id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
value |
|---|---|---|
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_380.txt | -sdk #ot-host-lst.ot-host-info,
#onetrust-consent-sdk #onetrust-pc-sdk #ot-fltr-modal #modal-header,
#onetrust-consent-sdk #onetrust-pc-sdk.ot-checkbox label span,
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_53.txt |
Sveconorwegian terrane boundary in the Baltic Shield. Precambrian Research 114, 121-147.
Andersson, M., Lie, J.E. & Husebye, E.S. 1996: Tectonic setting of postorogenic granites within SW Fennoscandia based on deep seismic
and gravity data. Terra Nova 8, 558-566.
Andersson, U.B., Neymark, L.A. & Billström, K. 2002b: P... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_74.txt | this.ee), (0, F.u5)(this.ee), (0, F.Kf)(this.ee), function (e, t, i, o) {
function a(e) {
var t = this;
t.totalCbs = 0, t.called = 0, t.cbTime = 0, t.end = E, t.ended | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1460.txt | -label="Cookie Details List" data-parent-id="3">Cookie Details List</button></div></div></div><div class="ot-accordion-layout ot-cat-item ot-vs-config" data-optanongroupid="2"><button aria-expanded="false" ot-accordion="true" aria-controls="ot-desc-id-2" aria-labelledby="ot-header-id-2"></button><!-- Accordion header ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1143.txt | _":"H.J."},{"#name":"surname","_":"Stein"}]},{"#name":"author","$$":[{"#name":"given-name","_":"Ø."},{"#name":"surname","_":"Skår"}]},{"#name":"author","$$":[{"#name":"given-name","_":"Ø."},{"#name":"surname","_":"Nordgulen"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Geochronology of high-grade metamorph | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_527.txt | -10.74c0-3.71-3.01-6.72-6.72-6.72l-10.1,0v-86.21 c0-8.2-6.71-14.9-14.9-14.9c-8.2,0-14.9,6.71-14.9,14.9v86.21l-115.42-0.02v-86.19c0-8.2-6.71-14.9-14.9- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_722.txt | Norway revisited"><span class="anchor-text"><span>Multiple reactivation and strain localization along a Proterozoic orogen-scale deformation zone: The Kongsberg-Telemark boundary in southern Norway revisited</span></span></a></h3><div class="article-source u-clr-grey6">August 2015</div><div class="authors"><span>Thoma... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_132.txt | =16,j=23;var U=6,T=10,R=15,O=21;s=J(s);C=e(s);Y=1732584193;X=4023233417;W=2562383102;V=271733878;for(P=0;P<C.length;P+=16){h=Y;E=X;v=W;g=V;Y=u(Y,X,W,V,C[P+0],S,361409 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_891.txt | and the felsic magmas were aggregated but did not interacted to yield hybrid magmas, possibly because the time interval was too short. They mingled in various proportions to form the norito-felsic gneisses. The aggregated magmas were intimately linked to the EGOG intrusion in which they played a role as a lubricating ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1073.txt | "},{"#name":"italic","_":"P"},{"#name":"__text__","_":" granulite facies conditions might be attributed to mineral re-equilibrium due to long dwell time under M"},{"#name":"italic","_":"P"},{"#name":"__text__","_":" granulite facies. Additionally, these granulite facies rocks record high apparent geothermal gradients a... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_31.txt | stén et al.
2000; Stein et al. 2000; Årebäck & Andersson 2002; Eliasson et al. 2003; Hellström et al. 2004). Extensional reactivation of major Sveconorwegian shear zones occurred
between 970 and 880 Ma (Johansson & Johansson 1993;
Mulch et al. 2005; Page et al. 1996a; Page et al. 1996b;
Scherstén et al. 2004).
