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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_706.txt | . The ca. 1050–1040 Ma granitic and mafic magmas show similar isotopic signatures with slightly negative or positive εHf(t) and moderate δ<sup>18</sup>O values (6–7‰), which indicates that crustal reworking was more dominant than juvenile inputs during their genesis. The generation of leucosomes and leucogranites ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_76.txt | Telemark Flåvatn granite gneiss Zrn U-Pb 1184 +7/-5 Dahlgren et al., 1990
Telemark Gjerstad augen gneiss, M5 Zrn U-Pb 1187 ±2 Heaman & Smalley, 1994
Telemark Vråvatn Co, Granitic gneiss, S Vrådal, TA01-13 Zrn U-Pb 1202 ±9 Andersen et al., 2007
Telemark Drivheia granite gneiss, M200 Zrn U | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_137.txt | 9994);Y=f(Y,X,W,V,C[P+5],A,3593408605);V=f(V,Y,X,W,C[P+10],z,38016083);W=f(W,V,Y,X,C[P+15],y,3634488961);X=f(X,W,V,Y,C[P+4],w,3889429448);Y=f(Y,X,W,V,C[P+ | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1373.txt | .pdf"}},{"refId":38,"pii":"S0012821X14004488","filesize":"9MB","pdf":{"urlType":"download","url":"/science/article/pii/S0012821X14004488/pdfft?md5=4b51f446b5ea550499ab1030895e5886&pid=1-s2.0-S0012821X14004488-main.pdf"}},{"refId":42,"pii":"S037702730800348X | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_994.txt | k State University"},{"#name":"city","_":"Tomsk"},{"#name":"postal-code","_":"634050"},{"#name":"country","_":"Russia"}]}]},{"#name":"correspondence","$":{"id":"cor0005"},"$$":[{"#name":"label","_":"⁎"},{"#name":"text","_":"Corresponding author. Tel.: +55 11 210 7844; fax: +55 11 210 4958."}]},{"#name":"footnote","$":{... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1382.txt | 15","type":"sections","depth":"1"},"$$":[{"#name":"label","_":"3"},{"#name":"title","$":{"id":"sect0030"},"_":"Importance of rock nomenclature"}]},{"#name":"entry","$":{"id":"sec0020","type":"sections","depth":"1"},"$$":[{"#name":"label","_":"4"},{"#name":"title","$":{"id":"sect0035"},"_":"Field description and petrogr... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_23.txt | b). Available data support the
view that the event at 1110-1080 Ma includes the peak
of amphibolite-facies metamorphism in the Kongsberg
Terrane, as opposed to a phase of regional cooling and
unroofing in the Bamble Terrane. Importantly, both
events at 1140-1125 and 1110-1080 Ma are recorded in
one sample from the amph... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_96.txt |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_47.txt | suite, Lake Åsunden, S2 Zrn 1692 ±3 Connelly et al., 1996
Rymmen gabbro, 2 samples Zrn 1692 ±7 Claeson, 1999
Porphyry, Nyhusen, TL9403 Zrn 1697 ±8 Lundqvist and Persson, 1999
Gällared S orthogneiss Zrn 1698 ±12 Söderlund et al., 2002
South Härene, paleosome, S1 Zrn 1699 ±3 Connelly et al., 1996
Qu | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_71.txt | 93ITo U-Pb SIMS 2 Knudsen et al., 1997
Bamble Zrn 1125±46 Gr Tonalitic gneiss, Tromøy, 6.95 U-Pb SIMS 1 Knudsen et al., 1999
Bamble Mnz 1135±6 Gr Metapelitic gneiss, Hisøy, B0111 U-Pb SIMS 7 Bingen et al., 2008
Bamble Mnz 1133±6 Gr Metapelitic gneiss, Hisøy, B | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_3.txt | veconorwegian
orogeny.
