id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
value |
|---|---|---|
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_26.txt | 20.
Cosca, M.A., Mezger, K. & Essene, E.J. 1998: The Baltica-Laurentia
connection: Sveconorwegian (Grenvillian) metamorphism, cooling, and unroofing in the Bamble Sector, Norway. The Journal of
Geology 106, 539-552.
Dahlgren, S., Heaman, L. & Krogh, T. 1990a: Precise U-Pb zircon and
baddeleyite age of the | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_411.txt | em;margin:0}div#onetrust-consent-sdk #onetrust-policy-text a[href]{font-weight:400;margin-left:8px}div#onetrust-banner-sdk #onetrust-button-group-parent{flex:0 0 auto;margin:32px 0 0;width:100%}div#onetrust-banner-sdk #onetrust-button-group{display:flex;flex-direction:row;flex-wrap:wrap;justify-content:flex- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_115.txt | ifier = r, this.sharedAggregator = new y({
agentIdentifier: this.agentIdentifier
}), this.features = {}, this.desiredFeatures = new Set(t.features || []), this.desiredFeatures.add(m), Object.assign(this, (0, s.j)(this.agentIdentifier, t, t.loaderType || "agent")), this.start()) : (0, e.Z | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1013.txt | with intraplate magmatism in the Congo, Kalahari and Indian cratons, and the Keweenawan event of central Laurentia among others. While a reconstruction history of Amazonia and Laurentia is still a matter of debate on paleomagnetic grounds, a reconstruction link with other crustal blocks remains possible."}],"$":{"view... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1329.txt | ame","_":"Longhi"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Sveconorwegian massif-type anorthosites and related granitoids result from post-collisional melting of a continental arc root"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_130.txt | #onetrust-consent-sdk #onetrust-policy-title,
#onetrust-consent-sdk #onetrust-policy-text,
#onetrust-consent-sdk.ot-b-addl-desc,
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_7.txt | rocks show
increased deformation and grade into a gneiss complex
to the southwest (Torske 1982). An augen gneiss sample
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 95
Fig. 9. Concordia diagrams presenting SIMS U-Pb data on zircon from 4 samples.
96 B. Bingen et al. NORWEGIA... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_140.txt | 0, n.D.metrics, p), i && (0, o.p)(e + t, [(0, s.z)(),...arguments], r? null : this, i, p), r? void 0 : this;
};
}
function x() {
r | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_802.txt | h.gif","https://s3-eu-west-1.amazonaws.com/prod-ucs-content-store-eu-west/content/pii:S0301926815X00088/cover/DOWNSAMPLED200/image/gif/d2f0812cff75696ba55d5092ea648ceb/cov200h.gif"],"attachment-type":"IMAGE-COVER-H200","filesize":"18050","pixel-height":"200","pixel-width":"148"},{" | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_519.txt | -button-small u-margin-s-right link-button-text-only" href="/user/register?targetURL=%2Fscience%2Farticle%2Fpii%2FS0301926815001424" id="gh-cta-btn" data-aa-region="header" data-aa-name="Register"><span class="link-button-text">Register</span></a><a class="link-button link-button-primary link-button-small link-button-t... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_11.txt | Älv Shear Zone (Ahlin et al. 2006)
suggests that this zone was active at c. 970 Ma. The
Mylonite Zone, bounding the Idefjorden Terrane in the
east (Fig. 1), is an arcuate, generally west-dipping shear
zone. It is interpreted as a sinistral transpressional thrust
zone with an overall top-to-the-southeast transport
dire... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_174.txt | [i] = s[i]? s[i] : _satellite.getVar(vars[i]);
}
}
};
// async support fallback
(function(w) {
var eventBuffer = [];
if(w.appData) {
if(Array.isArray(w.appData)) {
eventBuffer = w.appData;