The volu... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_23.txt | & Connelly, 2008
Eastern Segment, Protogine Zone, and Sveconorwegian Frontal Deformation Zone
North Riddaho pegmatite Clm U-Pb 942 ±2 Romer & Smeds, 1996
South Undeformed granite dyke, Högabjär, HB4 Zrn U-Pb 945 ±7 Möller et al., 2007
South Undeformed granite dyke, Tjärnesjö granite, Sundhult Zrn Pb-Pb 947 ±12 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1389.txt | title","$":{"id":"sect0100"},"_":"Host rock characteristics and relationships to the SMB"},{"#name":"entry","$":{"id":"sec0090","depth":"2"},"$$":[{"#name":"label","_":"5.1"},{"#name":"title","$":{"id":"sect0105"},"_":"Gyadalen transect"}]},{"#name":"entry","$":{"id":"sec0095","depth":"2"},"$$":[{"#name":"label","_":"5... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_165.txt | over_Arrow span {display: block; background-color: #AAA; border: 1px solid; border-radius: 3px; line-height: 0; padding: 4px}
.MathJax_Hover_Arrow:hover {color: white!important; border: 2px solid #CCC!important}
.MathJax_Hover_Arrow:hover span {background-color: #CCC!important}
</style><style type="text/css">#MathJax_A... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_50.txt |
al. 2006). A deformation event younger than 917 ±3 Ma
is recorded in direct contact to the anorthosite plutons.
These data imply that intrusion of the post-collisional
granite plutons and anorthosite plutons was associated
with ductile deformation, in accordance with structural
data on the plutons (Bolle et al. 2000; ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1376.txt | a1def8c4a2586c9854227&pid=1-s2.0-0301926895000976-main.pdf"}},{"refId":64,"pii":"S0012825211000584","filesize":"2MB","pdf":{"urlType":"download","url":"/science/article/pii/S0012825211000584/pdfft?md5=7d853a02765498f84ee6aad260843b1d&pid=1-s2.0-S | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_157.txt | 12e4);
s.onerror = f.bind(null, s.onerror), s.onload = f.bind(null, s.onload), c && document.head.appendChild(s);
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_132.txt | #onetrust-consent-sdk.ot-dpd-desc *:not(.onetrust-vendors-list-handler),
#onetrust-consent-sdk #onetrust-banner-sdk #banner-options *,
#onetrust-banner-sdk.ot-cat- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1403.txt | 31649ea5c81fa189gxrqa%7C%24%7C9A361342D5830378190D3D7AFF9457691EF0BE933086A4258E4D7FB42E5CDA3EC3BE1A2AD34978E6E467FBA88B160B471687035859AC27543FBA44D1BD4E4F2EB0469A67597464825D387A21AFA2E514&utt= | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_182.txt | :55%;font-weight:700}#onetrust-pc-sdk.ot-cat-item p{clear:both;float:left;margin-top:10px;margin-bottom:5px;line-height:1.5;font-size:.812em;color:dimgray}#onetrust-pc-sdk.ot-close-icon{height:44px;width:44px;background-size:10px}#onetrust-pc-sdk #ot-pc-title{float:left; | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1170.txt | maintitle","_":"Atlas of igneous zircon"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Rev. Mineral. Geochem."}]},{"#name":"volume-nr","_":"53"}]},{"#name":"date","_":"2003"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"470"},{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_33.txt | . Two possible models for terrane assembly at the onset of the
Sveconorwegian orogeny. One model features Telemarkia attached to
an unknown craton (exotic Telemarkia) and the other to Fennoscandia (indigenous Telemarkia). Colour coding follows Fig. 1. See text
for more explanations. After 1.10 Ga, oblique (sinistral) c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_25.txt | if (data && data.action) {
window.eventData.action.name = pageData.page.productName + ':' + data.action.name;
}
break;
case'searchWithinContent':
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1221.txt | ","$$":[{"#name":"given-name","_":"B.E."},{"#name":"surname","_":"Leake"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.R."},{"#name":"surname","_":"Woolley"}]},{"#name":"author","$$":[{"#name":"given-name","_":"C.E.S."},{"#name":"surname","_":"Arps"}]},{"#name":"author","$$":[{"#name":"given-name","_":" | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_544.txt | </span><button class="button-link button-link-primary" type="button" data-sd-ui-side-panel-opener="true" data-xocs-content-type="author" data-xocs-content-id="aut0005"><span class="button-link-text"><span class="react-xocs-alternative-link"><span class="given-name">N.</span> <span class="text surname">Coint</span> </sp... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_21.txt | Göta-Älv Shear Zone at 980-970 Ma
(Andersson et al. 2002a; Ahlin et al. 2006) are possibly
related to SE-directed oblique thrusting of the Idefjorden
Terrane onto the Eastern Segment (Park et al. 1991; Stephens et al. 1996).
