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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1262.txt | _":"Formation and transfer of stoped blocks into magma chambers: the high-temperature interplay between focused porous flow, cracking, channel flow, host-rock anisotropy, and regional deformation"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1273.txt | author","$$":[{"#name":"given-name","_":"D."},{"#name":"surname","_":"Young"}]},{"#name":"author","$$":[{"#name":"given-name","_":"N.M.W."},{"#name":"surname","_":"Roberts"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Tectono-metamorphic evolution of the Jomolhari massif: variations in timing of syn-collisiona... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_56.txt | esdalen
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_808.txt | ":[{"#name":"author-group","$":{"id":"aug0005"},"$$":[{"#name":"author","$":{"id":"aut0005"},"$$":[{"#name":"given-name","_":"N."},{"#name":"surname","_":"Coint"},{"#name":"cross-ref","$":{"id":"crf0125","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]},{"#name":"cross-ref","$":{"id":"crf0130","refi... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_41.txt | K.I., Cornell, D.H. & Armstrong, R. 1998: Ion probe zircon
dating of metasedimentary units across the Skagerrak: new constraints for early Mesoproterozoic growth of the Baltic Shield. Precambrian Research 87, 117-134.
Åhäll, K.I. & Schöberg, H. 1999: The 963 Vinga intrusion and postcompressional deformation in the Sve... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1151.txt | #name":"surname","_":"Liegeois"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Timing of continental building in the Sveconorwegian orogen, SW Scandinavia"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nor. J. Geol."}]},{"#name":"volume... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1309.txt | ":"Weijermars"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.R."},{"#name":"surname","_":"Cruden"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Left-lateral transpressive deformation and its tectonic implications, Sveconorwegian orogen, Baltic Shield, southwestern Sweden"}]}]},{"#name":"host","$$":[{"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_921.txt | \">Available online</span>: The date a version of the article was made available online in the journal.</li><li><span class=\"u-text-italic\">Version of Record</span>: The date the finalized version of the article was made available in the journal.</li></ul><p>More information on publishing policies can be found on the... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1487.txt | -scrn-rdr" aria-atomic="true" aria-live="polite">Your Privacy [`dialog closed`]</span><!-- Vendor Service container and item template --></div><iframe class="ot-text-resize" sandbox="allow-same-origin" title="onetrust-text-resize" style="position: absolute; top: -50000px; width: 100em;" aria-hidden="true"></iframe></di... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_67.txt | b data on zircon from orthogneiss and metarhyolite samples Concentrations Atomic ratios Ages Sample/ U Th Pb 206Pb 207Pb ±σ 207Pb ±σ 206Pb ±σ rho 207Pb ±σ 206Pb ±σ Disc. analysis 204Pb 206Pb 235U 238U 206Pb 238U (ppm) (ppm) (ppm) (%) (%) (%) (Ma) (Ma) (%) (1) (2) (2) (2) (3) (4) J482A | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_662.txt | sup>Ar geochronology of Meso-Neoproterozoic rocks from southwest Norway. Implications for magnetic remanence ages and the paleogeography of Baltica in a Rodinia supercontinent context</span></a></h3><div class="text-s">2022, Precambrian Research</div></div><div class="buttons text-s"><button class="button-link butto... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_46.txt | -t path of the Modum Complex, South Norway. Lithos
24, 181-200.
Munz, I.A. & Morvik, R. 1991: Metagabbros in the Modum Complex,
southern Norway: an important heat source for Sveconorwegian
metamorphism. Precambrian Research 52, 97-113.
Munz, I.A., Wayne, D. & Austrheim, H. 1994: Retrograde fluid infiltration in the hig... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_12.txt | & von Quadt, A. (eds.), The timing and
location of major ore deposits in an evolving orogen. Geological
Society, London, Special Publications 204, 319-335.