The Sveconorwegian belt
The continental crust affected by Sveconorwegian
reworking and attached to Fennoscandia before the Phanerozoic Caledonian orogeny includes the c. 500 km wide
Sveconorwegian belt, sensu stricto, exposed to the southeast of the Caledonian front, and several lithotectonic
uni... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_832.txt | -brittle forming open structures in an extensional tectonic regime where partial melts drained into. Granitic gneisses react in a ductile manner and do not have the ability to drain partial melt."},{"$":{"view":"all","id":"sp0020"},"#name":"simple-para","_":"Pegmatite formation in the Grenville Province, i.e., the Laur... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_633.txt | 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">Geochronology of high-grade metamorphism in the Sveconorwegian belt, S. Norway: U–Pb, Th–Pb and Re–Os data</h3><span class="host u-clr-grey6 u-font-sans"><div class="serie... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_607.txt | Earth Planet. Sci. Lett.</h3></div><div class="series">(2014)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>C.F. </span>Gower</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S03019268080013... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_13.txt | .9
16 0.0935 0.0007 3.07 0.04 0.238 0.002 0.82 1498 14 1375 13 91.8
14 0.0936 0.0009 3.14 0.06 0.243 0.004 0.84 1501 19 1403 19 93.5
13 0.0937 0.0012 3.44 0.10 0.266 0.007 0.90 1503 25 1521 36 101.2
8 0.0939 0.0010 2.89 0.06 0 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_44.txt | and stratigraphic position of the 1614 Delsjön augen granite-gneiss in the
Median Segment of south-west Sweden. GFF 128, 21-32.
Alm, E., Sundblad, K. & Schöberg, H. 2002: Geochemistry and age of
two orthogneisses in the Proterozoic Mjøsa-Vänern ore district,
southwestern Scandinavia. GFF 124, 45-61.
Andersen, T. & Mun... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_831.txt | required heat for partial melting was provided by mafic magma underplating."}],"$":{"view":"all","id":"sp0010"},"#name":"simple-para"},{"$":{"view":"all","id":"sp0015"},"#name":"simple-para","_":"Differences in the rheological behavior of amphibolite and granitic gneiss during extensional tectonics are the major reaso... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_15.txt | of
1499 ± 11 Ma (samples B00-149; Tables 1, 5; Fig. 10H).
A sample of weakly deformed granite in the Ølen area,
west of Sauda, yields an intrusion age of 1506 ± 2 Ma
(sample R94-66, Tables 1, 2, Figs. 3, 8G). Two additional
samples define imprecise Sveconorwegian intrusion
ages of 1065 ± 74 and 1018 ± 33 Ma (samples B... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1381.txt | Keywords"}]},{"#name":"entry","$":{"id":"sec0005","type":"sections","depth":"1"},"$$":[{"#name":"label","_":"1"},{"#name":"title","$":{"id":"sect0020"},"_":"Introduction"}]},{"#name":"entry","$":{"id":"sec0010","type":"sections","depth":"1"},"$$":[{"#name":"label","_":"2"},{"#name":"title","$":{"id":"sect0025"},"_":"Re... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir6.txt | part6 -------------------
Estimating reserves[edit]
Main article: Oil & gas reserves and resource quantification
After the discovery of a reservoir, a petroleum engineer will seek to build a better picture of the accumulation. In a simple textbook example of a uniform reservoir, the first stage is to conduct a seismic... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_56.txt | .
Årebäck, H. & Stigh, J. 2000: The nature and origin of an anorthosite
associated ilmenite-rich leuconorite, Hakefjorden Complex, southwest Sweden. Lithos 21, 247-267.
Årebäck, H. & Andersson, U.B. 2002: Granulite-facies contact metamorphism around the Hakefjorden norite-anorthosite complex,
SW Sweden. Norwegian Journ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1080.txt | _":"Nick M.W."},{"#name":"surname","_":"Roberts"},{"#name":"cross-ref","$":{"id":"crf0170","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]}]},{"#name":"author","$":{"id":"aut0015"},"$$":[{"#name":"given-name","_":"Peter A."},{"#name":"surname","_":"Cawood"},{"#name":"cross-ref","$":{"id":"crf0175",... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_34.txt | holm Förhandlingar 113, 335-337.