In the hinterland of the orogen, in the Rogaland-Vest
Agder Sector, the Falkenberg phase is al... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_990.txt | de Geologia Geral, Universidade Federal de Mato Grosso"},{"#name":"city","_":"Cuiabá"},{"#name":"state","_":"MT"},{"#name":"postal-code","_":"78060-900"},{"#name":"country","_":"Brazil"}]}]},{"#name":"affiliation","$":{"id":"aff0025"},"$$":[{"#name":"label","_":"e"},{"#name":"textfn","_":"Instituto de Investigaciones ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_57.txt | b age of c. 926 Ma (Eliasson &
Schöberg 1991). The age estimates on the Flå and Bohus
granites overlap, confirming that these two very similar
plutons are coeval.
Review
Published, mainly U-Pb, geochronological data recording magmatic and metamorphic events in the Sveconorwegian belt are summarized in Tables 3, 4 and 5... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_136.txt | i = this,
a = "function" == typeof t;
return (0, o.p)(v + "tracer", [(0, s.z)(), e, r], i, n.D.spa, p), function () {
if (g. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_42.txt | �häll, K.I., Connelly, J.N. & Brewer, T.S. 2000: Episodic rapakivi magmatism due to distal orogenesis? Correlation of 1.69-1.50 Ga orogenic and inboard, “anorogenic” events in the Baltic shield. Geology
28, 823-826.
Åhäll, K.I. & Larson, Å. 2000: Growth-related 1.85-1.55 Ga magmatism in the | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_161.txt | ot-accordion-layout h4~.ot-always-active{color:inherit;font-size:12px;font-weight:400;line-height:1.5;padding-right:48px}div#onetrust-pc-sdk.ot-accordion-layout h4~.ot-always-active:before{border-radius:12px;position:absolute;right:0;top:0;content:'';background:#fff;border:2px solid #939393;box-sizing | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_622.txt | ="u-font-sans"><span class="author u-font-sans"><span>J. </span>Vander Auwera</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0012825211000584" target="_self"><span class="anchor-text">Sveconorwegian massif-type anorthosites and related granitoids result from post-col... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1384.txt | ":"label","_":"4.3"},{"#name":"title","$":{"id":"sect0050"},"_":"Xenolith-rich zones within the SMB"},{"#name":"entry","$":{"id":"sec0040","depth":"3"},"$$":[{"#name":"label","_":"4.3.1"},{"#name":"title","$":{"id":"sect0055"},"_":"Fine-grained, grey migmatitic gneiss"}]},{"#name":"entry","$":{"id":"sec0045","depth":"3... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1083.txt | -ref","$":{"id":"crf0190","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0035"},"$$":[{"#name":"given-name","_":"Matthew S.A."},{"#name":"surname","_":"Horstwood"},{"#name":"cross-ref","$":{"id":"crf0195","refid":"aff0010"},"$$":[{"#name":"sup","$":{"loc":"post"}... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_63.txt | ockite Zrn 1152 ±2 Kullerud and Machado, 1991
Levang granitic gneiss dome, Southern part Zrn 1167 ±50 O'Nions and Baadsgaard, 1971
Hovdefjell metacharnockite Zrn 1168 ±2 Råheim unpublished
Tromøy complex, Hisøy tonalite, HGG Zrn 1178 ±9 Andersen et al., 2004
Tromøy gneiss complex, 4 samples Zrn 1198 ±13 Knudsen and And... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_66.txt | pulses (1215-1224 and
ca. 1205 Ma) of bimodal magmatism along the Protogine Zone, S
Sweden. GFF 128, 303-310.
Söderlund, U., Elming, S.Å., Ernst, R.E. & Schissel, D. 2006: The Central Scandinavian Dolerite Group - Protracted hotspot activity or
back-arc magmatism? Constraints from U-Pb baddeleyite geochronology and Hf... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_129.txt | )("bst", [e[0], t, this.bstStart, (0, g.z)()], void 0, r.D.sessionTrace, n);
}), n.on(oe + ee, function (e) {
this.time = (0, g.z)(), this.startPath = location.pathname + location.hash;
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_64.txt | rheim, H. 2001b: Zircon U-Pb geochronology in the Bergen Arc eclogites and their Proterozoic protoliths,
and implications for the pre-Scandian evolution of the Caledonides
in western Norway. Geological Society of America Bulletin 113, 640-
649.
