic" events in the Baltic shield.
Geology 28, 823-826.
Åhäll, K.-I. & Larson, Å. 2000: Growth-related 1.85-1.55 Ga
magmatism | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_22.txt | -Pb 1631 ±3 Åhäll & Connelly, 2008
Göteborg batholith, Kabbosjön granite Zrn U-Pb 1634 +3/-2 Åhäll & Connelly, 2008
Horred Fm, Mjösjö dacite Zrn U-Pb 1643 ±29 Åhäll et al., 1995
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_599.txt | belt. Cross-cutting relationships along the length of the belt show that the SMB was emplaced into a regionally deformed and metamorphosed crust. In</p></section></section><section><section id="ack0005"><h2 id="sect0200" class="u-h4 u-margin-l-top u-margin-xs-bottom">Acknowledgements</h2><p id="par0480">We would like ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_1.txt | wegian bimodal continental magmatism
are recorded between 1220 and 1200 Ma (Larsson &
Söderlund 2005; Söderlund & Ask 2006). The spatial link
between this magmatism and the Protogine Zone, suggests that the eastern limit of the Sveconorwegian belt
was a zone of protracted lithospheric weakness during
the Mesoproterozoi... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_110.txt | ; Möller 1999; Austin Hegardt et al.
2005). These boudins show evidence of a clockwise pressure-temperature path, with peak conditions exceeding
1.5 GPa and decompression through 0.96-1.2 GPa and
705-795 °C (Fig. 8d; Möller 1998; Möller 1999). Metamorphic zircon from several samples brackets Sveconorwegian high-grade m... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_38.txt | arp syenite Zrn 1204 +14/-8 Hansen and Lindh, 1991
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_579.txt | (s) that affected the region.</p><p id="spar0020">Our observations of cross-cutting relationships between previously metamorphosed gneisses and SMB rocks indicate that at least one episode of amphibolite- to granulite-facies metamorphism occurred in the region during or prior to emplacement. A lack of widespread metamo... | |
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