Heaman, L.M. & Smalley, P.C. 1994: A U-Pb study of the Morkheia
Complex and associated gneisses, south Norway: implications for
disturbed Rb-Sr systems and for the temporal evolution of Mesoproterozoic magmatism in Laurentia. Geochimica et Cosmochimica
Acta 58, 1899-1911.
Heim, M., Skiö... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_23.txt | .
Holland, T.J., Babu, E.V. & Waters, D.J. 1996: Phase relations of osumilite and dehydration melting in pelitic rocks: a simple thermodynamic model for the KFMASH system. Contributions to Mineralogy
and Petrology 124, 383-394.
Hynes, A. & Eaton, D. 1999: Lateral ramps as an aid to the unroofing of
deep-crustal rocks: ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1157.txt | Tectonic regimes and terrane boundaries in the high-grade Sveconorwegian belt of SW Norway, inferred from U–Pb zircon geochronology and geochemical signature of augen gneiss suites"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"J. Geol. Soc. L... | |
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(5) n tot: total number of analyses; n sel: number of analyses selected for age calculation.
(6) MSWD: Mean Square Weighed Deviation obtained for weighted mean 207Pb/206Pb age calculation; U.I.: upper intercept age.; se Table 2 for decay constants.
(7) Interpretation of the nature of the event dated based on petrograp... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_642.txt | </span><em> et al.</em></span><h3 class="title">Sveconorwegian mid-crustal ultrahigh-temperature metamorphism in Rogaland, Norway: U–Pb LA-ICP-MS geochronology and pseudosections of sapphirine granulites and associated paragneisses</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">J. ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_840.txt | "},{"$":{"view":"all","id":"p0020"},"#name":"para","_":"New data are more in line with geolgogical record within the Sveconorwegian orogen."}],"$":{"id":"o0020"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0025"},"#name":"para","_":"Combined with existing data, new results do not sup... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_508.txt | .18 45 45 0 12.02-4.68 23.32-13.18 31.82s-19.8 13.18-31.82 13.18c-24.82 0-45-20.18-45-45 0-12.02 4.68-23.32 13.18-31.82s19.8-13.18 31.82-13.18zm-0.14 14c-11.55 0.26-16.86 8.43-16.86 18v2h1e1 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_883.txt | . After 900 Ma, magmatic activity had ceased in all areas investigated, attesting to the position of most of them within the stable interior of Rodinia."}],"$":{"view":"all","id":"as015"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab015","lang":"en","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xml... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_20.txt | %.
Geochronology of the Sveconorwegian
orogen
The Sveconorwegian orogen corresponds to the portion
of Scandinavia affected by the Sveconorwegian orogeny
at the end of the Mesoproterozoic (Figs. 1, 2; Berthelsen
1980). The Western Gneiss Complex, representing a
basement window in the Caledonides of western Norway,
and ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1236.txt | ":"R.E."},{"#name":"surname","_":"Ernst"}]},{"#name":"author","$$":[{"#name":"given-name","_":"I.C.W."},{"#name":"surname","_":"Fitzsimons"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R.A."},{"#name":"surname","_":"Fuck"}]},{"#name":"author","$$":[{"#name":"given-name","_":"D.P."},{"#name":"surn | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_65.txt | ite, Justøy, JUS Zrn 1557 ±24 Andersen et al., 2004
Justøy tonalite, Homborsund, HOM Zrn 1569 ±23 Andersen et al., 2004
Gjerstadvatn tonalite, NES Zrn 1572 ±20 Andersen et al., 2004
(1) Zrn: zircon, Clm: columbite, Bdl: baddeleyite, Mnz: monazite, Ttn: titanite, Urn: uraninite, Eux: euxen | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1359.txt | opusHubEid":"2-s2.0-84905474596"},{"refId":39,"scopusHubEid":"2-s2.0-85076632186"},{"refId":40,"scopusHubEid":"2-s2.0-84879882186","crossRefDoi":"10.1130/0091-7613(1992)020<0725:PKHOBD>2.3.CO;2"},{"refId":41,"scopusHubEid":"2-s2.0 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_515.txt | header-opened-from-article" aria-label="Search ScienceDirect" role="button"><span class="link-button-text">Search</span><svg focusable="false" viewBox="0 0 100 128" aria-hidden="true" alt="Search" width="18.75" height="24" class="icon icon-search"><path d="m19.22 76.91c-5.84-5.84-9.05-13.6-9.05-21.85s3.21-16.01 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_17.txt | 1500 reference zircon.