Bingen, B., Mansfeld, J., Sigmond, E.M.O. & Stein, H.J. 2002: Baltica–
Laur... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1243.txt | ","$$":[{"#name":"maintitle","_":"J. Metamorph. Geol."}]},{"#name":"volume-nr","_":"20"}]},{"#name":"date","_":"2002"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"727"},{"#name":"last-page","_":"740"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0180"},"$$":[{"#name":"label","_":"Möller et al., 2003"},{"#name... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_13.txt | obtained with a scanning electron microscope of all
crystals before U-Pb analysis (Fig. 6).
The SIMS analytical method, data reduction, error
propagation and assessment of the results are outlined
in Whitehouse et al. (1997, 1999). The analyses were
conducted with a spot size of ca. 30 µm, and calibrated
to the Geostan... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1182.txt | name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Falkum"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Sveconorwegian magmatic and tectonometamorphic evolution of the high grade Proterozoic Flekkefjord complex, south Norway"}]}]},{"#name":"host","$$":[{"#... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_69.txt | 1 T Mnz 939 ±20 Andersen et al., 2002 a
Tovdal granite T Zrn 940 ±10 Andersen et al., 2002 a
Bessefjell granite T Zrn 940 ±19 Andersen et al., 2002 a
Lyngdal granodiorite, La68A-Pa69K R Zrn 950 ±5 Pasteels et al., 1979
Holum granite, 98BN21D R Zrn 957 ±7 Bingen et al., submitted
Sæbyggjenut granite R Zrn 959 +50/-32 An... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1343.txt | ":"host","$$":[{"#name":"edited-book","$$":[{"#name":"editors","$$":[{"#name":"editor","$$":[{"#name":"given-name","_":"S.M."},{"#name":"surname","_":"Kay"}]},{"#name":"editor","$$":[{"#name":"given-name","_":"C.W."},{"#name":"surname","_":"Rapela"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Plutonism from An... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_77.txt | 3 Åhäll et al., 2008 Zrn 1540±32 Am Nord-Koster metapsamite U-Pb SIMS 1 Åhäll et al., 2008 Eastern Segment South Zrn 949 ±4 Am Interboudin pegmatite, Vistbergen, 7 U-Pb ID-TIMS 10 Connelly et al. 1996 South Zrn 954±21 Am Interboudin pegmatite, Tjärnesjö granite, DC9719 U-Pb SIMS 9 Andersson et | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_32.txt | ramatically westwards towards the hinterland of the
Sveconorwegian belt and peaked at 930-920 Ma with
intrusion of the Rogaland AMC Complex (Schärer et al.
1996) and the large Bohus and Flå plutons (Figs. 5, 6).
The surge of magmatism and associated high-temperature metamorphism (M2 in Rogaland-Vest Agder) may
be relat... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_596.txt | h4 u-margin-l-top u-margin-xs-bottom">Relationships between metamorphism and SMB magmatism</h2><p id="par0355">The metamorphic evolution of SW Norway has generally been ascribed to a ca. 1035–970<!-- --> <!-- -->Ma (Bingen et al., 2008a) regional event, followed by a younger, contact-metamorphic event related to e... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_4.txt | ongsberg sector is interpreted as an early-Sveconorwegian collision zone
between Telemarkia and the Idefjorden terrane.
Acknowledgements: SIMS data were produced at the NORDSIM
laboratory, operated and financed under an agreement between the
research councils of Denmark, Norway, and Sweden, the Geological
Survey of Fin... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_19.txt | of the Görbjörnarp
syenite in Skåne, southern Sweden. Geologiska Föreningens i Stockholm Förhandlingar 113, 335-337.
Harlov, D.E. 2000: Pressure-temperature estimation in orthopyroxene-garnet bearing granulite facies rocks, Bamble Sector, Norway.
Mineralogy and Petrology 69, 11-33.
