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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1163.txt | Parrish"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Mesoproterozoic bimodal volcanism in SW Norway, evidence for recurring pre-Sveconorwegian continental margin tectonism"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Precambrian Re... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_16.txt | & Jansen, J.B.H. 1985: Metamorphic zoning in the high-grade Proterozoic of Rogaland-Vest Agder,
SW Norway. In Tobi, A.C. & Touret, J.L. (eds.): The deep Proterozoic
crust in the north Atlantic provinces, NATO-ASI C158, 477-497.
Reidel, Dordrecht.
Torske, T. 1982: Structural effects on the Proterozoic Ullensvang
Group ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_639.txt | r-grey6 u-font-sans"><div class="series"><h3 class="title">Contrib. Mineral. Petrol.</h3></div><div class="series">(1998)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>F. </span>Corfu</span><em> et al.</em></span><h3 class="title">Atlas of ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_609.txt | -bottom"><span class="author u-font-sans"><span>Å. </span>Johansson</span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0301926809002010" target="_self"><span class="anchor-text">Baltica, Amazonia and the SAMBA connection –1000 million years of neighbourhood during the Proterozoic?</span></a></... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_51.txt | (e) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_55.txt | on magmatic events in the five lithotectonic units of the Sveconorwegian belt.
Data from Table 3.
54 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY Table 4. Compilation of monazite, zircon and molybdenite geochronological data in the Sveconorwegia
n belt attributed to high-grade metamorphism
Terrane Min Age ±2
s (Ma) ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_853.txt | igmatite in Ørsdalen was interpreted to date biotite dehydration melting during regional high-grade metamorphism (Bingen and Stein, 2003). Our observations show, however, that the migmatites are found as xenoliths inside weakly metamorphosed, ca. 1050–1030 Ma granites of the Sirdal Magmatic Belt (SMB, Coint et al., 201... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_44.txt | age of the Hinneryd granite - its significance for
interpreting the terranes of the southern Baltic Shield. GFF 118,
163-168.
Ludwig, K.R. 1980: Calculation of U-Pb isotopic data. Earth and
Planetary Science Letters 46, 212-220.
Ludwig, K.R. 2001: Users manual for Isoplot/Ex version 2.49, a
geochronological toolkit fo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_228.txt | nth-child(n+3) p:nth-of-type(even){width:50%;word-break:break-word;word-wrap:break-word}#onetrust-pc-sdk.ot-ven-dets.ot-ven-disc p,#onetrust-pc-sdk.ot-ven-dets.ot-ven-disc h4{padding-top:5px;padding-bottom:5px;display:block}#onetrust-pc-sdk.ot-ven-dets | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_31.txt | , 145-169.
Knudsen, T.L., Andersen, T., Whitehouse, M.J. & Vestin, J. 1997b:
Detrital zircon ages from southern Norway - implications for the
Proterozoic evolution of the southwestern Baltic Shield. Contributions to Mineralogy and Petrology 130, 47-58.
Knudsen, T.-L. & Andersen, T. 1999: Petrology and geochemistry of
t... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir5.txt | part5 -------------------
Geology[edit]
Traps[edit]
A trap forms when the buoyancy forces driving the upward migration of hydrocarbons through a permeable rock cannot overcome the capillary forces of a sealing medium. The timing of trap formation relative to that of petroleum generation and migration is crucial to ensu... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1314.txt | date","_":"1985"},{"#name":"publisher","$$":[{"#name":"name","_":"Reidel"},{"#name":"location","_":"Dordrecht"}]}]},{"#name":"pages","$$":[{"#name":"first-page","_":"477"},{"#name":"last-page","_":"497"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0300"},"$$":[{"#name":"label","_":"Tomkins et al., 2005"},{"#name":"r... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_504.txt | links-container-h u-hide-from-print gh-nav-content-container"><nav aria-label="links" class="gh-nav gh-nav-links gh-nav-h"><ul class="gh-nav-list u-list-reset"><li class="gh-nav-item gh-move-to-spine"><a class="anchor gh-nav-action anchor-default" href="/browse/journals-and-books" data-aa-region="header" data-aa-name="... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_75.txt | -Pb 1159 ±8 Bingen et al., 2003
Telemark Vennesla augen gneiss, B603 Zrn U-Pb 1166 +61/-21 Bingen & van Breemen, 1998
Telemark Åmannsbru rhyolite porphyry dyke, 082896 Zrn U-Pb 1168 ±27 Andersen et al., 2007
Telemark Nore Gp, Rødberg rhyodacite, B9840 Zrn U-Pb 1169 ±9 Bingen et al., 2003
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_33.txt | px;transform:scale(0.5)}#onetrust-banner-sdk.ot-optout-signal svg path,#onetrust-pc-sdk.ot-optout-signal svg path{fill:#32ae88}#onetrust-banner-sdk,#onetrust-pc-sdk,#ot-sdk-cookie-policy,#ot-sync-ntfy{font-size:16px}#onetrust-banner-sdk *,#onetrust-banner-sd | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_92.txt | e[0] instanceof URL? t = e[0].href : "function" == typeof e[0].toString && (t = e[0].toString()), "string" == typeof t && 0!== t.length) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_50.txt | b/206Pb
age of 1693 ±8 Ma (Fig. 3), which dates the magmatic
crystallization of this massive plutonic rock.
