id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
value |
|---|---|---|
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_761.txt | width="1em" height="1em" class="icon icon-arrow-up-right arrow-external-link"><path d="m4 36h57.07l-59.5 59.5 7.07 7.08 59.36-59.36v56.78h1e1v-74h-74z"></path></svg></a></li><li><a class="anchor u-display-block u-clr-grey8 u-margin-s-bottom u-margin-0-bottom-from-sm u | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_44.txt |
var id = '';
if (window.pageData && pageData.visitor && (pageData.visitor.consortiumId || pageData.visitor.accountId)) {
id = (pageData.visitor.consortiumId || 'no consortium ID') + '|' + (pageData.visitor.accountId || 'no account ID');
}
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_51.txt | 22 ±5 Eliasson and Schöberg, 1991
Flå granite Zrn 928 ±3 Nordgulen et al., 1997
Göteborg dolerite, Tuve dyke Bdl 935 ±3 Hellström et al., 2004
Vinga porphyry Zrn 963 ±17 Åhäll and Schöberg, 1999
Skuleboda rare-mineral pegmatite Clm 984 ±6 Romer and Smeds, 1996
Högsbo rare-mineral pegmatite Cl | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1385.txt | ","_":"4.3.2"},{"#name":"title","$":{"id":"sect0060"},"_":"Granitic flaser gneiss"}]},{"#name":"entry","$":{"id":"sec0050","depth":"3"},"$$":[{"#name":"label","_":"4.3.3"},{"#name":"title","$":{"id":"sect0065"},"_":"Amphibolite"}]}]},{"#name":"entry","$":{"id":"sec0055","depth":"2"},"$$":[{"#name":"label","_":"4.4 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_168.txt | adow(OffX=2, OffY=2, Color='gray', Positive='true')}
#MathJax_About.MathJax_MousePost {outline: none}
.MathJax_Menu {position: absolute; background-color: white; color: black; width: auto; padding: 5px 0px; border: 1px solid #CCCCCC; margin: 0; cursor: default; font: menu; text-align: left; text-indent: 0; text-transfo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_106.txt | }
if (prodList[i].provider) {
merch.push('evar164=' + this.stripProductDelimiters(prodList[i].provider));
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_83.txt | u = f._A.setInterval,
d = "readystatechange",
l = ["onload", "onerror", "onabort", "onloadstart", "onloadend", "onprogress", "ontimeout"],
h = [],
p = f | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_24.txt | otdokki-Nesflaten supracrustals as 1.52-1.48 Ga rocks in Figs. 2-3 is
thus a speculative extrapolation. The deformation recorded in this
outcrop is regarded Sveconorwegian in age by the first author of this
publication, though this interpretation requires demonstration.
al. 1985; Bingen & van Breemen 1998b; Möller et a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_337.txt | ordion-layout.ot-checkbox-consent.ot-acc-hdr.ot-plus-minus{top:0}#onetrust-pc-sdk.ot-vs-config.ot-acc-hdr.ot-arw-cntr,#onetrust-pc-sdk ul.ot-subgrps.ot-acc-hdr.ot-arw-cntr,#onetrust-pc-sdk.ot-subgrp-cntr ul.ot-subgrps.ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1032.txt | ","id":"abst0010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"abs0010","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstracts"},"pdf":{"urlType":null},"iss-first":"","vol-first":"265","isThirdParty":false,"language":"en","issn-primary-unformatted":"03019268... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1352.txt | external":[{"refId":1,"scopusHubEid":"2-s2.0-0028870789"},{"refId":2,"scopusHubEid":"2-s2.0-85022981523"},{"refId":3,"scopusHubEid":"2-s2.0-84880176773","crossRefDoi":"10.1130/MEM159-p241"},{"refId":4,"scopusHubEid":"2-s2.0-0027803111","crossRefDoi":"10. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_113.txt | FN_END: me
} = ae;