Heaman, L.M. & Smalley, P.C. 1994: A... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_778.txt | lack of widespread metamorphic overprinting and common preservation of igneous textures in most of the SMB indicate that high-grade Sveconorwegian metamorphism after ca. 1020"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma was local rather than regional in SW Norway."}],"$":{"view":"all","id":"spar0020... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_90.txt | berg Morud metagrabbro Cpx SmNd 1224 ±15 Munz & Morvik, 1991
Bamble Nelaug gneiss Zrn U-Pb 1460 ±21 de Haas et al., 2002
Kongsberg Granodiorite gneiss, Veldstad, N95-66 Zrn U-Pb 1500 ±5 Bingen et al., 2005
Bamble Jomås granodiorite, 8/97 JOM Zrn U-Pb 1522 ±14 Andersen et al., 2004
K | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_152.txt | }, i.e = e => Promise.all(Object.keys(i.f).reduce((t, r) => (i.f[r](e, t), t), [])), i.u = e => "nr-spa.1097a448-1.238.0.min.js", i.o = (e, t) => Object.prototype.hasOwnProperty.call(e, t), e = {}, t = "NRBA-1.238.0.PROD:", i.l = (r | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_93.txt | ord granite Am Min. isochron 4 1009 ±10 Andersen et al., 2002
Rogaland-VA Tinn granite, 2 samples (071996-2 + 083196-2) Am Min. isochron 7 1031 ±32 Andersen et al., 2002
Vardefjell SZ Tonalitic banded gneiss, Flå, B99111 Am 207Pb/206Pb 2 985 ±16 Bingen et al., 2008
Vardefjell SZ Granodioritic banded gneiss, Flå | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_64.txt | 2007b) or a Basin and
Range setting (Bingen et al. 2003). The 1220-1130 Ma
magmatism is widespread in the Telemarkia Terrane but
totally absent in the Idefjorden Terrane. This difference
is compatible with a separation of the two terranes at
the onset of the Sveconorwegian orogeny. It also underscores the contrast bet... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_342.txt | .ot-acc-hdr.ot-tgl,#onetrust-pc-sdk ul.ot-subgrps.ot-acc-hdr.ot-tgl,#onetrust-pc-sdk.ot-subgrp-cntr ul.ot-subgrps.ot-acc-hdr.ot-tgl,#onetrust-pc-sdk.ot-vs-list.ot-vnd-item.ot-acc-hdr.ot-tgl,#onetrust-pc-sd | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_12.txt | of Norway, 7491 Trondheim, Norway (bernard.bingen@ngu.no).
44
day position, their exact location and linkage to pre-Caledonian Fennoscandia remains speculative.
The Sveconorwegian belt sensu stricto is the focus of
this paper. It is divided into five main lithotectonic units
separated by crustal scale shear zones (Fi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_374.txt | onetrust-pc-sdk.ot-switch.ot-toggle,
#onetrust-consent-sdk #onetrust-pc-sdk ot-grp-hdr1.checkbox,
#onetrust-consent-sdk #onetrust-pc-sdk #ot-pc-title:after
,# | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_63.txt | b 932 ±4 Andersen et al., 2007
Telemark Vrådal granite, 0816961 Mnz U-Pb 939 ±20 Andersen et al., 2002
Telemark Tovdal granite Zrn U-Pb 940 ±10 Andersen et al., 2002
Telemark Bessefjell granite Zrn U-Pb 940 ±19 Andersen et al., 2002
Rogaland Lyngdal granodiorite, La68A-Pa69K Zrn U-Pb 950 ±5 Pasteels et al., 1979
Rog | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_728.txt | ></div><div class="authors"><span>C.L.</span> <span>Kirkland</span>, …, <span>C.V.</span> <span>Spaggiari</span></div></div><div class="buttons"></div></li><li class="RelatedContentPanelItem u-display-block"><div class="sub-heading u-padding-xs-bottom"><h3 class="related-content-panel-list-entry-outline-padding text-s ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_124.txt | for (const e in this.features) this.features[e].abortHandler?.();
const n = (0, T.fP)();
return delete n.initializedAgents[this.agentIdentifier]?.api, delete n.initializedAgents[this.agentIdentifier]?.[t], delete this.sharedAggregator, n.ee?.abort(), delete n.ee?.get(this.agentIdent | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1281.txt | name":"last-page","_":"25"}]},{"#name":"doi","_":"10.1080/00206814.2014.958579"}]}]}]},{"#name":"bib-reference","$":{"id":"bib0240"},"$$":[{"#name":"label","_":"Roberts et al., 2013"},{"#name":"reference","$":{"id":"sbref0240","refId":"48"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_836.txt | Kulakov E.V., Slagstad T., Ganerød M., Torsvik T.H.","doi":"10.1016/j.precamres.2022.106786","externalArticle":false,"issn":"03019268","openAccess":1,"pii":"S0301926822002303","publicationDate":"2022-09-01","publicationTitle":"Precambrian Research","publicationYear":"2022","scopusArticleUrl":"http://www.scopus.com/scop... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_740.txt | ockite-granite) ferroan Farsund intrusion (SW Norway)</span></span></a></h3><div class="article-source u-clr-grey6"><div class="source">Precambrian Research, Volume 251, 2014, pp. 141-163</div></div><div class="authors"><span>Jacqueline</span> <span>Vander Auwera</span>, …, <span>Michel</span> <span>Bogaerts</span></di... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_564.txt | ="icon icon-cited-by-66"><path xmlns="http://www.w3.org/2000/svg" d="m2 58.78v47.22h44v-42h-34v-5.22c0-18.5 17.08-26.78 34-26.78v-1e1c-25.9 0-44 15.12-44 36.78zm1e2 -26.78v-1e1c-25.9 0-44 15.12-44 36 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_888.txt | conoritic margin of the anorthosite suggests that the deformation was linked to the 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 acros... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_186.txt | display: inline-block}
.MJXp-box {display: block!important; text-align: center}
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_12.txt | acrustal rocks exposed
in Suldal are coeval to marginally older than the ones
exposed in Sauda. An intensely deformed (strong lineation) granodioritic gneiss interlayered with metarhyolite
provides an age of 1519 ± 12 Ma (sample B00-140;
Tables 1, 5; Fig. 10D). The gneiss complex surrounding
the supracrustal rocks cons... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_75.txt | button-primary,#onetrust-pc-sdk button.ot-sdk-button-primary,#onetrust-pc-sdk input[type=submit].ot-sdk-button-primary,#onetrust-pc-sdk input[type=reset].ot-sdk-button-primary,#onetrust-pc-sdk input[type=button].ot-sdk-button-primary,#ot-sdk-cookie-policy.ot-sdk-button.ot-sdk-button-primary,#ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_4.txt | s.message = "Loading chunk " + t + " failed.\n(" + o + ": " + a + ")", s.name = "ChunkLoadError", s.type = o, s.request = a, n[1](s);
}
}, "chunk-" + t, t);
}
};
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_592.txt | to understand the regional geologic evolution, as SMB granitoids can be used as time markers. In the following section we describe in detail the nature of the host rocks and their contacts with the SMB, focusing on the western and southwestern part of the SMB.</p></section></section><section><section id="sec0100"><h2 ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_364.txt | width:100%}#onetrust-pc-sdk #ot-fltr-cnt{max-width:320px;width:90%;border-top-right-radius:0;border-bottom-right-radius:0;margin:0;margin-left:15px;left:auto;right:40px;top:85px}#onetrust-pc-sdk.ot-fltr-opt{margin-left:25px;margin-bottom:10px}#onetrust-pc-sdk.ot-pc | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_31.txt | data.user) {
if (Object.prototype.toString.call(data.user) === "[object Array]") {
window.eventData.user = data.user[0];
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_22.txt | (0, e.Z)("Downloading and initializing ".concat(this.featureName, " failed..."), t), this.abortHandler?.(), o(!1);
}
};
u.il? (0, f.b)(() => a(),!0) : a();
}
should | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_28.txt | maskAllInputs:!0,
get blockClass() {
return "nr-block";
},
get ignoreClass() {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1347.txt | "},{"#name":"last-page","_":"1162"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0350"},"$$":[{"#name":"label","_":"Whitney and Evans, 2010"},{"#name":"reference","$":{"id":"sbref0350","refId":"70"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"gi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_543.txt | -serif u-h2 u-margin-s-ver"><span class="title-text">The Late Mesoproterozoic Sirdal Magmatic Belt, SW Norway: Relationships between magmatism and metamorphism and implications for Sveconorwegian orogenesis</span></h1><div class="Banner" id="banner"><div class="wrapper truncated"><div class="AuthorGroups text-s"><div c... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_10.txt | itefacies conditions in the Rogaland-Vest Agder Sector. (3) At 980-970 Ma, the Falkenberg phase reflects final convergence in the belt, shortly followed
by divergence. Foreland propagationof the orogeny is indicated by underthrusting of the Eastern Segment to eclogites facies conditions at c. 970 Ma.