Stephens, M.B., Wahlgren, C.H., Weijermars, R. & Cruden, A.R. 1996:
Left lateral transpressive deformation and its tectonic implications,
Sveconorwegian Orogen, Ba... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1229.txt | "},{"#name":"reference","$":{"id":"sbref0165","refId":"33"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"R.W."},{"#name":"surname","_":"Le Maitre"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P."},{"#name":"surname","_":"B... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1305.txt | name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Terra Nova"}]},{"#name":"volume-nr","_":"25"}]},{"#name":"date","_":"2013"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"30"},{"#name":"last-page","_":"37"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0285"},"$$":[{"#name":"label","_":"Spea... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1283.txt | },{"#name":"surname","_":"Norry"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Marker"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M.S.A."},{"#name":"surname","_":"Horstwood"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Sedimentary recycling in arc magmas: geochem... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1247.txt | comment","_":"(special publications)"}]}]},{"#name":"bib-reference","$":{"id":"bib0185"},"$$":[{"#name":"label","_":"Möller et al., 2013"},{"#name":"reference","$":{"id":"sbref0185","refId":"37"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-n... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_4.txt | ; Ebbing et al. 2005), containing lithologies characteristic of
both the Telemarkia and Idefjorden Terranes (Fig. 6).
The succession of pre- to early-Sveconorwegian events
in the Sveconorwegian belt can be integrated in a tentative geotectonic scenario (Figs. 8a, 9), compatible with
both an exotic or indigenous origin ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_82.txt | m(e), d = c.length, l = 0; l < d; l++) c[l].apply(a, r);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_930.txt | wegian orogen. We focus on primary observations, i.e., field data and cross-cutting relationships, that provide first order constraints on the orogenic evolution. The new data reveal a more complex history for this part of the Sveconorwegian orogen, with several geographically overlapping events of different character ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_493.txt | 93 1.98 103.9 1.98M103.14 19.8h-3.76V4.1h4.09c5.38 0 6.96 4.39 6.96 7.79C110.43 16.87 108.19 19.8 103.14 19.8zM118.38 0.7c-0.92 0-1.65 0.92-1.65 1.81 0 0.93 0.76 1.85 1.65 1.85 0.89 0 1.69-0. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_28.txt | Förhandlingar 115, 1-7.
Johansson, L., Möller, C. & Söderlund, U. 2001: Geochronology of
eclogite facies metamorphism in the Sveconorwegian Province of
SW Sweden. Precambrian Research 106, 261-275.
Juhlin, C., Wahlgren, C.H. & Stephens, M.B. 2000: Seismic imaging in
the frontal part of the Sveconorwegian orogen, south... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_595.txt | ende were acquired on a CAMECA SX100 instrument at the Microsonde Ouest, in Brest, France. The operating conditions were 15<!-- --> <!-- -->kV and 20<!-- --> <!-- -->nA with a focused beam of 1<!-- --> <!-- -->μm. Concentrations below 0.3% are considered qualitative. The full dataset </p></section></sect... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_36.txt | Dahlgren 1993;
Andersen et al. 2002b; Andersen et al. 2004). Younger
orthogneisses are also reported. These include a 1500 ±
5 Ma granodiorite gneiss (the Veldstad gneiss fringing
the Modum metasedimentary complex; sample
N95-66; Tables 1, 2; Figs. 3, 8C) and a 1.46 Ga orthogneiss in Bamble (the Nelaug gneiss associat... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_79.txt | .27117 1.04 0.71 1478 20 1547 14 104.7
12a 386 120 118 20608 0.09263 0.75 3.3006 1.60 0.25844 1.41 0.88 1480 14 1482 19 100.1
04a 396 124 123 27677 0.09311 0.66 3.3612 1.25 0.26182 1.07 0.85 1490 12 1499 14 100.6
16a 145 42 45 13728 0.09341 0.88 3.4275 1 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_78.txt | al., 2002
Breive gp, Hovden metarhyolite, B9824 S Zrn 1264 ±4 Bingen et al., 2002
Breive gp, quartz porphyry, B9818 S Zrn 1275 ±8 Bingen et al., 2002
Iveland-Gautestad metagabbro T Zrn 1279 ±3 Pedersen and Konnerup-Madsen, 2000
Tinn granite, 0831962 T Zrn 1476 ±13 Andersen et al., 2002 c
Lyngdal granite gneiss | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_14.txt | sberg Terranes
The Bamble and Kongsberg Terranes (Fig. 1) are made
up of 1570-1460 Ma, mainly calc-alkaline, plutonic
suites associated with quartzite or greywacke-dominated
metasediment complexes (Figs. 2, 6; Table 3; Starmer
1985; Starmer 1991; Nijland et al. 1993; Knudsen et al.