var ve = i(4649);
class be extends h {
static featureName = ve.t;
constructor(e, t) {
let r =!(arguments.length > 2 && void 0!== arguments[2]) || arguments[2];
super( | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_101.txt | E2, TA Am 207Pb/206Pb 1 1638 c. Söderlund et al., 1999
Centre Metagranite, Övre Fryken, W2, TB Am 207Pb/206Pb 1 1674 c. Söderlund et al., 1999
South Mafic boudin in Mylonite Zone, Lerhuvud Am 207Pb/206Pb 1 917 ±14 Johansson & Johansson, 1993
South Paleosome in orthogneiss, South Härene, 1, T | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir8.txt | part8 -------------------
Drive mechanisms[edit]
A virgin reservoir may be under sufficient pressure to push hydrocarbons to the surface. As the fluids are produced, the pressure will often decline, and production will falter. The reservoir may respond to the withdrawal of fluid in a way that tends to maintain the pres... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_368.txt | -sdk.ot-pc-footer{max-height:60px;overflow-y:auto}#onetrust-pc-sdk #ot-pc-content,#onetrust-pc-sdk #ot-pc-lst{bottom:70px}#onetrust-pc-sdk.ot-ftr-stacked #ot-pc-content{bottom:70px}#onetrust-pc-sdk #ot-anchor{left:initial;right:50px}#onetrust-pc-sdk | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_43.txt | void 0, N.t, this.ee)), this.importAggregator());
}
}
var S = i(3081);
class P extends h {
static featureName = S.t9;
constructor(e, t) {
let r =!(arguments.length > 2 && void 0!== arguments[2 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_92.txt | , 1998
Rogaland-VA Augen gneiss, Sirdal, B185, TB Am 207Pb/206Pb 2 925 ±13 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Mandal, B206, TA Am 207Pb/206Pb 2 927 ±9 Bingen & van Breemen, 1998
Rogaland-VA Byklom granite Am Min. isochron 6 983 ±68 Andersen et al., 2002
Rogaland-VA Rosskreppfj | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_96.txt | matite, Kragerø, 92-2, Sph922a2 Am 207Pb/206Pb 3 1106 ±2 Cosca et al., 1998
Kongsberg Albitite margin Øverbykollen metagabbro, G-10 Am 207Pb/206Pb 4 1079.6 ±2.5 Munz et al., 1994
Bamble Marble, Arendal, 92-15, Sph9215b Gr 207Pb/206Pb 1 1103 ±2 Cosca et al., 1998
Bam | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_5.txt | U-Pb 1336 ±10 Austin Hegardt et al., 2007
Askim granite, 78170 Zrn U-Pb 1362 ±9 Welin & Samuelsson, 1987
Orust dyke swarm, Islandsberg dyke Zrn U-Pb 1457 ±6 Åhäll & Connelly, 1998
Begna Hensmoen, granodioritic gneiss, B99143 Zrn U-Pb 1495 ±11 Bingen et al., 2008
Brevik gabbro Zrn U-Pb 1502 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_200.txt | height:25px}#onetrust-pc-sdk.ot-switch-nob{position:absolute;cursor:pointer;top:0;left:0;right:0;bottom:0;background-color:#767676;border:1px solid #ddd;transition:all.2s ease-in 0s;-moz-transition:all.2s ease-in 0s;-o-transition:all.2s ease-in 0s;-webkit-transition:all.2s ease-in | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_418.txt | pc-sdk a:hover{color:inherit!important;text-decoration-color:#eb6500!important}div#onetrust-pc-sdk{border-radius:0;bottom:0;height:auto;left:0;margin:auto;max-width:100%;overflow:hidden;right:0;top:0;width:512px;max-height:800px}div#onetrust-pc-sdk.ot-pc-header{display:none}div#onetrust-pc-sd | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_10.txt | ic craton, possibly Fennoscandia. No basement older than 1.5 Ga can be positively identified. In the early stage of the Sveconorwegian orogeny, Telemarkia collided with the Idefjorden terrane. The Bamble-Kongsberg sector, characterized by a mixed lithology and