(4) Between 970 an... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_43.txt | derlund, U. 1997: Age constraints on the regional
deformation within the Eastern Segment, S Sweden: Late Sveconorwegian granite dyke intrusion and metamorphic deformational
relations. GFF 119, 1-12.
Möller, C. 1998: Decompressed eclogites in the Sveconorwegian (-
Grenvillian) orogen of SW Sweden: petrology and tectonic... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_11.txt | Zrn U-Pb 1555 ±3 Bingen et al., 2005
Rivöfjorden layered gabbro Zrn U-Pb 1555 ±2 Åhäll et al., 2000
Burö-Hällsö diorite Zrn U-Pb 1555 ±2 Connelly & Åhäll, 1996
Hisingen suite, Landvetter granodiorite Zrn U-Pb 1558 ±10 Åhäll & Connelly, 2008
Förö granite dyke Z | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_18.txt | component is
probable, in accordance with sinistral strike-slip relations
recorded in the Østfold-Marstrand Boundary zone, east
of the Oslo rift (Fig. 1; Hageskov 1985).
The high-pressure signature of metamorphism in the
Idefjorden Terrane (1.0-1.5 GPa) contrasts with the
medium-pressure signature of metamorphism in t... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_441.txt | ot-sdk-cookie-policy h6,.ot-sdk-cookie-policy p,.ot-sdk-cookie-policy li,.ot-sdk-cookie-policy a,.ot-sdk-cookie-policy th,.ot-sdk-cookie-policy #cookie-policy-description,.ot-sdk-cookie-policy.ot-sdk-cookie-policy-group,.ot-sdk-cookie-policy #cookie-policy-title{color:dimgray}.ot-sdk-cookie-policy #cookie-policy-descri... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_22.txt | a) : n || {};
} catch (t) {
u([t, "", [o, a, s], d], e);
}
i(r + "start", [o, a, s], d, c);
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1521.txt | ');
}
}
}
} catch (e) { }
}
,getMessages: function() {
return ['v1'].concat(this.warnings).join('|');
}
, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_25.txt | , 84083 Zrn U-Pb 1204 ±3 Söderlund & Ask, 2006
PZ Taberg ultramafic intrusion, leucogabbro A1 Ap U-Pb 1204 ±2 Larsson & Söderlund, 2005
PZ Rumperöd dolerite dyke Bdl U-Pb 1215 ±5 Söderlund et al., 2005
PZ Aplite dyke in Vaggeryd syenite, 19.2 Zrn U-Pb 1218 ±3 Söderlund | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_25.txt | 0.73 1522 27 1458 21 95.8
B00-147, garnet granite gneiss, Vanvik, Fig. 10I
7 0.0704 0.0035 1.72 0.09 0.177 0.003 0.32 941 102 1049 16 111.4
4 0.0745 0.0024 1.71 0.06 0.166 0.002 0.41 1056 65 991 13 93.9
2 0.0763 0.0020 1.85 0.06 0.176 0 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_36.txt | neiss, Visbergen, 4 Zrn U-Pb 1660 ±5 Connelly et al., 1996
Centre Metagranite, Karlstad, W1 Zrn U-Pb 1661 ±27 Söderlund et al., 1999
South Särdal orthogneiss, paleosome, 1 Zrn U-Pb 1664 ±7 Christoffel et al., 1999
South Migmatite granitic gneiss, Oxanäset, mesosome OX1 Zrn U-Pb 1668 ±11 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1057.txt | #name":"abstract-attachment","_":"true"},{"#name":"filename","_":"fx1.jpg"},{"#name":"extension","_":"jpg"},{"#name":"filesize","_":"48522"},{"#name":"pixel-height","_":"200"},{"#name":"pixel-width","_":"470"},{"#name":"attachment-type","_":"IMAGE-DOWNSAMPLED"}],"$":{"xmlns:xocs":true},"#name":"attachment"},{"$$":[{"#n... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_40.txt |
,registerCallbacks: function() {
var self = this;
if(window.usabilla_live) {
window.usabilla_live('setEventCallback', function(category, action, label, value) {
if(action == 'Campaign:Open') {
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_10.txt | the Geological
Society, London 160, 935-946.