} else {
console.error('Elsevier DataLayer " | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_573.txt | •</span><span><p id="par0020">The magmatic and metamorphic evolutions suggest formation in an Andean-type, accretionary <a href="/topics/earth-and-planetary-sciences/continental-shelf" title="Learn more about continental margin from ScienceDirect's AI-generated Topic Pages" class="topic-link">continental margin</a>.</p... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_108.txt | getBibliographicInfo(prodList[i]);
if (biblio) {
merch.push('evar28=' + biblio);
}
if (pro | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_850.txt | ":"abstracts"},"pdf":{"urlType":"download","url":"/science/article/pii/S0301926822002303/pdfft?md5=6719b8cf8d29553a1550d4785925cc93&pid=1-s2.0-S0301926822002303-main.pdf"}},{"articleTitle":"Anorthosite formation and emplacement coupled with differential tectonic exhumation of ultrahigh-temperature rocks in a Sveconorwe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_125.txt | if (Object.defineProperty && Object.keys) try {
return Object.defineProperty(e, t, {
value: i,
writable:!0,
enumerable:!1
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_183.txt | font-size:1em;line-height:1.5;margin-bottom:10px;margin-top:10px;width:100%}#onetrust-pc-sdk #accept-recommended-btn-handler{margin-right:10px;margin-bottom:25px;outline-offset:-1px}#onetrust-pc-sdk #ot-pc-desc{clear:both;width:100%;font-size:.812em;line-height:1.5;margin-bottom:25px | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_510.txt | -0.76-0.01-1.14 0zm-4.86 5e1v1e1h1e1v-1e1h-1e1z"></path></svg></button></div></div></li><li class="gh-search-toggle gh-nav-item search-button-link search-with-button-link"><a class="anchor button-link-primary gh-nav-action gh-icon-btn search-input-fallback-link anchor-default anchor-icon-only" href="/ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_70.txt | (0,0,0,0);border-radius:2px;border:1px solid #bbb;cursor:pointer;box-sizing:border-box}#onetrust-banner-sdk.ot-sdk-button:hover,#onetrust-banner-sdk :not(.ot-leg-btn-container)>button:not(.ot-link-btn):hover,#onetrust-banner-sdk :not(.ot-leg-btn-container)>button:not(. | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_72.txt | 2.25 0.2715 2.23 0.99 1497 5 1549 31 103.5
11a 310 40 97 11444 0.09344 0.35 3.543 2.27 0.2750 2.24 0.99 1497 7 1566 31 104.6
07a 230 34 67 16650 0.09358 0.40 3.297 2.26 0.2555 2.23 0.98 1500 7 1467 29 97.8
05a 286 47 87 21538 0.09364 0.37 3.439 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_22.txt | 4 0.0924 0.0009 3.22 0.05 0.253 0.003 0.71 1477 19 1452 13 98.3
5 0.0927 0.0008 3.28 0.05 0.256 0.003 0.85 1483 16 1470 18 99.2
1 0.0932 0.0008 3.27 0.06 0.254 0.004 0.85 1492 17 1460 19 97.9
2 0.0933 0.0008 3.24 0.05 0.252 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1506.txt | data) {
if(!data) {
this.warnings.push('dv0');
return;
}
// top 5
if(!(data.visitor && data.visitor.accessType)) {
this.warnings.push('d | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_34.txt | Skånevik supra metarhyolite weak J-482A 331550 6625250 Bt, Ms SIMS 15 14 1.3 1491 5 extrusion 9B
Røldal Røldal augen gneiss strong B00-127 374822 6632511 Bt, Ep, Ttn LA-ICPMS 11 11 0.50 1495 13 intrusion 10A
Sauda Sauda supra augen gneiss strong B00-106 355423 6616505 Bt, Ttn, Ep LA-IC | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_688.txt | Correlation factors between Laurentia and Baltica, or Laurentia and Amazonia, are below 0.14. Comparison between the Grenville Province in northeastern Laurentia and the Sveconorwegian Province in southwestern Fennoscandia (Baltica) shows some striking similarities, especially in the Mesoproterozoic, but also exhibits... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_38.txt | P. Padget read the manuscript. This paper benefited from constructive reviews by J. Andersson and F. Corfu.
