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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_975.txt | aser Orogen reveals a much more evolved signature, charting progressive juvenile input into an Archean source with strong isotopic and age similarity to the Yilgarn Craton of the West Australian Craton."}],"$":{"view":"all","id":"spar0010"},"#name":"simple-para"}],"$":{"view":"all","id":"abst0010"},"#name":"abstract-se... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_52.txt | ic granite intrusion. Precambrian
Research 98, 151-171.
Andersson, J. 2001: Sveconorwegian orogenesis in the southwestern
Baltic Shield. Zircon geochronology and tectonothermal setting of
orthogneisses in SW Sweden. PhD thesis, Lund University, Lund.
Andersson, J., Möller, C. & Johansson, L. 2002a: Zircon chronology of... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_36.txt | continent-continent collision.
The high-pressure metamorphism at 1050 Ma towards
the foreland of the belt (Idefjorden Terrane) contrasts
with the protracted medium-pressure metamorphism
between 1035 and 970 Ma towards the hinterland (Telemarkia Terrane). (3) At 980-970 Ma, the Falkenberg
phase represents the last step... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_41.txt | .88 1676 26 1691 18 0.9
14p 23435 0.10450 0.8 4.292 1.6 0.2979 1.4 0.88 1681 20 1706 14 1.4
24 8110 0.10357 1.0 4.327 1.5 0.3030 1.1 0.74 1706 16 1689 18 -1.0
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_50.txt | con
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. Geological Society of London, Special Publications, 220,
65-81.
Möller, C. 1998: Decompressed eclogites in ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1201.txt | .J."},{"#name":"surname","_":"Treoloar"}]},{"#name":"editor","$$":[{"#name":"given-name","_":"P.J."},{"#name":"surname","_":"O’Brien"}]}]},{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"What Drives Metamorphism and Metamorphic Reactions?"}]},{"#name":"volume-nr","_":"vol. 138"}]}]},{"#name":"d... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_51.txt | ites (Söderlund et al. 2005). The
rapakivi plutons are unconformably overlain by an undeformed cover of continental sandstone, known as the Jotnian sandstones. The latter are older than 1270 Ma and
interlayered with the Jotnian basalts, possibly coeval with
the 1460 Ma Tuna dolerites (Söderlund et al. 2005).
Eastern Se... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_698.txt | .</p></div></div></div></li><li class="ListArticleItem u-margin-l-bottom"><div class="sub-heading u-margin-xs-bottom"><h3 class="u-font-serif" id="citing-articles-article-5-title"><a class="anchor anchor-default" href="/science/article/pii/S0301926821002291"><span class="anchor-text">Tracing the Sveconorwegian orogen i... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_104.txt | Ullared Ecl 206Pb/238U 5 945 ±4 Johansson et al., 2001
South Migmatitic orthogneiss, Vistbergen, 4 samples Am Low. intercept 17 949 ±4 Connelly et al., 1996
South Aplitic dyke, Vråna, 3 Am Low. intercept 7 950 ±10 Connelly et al., 1996
South Vårgårda quartz-monzonite, deformed facies, T1-T3 Am 207Pb/206Pb 3 950 ±5 Ber... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_60.txt | berggrunnskart
Odda, 1:250000. Norges geologiske undersøkelse, Trondheim.
Skår, Ø. & Pedersen, R.B. 2003: Relations between granitoid magmatism and migmatization: U-Pb geochronological evidence from the
Western Gneiss Complex, Norway. Journal of the Geological Society,
London 160, 935-946.
Smalley, P.C., Field, D., La... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_644.txt | ="title">Geology</h3></div><div class="series">(2007)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="author u-font-sans"><span>T. </span>Falkum</span><h3 class="title">Geologisk kart over Norge, berggrunnskart MANDAL, 1:250,000</h3><span class="host u-clr-grey6 u-font-sans"><div class="series | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_0.txt | Hakefjorden norite, contact melt HAS96003 Zrn U-Pb 916 ±11 Scherstén et al., 2000
Bohus granite, pegmatite-aplite, 88102 Mnz U-Pb 922 ±5 Eliasson & Schöberg, 1991
Begna Flå granite, phenocryst granite, N9438 Zrn U-Pb 928 ±3 Bingen et al., this work
Göteborg dolerite, Tuve dyke Bdl U-Pb 935 ± | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_22.txt | 0.84 1282 26 1677 26 24
13p 5992 0.10337 0.8 3.303 1.6 0.2317 1.4 0.87 1344 17 1686 14 20
04p,x 2014 0.09961 1.4 3.256 2.5 0.2371 2.1 0.83 1372 26 1617 26 15
07p,x 1376 0.10694 1.3 3.673 2.1 0.2491 1.7 0.79 1434 21 1748 24 18
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_40.txt | and anorthosite-mangerite-charnockite (AMC) complex (Fig. 4; Tobi et al. 1985). These are,
from northeast to southwest, clinopyroxene-in in granodioritic gneiss, orthopyroxene-in in granitic gneiss,
osumilite-in in paragneiss, and pigeonite-in in granitic
gneiss. The osumilite and pigeonite isograds are parallel
to the... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_631.txt | -derived and crustal components</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">J. Geol.</h3></div><div class="series">(1993)</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 ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_5.txt |
(marginal to Fennoscandia, or not) produced the 1200-
1180 Ma Tromøy volcanic arc offboard Telemarkia (now
in the Bamble Terrane) and possibly a granite batholith
in the southern part of the Telemarkia Terrane (1200
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_5.txt |
Contributions to Mineralogy and Petrology 139, 115-125.