Sample FUN38 is granitic gneiss collected in a quarry
situated in the vicinity of the Mylonite Zone (Fig. 2). The
quarry exposes variably mylonitic, west dipping, N-S
trending granitic to granodioritic gneiss. Th... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_119.txt | Arendal phase: 1140-1080 Ma.
(b, c) Agder phase: 1050-980 Ma.
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_711.txt | 78h1e1v-74h-74z"></path></svg></a></div></div></section></div><div class="PageDivider"></div><a class="anchor full-text-link text-s anchor-default" href="/science/article/pii/S0301926815001424" aria-disabled="true" tabindex="-1"><span class="anchor-text">View full text</span></a><div class="Copyright"><span class="copy... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_10.txt | & Connelly, 2008
Hisingen suite, Bifrost granodiorite Zrn U-Pb 1547 ±6 Åhäll & Connelly, 2008
Ranrike granodiorite east Zrn U-Pb 1550 +9/-5 Åhäll & Connelly, 2008
Röseskär felsic dyke Zrn U-Pb 1553 ±2 Connelly & Åhäll, 1996
Begna Follum diorite, metatonalite, N95-130 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_31.txt | & Schöberg, H. 1991: U-Pb dating of the post-kinematic
Sveconorwegian (Grenvillian) Bohus granite, SW Sweden:
evidence of restitic zircon. Precambrian Research 51, 337-350.
Falkum, T. 1985: Geotectonic evolution of southern Scandinavia in
light of a late-Proterozoic plate-collision. In Tobi, A.C. & Touret,
J.L. (eds.)... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_72.txt | 0109 U-Pb SIMS 12 Bingen et al., 2008
Bamble Mnz 1137±7 Gr Metapelitic gneiss, Hisøy, B0109 U-Pb LA-ICPMS 31 Bingen et al., 2008
Bamble Mnz 1137±1 Gr Metapelitic gneiss, Hisøy, B0109 U-Pb ID-TIMS 3 Bingen et al., 2008
Bamble Mnz 1145±3 Gr Metapelitic gneiss, Arend | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_23.txt | 0.003 0.81 1495 17 1446 16 96.8
14 0.0935 0.0009 3.20 0.05 0.248 0.003 0.80 1498 18 1430 16 95.5
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1065.txt | Huai’an Complex, North China Craton (NCC) since 1992 has attracted broad attention from geologists, and accordingly various Early Precambrian continent-continent collision or micro-blocks amalgamation hypotheses were suggested. However, one important issue is still controversial whether the pelitic granulites and ass... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_15.txt |
beam rastered over an area of ca. 60 x 80 µm over the
crystal section (Fig. 6). The beam frequency is 10 Hz.
