id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
value |
|---|---|---|
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_14.txt | : void 0
},
a = {};
function s(e) {
if (!e) throw new Error("All info objects require an agent identifier!");
if (!a[e]) throw new Error("Info for ".concat(e, " was never set"));
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_9.txt | if(data[x].hasOwnProperty(y)) {
pageData[x][y] = data[x][y];
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1108.txt | "},{"#name":"surname","_":"Charlier"},{"#name":"cross-ref","$":{"id":"crf0870","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0035","orcid":"0000-0002-1972-4098"},"$$":[{"#name":"given-name","_":"Jean Clair"},{"#name":"surname","_":"Duchesne"},{"#name":"cross-ref... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_86.txt | Moly: molybdenite, Zrn: zircon (3) Metamorphic facies: Am: amphibolite-facie, Gr: granulite-facies, Ecl: decompressed eclogite boudin (4) For Th-Pb ID-TIMS, the listed age is 208Pb/232Th age, equivalent to both 207Pb/235U and 206Pb/238U ages (5) n: number of analysed fractions Table 4. Compilation of monazite, zircon ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_9.txt | ite data (Hansen et al. 1989; Austin Hegardt et al.
2007). West of the Oslo rift, high-pressure amphibolitefacies conditions (1.0-1.2 GPa, 690-780 °C) are recorded
(Hensmoen locality; Fig. 8b; Bingen et al. 2008b). U-Pb
data define three age clusters for high-grade metamorphism at 1091 ±18 Ma (zircon rim), 1052 ±4 to 1... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_22.txt | terranes. The term has no connotation of
an exotic origin, but suggests significant transport. In
this context, we divide the Sveconorwegian orogen into
one parautochthonous segment, the Eastern Segment,
and two allochthonous terranes, the Idefjorden and
Telemarkia terranes (Figs. 1, 2). As discussed later in
this pap... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_935.txt | /or wrong usage of rock nomenclature on regional-scale maps (e.g., Falkum, 1982) and in the literature (e.g., Bingen and van Breemen, 1998b). It is not our intention to place the blame for this confusion on a few persons or studies, but rather point out that there appears to have been a common practice of labeling Prec... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1035.txt | -Lin"},{"#name":"surname","_":"Wu"},{"#name":"cross-ref","$":{"refid":"af005","id":"c0070"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"orcid":"0000-0002-0455-1016","id":"au010","author-id":"S0301926816300146-baf469150d4d0888b73ef128b74f5220"},"$$":[{"#name":"given-name"," | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_827.txt | ological behavior."}],"$":{"id":"o0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0020"},"#name":"para","_":"The majority of Sveconorwegian pegmatites is derived from anatectic melting."}],"$":{"id":"o0020"},"#name":"list-item"}],"$":{"id":"l0005"},"#name":"list"}],"$":{"view":"al... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_51.txt | ectonic
implications. Journal of Metamorphic Geology 16, 641-656.
Möller, C. 1999: Sapphirine in SW Sweden: a record of Sveconorwegian
(-Grenvillian) late-orogenic tectonic exhumation. Journal of
Metamorphic Geology 17, 127-141.
Nordgulen, Ø., Tucker, R.D., Sundvoll, B., Solli, A., Nissen, A.L.,
Zwaan, K. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_81.txt | h, A. & Johansson, L. 1998: U-Pb and
Sm-Nd dating of high-pressure granulite- and upper amphibolite
facies rocks from SW Sweden. Precambrian Research 92, 319-339.
Welin, E., Lindh, A. & Kähr, A.M. 1981: The radiometric age of the
Proterozoic granite at Sandsjön, western Värmland, Sweden. Geologiska Föreningens i Stockh... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_71.txt | 0.2470 2.23 0.98 1487 8 1423 29 95.7
14a 357 64 113 10872 0.09304 0.44 3.541 2.30 0.2760 2.26 0.98 1489 8 1571 32 105.5
01a 568 121 165 24426 0.09327 0.23 3.195 2.31 0.2484 2.30 1.00 1493 4 1430 30 95.8
02a 459 74 143 21464 0.09343 0.25 3.498 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1100.txt | transgressive sedimentation. This tectonic scenario represents a pre-Sveconorwegian stage of orogenesis that can be related to convergent margin processes. The surface expression of crustal growth during this time is relatively small; however, the volume of a postulated mafic underplate that accreted and intruded the ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_2.txt | This suggests that major displacement along the Protogine Zone and Sveconorwegian Frontal Deformation
Zone is lacking (Andréasson & Rodhe 1990).
