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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1470.txt | l-21.409-21.416C323.432,3.521,314.817,0,304.637,0s-18.791,3.521-25.841,10.561L92.649,196.425
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1161.txt | ","$":{"id":"bib0060"},"$$":[{"#name":"label","_":"Brewer et al., 2004"},{"#name":"reference","$":{"id":"sbref0060","refId":"12"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T.S."},{"#name":"surname","_":"Brewer"}]},{"#name":"auth... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_53.txt |
km) of fine-grained, equigranular granite surrounded
by a variably megacrystic, mainly medium-grained
granite consisting of grey to pink-red microcline, grey
quartz, greyish white plagioclase and biotite. The pluton
is unfoliated and contacts with the wall rocks are discordant. Undeformed pegmatite dykes probably rela... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_116.txt | rative Sveconorwegian reworking. Further to the east, the Sveconorwegian Frontal Deformation Zone marks the easternmost
limit of Sveconorwegian deformation along discrete
shear zones. South of lake Vättern, these two lineaments
merge into a broad zone (20-30 km wide) of steep, ductile to brittle, N-S trending and anast... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_2.txt | Brewer, T.S., Åhäll, K.I., Darbyshire, D.P.F. & Menuge, J.F. 2002:
Geochemistry of late Mesoproterozoic volcanism in southwestern
Scandinavia: implications for Sveconorwegian / Grenvillian plate
tectonic models. Journal of the Geological Society, London 159, 129-
144.
Brewer, T.S., Åhäll, K.I., Menuge, J.F., Storey, C. | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1278.txt | 2011"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"239"},{"#name":"last-page","_":"246"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0235"},"$$":[{"#name":"label","_":"Roberts and Slagstad, 2015"},{"#name":"reference","$":{"id":"sbref0235","refId":"47"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_482.txt | 2.64c1.55 0.76 3.57 1.06 5.15 1.06 4.26 0 6.7-2.48 6.7-5.51C12.59 11.49 3.81 10.76 3.81 6.9M20.27 9.01c0.23-0.13 0.69-0.26 1.72-0.26 1.72 0 2.41 0.3 2.41 1.58h2.38c0-0.36 0-0.79- | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_76.txt | ±5 Zhou et al., 1995
Sørkjevatn fm, metarhyolite, B9825 T Zrn 1159 +/-8 Bingen et al., 2003
Vennesla augen gneiss, B603 T Zrn 1166 +61/-21 Bingen and van Breemen, 1998 a
Nore gp, Rødberg rhyodacite, B9840 T Zrn 1169 ±9 Bingen et al., 2003
Flåvatn granite gneiss T Zrn 1184 +7/-5 Dahl | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_25.txt | of this A-type pluton for the Sveconorwegian
belt in Vest Agder (SW Norway). Lithos 36, 51-66.
Åhäll, K.-I., Persson, P.-O. & Skiöld, T. 1995: Westward accretion of the
Baltic Shield: implications from the 1.6 Åmål-Horred Belt, SW
Sweden. Precambrian Research 70, 235-251.
Åhäll, K.-I., Samuelsson, L. & Persson | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_52.txt | Gneisses (Bingen & van Breemen 1998a).