1.13-1.10 Ga early-Sveconorwegian high-grade metamorphism, ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_46.txt | a cooling age. Available geochronological data carry several important implications for the
regional metamorphic evolution. (1) Monazite data from
a felsic granulite, situated outside the area affected by M2
(Øvstabø locality), demonstrate granulite-facies metamorphism during M1 at 1032 ±5 or 990 ±8 Ma (Fig. 8c;
Binge... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_303.txt | px;padding-bottom:11.5px;padding-left:20px;padding-right:20px;width:calc(100% - 40px);display:inline-block}#onetrust-pc-sdk.ot-accordion-layout.ot-acc-txt{width:100%;padding:0}#onetrust-pc-sdk.ot-accordion-layout.ot-subgrp-cntr{padding-left:20px;padding-right:15px;padding-bottom:0; | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_11.txt | 0.005 0.86 1531 20 1580 24 103.2
4b 0.0960 0.0012 3.40 0.07 0.257 0.004 0.76 1548 24 1473 20 95.1
3b 0.0961 0.0011 3.49 0.06 0.263 0.004 0.80 1550 21 1506 19 97.2
B00-137, augen gneiss, Sand, Fig. 10E
1 (4) 0.0894 0.0008 2.30 0 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_214.txt | :13px;width:13px;background-repeat:no-repeat;margin-left:1px;margin-top:6px;cursor:pointer}#onetrust-pc-sdk.ot-ven-hdr.ot-ext-lnk{margin-bottom:-1px}#onetrust-pc-sdk.back-btn-handler{font-size:1em;text-decoration:none}#onetrust-pc-sdk.back-btn-handler:hover{opacity:.6}#onet | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1271.txt | #name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Geophys. J. Int."}]},{"#name":"volume-nr","_":"166"}]},{"#name":"date","_":"2006"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"1095"},{"#name":"last-page","_":"1104"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0225"},"$$":[{"#name":"labe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_176.txt | 16px}div#onetrust-pc-sdk #ot-lst-cnt{margin-left:24px;width:calc(100% - 48px)}div#onetrust-pc-sdk #ot-anchor{display:none!important}
/* 2023-12-04 Fix for button order in mobile view*/
@media (max-width: 550px) {
#onetrust-accept-btn-handler {order: 1; }
#onetrust-reject-all-handler { | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_112.txt | sdk.onetrust-close-btn-ui{top:10px;right:10px}#onetrust-banner-sdk:not(.ot-iab-2) #onetrust-group-container{width:95%}#onetrust-banner-sdk.ot-iab-2 #onetrust-group-container{width:100%}#onetrust-banner-sdk.ot-bnr-w-logo #onetrust-button-group-parent{padding-left:50px} | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_116.txt | .cookie-setting-link{text-align:center}}@media only screen and (min-width: 550px){#onetrust-banner-sdk.banner-option:not(:first-child){border-left:1px solid #d8d8d8;padding-left:25px}}@media only screen and (min-width: 425px)and (max-width: 550px){#onetrust-banner-sdk.ot-iab-2 #onetrust-button-group,#onetrust- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_16.txt | Bohus granite, SW
Sweden. GFF 125, 113-130.
Gorbatschev, R. & Bogdanova, S. 1993: Frontiers in the Baltic Shield.
Precambrian Research 64, 3-21.
Gower, C.F., Ryan, B. & Rivers, T. 1990: Mid-Proterozoic LaurentiaBaltica: an overview of its geological evolution and a summary of
the contributions made by this volume. In ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_25.txt | wall of
the Mylonite Zone. Initially rapid exhumation of highpressure lithologies at 970 Ma was followed by comparatively slower exhumation and regional cooling between
960 and 920 Ma. Exhumation of the Eastern Segment
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
66
ov... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_1.txt | son, P.-O., Lindh, A., Schöberg, H., Hansen, B.T. & Lagerblad, B.