Idefjorden Terrane
The Idefjorden Terrane (Fig. 1) is made up of 1660-1520
Ma mainly calc-alkaline and tholeiitic plutonic and volcanic rocks, associated with greywacke-bearin... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1096.txt | zircon age spectra implying derivation from a wide array of sources. The Morgedal and Gjuve formations have unimodal U-Pb age spectra, suggesting input from a single source and probably accumulation in restricted basins. The overlying Eidsborg Formation displays a wide range of detrital zircon age peaks indicative of ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_27.txt | most Sweden. Precambrian
Research 64, 361-388.
Johansson, L., Lindh, A. & Möller, C. 1991: Late Sveconorwegian
(Grenville) high-pressure granulite facies metamorphism in southwest Sweden. Journal of Metamorphic Geology 9, 283-292.
Johansson, L. & Johansson, Å. 1993: U–Pb age of titanite in the Mylonite Zone, southweste... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_110.txt | h = "spaNode",
p = "jsonpNode",
g = "fetch-start",
m = "fetch-done",
v = "fetch-body-",
b = "jsonp-end",
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1325.txt | ro-potassic A-type granitoids of southern Norway by extreme differentiation from basic magmas"}]}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Precambrian Res."}]},{"#name":"volume-nr","_":"124"}]},{"#name":"date","_":"2003"}]},{"#name":"pages... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_80.txt | , 1996 South Zrn 972±14 Ecl Zircon in garnet, eclogite boudin, Lilla Hammås,Ullared U-Pb SIMS 4 Johansson et al., 2001 South Moly 974±3 Ecl Felsic vein along eclogite boudin, Viared, VR1 Re-Os ID-NTIMS 1 Austin Hegardt et al., 2005 South Zrn 974±25 Am Garnet amphibolite, Ljungby, 8705 U-Pb ID-T | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_859.txt | wegian Orogen. Earlier studies suggest that the RAP was emplaced over 1–3 Myr around 930 Ma towards the end of orogenesis, resulting in an up to 15–20 km-wide contact metamorphic aureole. However, our structural observations show that the RAP is located in the footwall of a 15 km-wide extensional detachment (Rogaland E... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_434.txt | :66px!important;max-width:none!important;width:calc(100% - 5px)!important;transform:translate(2px,2px)}div#onetrust-pc-sdk.ot-host-item{border-bottom:2px solid #b9b9b9;padding:0}div#onetrust-pc-sdk.ot-host-item.ot-acc-hdr{margin:0 0 -6px;padding:8px 0}div#onetrust-pc-sdk ul | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1010.txt | sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"2"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma) and the Huanchaca mafic suite (1112"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"±"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"2"},{"$":{"sp":"0.25"},"# | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1469.txt | 0 444.531 444.531" xml:space="preserve"><title>Back Button</title><g><path fill="#656565" d="M213.13,222.409L351.88,83.653c7.05-7.043,10.567-15.657,10.567-25.841c0-10.183-3.518-18.793-10.567-25.835
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_780.txt | ":[]},"accessbarConfig":{"fallback":false,"id":"accessbar","version":"0.0.1","analytics":{"location":"accessbar","eventName":"ctaImpression"},"ariaLabel":{"accessbar":"Download options and search","componentsList":"PDF Options"},"banner":{"id":"Banner"},"banners":[{"id":"Banner"},{"id":"BannerSsrn"}],"components":[{"an... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_53.txt | } catch (t) {
return e.reason;
}
if (void 0 === e.reason) return new I(t);
const r = this.#t(e.reason);
return r.message = t + r.message, r;
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_7.txt | 0.08 0.264 0.003 0.50 1501 39 1508 16 100.5
6 0.0938 0.0007 3.20 0.04 0.247 0.003 0.83 1504 13 1424 13 94.7
8 0.0941 0.0007 3.45 0.04 0.266 0.003 0.78 1510 14 1521 13 100.8
14 0.0943 0.0018 3.29 0.08 0.253 0.004 0.63 1513 36 1455 20 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_27.txt | }
this.importAggregator();
}
}
var v = i(1117),
b = i(1284);
class y extends v.w {
constructor(e) {
super(e), this.aggregatedData = {};
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_127.txt | static featureName = re;
constructor(e, t) {
if (super(e, t, re,!(arguments.length > 2 && void 0!== arguments[2]) || arguments[2]),!u.il) return;
const n = this.ee;
let i;
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_66.txt | ite.