References
Åhäll, K.I. 1991: An investigation of the Proterozoic Stenungsund granitoid intrusion, southwest Sweden; conflicting geochronological
and field evidence. In Gower, C.F., Rivers, T. & Ryan, B. (eds.), ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_916.txt | ","_":"Dr."},{"#name":"given-name","_":"Trond"},{"#name":"surname","_":"Slagstad"}]}]},{"#name":"author-group","$$":[{"#name":"author","$$":[{"#name":"degrees","_":"Dr."},{"#name":"given-name","_":"Giulio"},{"#name":"surname","_":"Viola"}]}]}]}]}],"floats":[],"footnotes":[],"attachments":[]},"crossMark":{"isOpen":false... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_15.txt | -by-logo,#ot-sync-ntfy.ot-pc-footer-logo a{background-size:contain;background-repeat:no-repeat;background-position:center;height:25px;width:152px;display:block;text-decoration:none;font-size:.75em}#onetrust-banner-sdk.powered-by-logo:hover,#onetrust-banner-sdk.ot-pc-footer-logo a:hover,#onetrust | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_5.txt | data were obtained at the
laboratory of the Geological Survey of Norway, with the collaboration
of B. Davidsen. S. Dahlgren and W.J. Davis are thanked for providing
reference zircons from the Larvik district and Slave Province respectively, together with related U-Pb data. H. Schiellerup and T. Slagstad are
thanked fo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_451.txt | -sdk-cookie-policy-v2.ot-sdk-cookie-policy.ot-sdk-subgroup ul li{list-style:disc;margin-left:1.5em}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy.ot-sdk-subgroup ul li h4{display:inline-block}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table{border-collapse:inherit;margin:auto | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_807.txt | open-research":{},"titleString":"The Late Mesoproterozoic Sirdal Magmatic Belt, SW Norway: Relationships between magmatism and metamorphism and implications for Sveconorwegian orogenesis","ssrn":{},"renderingMode":"Preview","isAbstract":true,"isContentVisible":false,"ajaxLinks":{"referredToBy":true,"specialIssueArticle... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_7.txt | Kongsberg, Bamble and Telemarkia Terranes. The Eastern Segment is lithologically related to the Transcandinavian Igneous Belt (TIB), in the Fennoscandian foreland of the belt. The terranes are possibly endemic to Fennoscandia,
though an exotic origin for the Telemarkia Terrane is possible. A review of existing geologi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_120.txt | :absolute;top:50%;left:75%;transform:translateY(-50%)}#onetrust-banner-sdk #onetrust-close-btn-container{top:50%;margin:auto;transform:translate(-50%, -50%);position:absolute;padding:0;right:0}#onetrust-banner-sdk #onetrust-close-btn-container button{position:relative;margin:0;right:-22px;top:2px}}@media only screen an... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_26.txt | titanite U-Pb ages recording regional cooling at c. 1090-
1080 Ma. Secondary titanite at 994 ±30 Ma in the hanging wall of the shear zone may relate to reactivation of
the shear zone or reheating in relation to metamorphism
in the Telemarkia footwall (Fig. 4; de Haas et al. 2002).
UV-laser 40Ar/39Ar data on muscovite p... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_799.txt | Url":"","recentInstitutions":[],"canActivatePersonalization":false,"hasInstitutionalAssociation":false,"hasMultiOrg":false,"userType":"GUEST","userAnonymity":"ANON_GUEST","allowCart":true,"environment":"prod","cdnAssetsHost":"https://sdfestaticassets-us-east-1.sciencedirectassets.com"},"isCorpReq":false,"isPdfFullText"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_718.txt | Sweden</span></span></a></h3><div class="article-source u-clr-grey6">August 2015</div><div class="authors"><span>Jan</span> <span>Ulmius</span>, …, <span>Charlotte</span> <span>Möller</span></div></div><div class="buttons"></div></li><li class="RelatedContentPanelItem u-display-block"><div class="sub-heading u-padding... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_61.txt | 2002; Laajoki
et al. 2002; Bingen et al. 2003; Andersen et al. 2007b). It
includes, a juvenile granite batholith formed between
1220 and 1190 Ma and possibly with associated mafic
underplates, 1190-1140 Ma A-type granite-charnockite plutonism, and the alkaline 1134 ±2 Ma Morkheia
monzonite suite. It also includes, as ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_28.txt |
case 'contentLinkClick':
if (data && data.link) {
window.eventData.action = { name: pageData.page.productName + ':' + (data.link.type || 'no link type') + ':' + (data.link.name || 'no link name') };
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_80.txt | 2000
Telemark Vindeggen gp, Sandvik metadiabase, KLN7076 Zrn U-Pb 1347 ±4 Corfu and Laajoki, 2008
50 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Location Lithology, sample Min System Age ±2s Reference
(1) (2) (Ma)
Telemark Tinn granite, 0831962 Zrn U-Pb 1476 ±13 Andersen et al., 2002
Rogaland Lyngdal granite gneiss,... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_58.txt | is not known whether
the belt hosts a suture zone, and consequently if the belt
includes exotic lithotectonic units.