The beam energy ranges from 0.1 to 1.0 mJ and is
adjusted for every sample or standard to obtain a 238U
signal around 2x106 counts/sec. The aerosol is transported from the sample chamber in He gas, and
introduc... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_64.txt | aland Holum granite, 98BN21D Zrn U-Pb 957 ±7 Bingen et al., 2006
Rogaland Sæbyggjenut granite Zrn U-Pb 959 +50/-32 Andersen et al., 2002
Telemark Vrådal granite, granite TA01-7 Zrn U-Pb 964 ±18 Andersen et al., 2007
Telemark Vrådal granite, “hybrid rock” TA01-10 Zrn U-Pb 970 ±6 Andersen et al., 2007
Suld | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1356.txt | 12109027"},{"refId":21,"crossRefDoi":"10.1007/978-94-009-5450-2_18"},{"refId":22,"crossRefDoi":"10.1007/978-94-009-5450-2_15"},{"refId":23,"scopusHubEid":"2-s2.0-48449083951"},{"refId":24,"scopusHubEid":"2-s2.0-85045548724"},{"refId":25,"scopusHubEid":"2-s | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_11.txt | J.L. (eds.): The deep Proterozoic crust in the north Altantic provinces, NATO-ASI C158, 259-290.
Reidel, Dordrecht.
Stein, H.J. & Bingen, B. 2002: 1.05-1.01 Ga Sveconorwegian metamorphism and deformation of the supracrustal sequence at Sæsvatn,
South Norway: Re-Os dating of Cu-Mo mineral occurrences. In
Blundell, D., ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_558.txt | 1e1z"></path></svg><span class="button-link-text">Add to Mendeley</span></button><div class="Social u-display-inline-block" id="social"><div class="popover social-popover" id="social-popover"><div id="popover-trigger-social-popover"><button class="button-link u-margin-s-right button-link-primary button-link-icon-left" ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1070.txt | #name":"hsp"},{"#name":"__text__","_":"kbar, 810–860"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"°C and ∼9.5"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"kbar, ∼850"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"°C, respectively, comparable with those of associated mafic H | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_21.txt | Tobi et
98 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 11. Site of sample B02027 in the Botsvatn gneiss complex surrounding the Grjotdokki-Nesflaten supracrustals in the Bykle area.
The outcrop is made of a highly sheared banded gneiss, with common boudinaged coarse-grained leucosomes parallel to or cutting the
... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_42.txt | locally showing evidence for extrusive modes of
deposition. The unconformably overlying Vindeggen
92 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 5. Geological map of the coastal area in Skånevik, with sampling site.
group starts with mafic metavolcanic rocks (Vemork fm)
interlayered with arkoses (Heddersvatnet ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_44.txt | session: void 0,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_855.txt | a","_":"The Rogaland Anorthosite complex took about 100 Myr to form."}],"$":{"id":"o0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0010"},"#name":"para","_":"Anorthosite emplacement involved different processes in an evolving stress regime."}],"$":{"id":"o0010"},"#name":"list-ite... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_35.txt | ff, F.C. 1996: Geology, geochemistry and
age of the ‘Tricolor’ granite and some other Proterozoic (TIB)
granitoids at Trysil, southeast Norway. Norsk Geologisk Tidsskrift
76, 45-54.
Hellström, F.A., Johansson, Å. & Larson, S.Å. 2004: Age emplacement
of late Sveconorwegian monzogabbroic dykes, SW Sweden.
Precambrian | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_18.txt | 92.3
15 0.0952 0.0013 3.14 0.07 0.239 0.004 0.77 1531 27 1383 21 90.3
B00-139, granodiorite, Sand, Fig. 10G
9 0.0923 0.0009 3.10 0.06 0.244 0.004 0.86 1474 18 1406 20 95.4
12 0.0931 0.0011 3.61 0.09 0.281 0.006 0.89 1489 22 1598 32 107 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_98.txt | augen gneiss, Hensmoen, B99140 Am 207Pb/206Pb 2 1024 ±9 Bingen et al., 2008
Begna Migmatitic augen gneiss, Hensmoen, B99140 Am 207Pb/206Pb 1 1040 ±14 Bingen et al., 2008
Kungsbacka, W of Göta Älv Shear Zone Am 207Pb/206Pb 1 1040 c. Johansson, 1993
Begna Hensmoen, granodioritic gneiss | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1298.txt | ":"maintitle","_":"Beskrivelse til det berggrunnsgeologiske kartbladet Sauda 1:250000"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"NGU Bull."}]},{"#name":"volume-nr","_":"341"}]},{"#name":"date","_":"1978"}]},{"#name":"pages","$$":[{"#name":... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_41.txt | et al.