1997a; de Haas et al. 1999; Andersen ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_48.txt | artz monzodiorite Zrn 1699 ±7 Stephens cited in Söderlund et al., 1999
Granite, Grå-Larsknipen, TL9406 Zrn 1702 ±11 Lundqvist and Persson, 1999
Alvesta granite gneiss, 86011 Zrn 1713 ±3 Johansson, 1990
Mo Tonalite Zrn 1731 ±7 Mansfeld, 2000
Granite gneiss Zrn 1777 +38/-22 Welin cited in Söderlund et al., 1999
Filip | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_835.txt | 5=6b2544241825cc824e3d10083d8e0c29&pid=1-s2.0-S0301926822003886-main.pdf"}},{"articleTitle":"Paleomagnetism and <sup>40</sup>Ar/<sup>39</sup>Ar geochronology of Meso-Neoproterozoic rocks from southwest Norway. Implications for magnetic remanence ages and the paleogeography of Baltica in a Rodinia supercontinent context... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_569.txt | v56.78h1e1v-74h-74z"></path></svg></a></div><section class="ReferencedArticles"></section><section class="ReferencedArticles"></section><div id="preview-section-abstract"><div class="PageDivider"></div><div class="Abstracts u-font-serif text-s" id="abstracts"><div class="abstract author-highlights" id="abs0005"><h2 cla... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_762.txt | -margin-m-right-from-sm u-margin-l-right-from-md anchor-default" href="https://www.elsevier.com/legal/privacy-policy" target="_blank" id="els-footer-privacy-policy" rel="nofollow"><span class="anchor-text">Privacy policy</span><svg focusable="false" viewBox="0 0 78 128" aria-label="Opens in new window" width="1em" heig... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_19.txt | .3
8 0.0935 0.0008 3.30 0.05 0.256 0.003 0.81 1498 16 1471 16 98.2
5 0.0935 0.0007 3.15 0.04 0.244 0.003 0.84 1499 13 1408 14 94.0
4 0.0935 0.0008 3.18 0.05 0.246 0.003 0.83 1499 17 1419 17 94.7
6 0.0936 0.0007 3.12 0.05 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_55.txt | Ragnhildstveit, J., Sigmond, E.M.O. & Tucker, R.D. 1994: Early Proterozoic supracrustal rocks west of the Mandal-Ustaoset fault zone,
Hardangervidda, South Norway. Terra Nova Abstract Supplement 2,
15-16.
Rimsa, A., Johansson, L. & Whitehouse, M.J. 2007: Constraints on
incipient charnockite formation from zircon geochr... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_27.txt | 4 Zrn U-Pb 1221 ±3 Söderlund & Ask, 2006
PZ Bjärehalla dolerite dyke Bld U-Pb 1221 ±16 Söderlund et al., 2005
South Vårgårda quartz-monzonite, deformed facies Zrn U-Pb 1224 +9/-8 Berglund, 1997
52 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Location Lithology, sample Min System Age ±2s Reference
(1 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_21.txt | and titanite ages
between 1106 ±2 and 1091 ±2 Ma (Fig. 4; Cosca et al.
1998; de Haas et al. 2002; Bingen et al. 2008b). These
data overlap with the main cluster of amphibole 40Ar/39Ar
cooling ages, ranging from 1099 ±3 to 1079 ±5 Ma, in
samples distributed in the amphibolite- and granulite-facies domains (Cosca & O’Ni... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_46.txt | western Dalarna, south-central Sweden. GFF 121, 307-322.
Laajoki, K., Corfu, F. & Andersen, T. 2002: Lithostratigraphy and U-Pb
geochronology of the Telemark supracrustals in the Bandak-Sauland area, Telemark, South Norway. Norwegian Journal of Geology
82, 119-138.