Exotic Telemarkia
Two main lines of evidence from the pre-Sveconorwegian
1220-1130 Ma history (Fig. 7) can be used to suggest an
exotic ancestry for the Telemarkia Terrane (Bingen et al.
2005; Corfu & L... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_440.txt | rust-pc-sdk #ot-anchor{display:none!important}
/*! Extra code to blur our background */
.onetrust-pc-dark-filter{
backdrop-filter: blur(3px)
}
.ot-sdk-cookie-policy{font-family:inherit;font-size:16px}.ot-sdk-cookie-policy.otRelFont{font-size:1rem}.ot-sdk-cookie-policy h3,.ot-sdk-cookie-policy h4,. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_46.txt | checkbox{font-family:inherit;font-weight:normal;-webkit-font-smoothing:auto;letter-spacing:normal;line-height:normal;padding:0;margin:0;height:auto;min-height:0;max-height:none;width:auto;min-width:0;max-width:none;border-radius:0;border:none;clear:none;float:none;position:static;bottom:auto;left:auto;right:auto;top:au... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_689.txt | and during the final Grenvillian collision is also largely diachronous. 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.</p></div></div></div></li><li class="ListArticleItem u-margin-l-bottom"><div class="sub-hea... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_61.txt | 87 30 98.9 01a 72 76 25 26688 0.09426 0.76 3.247 2.36 0.2499 2.23 0.95 1513 14 1438 29 95.0 06a 109 61 36 15528 0.09458 0.64 3.431 2.32 0.2631 2.23 0.96 1520 12 1506 30 99.1 11a 86 54 28 42937 0.09537 0.96 3.369 2.43 0.2562 2.23 0.92 1535 18 1471 29 95 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_708.txt | processes involving significant sedimentary recycling. This accretionary margin was most likely transformed into the Sveconorwegian orogen through collisional interactions of Baltica, Laurentia and Amazonia in the context of Rodinia amalgamation.</p></div></div></div></li></ul><a class="button-alternative button-alter... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_86.txt | }), (0, S.m$)(!1));
} catch (e) {
(0, W.Z)("An error occurred while intercepting XHR", e);
try {
r.em | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1296.txt | and the role of epidote in magmatic evolution"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Am. Mineral."}]},{"#name":"volume-nr","_":"81"}]},{"#name":"date","_":"1996"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"462"},{"#name":"las... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_952.txt | ":true,"xmlns:cals":true,"xmlns:sb":true,"xmlns:sa":true,"xmlns:ja":true,"xmlns":true,"id":"sec0170","role":"conclusion","view":"all"},"$$":[{"#name":"label","_":"9"},{"#name":"section-title","$":{"id":"sect0195"},"_":"Conclusions"},{"#name":"para","$":{"id":"par0460","view":"all"},"_":"A major conclusion of this work ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_341.txt | item.ot-acc-hdr.ot-cat-header,#onetrust-pc-sdk #ot-pc-lst.ot-vs-list.ot-vnd-item.ot-acc-hdr.ot-cat-header,#onetrust-pc-sdk.ot-accordion-layout.ot-checkbox-consent.ot-acc-hdr.ot-cat-header{flex:1;margin:0.5rem}#onetrust-pc-sdk.ot-vs-config | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1448.txt | o" role="img" aria-label="Company Logo"><img alt="Company Logo" src="https://cdn.cookielaw.org/logos/static/ot_company_logo.png"></div></div><!-- Close Button --><div id="ot-pc-content" class="ot-pc-scrollbar"><div class="ot-optout-signal ot-hide"><div class="ot-optout-icon"><svg xmlns="http://www.w3.org/2000/svg"><pat... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1505.txt | data.visitor[idPlusFields[i]] = data.visitor.idPlusData[idPlusFields[i]];
}
}
data.visitor.idPlusData = undefined;
}
}