116 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Table 10. Selection of U-Pb dates on magmatic events in Telemarkia
Lithology, Sample Mineral - Age Reference
(1) (2) (Ma)
Rymteland pegmatite R Urn 914 ±6 Pasteels et al., 1979
Egersund-Ogna anorthosite, margin 75-32 R Bdl 915 ±4 Schärer et al., 1996
Vehuskjerringa... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_89.txt | merch.push('evar111=' + this.stripProductDelimiters(prodList[i].previousStatus));
}
if (prodList[i].entitlementType) {
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_48.txt | Zone
(2) Ap: apatite, Bdl: baddeleyite, Cpx: clinopyroxene, Mnz: monazite, Moly: molybdenite, Ttn: titanite, Urn: uraninite, Zrn: zircon
Table 3. Compilation of geochronological data on magmatic events in the Sveconorwegian belt.
53
Fennoscandia foreland
The Fennoscandia foreland of the Sveconorwegian belt
(Fig. 1) | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1353.txt | 1086/648273"},{"refId":5,"scopusHubEid":"2-s2.0-0036026109"},{"refId":6,"scopusHubEid":"2-s2.0-54349105450"},{"refId":7,"scopusHubEid":"2-s2.0-54049110101"},{"refId":8,"scopusHubEid":"2-s2.0-20844441259"},{"refId":9,"scopusHubEid":"2-s2.0-336 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1277.txt | sp":"0.25"}},{"#name":"__text__","_":"Ga Fjellhovdane rhyolite Grossae-Totak; a new age within the Telemark supracrustals, southern Norway"}]}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nor. J. Geol."}]},{"#name":"volume-nr","_":"91"}]},{"#n... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_11.txt | lique (sinisB. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Fig. 10. Cumulative probability curves of detrital zircon
data in clastic sediment
sequences of the Telemarkia,
Bamble, Kongsberg and Idefjorden Terranes. Data from
Knudsen et al. (1997b), Åhäll
et al. (1998), de Haas et al.
(1999) Bingen et al. (2001a;
2002; 20... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_907.txt | the gradual transition from Telemarkian to Gothian crust. These Precambrian crustal heterogeneities largely controlled the development of Caledonian shear zones. The ca. 1050–1040 Ma granitic and mafic magmas show similar isotopic signatures with slightly negative or positive εHf(t) and moderate δ"},{"$":{"loc":"post"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1523.txt | .measures[attr];
}
}
this.measures = {};
return copy;
}
,dtmCodeDesc: {
dtm1:'satellite-lib must be placed in the <head> section',
dtm2: 'trackPageLoad() must be placed and called before the closing | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_497.txt | 0-4.89-1.95-4.89-5.51v-0.49H145.87M137.72 9.18c0.17-0.17 1.29-0.46 1.98-0.46 2.48 0 3.76 0.53 3.86 3.43h-7.46C136.37 10.27 137.52 9.37 137.72 9.18zM153.23 9.01c0.23-0.13 0.69-0.26 1. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1105.txt | ":"aut0010"},"$$":[{"#name":"given-name","_":"Olivier"},{"#name":"surname","_":"Bolle"},{"#name":"cross-ref","$":{"id":"crf0850","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0015"},"$$":[{"#name":"given-name","_":"Alain"},{"#name":"surname","_":"Dupont"},{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_77.txt | if (prodList[i].title) {
merch.push('evar75=' + this.stripProductDelimiters(prodList[i].title.toLowerCase()));
}
if ( | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_485.txt | 85 0.89 0 1.68-0.96 1.68-1.88C32.35 1.55 31.56 0.7 30.67 0.7M48.06 14.13c0-5.18-1.42-7.56-6.01-7.56 -3.86 0-6.67 2.77-6.67 7.92 0 4.92 2.97 7.82 6.73 7.82 2.81 0 4.36-0.63 5.68-1.42 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_55.txt | rmarka granodiorite, TA121 Zrn 1517 ±12 Andersen et al., 2004