1995: A comparison of the geochronology and geochemistry of
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 103
plagioclase-dominated granitoids across a major terrane boundary
in the SW Baltic Shield. Precambrian... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_22.txt | obfuscate: void 0,
jserrors: {
enabled:!0,
harvestTimeSeconds: 10
},
metrics: {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1025.txt | name":"label","_":"•"},{"$":{"view":"all","id":"par0010"},"#name":"para","_":"Deformation involved interplay between folding, shearing and melt."}],"$":{"id":"lsti0010"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0015"},"#name":"para","_":"The ductile shear zone records high-tempe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1256.txt | ies metamorphism: a microtextural, U–Pb, Lu–Hf and trace element study of Caledonian rocks from the Arctic"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Contrib. Mineral. Petrol."}]},{"#name":"volume-nr","_":"168"}]},{"#name":"date","_":"2014... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_695.txt | aland anorthosite province. Instead they have strong similarities with a high-alumina basalt that is the possible parental magma of the EGOG anorthosite. Slight variations from norite to leuconorite compositions were induced by metamorphic differentiation. The felsic rocks encompass a large interval of rock types from ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_786.txt | orogenesis&rft_id=info:doi/10.1016/j.precamres.2015.05.002","label":"Find it here!"}],"search":{"inputPlaceHolder":"Search ScienceDirect","ariaLabel":{"input":"Search ScienceDirect","submit":"Submit search"},"formAction":"/search#submit","analytics":[{"ids":["accessbar:search"],"eventName":"searchStart"}],"id":"QuickSe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1088.txt | ":"EH9 3JW"},{"#name":"country","_":"UK"}]}]},{"#name":"correspondence","$":{"id":"cor0005"},"$$":[{"#name":"label","_":"⁎"},{"#name":"text","_":"Corresponding author at: Geochronology and Tracers Facility, NERC Isotope Geosciences Laboratory, British Geological Survey, Keyworth, Nottingham NG12 5GG, UK."}]}]}],"floats... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_588.txt | the Sveconorwegian orogeny – is commonly interpreted to reflect a continent–continent collision between Baltica–Laurentia on one side and a third continent,</p></section></section><section><section id="sec0015"><h2 class="section-title u-h4 u-margin-l-top u-margin-xs-bottom">Importance of rock nomenclature</h2><p id="... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_205.txt | .ot-chkbox input,#onetrust-pc-sdk.ot-tgl input{position:absolute;opacity:0;width:0;height:0}#onetrust-pc-sdk.ot-arw-cntr{float:right;position:relative;pointer-events:none}#onetrust-pc-sdk.ot-arw-cntr.ot-arw{width:16px;height:16px;margin-left:5px;color:dimgray;display:inline | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_29.txt | 1693 16 6.7
02 8394 0.10360 1.0 3.988 1.7 0.2792 1.4 0.81 1587 20 1690 19 6.1
03p 6486 0.10433 1.1 4.037 1.7 0.2806 1.3 0.75 1595 18 1703 21 6.3
17p 17162 0.10285 1.0 4.002 1.7 0.2822 1.3 0.80 1602 19 1676 19 4.4
21 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_120.txt |
};
function c(e, t) {
const r = n.ee.get(t);
e && "object" == typeof e && (Object.entries(e).forEach(e => {
let [t, n] = e;
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1008.txt | label","_":"•"},{"$":{"view":"all","id":"par0020"},"#name":"para","_":"There is a tight age match with intraplate magmatism in other crustal blocks."}],"$":{"id":"lsti0020"},"#name":"list-item"}],"$":{"id":"lis0005"},"#name":"list"}],"$":{"view":"all","id":"spar0005"},"#name":"simple-para"}],"$":{"view":"all","id":"abs... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_289.txt | ;top:auto;height:20px}#onetrust-pc-sdk #ot-lst-cnt.ot-chkbox{position:relative;display:inline-block;width:20px;height:20px}#onetrust-pc-sdk #ot-lst-cnt.ot-chkbox label{position:absolute;padding:0;width:20px;height:20px}#onetrust-pc-sdk #ot-lst-cnt.ot-vnd-info-c | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_14.txt | entered a period
of crustal thickening. Available data demonstrate that
the different sectors of the Telemarkia Terrane, though
of variable metamorphic grade, share a common metamorphic event starting at around 1035 Ma (Fig. 8c, Table
4). The oldest metamorphic dates at 1035-1030 Ma are
recorded in the low-grade litho... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_91.txt | 5546: (e, t, r) => {
r.d(t, {
E: () => n,
p: () => i
});
var n = r(8325).ee.get("handle");
function i(e, t, r, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_905.txt | _":"Abstract"},{"$$":[{"$$":[{"#name":"__text__","_":"The Sveconorwegian orogen represents a branch of Grenville-age (~1250–950 Ma) orogenic belts that formed during the construction of the supercontinent Rodinia. This study traces the Sveconorwegian records from its type-area in the Baltic Shield of South Norway into ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1409.txt |
})
} catch(e) {
console.warn("There was an error loading or running Adobe DTM: ", e);
}
</script>
<script nomodule="" src="https://sdfestaticassets-us-east-1.sciencedirectassets.com/shared-assets/73/js/core-js/3.20.2/core-js.es.minified.js" type="text/javascript"></script>
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_375.txt | onetrust-consent-sdk #onetrust-pc-sdk #ot-sel-blk,
#onetrust-consent-sdk #onetrust-pc-sdk #ot-fltr-cnt,
#onetrust-consent-sdk #onetrust-pc-sdk #ot-anchor | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_41.txt |
Vråna deformed aplitic dyke, S3 Zrn 1457 ±7 Connelly et al., 1996
Mölle granite gneiss, 84093 Zrn 1497 +47/-34 Johansson et al., 1993
Flackarp granite gneiss, 76314 Zrn 1531 ±8 Johansson, 1990
Hinneryd granite gneiss, 8712 Zrn 1548 ±10 Lindth, 1996
Åker metabasite Zrn 1562 ±6 Söderlund et al., 2004
Vagger | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_57.txt | anorogenic character of anorthosite magmatism: U-Pb dating
of the Rogaland complex, Norway. Earth and Planetary Science Letters 139, 335-350.