,validateData: function( | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_459.txt | cookie-policy-v2) td:before{content:attr(data-label);font-weight:bold}.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) li{word-break:break-word;word-wrap:break-word}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table{overflow:hidden}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table td{border | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_74.txt | Racken, DC972 U-Pb SIMS 3 Larson et al., 1999 Zrn 974±22 Am Migmatitic Delsjön augen gneiss, Stora Delsjön, EAH0309 U-Pb SIMS Ahlin et al., 2006 Zrn 980±13 Am Migmatitic banded gneiss, Bua, TK1+TK2 U-Pb SIMS 8 Andersson et al., 2002 Zrn 1024±52 Am Metagreywacke, Skagerrak Fm, DC94 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_660.txt | nbsp;Ma. These pegmatites formed in similar orogenic settings, implying that similar tectono-metamorphic developments along the Grenville–Sveconorwegian orogenic belt were diachronous.</p><p id="sp0025">We conclude that local anatexis is the major pegmatite-melt forming process in the Sveconorwegian as well as Grenvill... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_16.txt | 9a 0.0932 0.0006 3.55 0.06 0.276 0.004 0.90 1492 13 1573 20 105.4
18b 0.0942 0.0008 3.15 0.05 0.242 0.003 0.86 1513 15 1398 17 92.4
22a 0.0944 0.0007 3.45 0.06 0.265 0.004 0.89 1515 14 1517 20 100.1
22b 0.0945 0.0008 3.09 0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_115.txt | o.pathname = "/" + o.pathname);
var s =!t.protocol || ":" === t.protocol || t.protocol === r.protocol,
c = t.hostname === r.hostname && t.port === r.port;
return o.sameOrigin = s && (!t.hostname || c), "/" === o.path | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_858.txt | ":"abstract"},{"$$":[{"$":{"id":"st010"},"#name":"section-title","_":"Abstract"},{"$$":[{"$":{"view":"all","id":"sp0010"},"#name":"simple-para","_":"The tectonic setting and mechanisms and duration of emplacement of Proterozoic massif-type anorthosites and the significance of typically associated ultrahigh-temperature ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_54.txt | ozoic (Subjotnian) rapakivi complexes of central
Sweden: implications for U-Pb zircon ages, Nd, Sr and Pb isotopes. Transactions of the Royal Society of Edinburgh: Earth Sciences
92, 201-228.
Andréasson, P.G. & Rodhe, A. 1990: Geology of the Protogine Zone
south of Lake Vättern, southern Sweden: a reinterpretation. Geo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_673.txt | ans">Citation Excerpt :</div><p class="u-font-serif text-xs">An earlier Re–Os age of 973 Ma from a migmatite 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... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_75.txt | =!1, t.xhrGuids = {}, t.lastSize = null, t.loadCaptureCalled =!1, t.params = this.params || {}, t.metrics = this.metrics || {}, e.addEventListener("load", function (r) {
_(t, e);
}, (0, C.m$)(!1)), u.IF || e.add | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_793.txt | ":true},"contentType":"JL","crossmark":true,"document-references":71,"freeHtmlGiven":false,"ssoUrls":["//acw.sciencedirect.com/SSOCore/update?acw=e6b5cb79974fb545060b31649ea5c81fa189gxrqa%7C%24%7C9A361342D5830378190D3D7AFF9457691EF0BE933086A4258E4D7FB42E5 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1003.txt | -content-store-eu-west/content/pii:S0301926814002514/fx1/THUMBNAIL/image/gif/158f828ce793c12f1ea0f447c452053f/fx1.sml"},{"#name":"file-basename","_":"fx1"},{"#name":"abstract-attachment","_":"true"},{"#name":"filename","_":"fx1.sml"},{"#name":"extension","_":"sml"},{"#name":"filesize","_":" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_81.txt | IMS 5 Wang et al., 1998 South Zrn 975±17 Am Garnet amphibolite, Knäred, 9015 U-Pb ID-TIMS 3 Wang et al., 1998 South Zrn 976±7 Am Syn-tectonic leucosome, Oxanäset, OX3 U-Pb SIMS 11 Möller et al., 2007 South Zrn 982±15 Am Deformed granitic dyke, Gällared S Pb-Pb TIMS 4 Söderlund et al., 2002 South | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_180.txt | minus *,#onetrust-pc-sdk.ot-hide-tgl *{visibility:hidden}#onetrust-pc-sdk #ot-gn-venlst.ot-ven-item.ot-acc-hdr{min-height:40px}#onetrust-pc-sdk.ot-pc-header{height:39px;padding:10px 0 10px 30px;border-bottom:1px solid #e9e9e9}#onetrust-pc-sdk #ot-pc- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_13.txt | D., Michot, J. & Duchesne, J.C. 1986: Isotopic constraints on the genesis of the Rogaland anorthositic suite (SW Norway). Chemical Geology 57, 167-179.