The Vardefjell Shear Zone between the Telemarkia and
Idefjorden Terranes (Fig. 1) dips to the southwest. It is
characterized by amphibolite-facies banded gneiss rich
in amphibolite-layers and amphibolite boudins. The
timing of amphibolite-facies metamorphism in banded
gneiss is es... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_76.txt | b ID-TIMS 3 Söderlund et al., 2008 Begna Zrn 1091±18 Am Granodioritic gneiss, Hensmoen, B99143 U-Pb SIMS 3 Bingen et al., 2008 Begna Mnz 1538±8, 1052±4, 1025±9 Am Metapelitic gneiss, Hensmoen, B99137 U-Pb SIMS 13 Bingen et al., 2008 Zrn 1540±7 Am Burholmen migmatite U-Pb SIMS | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_161.txt | kiOjE3MTkzNTk5OTksImlzU3ViZG9tYWluIjp0cnVlLCJpc1RoaXJkUGFydHkiOnRydWV9"><script src="https://securepubads.g.doubleclick.net/pagead/managed/js/gpt/m202403190101/pubads_impl.js" async=""></script><link id="plx-css-summary" type="text/css" rel="stylesheet" | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1140.txt | _":"Ga development of continental basins in the Sveconorwegian Orogen, southern Norway"}]}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Can. J. Earth Sci."}]},{"#name":"volume-nr","_":"39"}]},{"#name":"date","_":"2002"}]},{"#name":"pages","$$"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1454.txt | ion header --><div class="ot-acc-hdr ot-always-active-group"><div class="ot-plus-minus"><span></span><span></span></div><h4 class="ot-cat-header" id="ot-header-id-1">Strictly Necessary Cookies</h4><div id="ot-status-id-1" class="ot-always-active">Always active</div></div><!-- accordion detail --><div class="ot-acc-grpc... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir3.txt | part3 -------------------
Gas field[edit]
Location of the gas fields of Iran
Vučkovec Gas Field facility, Croatia
The drillship Discoverer Enterprise is shown in the background, at work during exploratory phase of a new offshore field. The Offshore Support Vessel Toisa Perseus is shown in the foreground, illustrating p... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_73.txt | 2.29 0.2664 2.26 0.99 1501 7 1522 31 101.4
B02-022, Botsvatn gneiss complex, granodiorite gneiss, Fig. 9C
08a (5) 297 1 82 26522 0.08971 0.47 3.1183 1.49 0.25209 1.41 0.95 1419 9 1449 18 102.1
07a (5) 314 146 105 28532 0.09188 0.47 3.4665 1.60 0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_50.txt | typeof t) return (0, n.Z)("Setting a Configurable requires a model to set its initial properties");
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1530.txt | if(this.warnings.length > 0) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_25.txt | NATO-ASI
C158, 499-516. Reidel, Dordrecht.
Jarl, L.G. & Johansson, Å. 1988: U–Pb zircon ages of granitoids from
Småland–Värmland granite-porphyry belt, southern and central
Sweden. Geologiska Föreningens i Stockholm Förhandlingar 110, 21-
28.
Johansson, Å. 1990: Age of the Önnestad syenite and some gne | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1335.txt | id":"bib0330"},"$$":[{"#name":"label","_":"Vernon and Paterson, 2006"},{"#name":"reference","$":{"id":"sbref0330","refId":"66"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"R.H."},{"#name":"surname","_":"Vernon"}]},{"#name":"author... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_14.txt | ochronological data are reported on zircon from
4 samples. Standard methods of mineral separation were
used, including water-table, magnetic, and heavy liquid
separation. Crystals were selected for analysis by handpicking under alcohol.
Zircon from three samples was analysed by laser ablation
- inductively coupled plas... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_48.txt | return!1;
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_43.txt | orwegian orogeny corresponds to the collision
between Fennoscandia and an unknown craton at the
end of the Mesoproterozoic. The Sveconorwegian orogen
has a total width of ca. 500 km, including a ca. 100 km
wide zone of reworking of cratonic Fennoscandia (Eastern Segment). An orogenic belt of this size can only be