One analysis of the standard is run after every five analyses of the unknown. The analytical setting provides
an intensity for the 207Pb signal higher than 1.5x104
counts/sec. Analyses during which the zircon crystal
brake are discarded. A common Pb correction is
applied using the 204Pb analysis.... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_666.txt | natural remanent magnetization at ∼ 1090 Ma (Bamble Lithotectonic unit), 1000 Ma (Central Telemark), and at around 900 Ma in the westernmost part of the Telemark Lithotectonic Unit. Accordingly, the new paleomagnetic poles for the Bamble (P<sub>lat</sub> = -6.6°N, P<sub>long</sub>&nb... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_42.txt | ot-sdk-cookie-policy a,#ot-sdk-cookie-policy label,#ot-sdk-cookie-policy input,#ot-sdk-cookie-policy ul,#ot-sdk-cookie-policy li,#ot-sdk-cookie-policy nav,#ot-sdk-cookie-policy table,#ot-sdk-cookie-policy thead,#ot-sdk-cookie-policy tr,#ot-sdk-cookie-policy td,#ot-sdk-cookie-policy t | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1174.txt | ib-reference","$":{"id":"bib0080"},"$$":[{"#name":"label","_":"Drüppel et al., 2013"},{"#name":"reference","$":{"id":"sbref0080","refId":"16"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"K."},{"#name":"surname","_":"Drüppel"}]},{"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1318.txt | ":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Torske"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Metal provinces of a cordilleran-type orogen in the Precambrian of South Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#na... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_745.txt | ="plx-citation"><div class="pps-title">Citations</div><ul><li class="plx-citation"><span class="pps-label">Citation Indexes: </span><span class="pps-count">44</span></li></ul></div></div><div class="pps-col plx-capture"><div class="plx-capture"><div class="pps-title">Captures</div><ul><li class="plx-capture"><span clas... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_46.txt | 8C
1 4gr,+75,c,tu,t-pr 4 167 639 2 0.28 25663 0.09351 5 3.34059 393 0.25911 30 1498.2 0.9 1.4
2 4gr,+75,pb,t-pr 10 151 574 5 0.33 20213 0.09327 5 3.30433 624 0.25670 48 1493.4 0.9 2.5
3 2gr,+75,pb,t-pr 10 106 405 11 0 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_58.txt | mid-Proterozoic Kungsbacka Bimodal
Suite, SW Sweden. GFF 129, 227-234.
Baadsgaard, H., Chaplin, C. & Griffin, W.L. 1984: Geochronology of
the Gloserheia pegmatite, Froland, southern Norway. Norsk Geologisk Tidsskrift 64, 111-119.
Berglund, J. 1997: Mid-Proterozoic evolution in south-western Sweden, PhD thesis. Publica... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1184.txt | $":{"id":"sbref0100","refId":"20"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Falkum"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J.S."},{"#name":"surname","_":"Petersen"}]}]},{"#name":"titl... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_46.txt | . and spike is radiogenic
(5) Measured. uncorrected ratio
(6) Ratio corrected for fractionation, spike, blank, and initial common-Pb (at the determined age from Stacey and Kramers. 1975). Pb fractionation
correction = 0.094%/amu (±0.025% 1s); U fractionation correction = 0.111%/amu (±0.025% 1s). U blank = 0.2 pg; Pb bl... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_723.txt | ="buttons"></div></li></ul><a class="anchor text-s u-margin-s-bottom anchor-default anchor-icon-right" href="/science/journal/03019268/265/supp/C" target="_blank"><span class="anchor-text">View more articles</span><svg focusable="false" viewBox="0 0 54 128" height="20" width="10.125" class="icon icon-navigate-right"><p... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1166.txt | ","_":"M."},{"#name":"surname","_":"Horan"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Mock"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T.B."},{"#name":"surname","_":"Andersen"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Pyroxene megacrysts in Proterozoic anor... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_819.txt | #name":"label","_":"b"},{"#name":"textfn","_":"NERC Isotope Geosciences Laboratory, British Geological Survey, Nottingham NG12 5GG, UK"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"NERC Isotope Geosciences Laboratory, British Geological Survey"},{"#name":"city","_":"Nottingham"},{"#n... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_8.txt | ±14 Welin et al., 1982