Röseskär felsic dyke Zrn 1553 ±2 Connelly and Åhäll, 1996
Rivöfjorden layered gabbro Zrn 1555 ±2 Åhäll et al., 2000
Burö-Hällsö diorite Zrn 1555 ±2 Connelly and Åhäll, 1996
Förö granite dyke Zrn 1558 ±3 Åh | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_201.txt | 0s;border-radius:20px}#onetrust-pc-sdk.ot-switch-nob:before{position:absolute;content:"";height:18px;width:18px;bottom:3px;left:3px;background-color:#fff;-webkit-transition:.4s;transition:.4s;border-radius:20px}#onetrust-pc-sdk.ot-chkbox input:checked~label::before{background-color:#3860be}#onetrust-pc- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_92.txt | t.on("fn-end", function (e) {
e[0] && e[0].type === d || w();
});
function w() {
for (var e = 0; e < h.length; e++) g(0, h[e]);
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_247.txt | :none;color:#fff}#onetrust-pc-sdk.ot-chkbox input[type=checkbox]:checked+label::after{content:""}#onetrust-pc-sdk.ot-chkbox input[type=checkbox]:focus+label::before{outline-style:solid;outline-width:2px;outline-style:auto}#onetrust-pc-sdk #ot-selall-vencntr,#onetrust-pc-sdk #ot-selall-ad | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_259.txt | -cnt) #ot-sel-blk.ot-vnd-list-cnt{border:unset;background-color:unset}#onetrust-pc-sdk.ot-addtl-vendors #ot-lst-cnt:not(.ot-host-cnt) #ot-sel-blk.ot-vnd-list-cnt.ot-sel-all-hdr{display:none}#onetrust-pc-sdk.ot-addtl-vendors #ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_179.txt | rust-pc-sdk #ot-addtl-venlst.ot-arw-cntr,#onetrust-pc-sdk #ot-addtl-venlst.ot-plus-minus,#onetrust-pc-sdk.ot-hide-tgl{visibility:hidden}#onetrust-pc-sdk #ot-addtl-venlst.ot-arw-cntr *,#onetrust-pc-sdk #ot-addtl-venlst.ot-plus- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_60.txt | from
Precambrian to the post-Hercyninan sedimentary basins, 108, 5-21.
Mémoires du B.R.G.M., Paris.
Bingen, B., Demaiffe, D., Hertogen, J., Weis, D. & Michot, J. 1993: Krich calc-alkaline augen gneisses of Grenvillian age in SW Norway:
mingling of mantle-derived and crustal components. Journal of
Geology 101, 763-778.... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_33.txt | end of the Sveconorwegian
orogenic cycle (Bingen et al. 2006).
Conclusions
The Sveconorwegian orogeny is bracketed between 1140
and 900 Ma. Division of the Sveconorwegian orogeny into four genetic orogenic phases is a step towards
improved correlation of the Sveconorwegian belt with
other Grenvillian belts, and improv... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_64.txt | elaug gneiss Zrn 1460 ±21 de Haas et al., 2002
Jomås granodiorite, JOM Zrn 1522 ±14 Andersen et al., 2004
Bingen metadacite gneiss, 01/19 Zrn 1529 ±7 Andersen et al., 2004
Snarum granodiorite, HFG Zrn 1534 +9/-8 Andersen et al., 2004
Flosta charnockitic gneiss Zrn 1542 ±8 Kullerud and Machado, 1991
Justøy tonal | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_155.txt | '
,currencyCode : 'Page - Currency Code'
,purchaseID : 'Order - ID'
,prop1 : 'Visitor - Account ID'
,prop2 : 'Page - Product Name'
,prop4 : 'Page | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_59.txt | massif-type anorthosites. Nature 405, 781-784.
Sigmond, E.M.O. 1985: The Mandal-Ustaoset line, a newly discovered major fault zone in south Norway. In Tobi, A.C. & Touret,
J.L. (eds.), The deep Proterozoic crust in the north Atlantic provinces,
C158, 323-331. Reidel, Dordrecht.