the p... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_620.txt | "><h3 class="title">Lithos</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>M.B. </span>Stephens</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/0301926895... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_8.txt |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_753.txt | svg></a></li><li><a class="anchor u-display-block u-clr-grey8 u-margin-s-bottom u-margin-0-bottom-from-sm u-margin-m-right-from-sm u-margin-l-right-from-md anchor-default" href="/user/institution/login?targetURL=%2Fscience%2Farticle%2Fpii%2FS0301926815001424" id="els-footer-remote-access" rel="nof | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_29.txt | 910 Ma, was restricted to the
area southwest of the clinopyroxene isograd (Dalane
area), and was associated with intrusion of the 930-920
Ma Rogaland AMC suite (Schärer et al. 1996), and lowpressure high-temperature M2 metamorphism (Fig. 8f)
(Bingen & van Breemen 1998b; Möller et al. 2002; Möller
et al. 2003). The seco... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1012.txt | the intraplate geochemistry for the 1110"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma Huanchaca–Rincón del Tigre rocks support a relationship with mantle plume activity pre-dating Rodinia breakup. Contemporary anorogenic magmatism in Amazonia is probably linked to crustal melting caused by the LIP. ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_83.txt | 523 0.59 3.5206 3.09 0.26814 3.03 0.98 1533 11 1531 41 99.9
(1) Measured ratio
(2) Ratio after correction for common Pb, using present-day average terrestrial isotopic composition following Stacey & Kramers (1975)
(3) Coefficient of error correlation
(4) Discordance along a discordia line to the origin: 100 *(206Pb/238... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_12.txt | .04 0.186 0.003 0.85 1413 17 1101 14 77.9
9 0.0927 0.0013 3.24 0.07 0.253 0.004 0.74 1482 27 1456 21 98.2
12 0.0932 0.0008 3.15 0.04 0.245 0.002 0.77 1493 16 1415 13 94.8
2 0.0933 0.0007 3.16 0.04 0.246 0.002 0.77 1494 15 1417 12 94 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_70.txt | et al., 2002 a
Byklom granite S Zrn 970 +14/-18 Andersen et al., 2002 a
Høvring granite T Zrn 971 +63/-34 Andersen et al., 2002 a
Knaben Mo ore, granitic gneiss, B01028 R Mnz 1014 ±7 Bingen et al., unpublished
Fennefoss augen gneiss T Zrn 1031 ±2 Pedersen and Konnerup-Madsen, 2000
Mykleås diorite T Zrn 1034 ±2 Ped | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_45.txt | 1995: Radiogenic whole-rock lead in Precambrian metasedimentary gneisses from South Norway: evidence
of Sveconorwegian LILE mobility. Norsk Geologisk Tidsskrift 75,
156-168.
Andersen, T. 1997: Radiogenic isotope systematics of the Herefoss granite, South Norway: an indicator of Sveconorwegian (Grenvillian)
crustal evo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1061.txt | "},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab005","lang":"en","class":"graphical"},"#name":"abstract"},{"$$":[{"$":{"id":"st010"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0005"},"#name":"para","_":"Kyanite-bearing high pressure gr... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_657.txt | crystallized significantly earlier or later than adjacent granites. The Tørdal granite, yielding an age of 946 ± 4 Ma, is about 40 Ma older than the adjacent pegmatites. Field evidence and the age difference between pegmatites and granites supports an anatectic origin for these pegmatites. Sources ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1269.txt | bib0220"},"$$":[{"#name":"label","_":"Pisarevsky and Bylund, 2006"},{"#name":"reference","$":{"id":"sbref0220","refId":"44"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"S.A."},{"#name":"surname","_":"Pisarevsky"}]},{"#name":"autho... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_151.txt | var carray = document.cookie.split(';'), value;
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while (c.charAt(0) =='') {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_750.txt | a new tab)" rel="nofollow"><img class="footer-logo" src="https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/47/images/elsevier-non-solus-new-with-wordmark.svg" alt="Elsevier logo with wordmark" height="64" width="58" loading="lazy"></a></div><div class="els-footer-content"><div class="u-remove-if... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_125.txt | t || (0, c.R)(e, "api");
const h = {};
var p = a.ee.get(e),
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| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_49.txt | Pearson, N.J.
2004a: Mid-Proterozoic magmatic arc evolution at the southwest
margin of the Baltic shield. Lithos 73, 289-318.