Scherstén, A., Larson, S.Å., Cornell, D.H. & Stigh, J. 2004: Ion probe
dating of a migmatite in SW Sweden: the fate of zircon in crustal
processes. Precambrian Research 130, 251-266.
Schärer, U., Wilmart, E. & Duchesne, J.-C. 1996: The short duration
and anorogen... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_547.txt | 18.24-23.98c0-9.9-8.52-18.59-18.24-18.59zm0 52.29c-15.96 0-28-14.48-28-33.67 0-15.36 12.82-28.33 28-28.33s28 12.97 28 28.33c0 19.19-12.04 33.67-28 33.67"></path></svg><svg focusable="false" viewBox="0 0 102 128" title="Author | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_41.txt | Geologiske Vintermøte, 6–9 Jan 2000, 115. Norwegian Geological Society, Geonytt,
Trondheim.
Möller, A., O’Brien, P.J., Kennedy, A. & Kröner, A. 2002: Polyphase zircon in ultrahigh-temperature granulites (Rogaland, SW Norway):
constraints for Pb diffusion in zircon. Journal of Metamorphic Geology 20, 727-740.
Möller, A... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_43.txt | body,#ot-sdk-cookie-policy.ot-main-content,#ot-sdk-cookie-policy.ot-toggle,#ot-sdk-cookie-policy #ot-content,#ot-sdk-cookie-policy #ot-pc-content,#ot-sdk-cookie-policy.checkbox,#ot-sync-ntfy div,#ot-sync-ntfy span,#ot-sync-ntfy h1,#ot-sync-ntfy h2,#ot-sync-ntfy | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_57.txt | Austin Hegardt, E., Cornell, D.H., Claesson, L., Simakov, S., Stein, H.J.
& Hannah, J.L. 2005: Eclogites in the central part of the Sveconorwegian Eastern Segment of the Baltic Shield: support for an extensive eclogite terrane. GFF 127, 221-232.
Austin Hegardt, E., Cornell, D.H., Hellström, F.A. & Lundqvist, I. 2007:
E... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_49.txt | ,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_49.txt | 30 ±2
to 925 ±2 Ma indicates that the clinopyroxene isograd
relates to M2 metamorphism (Bingen & van Breemen
1998b; Bingen et al. 2008b). (6) Molybdenite Re-Os data,
collected from deformed rocks, constrain the last increment of regional ductile deformation to be younger than
947 ±3 Ma on a regional scale, and younger ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_626.txt | orwegian orogeny in Fennoscandia: back-thrusting and extensional shearing along the Mylonite Zone</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">(2011)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_46.txt | en, A. & Sylvester, A.G. 2001: Nature and distribution of deep crustal reservoirs in the southwestern part of the
Baltic Shield: evidence from Nd, Sr and Pb isotope data on late Sveconorwegian granites. Journal of the Geological Society, London 158,
253-267.
Andersen, T., Andresen, A. & Sylvester, A.G. 2002a: Timing of... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_82.txt | Zrn 992±24 Am Veined gneiss facies, Tjärnesjö granite, TJ25D U-Pb SIMS 6 Andersson et al., 1999 South Mnz 1410±9, 948±4 Am Deformed granite dyke, Särdal, 3 U-Pb ID-TIMS 5 Christoffel et al., 1999 South Zrn 1415±15 Am Migmatitic granodiorite, Viared, DC03116 U-Pb SIMS 8 Austin Hegardt et al., 2005 South | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_0.txt | Optical image of the same crystal after analysis, showing the size of a
typical ablation pit. (C) Concordia diagram showing the two
analyses from this pit.