Mansfeld, J. & Andersen, T. 1999: Formation of new cr... | |
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no_hydrocarbons_in_sveconorwegian_belt/Kerogen8.txt | part8 -------------------
Kerogen cycle[edit]
Kerogen cycle
The diagram on the right shows the organic carbon cycle with the flow of kerogen (black solid lines) and the flow of biospheric carbon (green solid lines), showing both the fixation of atmospheric CO2 by terrestrial and marine primary productivity. The combine... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1119.txt | "}],"$":{"id":"lis0005"},"#name":"list"}],"$":{"view":"all","id":"spar0005"},"#name":"simple-para"}],"$":{"view":"all","id":"abst0005"},"#name":"abstract-sec"}],"$":{"view":"all","id":"abs0005","class":"author-highlights"},"#name":"abstract"},{"$$":[{"$":{"id":"sect0010"},"#name":"section-title","_":"Abstract"},{"$$":[... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_565.txt | .78v47.22h44v-42h-34v-5.22c0-18.5 17.08-26.78 34-26.78z"></path></svg><span class="button-link-text">Cite</span></button></div></div></div></div></div><div class="ArticleIdentifierLinks u-margin-xs-bottom text-xs" id="article-identifier-links"><a class="anchor doi anchor-default" href="https://doi.org/10.1016/j | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_789.txt | S0301926815X00088","item-weight":"FULL-TEXT","language":"en","last-lp":"77","last-author":{"#name":"last-author","$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"$$":[{"#name":"author","$":{"id":"aut0030"},"$$":[{"#name":"given-name","_":"Bjørn E."},{"#name":"surname","_":"Sørensen"},{"#name":"cross-ref","$":{"id... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1377.txt | 0012825211000584-main.pdf"}},{"refId":65,"pii":"S0301926814001946","filesize":"3MB","pdf":{"urlType":"download","url":"/science/article/pii/S0301926814001946/pdfft?md5=5d5ceea51408ff4f5d845627e5d0f02a&pid=1-s2.0-S0301926814001946-main.pdf"}},{"refId":67,"pii | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_170.txt | width:16px;height:16px}div#onetrust-pc-sdk.ot-host-item>button{background:0 0!important;border:0!important;height:66px!important;max-width:none!important;width:calc(100% - 5px)!important;transform:translate(2px,2px)}div#onetrust-pc-sdk.ot-host-item{border-bottom:2px solid #b9b9b9;padding:0}div#onetrust- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_141.txt | .e(111).then(r.bind(r, 7438)).then(t => {
let {
setAPI: r
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r(e), (0, c.L)(e, "api | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_16.txt | al thickening at 1035 Ma, monazite and titanite data indicate
unroofing in the Idefjorden Terrane at 1025 Ma. This
suggests that exhumation of high-pressure metamorphic rocks in the Idefjorden Terrane took place in a convergent setting. Mechanisms for such exhumation have
been explored, for example, by Hynes and Eaton ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1055.txt | #name":"abstract-attachment","_":"true"},{"#name":"filename","_":"fx1.sml"},{"#name":"extension","_":"sml"},{"#name":"filesize","_":"21680"},{"#name":"pixel-height","_":"93"},{"#name":"pixel-width","_":"219"},{"#name":"attachment-type","_":"IMAGE-THUMBNAIL"}],"$":{"xmlns:xocs":true},"#name":"attachment"},{"$$":[{"#name... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_250.txt | k ul{list-style:none;padding:0}#onetrust-pc-sdk ul li{position:relative;margin:0;padding:15px 15px 15px 10px;border-bottom:1px solid #e2e2e2}#onetrust-pc-sdk ul li h3{font-size:.75em;color:#656565;margin:0;display:inline-block;width:70%;height:auto;word-break:break-word;word-wrap:break-word}# | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_56.txt | OURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
Fig. 3. LA-ICPMS U-Pb data on zircon from three granitoids from the
Eastern Segment.
48
The age of the Bohus granite pluton is estimated from
two concordant monazite and xenotime analyses from a
pegmatite. The monazite analysis yields a... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_40.txt | iss, Gällared N, old component Zrn U-Pb 1679 ±13 Söderlund et al., 2002
Centre Hagfors gneissic granite Zrn U-Pb 1684 ±13 Lindh et al., 1994
South Unveined + veined orthogneiss, Dagsås Zrn U-Pb 1686 ±14 Söderlund et al., 2002
South Migmatitic banded orthogneiss, Skene gneiss, SE-1 Zrn U-Pb 1686 ± | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_85.txt | ared S U-Pb SIMS 3 Söderlund et al., 2002 (1) Telemarkia Terrane: Vardefjell SZ: Vardefjell Shear Zone, Rogaland: Rogaland Vest Agder Sector Eastern Segment: North: Solør transect, Centre: Lake Vänern transect, South: South of Vårgårda, PZ: Protogine Zone SFDZ: Sveconorwegian Frontal Deformation Zone (2) Mnz: monazite, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_87.txt | molybdenite geochronological data in the Sveconorwegian belt attributed to high-grade metamorphism.