Dons, J.A. 1960: The stratigraphy of supracrustal rocks, granitization
and tectonics in the Precambrian Telemark area, southern Norway.
Norges geologiske undersøkelse ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_35.txt | function h(e, t) {
if (!e) throw new Error("All configuration objects require an agent identifier!");
l[e] = (0, i.D)(t, d()), (0, n.Qy)(e, l[e], "config");
}
function p(e, t) {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_407.txt | color:#eb6500!important}div#onetrust-consent-sdk a,div#onetrust-pc-sdk a{color:#007398!important;text-decoration:underline!important}div#onetrust-consent-sdk a,div#onetrust-consent-sdk button,div#onetrust-consent-sdk p:hover{opacity:1!important}div#onetrust-consent-sdk a:focus,div#onetrust-consent-sdk button:focus | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_135.txt | a = (0, F._L)(this.ee),
s = (0, F.Lg)(this.ee),
c = (0, F.BV)(this.ee),
d = (0, F.Kf)(this.ee),
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_3.txt | D. & Parrish, R.R. 2004:
Mesoproterozoic bimodal volcanism in SW Norway, evidence for
recurring pre-Sveconorwegian continental margin tectonism. Precambrian Research 134, 249-273.
Cawood, P.A. & Pisarevsky, S.A. 2006: Was Baltica right-way-up or
upside-down in the Neoproterozoic? Journal of the Geological Society, Lond... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_68.txt | )(r.allowed_origins[i]);
if (e.hostname === o.hostname && e.protocol === o.protocol && e.port === o.port) {
t =!0;
break;
}
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1307.txt | name":"book","$$":[{"#name":"date","_":"1995"},{"#name":"publisher","$$":[{"#name":"name","_":"Mineralogical Society of America Monograph"}]}]},{"#name":"pages","$$":[{"#name":"first-page","_":"799"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0290"},"$$":[{"#name":"label","_":"Stephens et al., 1996"},{"#name":"refe... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_414.txt | k #onetrust-policy{margin:0 40px 0 0}div#onetrust-banner-sdk.ot-sdk-row{align-items:center;flex-direction:row}div#onetrust-banner-sdk #onetrust-button-group-parent,div#onetrust-banner-sdk.ot-bnr-flift:not(.ot-iab-2) #onetrust-button-group-parent,div#onetrust-banner-sdk:not(.ot- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_41.txt | (385),
A = r(6818);
const x = {
buildEnv: A.Re,
bytesSent: {},
queryBytesSent: {},
customTransaction: void 0,
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_123.txt | -" + e, [!1], void 0, t, r)), u[e] =!1);
}), (0, o.L)(t, a.D.pageViewEvent));
}
const u = {};
},
2210: (e, t, r) => {
r | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_148.txt | date = new Date();
date.setTime(date.getTime() + (-1 * 1000));
expiresNow = "; expires=" + date.toGMTString();
if (typeof(seconds)!= 'undefined') {
date.setTime(date.getTime() + (seconds * 1000));
expires = '; expires=' + date | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1071.txt | "},{"#name":"italic","_":"P"},{"#name":"__text__","_":" granulites. Consistently, field geological observations and available geochronological data also indicate their similar deformation and metamorphic history from H"},{"#name":"italic","_":"P"},{"#name":"__text__","_":" granulite facies stage (∼1.96–1.90"},{"$":{"sp... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_155.txt | 0;width:512px;max-height:800px}div#onetrust-pc-sdk.ot-pc-header{display:none}div#onetrust-pc-sdk #ot-pc-content{overscroll-behavior:contain;padding:0 12px 0 24px;margin:16px 4px 0 0;top:0;right:16px;left:0;width:auto}div#onetrust-pc-sdk #ot-category-title,div#onetrust-pc-sdk # | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_15.txt | lund, U., Möller, C., Andersson, J., Johansson, L. & Whitehouse,
M.J. 2002: Zircon geochronology in polymetamorphic gneisses in
the Sveconorwgian orogen, SW Sweden: ion microprobe evidence
for 1.46-1.42 Ga and 0.98-0.96 Ga reworking. Precambrian
Research 113, 193-225.