Stacey, J.S. & Kramers, J.D. 1975: Approximation of terrestrial lead
isotope evolution by a two-stage model. Earth and Planetary
Science Letters 26, 207-221.
Starmer, I.C. 1985: The evolution of the south Norwegian Proterozoic
as revealed by the major and mega-tectonics of ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_116.txt | name && (i[e] = o), o;
}
},
50: (e, t, r) => {
function n(e, t) {
"function" == typeof console.warn && (console.warn("New Relic: ".concat(e)), t && console.warn(t));
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_29.txt | 1350 Ma (Fig. 4; Dons 1960; Bingen et al. 2001a; Laajoki et al. 2002; Andersen & Laajoki 2003; Corfu & Laajoki 2008). These rocks were intruded and unconformably overlain by several magmatic suites and sediments
between 1280 and 1130 Ma (Heaman & Smalley 1994;
Laajoki et al. 2002; Brewer et al. 2002; Bingen et al. 200... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1231.txt | surname","_":"Le Bas"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.A."},{"#name":"surname","_":"Sabine"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R."},{"#name":"surname","_":"Schmid"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H."},{"#name":"surname","_":"Sorensen"}]},{"#name":"author",... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_274.txt | bl-chr h4~.ot-tgl+.ot-tgl{right:120px}#onetrust-pc-sdk.ot-enbl-chr.ot-pli-hdr.ot-leg-border-color span:first-child{width:90px}#onetrust-pc-sdk.ot-enbl-chr li.ot-subgrp>h5+.ot-tgl-cntr{padding-right:25px}#onetrust-pc-sdk.ot- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_23.txt | . & Moorbath, S. 1999: Age significance
of U-Th-Pb zircon data from early Archaean rocks of west
Greenland - a reassessment based on combined ion-microprobe
and imaging studies. Chemical Geology 160, 201-224.
Wiedenbeck, M., Allé, P., Corfu, F., Griffin, W.L., Meier, M., Oberli, F.,
104 B. Bingen et al. NORWEGIAN JOURN... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_39.txt | if (!e) throw new Error("All loader-config objects require an agent identifier!");
if (!m[e]) throw new Error("LoaderConfig for ".concat(e, " was never set"));
return m[e];
}
function b(e, t) {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_967.txt | i0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$$":[{"#name":"__text__","_":"Musgrave magmatic rocks indicate 1950–1900"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma and 1600–1550"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma crust formation."}],"$":{"view":"all","id... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_38.txt | ", "formData"],
E = f._A.Request,
T = f._A.Response,
_ = "prototype";
const D = {};
function j(e) {
const t = function (e) {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_149.txt | .toGMTString();
}
var type = typeof(value);
type = type.toLowerCase();
if (type!= 'undefined' && type!='string') {
value = JSON.stringify(value);
}
// fix scoping issues
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_17.txt | ite-facies metamorphism) and 985 Ma (fabric-parallel
titanite; Bingen et al. 2008b). This timing is coeval with
high-grade metamorphism in the Telemarkia hanging
wall of the shear zone (1014 Ma), but post-dates exhumation of high-pressure rocks in the foot wall (1025 Ma).
The geometry along the Vardefjell Shear Zone is... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_154.txt | Cookie(name, '', -1, document.location.hostname);
}
,mapAdobeVars: function(s) {
var vars = {
pageName : 'Page - Analytics Pagename'
,channel : 'Page - Section Name'
,campaign : 'Campaign - ID | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_20.txt | of the
Sveconorwegian orogen, south-central Sweden. Precambrian
Research 79, 227-237.
Welin, E., Lindh, A. & Kähr, A.-M. 1981: The radiometric age of the
Proterozoic granite at Sandsjön, western Värmland, Sweden.
Geologiska Föreningens i Stockholm Förhandlingar 103, 514-518.
Welin, E., Gorbatschev, R. & Kähr, A.M. 198... |
Subsets and Splits
No community queries yet
The top public SQL queries from the community will appear here once available.