Sigmond, E.M.O. 1998: Geologisk kart ove... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_989.txt | ":"postal-code","_":"66075-110"},{"#name":"country","_":"Brazil"}]}]},{"#name":"affiliation","$":{"id":"aff0020"},"$$":[{"#name":"label","_":"d"},{"#name":"textfn","_":"Departamento de Geologia Geral, Universidade Federal de Mato Grosso, Cuiabá, MT 78060-900, Brazil"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_273.txt | }#onetrust-pc-sdk #clear-filters-handler:hover{color:#2285f7}#onetrust-pc-sdk #clear-filters-handler:focus{outline:#000 solid 1px}#onetrust-pc-sdk.ot-enbl-chr h4~.ot-tgl,#onetrust-pc-sdk.ot-enbl-chr h4~.ot-always-active{right:45px}#onetrust-pc-sdk.ot-en | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_139.txt | };
}
};
function A(e, t, r, i) {
return function () {
return (0, o.p)(f.xS, ["API/" + t + "/called"], void | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1219.txt | #name":"maintitle","_":"How long-lived is ultrahigh temperature (UHT) metamorphism? Constraints from zircon and monazite geochronology in the Eastern Ghats orogenic belt, India"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Precambrian Res."}]... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1484.txt | id="ot-selall-licntr"><input id="select-all-vendor-leg-handler" type="checkbox"> <label for="select-all-vendor-leg-handler"><span class="ot-label-txt">checkbox label</span></label> <span class="ot-label-status">label</span></div></div></div></div><div class="ot-sdk-row"><div class="ot-sdk-column"><ul id="ot-host-lst">... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_37.txt | clastic
sediments (Eidsborg Formation, Heddal Group and the
Kalhovd Formation; Fig. 8a). The timing of low-grade
metamorphism in the central part of the Telemark Sector is poorly known. A 1031 ±32 Ma mineral Pb-Pb
isochron reflects isotopic homogenisation during this
event (Andersen et al. 2002c). Towards the northeas... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_21.txt |
Aggregate: r
} = await e(this.featureName, "aggregate");
this.featAggregate = new r(this.agentIdentifier, this.aggregator, t), o(!0);
} catch (t) {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_671.txt | ia may have resided at broadly similar latitudes between 1000 and 900 Ma, there is no geologic and paleomagnetic evidence for placing them next to each other.</p></div></div></div></li><li class="ListArticleItem u-margin-l-bottom"><div class="sub-heading u-margin-xs-bottom"><h3 class="u-font-serif" id="citing-arti... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_211.txt | 0s;-webkit-transition:all 300ms ease-in 0s;-moz-transition:all 300ms ease-in 0s;-o-transition:all 300ms ease-in 0s}#onetrust-pc-sdk.ot-vlst-cntr{margin-bottom:0}#onetrust-pc-sdk.ot-hlst-cntr{margin-top:5px;display:inline-block;width:100%}#onetrust-pc-sdk.category- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1398.txt | ","$":{"id":"sect0190"},"_":"Implications for the Sveconorwegian Province"}]}]},{"#name":"entry","$":{"id":"sec0170","type":"sections","depth":"1"},"$$":[{"#name":"label","_":"9"},{"#name":"title","$":{"id":"sect0195"},"_":"Conclusions"}]},{"#name":"entry","$":{"id":"ack0005","type":"acknowledgment","depth":"1"},"$$":[... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_117.txt | nern, they define
a fan-like structure with predominant normal movement
(top down to-the-east) along the Protogine Zone and
later reverse movement to the east along the Sveconorwegian Frontal Deformation Zone (Wahlgren et al. 1994;
Juhlin et al. 2000). Muscovite 40Ar/39Ar plateau ages from
ductile shear zones range fro... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1436.txt | );
if (shouldSetOTDefaults) {
const date = new Date();
date.setFullYear(date.getFullYear() + 1);
document.cookie = `OptanonAlertBoxClosed=${new Date().toISOString()}; expires=${date.toUTCString()}; samesite=lax; path=/; domain=sciencedirect.com`;
}
observeOneTrustLoaded(shouldSetOTDefaults, isConsentP... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_691.txt | button-link-icon-right" type="button" data-aa-button="sd:product:journal:article:location=citing-articles:type=view-details" aria-describedby="citing-articles-article-4-title" aria-controls="citing-articles-article-4" aria-expanded="false"><span class="button-link-text">Show abstract</span><svg focusable="false" viewB... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1428.txt | ) {
const oneTrustConsentSdkId = 'onetrust-consent-sdk';
const emptyNodeSelectors = 'h3.ot-host-name, h4.ot-host-desc, button.ot-host-box';
const ariaLabelledByButtonNodes = 'div.ot-accordion-layout > button';
const ariaAttribute = 'aria-labelledby';
function adjustOneTrustDOM() {
const oneTrustRoot = doc... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_5.txt | outlined by Tucker et al.