56 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Table 5. Compilation of titanite U-Pb data in the Sveconorwegian belt
Location Lithology, sample, fraction Facies Type n Date ±2s Reference
(1) (2) (3) (4) (Ma)
Telemarki... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_101.txt | Time
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_452.txt | ;border:1px solid #d7d7d7;border-radius:5px;border-spacing:initial;width:100%;overflow:hidden}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table th,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table td{border-bottom:1px solid #d7d7d7;border-right:1px solid #d7d7d7}#ot-sdk | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_56.txt | if ("string" == typeof e && e.length) return e.length;
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_44.txt | e, r) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1306.txt | reference","$":{"id":"sbref0285","refId":"57"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"F.S."},{"#name":"surname","_":"Spear"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Metamorphic Phase Equilibria and Pressure–Tempe... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_91.txt | imiters(prodList[i].recordType));
}
if (prodList[i].exportType) {
merch.push('evar99=' + this.stripProductDelimiters(prodList[i].exportType));
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1123.txt | ation from the charnockitic one. Mineralogical, geochemical and petrological data indicate that the charnockitic facies belongs to the AMC suite and the granitic facies, to the HBG suite. Strontium, Nd and Pb isotopic data show that the Farsund intrusion was emplaced at the boundary between two different lithotectonic ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_26.txt | Andréasson & Rodhe 1994;
Wahlgren et al. 1994; Söderlund et al. 2004), and intrusion of the orogen-parallel (N-S trending) BlekingeDalarna dolerites, mainly between 950 and 940 Ma, in
the foreland of the Sveconorwegian belt (Söderlund et al.
2005).
In the Telemarkia Terrane, the amphibolite- to granulitefacies domain ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_32.txt | 3, Vråna, 3 Zrn U-Pb 1457 ±7 Connelly et al., 1996
PZ Stenshuvud porphyritic granite, SGU1 Zrn U-Pb 1458 ±6 Cecys et al., 2002
North Östmark dolerite, 77129 Zrn U-Pb 1465 ±11 Welin, 1994
PZ Flackarp granite gneiss, 76314 Zrn U-Pb 1531 ±8 Johansson, 1990
South Hinneryd adamellite-mon | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_729.txt | articles-article1-title"><a class="anchor u-clamp-2-lines anchor-default" href="/science/article/pii/S0301926814002514" title="Precise ID-TIMS U–Pb baddeleyite ages (1110–1112Ma) for the Rincón del Tigre–Huanchaca large igneous province (LIP) of the Amazonian Craton: Implications for the Rodinia supercontinent"><span c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1022.txt | $$":[{"#name":"label","_":"⁎"},{"#name":"text","_":"Corresponding author. Tel.: +46 729373025."}]}]}],"floats":[],"footnotes":[],"attachments":[]},"lastAuthor":{"content":[{"#name":"author","$":{"id":"aut0015"},"$$":[{"#name":"given-name","_":"Charlotte"},{"#name":"surname","_":"Möller"},{"#name":"cross-ref","$":{"id":... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_67.txt | ambrian Research 150, 136-152.
Söderlund, U., Hellström, F.A. & Kamo, S.L. 2008: Geochronology of
high-pressure mafic granulite dykes in SW Sweden; tracking the PT-t path of metamorphism using Hf isotopes in zircon and baddeleyite. Journal of Metamorphic Geology (in press).