1985). Osumilite assemblages indicate dry (water-poor),
high-temperature, low-pressure granulite-facies conditions (Holland et al. 1996), and pigeonite requires peak
temperatures exceeding 865 °C. Westphal et al. (2003)
estimate that peak temperature increased towards the
intrusive contact of the AMC complex, f... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_614.txt | class="author u-font-sans"><span>Z.X. </span>Li</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0301926807001635" target="_self"><span class="anchor-text">Assembly, configuration, and break-up history of Rodinia: a synthesis</span></a></h3><span class="host u-clr-gre... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_817.txt | Technology"},{"#name":"city","_":"Trondheim"},{"#name":"postal-code","_":"7491"},{"#name":"country","_":"Norway"}]}]},{"#name":"correspondence","$":{"id":"cor0005"},"$$":[{"#name":"label","_":"⁎"},{"#name":"text","_":"Corresponding author. Tel.: +47 73904329."}]}]}],"floats":[],"footnotes":[],"affiliations":{"aff0005"... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_71.txt | Stephens, M.B., Wahlgren, C.H., Weijermars, R. & Cruden, A.R. 1996:
Left lateral transpressive deformation and its tectonic implications,
Sveconorwegian Orogen, Baltic Shield, Southwestern Sweden. Precambrian Research 79, 261-279.
Tobi, A.C., Hermans, G.A., Maijer, C. & Jansen, J.B.H. 1985: Metamorphic zoning in the hi... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_45.txt | 8gr,+75,cl,c,s-pr 19 20.8 67 1 0.75 14398 0.09645 7 3.60957 606 0.27143 46 1556.5 1.4 0.6
4 15gr,-75,cl,c,s-pr 31 18.9 65 2 0.62 18223 0.09601 6 3.48688 571 0.26340 43 1547.9 1.1 4.2
N95-66, Veldstad granodiorite gneiss, Fig. | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_25.txt | 64 Ga deformed
granitoids (Table 7; Fig. 7A; Connelly et al. 1996;
Larson et al. 1999; Christoffel et al. 1999; Söderlund et
al. 1999, 2002), and is characterized by a distinctive
late-Sveconorwegian high-pressure metamorphic
overprint dated at 0.97 Ga (Möller 1998; Möller 1999;
Johansson et al. 2001). The orthogneisse... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_20.txt | 0.241 0.003 0.88 1500 14 1394 18 93.0
15 0.0938 0.0008 3.34 0.05 0.258 0.003 0.81 1504 17 1479 16 98.4
2 0.0938 0.0009 3.11 0.04 0.240 0.002 0.66 1505 18 1389 10 92.3
1 0.0940 0.0012 3.05 0.05 0.235 0.002 0.63 1509 23 1363 12 90.3
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_46.txt | Zrn 1684 ±13 Lindth et al., 1994
Dagsås unveined and veined orthogneiss Zrn 1686 ±14 Söderlund et al., 2002
Skene felsic orthogneiss, SE1 Zrn 1686 ±11 Andersson et al., 2002
Zachrisdal quartz-monzonite gneiss, AL84030 Zrn 1688 ±10 Persson et al., 1995
Torsby granite, DC9416 Zrn 1689 ±12 Larson et al., 1999
Hesta grani... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_653.txt | "><a class="anchor anchor-default" href="/science/article/pii/S0301926822003886"><span class="anchor-text">Geochronological constraints for a two-stage history of the Sveconorwegian rare-element pegmatite province formation</span></a></h3><div class="text-s">2023, Precambrian Research</div></div><div class="buttons tex... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_356.txt | 0;padding:0;margin-right:14px;justify-content:flex-end}#onetrust-pc-sdk.ot-vs-selc-all.ot-toggle-conf #ot-selall-vencntr.ot-chkbox,#onetrust-pc-sdk.ot-vs-selc-all.ot-toggle-conf #ot-selall-vencntr.ot-tgl{display:inline-block;right:unset;width:auto;height:auto; | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_17.txt | structural pattern in the Suldal-Sauda area is
Sveconorwegian in age, in accordance with conclusions
by Stein & Bingen (2002).
In the Bykle-Nesflaten area (Fig. 3), the GrjotdokkiNesflaten supracrustal rocks are dominated by finegrained rocks of intermediate composition, interpreted
as metaandesite-dacite (Sigmond 197... |
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