(1999). The analyses were done on non-magnetic, clear,
crystals, abraded before dissolution (Table 2). Zircon
from four samples was analysed by secondary ion mass
spectrometry (SIMS) using the CAMECA IMS 1270
instrument at the NORDSIM laboratory, Swedish
Museum of Natural History, Stockholm (... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_18.txt | if (r) {
const {
setupAgentSession: e
} = await i.e(111).then(i.bind(i, 3228));
n = e(this.agentIdentifier);
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_39.txt | �häll, K.I., Persson, P.O. & Skiöld, T. 1995: Westward accretion of the
Baltic Shield: implications from the 1.6 Åmål-Horred Belt, SW
Sweden. Precambrian Research 70, 235-251.
Åhäll, K.I., Samuelsson, L. & Persson, P.O. 1997: Geochronology and
stuctural setting of the 1.38 Ga Torpa granite; implications for
charnockite | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_410.txt | grow:1;width:auto}div#onetrust-banner-sdk #onetrust-policy,div#onetrust-banner-sdk.ot-bnr-flift #onetrust-policy{margin:0;overflow:visible}div#onetrust-banner-sdk.ot-bnr-flift #onetrust-policy-text,div#onetrust-consent-sdk #onetrust-policy-text{font-size:16px;line-height:24px;max-width:44 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_687.txt | duration from a few tens of million years up to around hundred million years, with intervening troughs of comparable length. Some magmatic peaks are observed on multiple cratons, either by coincidence or because of paleogeographic proximity and common tectonic setting, while others are not. The best overall correlatio... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_24.txt | tectonic units.
The Kristiansand-Porsgrunn Shear Zone forms the
boundary between the Bamble and Telemarkia Terranes
(Fig. 1). It dips to the southeast and is interpreted as a
Sveconorwegian thrust zone reworked as an extensional
detachment (Starmer 1991; Henderson & Ihlen 2004;
Mulch et al. 2005). Thrusting is associa... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_589.txt | usage of rock nomenclature on regional-scale maps (e.g., Falkum, 1982) and in the literature (e.g., Bingen and van Breemen, 1998b). It is not our intention to place the blame for this confusion on a few persons or studies, but rather point out that there appears to have been a common practice of labeling Precambrian f... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1082.txt | 25"},"$$":[{"#name":"given-name","_":"Anthony R."},{"#name":"surname","_":"Prave"},{"#name":"cross-ref","$":{"id":"crf0185","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0030"},"$$":[{"#name":"given-name","_":"Afra S.M."},{"#name":"surname","_":"Antonini"},{"#na... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_48.txt | p");
}(e);
if (!f.il || P[t.debugId]) return t;
P[t.debugId] =!0;
var r = c(t),
i = /[?&](?:callback|cb)=([^&#]+)/ | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_53.txt | 1460-1380
Ma granite dykes and plutons and 1250-1200 Ma granite plutons (Fig. 7; Andersson et al. 1999; Söderlund et
al. 2004; Larsson & Söderlund 2005; Söderlund & Ask
2006). A pre-Sveconorwegian 1460-1410 Ma amphibolite-facies metamorphic event, known as the Hallandian,
is recorded by metamorphic zircon and characte... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1372.txt | 126c94&pid=1-s2.0-S0301926812002938-main.pdf"}},{"refId":34,"pii":"S0301926807001635","filesize":"6MB","pdf":{"urlType":"download","url":"/science/article/pii/S0301926807001635/pdfft?md5=b1f71596268cca7df46fc2ec59835f8e&pid=1-s2.0-S0301926807001635-main | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_38.txt | and genetically linked
from the start and were part of a single piece of continent
at the onset of the Sveconorwegian orogeny. We propose
