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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_887.txt | simple-para","_":"Septa of banded gneisses crop out along the margin of the Proterozoic Sveconorwegian Egersund-Ogna (EGOG) anorthosite pluton. They permit the observation of the effects of a diapiric intrusion of anorthosite on its envelope of gneisses. The rocks are mylonitic and result from a strong deformation in U... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1109.txt | crf0875","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":"aut0040"},"$$":[{"#name":"given-name","_":"Nadine"},{"#name":"surname","_":"Mattielli"},{"#name":"cross-ref","$":{"id":"crf0880","refid":"aff0015"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"c"}]}]},{"#name":... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_79.txt | rn U-Pb 1260 ±8 Bingen et al., 2002
Suldal Breive Gp, Hovden metarhyolite, B9824 Zrn U-Pb 1264 ±4 Bingen et al., 2002
Suldal Breive Gp, quartz porphyry, B9818 Zrn U-Pb 1275 ±8 Bingen et al., 2002
Telemark Iveland-Gautestad metagabbro Zrn U-Pb 1279 ±3 Pedersen & Konnerup-Madsen, | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_1.txt | wegian belt is generally restored, in a variety of configurations, to the east of the Grenville belt of
Laurentia, facing Amazonia, at the end of the Mesoproterozoic and during the Neoproterozoic (Gower et al.
1990; Hoffman 1991; Torsvik et al. 1996; Karlstrom et al.
2001; Cawood & Pisarevsky 2006; Bogdanova et al. 200... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_21.txt | :
From Archaean to Proterozoic on Hardangervidda, South Norway.
Norges geologiske undersøkelse Bulletin 433, 4-5.
Brewer, T.S., Daly, J.S. & Åhäll, K.-I. 1998: Contrasting magmatic arcs
in the Palaeoproterozoic of the south-western Baltic Shield.
Precambrian Research 92, 297-315.
Brewer, T.S., Åhäll, K.-I., Men | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_175.txt | rust-pc-sdk #ot-fltr-cnt{box-shadow:0 0;border:1px solid #8e8e8e;border-radius:0}div#onetrust-pc-sdk.ot-fltr-scrlcnt{max-height:calc(100% - 80px)}div#onetrust-pc-sdk #ot-fltr-modal{max-height:400px}div#onetrust-pc-sdk.ot-fltr-opt{margin-bottom: | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1021.txt | Fort Wayne, IN 46805, USA"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Department of Geosciences, IPFW University"},{"#name":"address-line","_":"2101 E. Coliseum Blvd"},{"#name":"city","_":"Fort Wayne"},{"#name":"state","_":"IN"},{"#name":"postal-code","_":"46805"},{"#name":"countr... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_65.txt | a 148 61 61 38139 0.11190 0.51 5.176 2.30 0.3355 2.24 0.98 1831 9 1865 36 101.9 16a 240 169 102 45228 0.11220 0.40 4.962 2.27 0.3208 2.23 0.98 1835 7 1793 35 97.7 10a 163 74 65 26254 0.11460 0.49 5.052 2.29 0.3197 2.23 0.98 1874 9 1788 35 95.5 14a 115 111 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_61.txt | B., Boven, A., Punzalan, L., Wijbrans, J. & Demaiffe, D. 1998:
Hornblende 40Ar/39Ar geochronology across terrane boundaries in
the Sveconorwegian province of S Norway. Precambrian Research
90, 159-185.
Bingen, B. & van Breemen, O. 1998a: Tectonic regimes and terrane
boundaries in the high-grade Sveconorwegian belt of ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_30.txt | 2000; Andersen et al. 2004; Nordgulen & Skår 2004).
Geochronological data on two plutonic complexes situated
west of the Oslo rift, are reported in Tables 1-2. These
are the Vinflomyra granite gneiss giving an age of 1606
± 2 Ma (sample N95-95, Figs. 3, 8A) and the Follum
metapluton giving an age of 1555 ± 3 Ma (sampl... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_7.txt | Pb 1530 ±18 Åhäll & Connelly, 2008
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia 51
Location Lithology, sample Min System Age ±2s Reference
(1) (2) (Ma)
Stenungsund tonalite, Saxeröd sample, Hisingen suite Zrn U-Pb 1535 ±13 Åhall 1991
Lane granite, 79019 Zrn U-Pb 1535 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_737.txt | amp-2-lines anchor-default" href="/science/article/pii/S0301926814002551" title="Intermontane basins and bimodal volcanism at the onset of the Sveconorwegian Orogeny, southern Norway"><span class="anchor-text"><span>Intermontane basins and bimodal volcanism at the onset of the Sveconorwegian Orogeny, southern Norway</s... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_775.txt | and description of a newly discovered, ca. 200"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"km"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"×"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"50"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"km magmatic belt, th... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_70.txt | 1671.
Stein, H.J. & Bingen, B. 2002: 1.05-1.01 Ga Sveconorwegian metamorphism and deformation of the supracrustal sequence at Sæsvatn, South Norway: Re-Os dating of Cu-Mo mineral occurrences.