Fig. 7. Relative probability curves for magmatic events in the four
main continental domains exposed in the Sveconorwegian orogen.
(A) Eastern Segment, (B) Idefjord... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_981.txt | name":"surname","_":"Lima"},{"#name":"cross-ref","$":{"id":"crf0120","refid":"aff0015"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"c"}]},{"#name":"e-address","$":{"id":"eadd0015","type":"email"},"_":"gabilimagel@gmail.com"}]},{"#name":"author","$":{"id":"aut0020"},"$$":[{"#name":"given-name","_":"Amarildo S."},{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_533.txt | .05 21.85-9.05 8.25 0 16.01 3.22 21.84 9.05 5.84 5.84 9.05 13.6 9.05 21.85s-3.21 16.01-9.05 21.85c-5.83 5.83-13.59 9.05-21.84 9.05-8.26 0-16.01-3.22-21.85-9.05zm80.33 29.6l-26.32-26.32c5 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_982.txt | urname","_":"Ruiz"},{"#name":"cross-ref","$":{"id":"crf0125","refid":"aff0020"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"d"}]},{"#name":"e-address","$":{"id":"eadd0020","type":"email"},"_":"asruiz@gmail.com"}]},{"#name":"author","$":{"id":"aut0025"},"$$":[{"#name":"given-name","_":"Ramiro"},{"#name":"surname","_":"... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_30.txt | from titanite U-Pb data (Fig. 4; Table 5; Bingen & van
Breemen 1998b; Heaman & Smalley 1994).
In most of the exposed central and northern part of the
orogen, in the Telemarkia and Idefjorden Terrane, there
was comparatively little unroofing after 970 Ma. Shallow
plutons and discordant veins attest to generally brittle
... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_83.txt | try {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_26.txt | issic
granites along the southern part of the Protogine Zone, southern
Sweden. In Gower, C.F., Rivers, T. & Ryan, B. (eds.), Mid-Proterozoic
Laurentia-Baltica, 38, 131-148. Geological Association of Canada,
Special Paper 38.
Johansson, Å., Meier, M., Oberli, F. & Wikman, H. 1993: The early evolution of the Southwest Sw... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_33.txt | Nov 02 1778 ±22 5 -1.1 961 ±27 8 -0.5 10 Dec 02 1787 ±19 4 -0.6 12 Dec 02 1793 ±17 10 -0.2 2688 ±35 5 -0.4 962 ±21 5 -0.4 11 Apr 03 1783 ±14 5 -0.8 2684 ±72 3 -0.6 05 May 03 1797 ±23 6 0.0 06 May 03 1787 ±39 6 -0.6 967 ±46 9 0.1 12 May 03 1790 ± | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_977.txt | 08-01","volumeSupText":"Volume 265","articleNumber":"","pageRange":"273-285","trace-token":"AAAAQBmEilysDXkD7OK1VKES7UWiA9gDew_6uZ2wtPLYIO0Jfe4zVOanLO1LinKgbwsS13Xa2j3_7J6l3hfh69Q2bT0-iLmbwLicBgOKTdr9QD1l5puKFQ","authors":{"content":[{"#name":" | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_78.txt | yi, Vrådal, TA01-3 Zrn U-Pb 1219 ±8 Andersen et al., 2007
Rogaland Knaben I mine, granitic gneiss, B0126 Zrn U-Pb 1258 ±7 Bingen unpubl
Suldal Trossovdal Fm, Nyastøl metarhyolite Zrn U-Pb 1259 ±2 Brewer et al., 2004
Suldal Trossovdal Fm, Nyastøl metarhyolite, B9817 Z | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1120.txt | late-orogenic magmatism of southern Norway (970–916"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma) consists of two magmatic suites: the Hornblende–Biotite–Granitoids (HBG) suite and the Anorthosite–Mangerite–Charnockite (AMC) suite of the Rogaland Anorthosite Province (RAP), characterized by opx-bear... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1250.txt | ":[{"#name":"maintitle","_":"Terra Nova"}]},{"#name":"volume-nr","_":"25"}]},{"#name":"date","_":"2013"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"165"},{"#name":"last-page","_":"168"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0190"},"$$":[{"#name":"label","_":"Mottram et al., 2014"},{"#name":"reference"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1176.txt | amorphism in Rogaland, Norway: U–Pb LA-ICP-MS geochronology and pseudosections of sapphirine granulites and associated paragneisses"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"J. Petrol."}]},{"#name":"volume-nr","_":"54"}]},{"#name":"date",... | |
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