Scherstén, A., Årebäck, H., Cornell, D., Hoskin, P., Åberg, A. & Armstrong, R. 2000: Dating mafic-ultramafic intrusions by ion-microprobing contact-melt zircon: examples from SW... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_7.txt | agentID: "1118783207",
licenseKey: "7ac4127487",
applicationID: "814814845"
};
;
NREUM.info = {
beacon: "bam.nr-data.net",
errorBeacon: "bam.nr-data.net",
licenseKey: "7ac4127487",
applicationID: "814814845",
sa: 1 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1144.txt | ism in the Sveconorwegian belt, S. Norway: U–Pb, Th–Pb and Re–Os data"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nor. J. Geol."}]},{"#name":"volume-nr","_":"88"}]},{"#name":"date","_":"2008"}]},{"#name":"pages","$$":[{"#name":"first-page",... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_14.txt | 'facetOperation', 'details'];
for (var i=0; i<fields.length; i++) {
if (data.search[fields[i]]) {
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_76.txt | of north-central Madagascar. The Journal of Geology 107, 135-153.
Vander Auwera, J. 1993: Diffusion controlled growth of pyroxene-bearing margins on amphibolite bands in the granulite facies of Rogaland (southwestern Norway): implications for granulite formation.
Contributions to Mineralogy and Petrology 114, 203-220.... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_469.txt | color: #696969;
}
#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy #cookie-policy-title {
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_26.txt | wegian amphibolite-facies
metamorphic event, associated with partial melting
and leading to formation of metamorphic zircon in the
1.46-1.42 Ga interval (Christoffel et al. 1999; Söderlund
et al. 2002). A minor volume of 1.40-1.38 Ga, 1.25-1.20
Ga granite plutonism is recorded (Table 7, Fig. 7A).
Idefjorden terrane
The... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_5.txt | 1978, 1998; Torske
1982). We use the name Suldal sector for this domain.
In the Ullensvang area (Fig. 3), supracrustal rocks of
the Ullensvang group comprise, in stratigraphic ascending
order, andesitic to dacitic metatuff (Kinsarvik fm),
metarhyolite with minor metabasalt (Jåstad fm), quartzite
(Aga fm), conglomerate... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_649.txt | terozoic evolution of the southern margin of the Canadian and Baltic Shields</h3><span class="host u-clr-grey6 u-font-sans"></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 class="title">Mid-Proter... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1033.txt | pii":"S0301926816300146","doi":"10.1016/j.precamres.2016.03.001","journalTitle":"Precambrian Research","publicationYear":"2016","publicationDate":"2016-06-01","volumeSupText":"Volume 278","articleNumber":"","pageRange":"323-336","trace-token":"AAAAQBmEilysDXkD7OK1VKES7UVyZACTHP7s2y7d91WAfyP-UykC0TM8sSrQ99fRD | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_43.txt | 38 Zrn U-Pb 1692 ±7 Bingen et al., this work
North Granite, Austvatn, FUN26 Zrn U-Pb 1693 ±8 Bingen et al., this work
North Porphyry, Nyhusen, TL9403 Zrn U-Pb 1697 ±8 Lundqvist & Persson, 1999
South Grey orthogneiss with veinlets, Gällared S Zrn U-Pb 1698 ±12 Söderlund et al., 2002
South Paleosome in orthog | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_720.txt | oscandian margin along the Arctic Circle Caledonides in Sweden: The Sveconorwegian connection</span></span></a></h3><div class="article-source u-clr-grey6">August 2015</div><div class="authors"><span>David G.</span> <span>Gee</span>, …, <span>Jarosław</span> <span>Majka</span></div></div><div class="buttons"></div></li... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1395.txt | "},{"#name":"title","$":{"id":"sect0165"},"_":"Relationships between metamorphism and SMB magmatism"},{"#name":"entry","$":{"id":"sec0175","depth":"3"},"$$":[{"#name":"label","_":"8.1.1"},{"#name":"title","$":{"id":"sect0170"},"$$":[{"#name":"__text__","_":"Did regional metamorphism at 1030–970"},{"#name":"hsp","$":{"x... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1106.txt | ref","$":{"id":"crf0855","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0020"},"$$":[{"#name":"given-name","_":"Christian"},{"#name":"surname","_":"Pin"},{"#name":"cross-ref","$":{"id":"crf0860","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1297.txt | ib-reference","$":{"id":"bib0270"},"$$":[{"#name":"label","_":"Sigmond, 1978"},{"#name":"reference","$":{"id":"sbref0270","refId":"54"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"E.M.O."},{"#name":"surname","_":"Sigmond"}]}]},{"#... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1414.txt | ', 'identify', 'updateOptions', 'pageLoad'];
for (w = 0, x = v.length; w < x; ++w) (function (m) {
o[m] = o[m] || function () {
o._q[m === v[0]? 'unshift' : 'push']([m].concat([].slice.call(arguments, 0)));
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_498.txt | 72-0.26 1.72 0 2.41 0.3 2.41 1.58h2.38c0-0.36 0-0.79-0.03-1.09 -0.23-1.98-2.14-2.67-4.88-2.67 -3 0-6.7 2.31-6.7 7.76 0 5.22 2.77 7.99 6.63 7.99 1.69 0 3.47-0.36 4.95-1.39l | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_33.txt | Andersen 1999; Bingen et
al. 2001a; Andersen et al. 2004). One type is broad with
modes between 2.0 and 1.55 Ga. The other type, recorded
in turbidite sequences, is narrow with a mode between
1.66 and 1.53 Ga.
The Idefjorden terrane displays a specific plutonic suite
at 1.34-1.32 Ga (Cornell & Austin Hegardt 2004), a
... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_495.txt | c0.1 0.76 0.13 1.75 0.13 2.9v10.86h2.54v-9.51c0.53-1.29 1.72-3.7 3.17-3.7 0.96 0 1.06 0.99 1.06 1.22l2.08-0.6V9.18c0-0.03-0.03-0.17-0.06-0.4C132.8 7.36 131.91 6.6 130.2 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1175.txt | name","_":"L."},{"#name":"surname","_":"Elsasser"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S."},{"#name":"surname","_":"Brandt"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Gerdes"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Sveconorwegian mid-crustal ultrahi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_90.txt | merch.push('evar80=' + this.stripProductDelimiters(prodList[i].entitlementType));
}
if (prodList[i].recordType) {
merch.push('evar93=' + this.stripProductDel | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_44.txt | h3,#ot-sync-ntfy h4,#ot-sync-ntfy h5,#ot-sync-ntfy h6,#ot-sync-ntfy p,#ot-sync-ntfy img,#ot-sync-ntfy svg,#ot-sync-ntfy button,#ot-sync-ntfy section,#ot-sync-ntfy a,#ot-sync-ntfy label,#ot-sync-ntfy input,#ot-sync-ntfy ul,#ot-sync- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_175.txt | : 18px; -webkit-border-radius: 18px; -moz-border-radius: 18px; -khtml-border-radius: 18px; line-height: 0; padding: 8px 0 6px}
.MathJax_MenuClose:hover {color: white!important; border: 2px solid #CCC!important}
.MathJax_MenuClose:hover span {background-color: #CCC!important}
.MathJax_MenuClose:hover:focus {outline: non... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_62.txt | )), (e.sameOrigin &&!this.excludeNewrelicHeader() ||!e.sameOrigin && this.isAllowedOrigin(e) && this.useNewrelicHeaderForCors()) && (u.newrelicHeader = this.generateTraceHeader(a, s, c, r, i, o)), u;
}
generateTraceContextParentHeader(e, t) {
return "00-" + | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_51.txt | conorwegian shearzone network of SW Sweden in relation to mid-Proterozoic plate
movements. Precambrian Research 49, 245-260.
Pasteels, P. & Michot, J. 1975: Geochronologic investigation of the
metamorphic terrain of southwestern Norway. Norsk Geologisk
Tidsskrift 55, 111-134.