Tobi, A.C., Hermans, G.A., Maijer, C. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1313.txt | ":[{"#name":"editors","$$":[{"#name":"editor","$$":[{"#name":"given-name","_":"A.C."},{"#name":"surname","_":"Tobi"}]},{"#name":"editor","$$":[{"#name":"given-name","_":"J.L.R."},{"#name":"surname","_":"Touret"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Deep Proterozoic Crust in the North Atlantic Provin... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1204.txt | maintitle","_":"Classification of the amphiboles"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Rev. Mineral. Geochem."}]},{"#name":"volume-nr","_":"67"}]},{"#name":"date","_":"2007"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"55"},{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_290.txt | ntr{border:1px solid #d8d8d8;padding:.75rem 2rem;padding-bottom:0;width:auto;margin-top:.5rem}#onetrust-pc-sdk.ot-acc-grpdesc+.ot-leg-btn-container{padding-left:20px;padding-right:20px;width:calc(100% - 40px);margin-bottom:5px}#onetrust-pc-sdk.ot-subgrp.ot-leg-btn- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_40.txt | #onetrust-pc-sdk td,#onetrust-pc-sdk tbody,#onetrust-pc-sdk.ot-main-content,#onetrust-pc-sdk.ot-toggle,#onetrust-pc-sdk #ot-content,#onetrust-pc-sdk #ot-pc-content,#onetrust-pc-sdk.checkbox,#ot-sdk-cookie-policy div,#ot-sdk-cookie-policy span,#ot-sdk-cookie-policy | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_164.txt | _Button.MathJax_Hover_Arrow {position: absolute; cursor: pointer; display: inline-block; border: 2px solid #AAA; border-radius: 4px; -webkit-border-radius: 4px; -moz-border-radius: 4px; -khtml-border-radius: 4px; font-family: 'Courier New',Courier; font-size: 9px; color: #F0F0F0}
.MathJax_Menu_Button.MathJax_H | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_37.txt | 0), o = 2; o < n; o++) i[o - 2] = arguments[o];
r && t(r,...i);
}
var w = "fetch-",
A = w + "body-",
x = ["arrayBuffer", "blob", "json", "text | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_696.txt | show the signature (including high positive Eu anomalies) of anatectic processes in disequilibrium melting conditions and rapid extraction from the source rocks. Flowage differentiation in the emplacement process explains the various compositions, as commonly observed in migmatite leucosomes. The metaquartzites show a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_0.txt | return i._A.NREUM || (i._A.NREUM = {}), void 0 === i._A.newrelic && (i._A.newrelic = i._A.NREUM), i._A.NREUM;
}
function s() {
let e = a();
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_88.txt | 8 Andersen, 1997
Bamble Grimstad Granite Zrn U-Pb 989 ±9 Kullerud & Machado, 1991
Bamble Gloserheia pegmatite Eux U-Pb 1060 +8/-6 Baadsgaard et al., 1984
Bamble Gjeving charnockite gneiss Zrn U-Pb 1152 ±2 Kullerud & Machado, 1991
Bamble Levang granitic gneiss dome, Southern part Zrn U-Pb 1167 ±50 O | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_33.txt | a controversy: U-Pb geochronological evidence for significant Grenvillian activity in the Bamble
area, Norway. Terra Abstracts, supplement to Terra Nova 3, 504.