Andersen, T., Laajoki, K. & Saeed, A. 2004b: Age, provenance and tectonostratigraphic status of the Mesoproterozoic Blefjell quartzite,
Telemark sector, southern Norway. Precambrian Research 13... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_724.txt | 7 45 45-45 45z"></path></svg></a></div></div></section></section><section class="RelatedContentPanel u-margin-s-bottom"><header id="recommended-articles-header" class="related-content-panel-header u-margin-s-bottom"><button class="button-link related-content-panel-toggle is-up button-link-primary button-link-icon-right... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_44.txt | neiss, South Härene, 1 Zrn U-Pb 1699 ±3 Connelly et al., 1996
SFDZ Quartz monzodiorite Zrn U-Pb 1699 ±7 Stephens, in Söderlund et al., 1999
South Interboudin granite pegmatite, inherited zircon, EAH0207 Zrn U-Pb 1701 ±10 Austin Hegardt et al., 2005
SFDZ Granite, Grå-Larsknipen, TL9406 Zrn U-Pb 17 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_841.txt | ":"o0025"},"#name":"list-item"}],"$":{"id":"l0005"},"#name":"list"}],"$":{"view":"all","id":"sp0010"},"#name":"simple-para"}],"$":{"view":"all","id":"as010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab010","lang":"en","class":"author-highlights"},"#name":"abstract"},{"$$":[{"$":{"id":"st015"},"#name":"section-t... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_49.txt | 460 0.25892 37 1494.4 1.2 7.0
4 6gr,cl,c,e,s-pr 9 26.6 100 1 0.53 14070 0.09135 6 3.11663 459 0.24744 37 1453.9 1.3 21.7
5 4gr,-75,cl,c,l-pr 9 20.4 77 6 0.59 1861 0.09027 10 3.02146 541 0.24277 39 1431.2 2.1 27.2
N | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_43.txt | 3.84672 611 0.28158 44 1606.8 0.9
2 3gr,+75,pb,t-pr 10 36.7 118 4 0.60 5408 0.09904 6 3.85506 571 0.28231 40 1606.1 1.2
3 1gr,+75,pb,t-pr 3 32.8 106 2 0.59 2978 0.09890 15 3.83108 827 0.28095 50 1603.4 2.8
N95-130, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_129.txt | t, r) => {
if ("object" == typeof r && null!== r) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1189.txt | "},{"#name":"last-page","_":"322"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0110"},"$$":[{"#name":"label","_":"Gower, 1985"},{"#name":"reference","$":{"id":"sbref0110","refId":"22"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_"... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_66.txt | (1980) proposed closure of a marginal oceanic basin
between the Telemarkia Terrane and the rest of the belt.
Indigenous models are supported, but not demonstrated,
by various arguments based on geochronology and isotope geochemistry. (1) Three magmatic suites, characteristic of the Telemarkia Terrane, have time equival... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_744.txt | -Summary"><div class="pps-container pps-container-vertical plx-no-print"><div class="pps-branding pps-branding-top"><img alt="plumX logo" src="//cdn.plu.mx/3ba727faf225e19d2c759f6ebffc511d/plumx-inverse-logo.png" class="plx-logo"></div><div class="pps-cols"><div class="pps-col plx-citation"><div class | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_668.txt | <sub>95</sub> = 6.5 °, K = 22.6), and western Telemark Lithotetonic Unit (P<sub>lat</sub> = -46.2° N, P<sub>long</sub> = 209.4° E, N = 9, A<sub>95</sub> =  | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_212.txt | vendors-list-handler,#onetrust-pc-sdk.category-vendors-list-handler+a,#onetrust-pc-sdk.category-host-list-handler{clear:both;color:#3860be;margin-left:0;font-size:.813em;text-decoration:none;float:left;overflow:hidden}#onetrust-pc-sdk.category-vendors-list-handler:hover,#onetrust-pc-sdk.category-v | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_43.txt | (Tobi et al. 1985; Jansen
et al. 1985; Vander Auwera 1993; Westphal et al. 2003).
Metamorphic zircon from a variety of samples ranges
from 1068 ±28 to 901 ±18 Ma, with two principal modes,
one at 1030 -990 Ma attributed to M1 and the second at
930 -920 Ma attributed to M2-M3 (Table 4; Möller et al.
2002; Möller et al.... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_40.txt | .5 Ga. From the margin to the continent, this polarity is
calc-alkaline magmatism in the westernmost Suldal
sector, bimodal continental magmatism in the Telemark
sector and 1.53-1.50 Ga rapakivi granite plutonism in the
interior of the Fennoscandian craton (Ragunda suite in
Sweden) (Åhäll et al. 2000; Bingen et al. 200... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_54.txt | const n = "1.238.0",
i = "PROD",
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385: (e, t, r) => {
r.d(t, {
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return year + '-' + month + '-' + date;
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_135.txt | ,X,C[P+10],N,4294925233);X=u(X,W,V,Y,C[P+11],M,2304563134);Y=u(Y,X,W,V,C[P+12],S,1804603682);V=u(V,Y,X,W,C[P+13],Q,4254626195);W=u(W,V,Y,X,C[P+14],N,2792965006);X=u | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_942.txt | ns:cals":true,"xmlns:sb":true,"xmlns:sa":true,"xmlns:ja":true,"xmlns":true,"id":"sec0100","view":"all"},"$$":[{"#name":"label","_":"6"},{"#name":"section-title","$":{"id":"sect0115"},"_":"Geochronology"},{"#name":"para","$":{"id":"par0245","view":"all"},"_":"Samples of 38 granitoids have been dated to assess the spatia... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_86.txt | .xhrGuids[r] =!0, this.totalCbs += 1);
}
function h(e, t) {
var r = "" + M(e) +!!t;
this.xhrGuids && this.xhrGuids[r] && (delete this.xhrGuids[ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_125.txt | )+(k&1073741823);if(I&d){return(x^2147483648^F^H)}if(I|d){if(x&1073741824){return(x^3221225472^F^H)}else{return(x^1073741824^F^H)}}else{return(x^F^H)}}function r(d,F,k){return(d&F)|((~d)&k)}function q(d,F,k){return(d&k | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1245.txt | given-name","_":"A."},{"#name":"surname","_":"Kennedy"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Kröner"}]}]}]},{"#name":"host","$$":[{"#name":"book","$$":[{"#name":"book-series","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Linking Growth Episod... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_41.txt |
1960). The supracrustal sequence divides into three
main packages, namely the 1.51 Ga Rjukan group, the
Vindeggen group and an upper package coeval or
younger than 1.17 Ga (Dahlgren et al. 1990b; Laajoki et
al. 2002; Bingen et al. 2003; Andersen & Laajoki 2003).