Pasteels, P., Demaiffe, D. & Michot, J. 197... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_934.txt | xmlns:cals":true,"xmlns:sb":true,"xmlns:sa":true,"xmlns:ja":true,"xmlns":true,"id":"sec0015","view":"all"},"$$":[{"#name":"label","_":"3"},{"#name":"section-title","$":{"id":"sect0030"},"_":"Importance of rock nomenclature"},{"#name":"para","$":{"id":"par0060","view":"all"},"_":"A significant source of confusion regard... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_124.txt | .d(t, {
X: () => i
});
var n = Object.prototype.hasOwnProperty;
function i(e, t, r) {
if (n.call(e, t)) return e[t];
var i = r();
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1327.txt | wera"}]},{"#name":"author","$$":[{"#name":"given-name","_":"O."},{"#name":"surname","_":"Bolle"}]},{"#name":"author","$$":[{"#name":"given-name","_":"B."},{"#name":"surname","_":"Bingen"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J.-P."},{"#name":"surname","_":"Liégeois"}]},{"#name":"author","$$":[{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_557.txt | -xs-bottom text-s"><button class="button-link AddToMendeley u-margin-s-right u-show-inline-from-md button-link-primary button-link-icon-left" type="button"><svg focusable="false" viewBox="0 0 86 128" height="16" width="16" class="icon icon-plus"><path d="m48 58v-38h-1e1v38h-38v1e1h38v38h1e1v-38h38v- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_8.txt | (.4)}
.MJXp-scale5 {-webkit-transform: scaleX(.5); -moz-transform: scaleX(.5); -ms-transform: scaleX(.5); -o-transform: scaleX(.5); transform: scaleX(.5)}
.MJXp-scale6 {-webkit-transform: scaleX(.6); -moz-transform: scaleX(.6); -ms-transform: scaleX(.6); -o-transform: scaleX(.6); | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_106.txt | o;
let r,
i = 0;
t && t.getRandomValues && (r = t.getRandomValues(new Uint8Array(31)));
const a = [];
for (var s = 0; s < e; s++) a.push(o( | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_3.txt | ldspathic
gneiss analysed by Birkeland et al. (1997) and Sigmond
et al. (2000) yield bi- or multimodal zircon age distributions that are difficult to interpret in terms of a
single intrusion age. We suggest that these two samples
represent paragneiss units. Detrital zircons in two samples
of metasediment (Hettefjord an... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_738.txt | 6"><div class="source">Precambrian Research, Volume 252, 2014, pp. 107-118</div></div><div class="authors"><span>Christopher J.</span> <span>Spencer</span>, …, <span>Matthew S.A.</span> <span>Horstwood</span></div></div><div class="buttons"></div></li><li class="RelatedContentPanelItem u-display-none"><div class="sub-h... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1417.txt | .className?.includes("_pendo-badge")) {
const badge = mutation.addedNodes[0];
const altText = badge?.attributes['aria-label'].value? badge?.attributes['aria-label'].value : 'Feedback';
const pendoBadgeImage = pendo.dom(`#${badge? | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_34.txt | : Lithostratigraphy and U-Pb
geochronology of the Telemark supracrustals in the Bandak-Sauland area, Telemark, South Norway. Norwegian Journal of Geology
82, 119-138.
Laajoki, K. & Lamminen, J. 2006: The Mesoproterozoic sub-Røynstaul
unconformity, central Telemark, Norway. Norwegian Journal of
Geology 86, 29-40.
70
Laa... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_4.txt | ys, A., Bogdanova, S., Janson, C., Bibikova, E. & Kornfält, K.A.
2002: The Stenshuvud and Tåghusa granitoids: new representative of Mesoproterozoic magmatism in southern Sweden. GFF 124,
149-162.
Cecys, A. & Benn, K. 2007: Emplacement and deformation of the ca.
1.45 Ga Karlshamn granitoid pluton, southeastern Sweden, d... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_431.txt | er-logo{background-color:#fff}div#onetrust-pc-sdk #ot-lst-title span{font-size:24px;font-weight:400;line-height:32px}div#onetrust-pc-sdk #ot-host-lst.ot-host-desc,div#onetrust-pc-sdk #ot-host-lst.ot-host-expand,div#onetrust-pc-sdk #ot-host-lst.ot-host-name,div | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_79.txt | .M., Kamo, S. & Ingvald, E. 1996: U-Pb
baddeleyite dating of dolerite dykes in the eastern part of the Sveconorwegian orogen, south-central Sweden. Precambrian Research
79, 227-237.