Stacey, J.S. & Kramers, J.D. 1975: Approximat... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_110.txt | -group{display:block}#onetrust-banner-sdk #onetrust-accept-btn-handler,#onetrust-banner-sdk #onetrust-reject-all-handler,#onetrust-banner-sdk #onetrust-pc-btn-handler{width:100%}#onetrust-banner-sdk.onetrust-close-btn-ui{top:auto;transform:none}#onetrust-banner-sdk #onetrust-policy-title{display:inline;float: | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_6.txt | ist and metaarkose (Vendevatn fm)
(Torske 1982). A fine-grained (50-100 µm) platy metarhyolite of the Jåstad formation yields an extrusion age
of 1489 ± 1 Ma (sample S93-338; Tables 1, 2; Figs. 3,
8F). This age constrains deposition of the lower part of
the Ullensvang group. The base of the Ullensvang
group is not defi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_33.txt | c += e.c, t;
}(i, a[e]);
}
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storeMetric(e, t, r, n) {
var | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_951.txt | sp","$":{"sp":"0.25"}},{"#name":"__text__","_":"4"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"Ma ("}]}]}]}]},{"#name":"section","$$":[{"#name":"section","$":{"xmlns:ce":true,"xmlns:mml":true,"xmlns:xs":true,"xmlns:xlink":true,"xmlns:xocs":true,"xmlns:tb":true,"xmlns:xsi | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1299.txt | _":"1"},{"#name":"last-page","_":"94"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0275"},"$$":[{"#name":"label","_":"Slagstad et al., 2013a"},{"#name":"reference","$":{"id":"sbref0275","refId":"55"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_98.txt | t: () => n
});
const n = r(3325).D.pageAction;
},
7633: (e, t, r) => {
r.d(t, {
Dz: () => i,
OJ | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_18.txt | aconglomerate. The common
banding of the supracrustal rocks and stretching of the
conglomerate attest to important deformation. Zircon
was not successfully recovered from a metadacite sample.
Two samples of granodiorite and granite gneiss with
augen texture were collected in the directly surrounding and conformable Bot... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_571.txt | etary-sciences/batholith" title="Learn more about batholith from ScienceDirect's AI-generated Topic Pages" class="topic-link">batholith</a> in SW Norway.</span></p></span></li><li class="react-xocs-list-item"><span class="list-label">•</span><span><p id="par0010">The SMB host rocks were metamorphosed regionally during ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_121.txt | |') // events
,merch.join('|') // merchandising eVars
].join(';'));
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return | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1087.txt | country","_":"UK"}]}]},{"#name":"affiliation","$":{"id":"aff0015"},"$$":[{"#name":"label","_":"c"},{"#name":"textfn","_":"Edinburgh Ion Microprobe Facility, University of Edinburgh, Edinburgh EH9 3JW, UK"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Edinburgh Ion Microprobe Facility,... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_321.txt | -vnd-item.ot-vnd-info.ot-vnd-lbl{font-weight:bold;font-size:.85em;margin-bottom:.5rem}#onetrust-pc-sdk.ot-vs-list.ot-vnd-item.ot-vnd-info.ot-vnd-cnt,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-vnd-info.ot-vnd-cnt{margin- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1319.txt | oc. Can. Spec. Pap."}]},{"#name":"volume-nr","_":"14"}]},{"#name":"date","_":"1976"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"597"},{"#name":"last-page","_":"613"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0310"},"$$":[{"#name":"label","_":"Torske, 1977"},{"#name":"reference","$":{"id":"sbref0310","refI... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1480.txt | fltr-cnt"><button id="clear-filters-handler">Clear</button><div class="ot-fltr-scrlcnt ot-pc-scrollbar"><div class="ot-fltr-opts"><div class="ot-fltr-opt"><div class="ot-chkbox"><input id="chkbox-id" type="checkbox" class="category-filter-handler"> <label for="chkbox-id"><span class="ot-label-txt">checkbox label</span>... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1464.txt | cat-item ot-vs-config" data-optanongroupid="4"><button aria-expanded="false" ot-accordion="true" aria-controls="ot-desc-id-4" aria-labelledby="ot-header-id-4"></button><!-- Accordion header --><div class="ot-acc-hdr"><div class="ot-plus-minus"><span></span><span></span></div><h4 class="ot-cat-header" id="ot-header-id- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_0.txt | 43
Introduction
The Sveconorwegian orogenic belt is situated at the
southwestern margin of Fennoscandia. It is one of the
classical, well-exposed Grenvillian orogenic belts (Fig.
1) (Berthelsen 1980). Like most Grenvillian belts, it is
deeply eroded and its hinterland rifted away during Neoproterozoic continent dispers... |
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