the name Telemarkia for this piece of continent. The
widespread occurrence of Palaeoproterozoic and Archaean detrital zircons in sediment sequences associated with,
or covering, the... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_814.txt | ":"sup","$":{"loc":"post"},"_":"c"}]}]},{"#name":"affiliation","$":{"id":"aff0005"},"$$":[{"#name":"label","_":"a"},{"#name":"textfn","_":"Geological Survey of Norway, 7491 Trondheim, Norway"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Geological Survey of Norway"},{"#name":"city","... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1515.txt | this.warnings.push('dv13');
}
if(data.visitor && data.visitor.accountId && data.visitor.accountId.indexOf(':') == -1) {
this.warnings.push('dv14');
data.visitor.accountId = "data violation"
}
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_38.txt | return e;
}(t) : t? (t.c || (t = A(t.t)), t.c += 1, t.t += e, t.sos += e * e, e > t.max && (t.max = e), e < t.min && (t.min = e), t) : {
t: e
};
}
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_32.txt | 800 Bt, Amp, Ttn ID-TIMS 4 4 U.I. 1492 3 intrusion 8E
Uvdal Rjukan gp metarhyolite weak S93-305 493200 6678900 Bt, Ms ID-TIMS 5 5 U.I. 1512 10 extrusion 8D
Suldal sector
Suldal Suldal augen gneiss medium B00-144 361332 6598990 Bt, Ttn, Ep LA-ICPMS 12 11 0.41 1018 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_62.txt | ±6 Gr Augen gneiss, Liland, B195 U-Pb ID-TIMS 2 Bingen & van Breemen, 1998
Rogaland-VA Mnz 997±1, 986±2, 985±1, 972±1 Gr Charnockitic gneiss, Vikeså, B650 U-Pb ID-TIMS 4 Bingen & van Breemen, 1998
Rogaland-VA Zrn 1001±18, 981±3, 963±3, 927±7, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_22.txt | berg Terrane, data from the quartzite-rich Modum Complex include a zircon U-Pb age at
1102 ±28 Ma, a molybdenite Re-Os age at 1112 ±4 Ma in
a cobalt ore, a monazite U-Pb age at 1092 ±1 Ma, and a
titanite age at 1080 ±3 Ma recording hydrothermal activity in an albitite (Fig. 4; Munz et al. 1994; Bingen et al.
2001a; Bin... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1504.txt | Data) {
var idPlusFields = ['userId', 'accessType', 'accountId', 'accountName'];
for(var i=0; i < idPlusFields.length; i++) {
if(typeof data.visitor.idPlusData[idPlusFields[i]]!== 'undefined') {
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_730.txt | IMS U–Pb baddeleyite ages (1110–1112<!-- --> <!-- -->Ma) for the Rincón del Tigre–Huanchaca large igneous province (LIP) of the Amazonian Craton: Implications for the Rodinia supercontinent</span></span></a></h3><div class="article-source u-clr-grey6"><div class="source">Precambrian Research, Volume 265, 2015, pp.... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1445.txt | -react-modal"></div><div class="js-react-modal"></div><iframe id="ps_dcqdwf" src="https://service.seamlessaccess.org/ps/" style="display: none; position: absolute; top: -999px; left: -999px;"></iframe><div id="onetrust-consent-sdk"><div class="onetrust-pc-dark-filter ot-hide ot-fade-in" style="display: none;
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_158.txt | ,prop24 : 'Page - Language'
,prop25 : 'Page - Product Feature'
,prop28 : 'Support - Search Criteria'
,prop30 : 'Visitor - IP Address'
,prop33 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_52.txt | cl,c,eu,pr 10 52.9 201 2 0.30 13606 0.09300 6 3.31634 535 0.25863 42 1487.8 1.2
2 5gr,-75,cl,c,eu,pr,i 9 53.4 202 1 0.31 20995 0.09303 6 3.32410 484 0.25915 38 1488.5 1.2
3 1gr,+75,cl,c,pr,i 10 52.9 201 1 0.30 32517 0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1498.txt |
return false;
}
if (event) {
this.initWarnings();
if(event === 'newPage') {
// auto fillings
if(data && data.page | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_2.txt | === 'undefined') {