Koster segment, Hisingen suite, Segelskären gabbro Zrn U-Pb 1538 ±7 Åhäll & Connelly, 2008
Koster segment, Hisingen suite, Nord-Koster diorite Zrn U-Pb 1538 ±7 Åhäll & Connelly, 2008
Hisingen suite, Uddevalla granodiorite Zrn U-Pb 1539 ±10 Åhäll & Connelly, 2008
Koster | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_314.txt | -vnd-item,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item{border:none;margin:0;padding:0}#onetrust-pc-sdk.ot-vs-list.ot-vnd-item button,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item button{outline:none;border-bottom:1px solid #d8d8d8}#onetrust-pc-sdk.ot-vs | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1034.txt | XQPJBFDSdzSKiufJtQVgMPlRazUMiiEOwUq2PTZmYf_eIduzrWjRw","authors":{"content":[{"#name":"author-group","$":{"id":"ag005"},"$$":[{"#name":"author","$":{"id":"au005","author-id":"S0301926816300146-17c7f562b52d8db155f544daefdb4f27"},"$$":[{"#name":"given-name","_":"Jia | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_758.txt | -s-bottom u-margin-0-bottom-from-sm u-margin-m-right-from-sm u-margin-l-right-from-md anchor-default" href="https://service.elsevier.com/app/contact/supporthub/sciencedirect/" target="_blank" id="els-footer-contact-support" rel="nofollow"><span class="anchor-text">Contact and support</span><svg focusable="false" viewBo... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_21.txt | ön augen gneiss, Stora Delsjön, EAH0309 Zrn U-Pb 1618 ±7 Ahlin et al., 2006
Åmål Fm,Tösse dacite Zrn U-Pb 1619 ±5 Åhäll & Connelly, 2008
Olstorp ultramafic intrusion, contact melt OD16 Zrn U-Pb 1624 ±6 Scherstén et al., 2000
Åmål Fm, Kappebo rhyolite Zrn U | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_455.txt | ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) thead,.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) tbody,.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) th,.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) td,.ot-sdk-cookie-policy:not(#ot- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_11.txt |
Research 98, 151-171.
Andersson, J., Möller, C. & Johansson, L. 2002: Zircon chronology of
migmatite gneisses along the Mylonite Zone (S Sweden): a major
Sveconorwegian terrane boundary in the Baltic Shield.
Precambrian Research 114, 121-147.
Andersson, M., Lie, J.E. & Husebye, E.S. 1996: Tectonic setting of
post-orog... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_66.txt | Augen gneiss, Suldal, B00144 Zrn U-Pb 1018 ±33 Bingen et al., 2005
Telemark Otternes granite, 072696-2 Zrn U-Pb 1023 ±24 Andersen et al., 2007
Telemark Fennefoss augen gneiss Zrn U-Pb 1031 ±2 Pedersen & Konnerup-Madsen, 2000
Telemark Mykleås diorite Zrn U-Pb 1034 ±2 Pedersen & Konnerup-M | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1069.txt | ":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_":"-O (NCKFMASHTO) system to account for textural development, mineral composition and "},{"#name":"italic","_":"P"},{"#name":"__text__","_":"–"},{"#name":"italic","_":"T"},{"#name":"__text__","_":" evolution of the pelitic granulites. The estimated peak and retrog... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_29.txt | .003 0.18 1022 178 983 15 96.2
8 0.0735 0.0015 1.98 0.05 0.195 0.003 0.56 1027 40 1151 14 112.0
5 0.0743 0.0017 1.71 0.05 0.167 0.002 0.52 1050 46 996 13 94.8
12 0.0745 0.0020 1.74 0.06 0.169 0.003 0.57 1054 54 1008 17 95.6
6 0.07 |
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