Kullerud, L. & Dahlgren, S.H. 1993: Sm-Nd geochronology of Sveconorwegian granulite facies mineral assemblages in the Bamble
shear belt, south Norway. Precamb... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_700.txt | more combined Hf–O isotopic studies, especially on the samples from South Norway, are probably required (as one granite sample with high δ18O values of 11–12‰ was reported by Roberts, 2010). However, the isotopic data reported here are consistent with the geological expressions, as the granitic rocks are mostly I- and... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_288.txt | -ctgl{margin-left:66px}#onetrust-pc-sdk.ot-ven-litgl+.ot-arw-cntr{margin-left:81px}#onetrust-pc-sdk.ot-enbl-chr.ot-host-cnt.ot-tgl-cntr{width:auto}#onetrust-pc-sdk #ot-lst-cnt:not(.ot-host-cnt).ot-tgl-cntr{width:auto | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_402.txt | cntr > a:focus {
outline: 1px solid #000000;
}#onetrust-pc-sdk.ot-vlst-cntr.ot-ext-lnk, #onetrust-pc-sdk.ot-ven-hdr.ot-ext-lnk{
background-image: url('https | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1244.txt | $":{"id":"sbref0180","refId":"36"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Möller"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.J."},{"#name":"surname","_":"O’Brien"}]},{"#name":"author"... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_7.txt |
metamorphism is variable and ranges from greenschistfacies to amphibolite-facies and locally granulite-facies.
High-pressure mafic granulite boudins are reported in
the eastern part of the Idefjorden Terrane, east of the
Göta Älv Shear Zone (Trollhättan locality; Fig. 8b; Söderlund et al. 2008). They yield pressure-te... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_22.txt | };
}
break;
case 'linkOut':
if (data && data.content && data.content.length > 0) {
window.eventData.linkOut = data.content | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_17.txt | onetrust-banner-sdk button *,#onetrust-banner-sdk a[data-parent-id] *,#onetrust-pc-sdk h3 *,#onetrust-pc-sdk h4 *,#onetrust-pc-sdk h6 *,#onetrust-pc-sdk button *,#onetrust-pc-sdk a[data-parent-id] *,#ot-sync-ntfy h3 *,#ot-sync-ntfy h4 *,#ot- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_14.txt | r, e);
}), t;
}
var s = i(9144);
var c = i(5546),
u = i(385),
d = i(8e3),
l = i(5938),
f = i(3960);
class h extends | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_54.txt | .T. & Lagerblad, B.
1995: A comparison of the geochronology and geochemistry of
plagioclase-dominated granitoids across a major terrane boundary
in the SW Baltic Shield. Precambrian Research 74, 57-72.
Piontek, J.E., Connelly, J.N. & Åhäll, K.I. 1998: 1.3 Ga anorogenic magmatism in Southwest Sweden. Abstracts with prog... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_109.txt | const n = "NRBA",
i = 144e5,
o = 18e5;
},
7894: (e, t, r) => {
function n() {
return Math.round(performance.now());
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_153.txt | ner-sdk{padding:48px}}div#onetrust-consent-sdk #onetrust-pc-sdk h5{font-size:16px;line-height:24px}div#onetrust-consent-sdk #onetrust-pc-sdk p,div#onetrust-pc-sdk #ot-pc-desc,div#onetrust-pc-sdk.category-host-list-handler,div#onetrust-pc-sdk.ot-accordion-layout.ot-cat | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1365.txt | opusHubEid":"2-s2.0-80052720787"},{"refId":68,"scopusHubEid":"2-s2.0-84879613323","crossRefDoi":"10.1130/SPE241-p33"},{"refId":69,"scopusHubEid":"2-s2.0-0037672000"},{"refId":70,"scopusHubEid":"2-s2.0-77249112921","crossRefDoi":"10.2138/am.2010. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1194.txt | Krogh"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Proterozoic southward accretion and Grenvillian orogenesis in the interior Grenville Province in eastern Labrador: evidence from U–Pb geochronological investigations"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","... |
Subsets and Splits
No community queries yet
The top public SQL queries from the community will appear here once available.