expire = 86400;
}
console.log('You just enabled debug mode for Adobe Analytics tracking. This mode will persist for 24h.');
console.log("This mode can be disabled by calling 'pageDataTracker.disableDebug()'");
this.setCookie(this.debugCookie, 'true', expir... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_210.txt | all 300ms ease-in 0s;height:10px;width:10px}#onetrust-pc-sdk input:checked~.ot-acc-hdr.ot-arw{transform:rotate(90deg);-o-transform:rotate(90deg);-ms-transform:rotate(90deg);-webkit-transform:rotate(90deg)}#onetrust-pc-sdk.ot-arw{width:10px;margin-left:15px;transition:all 300ms ease-in | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_893.txt | _":"Highly strained norito-granitic gneisses in contact with an anorthosite diapir."}],"$":{"id":"li0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0010"},"#name":"para","_":"A high-alumina basalt is confirmed as the parent magma of labradorite anorthosite."}],"$":{"id":"li0010"},... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_514.txt | 97 28.88s4.25 21.17 11.97 28.88c7.71 7.71 17.97 11.96 28.88 11.96 9.23 0 17.98-3.07 25.13-8.68l26.32 26.32 7.03-7.03"></path></svg></a><a class="link-button link-button-small search-button-outline link-button-primary link-button-icon-right" href="/search" data-aa-button="search-in- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_84.txt | Botsvatn Co, Bykle, granite gneiss, B02027 Zrn U-Pb 1499 ±12 Bingen et al., 2005
Suldal Augen gneiss, Sand, B00-137 Zrn U-Pb 1501 ±11 Bingen et al., 2005
Telemark Rjukan Gp, Myrstul rhyolite dyke Zrn U-Pb 1502 ±1 Dahlgren et al., 1990
Suldal Granite, Aurdal, R94-66 Zrn U-P | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_94.txt | if (prodList[i].detail) {
merch.push('evar104=' + this.stripProductDelimiters(prodList[i].detail.toLowerCase()));
} else if(prodList[i].details) {
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_8.txt | Telemark Sector (Heddal Group, Eidsborg Formation, Kalhovd Formation;
Fig. 8a; de Haas et al. 1999; Bingen et al. 2003) possibly
represents a foreland or intramontane basin related to
mountain building and tectonic denudation of the Bamble and Kongsberg wedges. The 1080-1050 Ma time span
following unroofing of the Bam... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_16.txt | pegmatites and
990-920 Ma post-collisional granite plutons (Baadsgaard
et al. 1984; Kullerud & Dahlgren 1993; Andersen et al.
2002a; Knudsen & Andersen 1999; Andersen et al. 2004a).
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
60
Geophysical data suggest that the Bambl... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_46.txt | DZ Järna granite Zrn U-Pb 1786 +14/-12 Persson, in Söderlund et al., 1999
SFDZ Venjan porphyry, St. Kullsberget, TL9402 Zrn U-Pb 1792 +10/-8 Lundqvist & Persson, 1999
SFDZ Quartz-feldspar porphyry, L. Digerliden, TL9401 Zrn U-Pb 1795 ±4 Lundqvist & Persson, 1999
SFDZ Granite locally | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_31.txt | 9 4.056 1.9 0.2855 1.6 0.87 1619 23 1680 17 3.6
13p 6746 0.10381 0.8 4.106 1.5 0.2868 1.2 0.82 1626 17 1693 15 4.0
24 15160 0.10370 1.1 4.111 1.9 0.2875 1.5 0.81 1629 22 1691 20 3.7
07 10538 0.10330 0.9 4.105 1.7 0.28 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_923.txt | class=\"anchor u-display-inline anchor-alternative\" href=\"https://service.elsevier.com/app/phone/supporthub/publishing\" target=\"_blank\"><span class=\"anchor-text\">contact our Researcher support team.</span></a></p></div>","title":"What do these dates mean?"}},"glossary":{},"issueNavigation":{"previous":{},"next"... |
Subsets and Splits
No community queries yet
The top public SQL queries from the community will appear here once available.