At the bottom of the sequence, the voluminous Rjukan
gro... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_59.txt | )(this.agentIdentifier);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1340.txt | cambrian Res."}]},{"#name":"volume-nr","_":"189"}]},{"#name":"date","_":"2011"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"368"},{"#name":"last-page","_":"388"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0340"},"$$":[{"#name":"label","_":"Weaver et al., 1990"},{"#name":"reference","$":{"id":"sbref0340","re... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_694.txt | ballooning of the anorthosite. The septa lithology is dominated by noritic gneisses interleaved with felsic gneisses and comprises minor amounts of mafic granofels, metaquartzites and metagreywackes. A charnockitic dyke is cutting across the foliated structure. Geochemical data (major and trace elements) indicate that... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_42.txt | by granite, DC9416 Zrn U-Pb 1689 ±12 Larson et al., 1999
PZ Fryele granite, 88082 Zrn U-Pb 1690 ±5 Welin, 1994
South Granitoid, Hesta suite, Lake Åsunden, 2 Zrn U-Pb 1692 ±3 Connelly et al., 1996
PZ Rymmen gabbro, 2 samples Zrn U-Pb 1692 ±7 Claeson, 1999
North Granitic gneiss, Knappåsen quarry, FUN | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_192.txt | ot-subgrps.ot-switch-nob{top:0}#onetrust-pc-sdk ul.ot-subgrps.ot-acc-hdr{display:inline-block;width:100%}#onetrust-pc-sdk ul.ot-subgrps.ot-acc-txt{margin:0}#onetrust-pc-sdk ul.ot-subgrps li{padding:0;border:none}#onetrust-pc-sdk ul.ot-subgrps li h5{ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1323.txt | },{"#name":"author","$$":[{"#name":"given-name","_":"J.-P."},{"#name":"surname","_":"Liégeois"}]},{"#name":"author","$$":[{"#name":"given-name","_":"D."},{"#name":"surname","_":"Demaiffe"}]},{"#name":"author","$$":[{"#name":"given-name","_":"E."},{"#name":"surname","_":"Wilmart"}]},{"#name":"author","$$":[{"#name":"giv... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_458.txt | -policy-v2) td:before{position:absolute;height:100%;left:6px;width:40%;padding-right:10px}.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2).ot-mobile-border{display:inline-block;background-color:#e4e4e4;position:absolute;height:100%;top:0;left:45%;width:2px}.ot-sdk-cookie-policy:not(#ot-sdk- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1292.txt | ":"pages","$$":[{"#name":"first-page","_":"387"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0260"},"$$":[{"#name":"label","_":"Schmidt and Poli, 2004"},{"#name":"reference","$":{"id":"sbref0260","refId":"52"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_6.txt | en Terrane displays a general N-S to NWSE Sveconorwegian structural grain. It contains several
amphibolite-facies orogen-parallel shear zones, including the Ørje Shear Zone (Norway) or Dalsland Boundary
Zone (Sweden) and the Göta Älv Shear Zone (Park et al.
1991), as well as a nappe complex, the Glaskogen Nappes
(Fig. ... |
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