Wahlgren, C.H., Cruden, A.R. & Stephens, M.B. 1994: Kinematics of a
major fan-like structure in the eastern part of the Sveconorwegian
oro... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_77.txt | -sdk.ot-sdk-button.ot-sdk-button-primary:hover,#onetrust-banner-sdk button.ot-sdk-button-primary:hover,#onetrust-banner-sdk input[type=submit].ot-sdk-button-primary:hover,#onetrust-banner-sdk input[type=reset].ot-sdk-button-primary:hover,#onetrust-banner-sdk input[type=button].ot-sdk-button-primary: | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_82.txt | X[r.debugId] = 1, b(t);
var i = c(r),
o = f._A.XMLHttpRequest,
a = f._A.MutationObserver,
s = f._A.Promise,
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_556.txt | button button-link-icon-right" type="button" id="show-more-btn" data-aa-button="icon-expand"><span class="button-link-text">Show more</span><svg focusable="false" viewBox="0 0 92 128" height="20" width="17.25" class="icon icon-navigate-down"><path d="m1 51l7-7 38 38 38-38 7 7-45 45z"></path></svg></button><div class="b... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_63.txt | of SW Norway. Contributions to Mineralogy and Petrology 132, 336-353.
Bingen, B., Birkeland, A., Nordgulen, Ø. & Sigmond, E.M.O. 2001a:
Correlation of supracrustal sequences and origin of terranes in the
Sveconorwegian orogen of SW Scandinavia: SIMS data on zircon
in clastic metasediments. Precambrian Research 108, 29... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_566.txt | .precamres.2015.05.002" target="_blank" rel="noreferrer noopener" aria-label="Persistent link using digital object identifier" title="Persistent link using digital object identifier"><span class="anchor-text">https://doi.org/10.1016/j.precamres.2015.05.002</span><svg focusable="false" viewBox="0 0 78 128" aria-label="O... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_20.txt | } catch (e) {
u([e], r);
}
for (var n in e) a.call(e, n) && (t[n] = e[n]);
}(t | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_64.txt | 02a 84 44 33 14100 0.10980 0.72 4.715 2.35 0.3114 2.24 0.95 1796 13 1748 34 97.3 12a 133 80 54 39746 0.11040 0.72 4.807 2.36 0.3158 2.25 0.95 1806 13 1769 35 98.0 09a 117 86 51 10778 0.11074 0.60 5.014 2.31 0.3284 2.23 0.97 1812 11 1831 36 101.0 17 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_22.txt | ozoic igneous rocks in
south-western Sweden. GFF 116, 75-86.
Whitehouse, M.J., Claesson, S., Sunde, T. & Vestin, J. 1997: Ion microprobe U-Pb zircon geochronology and correlation of Archaean
gneisses from the Lewisian complex of Gruinard Bay, northwestern
Scotland. Geochimica et Cosmochimica Acta 61, 4429-4438.
Whiteho... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_77.txt | ;
}
}
var s = r(3117);
const c = "nr@context:".concat(s.a),
u = function e(t, r) {
var n = {},
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_79.txt | , Pa66R R Zrn 1486 ca. Pasteels and Michot, 1975
Rjukan Gp, Myrstul rhyolite dyke T Zrn 1502 ±1 Dahlgren et al., 1990 b
Grotte suite, tonalite -quartz diorite T Zrn 1509 +19/-3 Ragnhildstveit et al., 1994
Rjukan Gp, Runhellohovet metarhyolite T Zrn 1510 ca. Dahlgren et al., 1990 b
Mårsbro | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_60.txt | U-Pb ID-TIMS 4 Bingen & van Breemen, 1998
Rogaland-VA Mnz 914±4, 910±9 Am Augen gneiss, Feda, B113 Th-Pb ID-TIMS 2 Bingen et al., 2008
Rogaland-VA Mnz 1012±1, 1008±1, 990±1, 974±2, 904±5 Am Augen gneiss, Feda, B113 U-Pb ID-TIMS 5 Bingen & |
Subsets and Splits
No community queries yet
The top public SQL queries from the community will appear here once available.