In Blundell, D., Neubauer, F. & von Quadt, A. (eds.), The timing and
location of major ore deposits in an evolving orogen. Geolo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_73.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_830.txt | ites. The Tørdal granite, yielding an age of 946 ± 4 Ma, is about 40 Ma older than the adjacent pegmatites. Field evidence and the age difference between pegmatites and granites supports an anatectic origin for these pegmatites. Sources of these pegmatite melts are biotite- and biotite-amphibole gneisses and amphibolit... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_115.txt |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_215.txt | rust-pc-sdk #ot-lst-title h3{display:inline-block;word-break:break-word;word-wrap:break-word;margin-bottom:0;color:#656565;font-size:1em;font-weight:bold;margin-left:15px}#onetrust-pc-sdk #ot-lst-title{margin:10px 0 10px 0px;font-size:1em;text-align:left}#onetrust-pc-sdk #ot- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_21.txt | itoids at Trysil, southeast Norway. Norsk Geologisk Tidsskrift 76, 45-54.
Hellström, F.A., Johansson, Å. & Larson, S.Å. 2004: Age emplacement
of late Sveconorwegian monzogabbroic dykes, SW Sweden. Precambrian Research 128, 39-55.
Henderson, I.H.C. & Ihlen, P.M. 2004: Emplacement of polygeneration pegmatites in relation... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_28.txt | and (min-width: 426px)and (max-width: 896px)and (orientation: landscape){#onetrust-pc-sdk p{font-size:.75em}}#onetrust-banner-sdk.banner-option-input:focus+label{outline:1px solid #000;outline-style:auto}.category-vendors-list-handler+a:focus,.category-vendors-list-handler+a:focus-visible{outline:2px solid #000} | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_52.txt | compositionally similar to rocks of the TIB (Fig. 6; Table 3; Söderlund et al.
1999; Söderlund et al. 2002; Högdahl et al. 2004; Möller
et al. 2007). The new data on the Solør Complex (Figs. 2,
3) demonstrate that the northernmost part of the Eastern Segment conforms to this description. These granitoids are intruded ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_501.txt | .97 2-1.97s1.98 0.88 1.98 1.98C175.66 5.09 174.77 5.96 173.68 5.96zM173.67 2.46c-0.85 0-1.54 0.67-1.54 1.52 0 0.85 0.69 1.54 1.54 1.54 0.85 0 1.54-0.69 1.54-1.54C175.21 3.13 174.52 2.46 173.67 2.46 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_900.txt | as the granitic rocks are mostly I- and A-type, while S-type granites are mostly lacking in the Sveconorwegian (Slagstad et al., 2013; Coint et al., 2015; Granseth et al., 2020). Overall, presently available Hf–O isotopic data indicate that the 1050–930 Ma Sveconorwegian magmas show little isotopic fingerprint that ar... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_56.txt | ) (3) (4) (5)
Telemarkia Terrane
Telemark Zrn 1014±1 Am Amphibolite, Noresund, B99130 U-Pb ID-TIMS 3 Bingen et al., 2008
Suldal Moly 1032±2 Am Sulfide ore in metagabbro, Langvatn, LG1-LG3 Re-Os ID-NTIMS 3 Stein & Bingen, 2002
Suldal Moly 1047±2, 1025±2, 1017±2 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_906.txt | transect reveal multiple magmatic episodes during Gothian (ca. 1650 Ma), Telemarkian (ca. 1500 Ma) and Sveconorwegian (1050–1020 Ma vs. 980–930 Ma) orogenesis as well as Sveconorwegian migmatization (1050–950 Ma). Newly documented 1050–1020 Ma magmatism and migmatization extend the Sirdal Magmatic Belt to a 300 km-lon... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_17.txt | orwegian Province of SW Norway.
Contributions to Mineralogy and Petrology 132, 336-353.
Bingen, B., Birkeland, A., Nordgulen, Ø. & Sigmond, E.M.O. 2001a:
Correlation of supracrustal sequences and origin of terranes in the
Sveconorwegian orogen of SW Scandinavia: SIMS data on zircon
in clastic metasediments. Precambrian... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_18.txt | . (eds.), Mid-Proterozoic Laurentia-Baltica. Geological
Association of Canada, Special Paper 38, 149-173.
Tucker, R.D., Ashwal, L.D., Handke, M.J., Hamilton, M.A., Le Grange,
M. & Rambeloson, R.A. 1999: U-Pb geochronology and isotope
geochemistry of the Archean and Proterozoic rocks of northcentral Madagascar. The Jour... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_40.txt | formation in SW Sweden. Geologiska Föreningens i
B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
67
Stockholm Förhandlingar 119, 37-43.
Åhäll, K.I. & Connelly, J.N. 1998: Intermittent 1.53-1.13 Ga magmatism in western Baltica; age constraints and correlations within a
postulated supercontinent. Precambrian Research 92, ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1193.txt | _":"C.F."},{"#name":"surname","_":"Gower"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S.L."},{"#name":"surname","_":"Kamo"}]},{"#name":"author","$$":[{"#name":"given-name","_":"K."},{"#name":"surname","_":"Kwok"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T.E."},{"#name":"surname","_":" | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_7.txt | G. 2001: Nature and
distribution of deep crustal reservoirs in the southwestern part of
the Baltic Shield: evidence from Nd, Sr and Pb isotope data on late
Sveconorwegian granites. Journal of the Geological Society, London
158, 253-267.
Andersen, T., Andresen, A. & Sylvester, A.G. 2002a: Timing of late- to
post-tectoni... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_25.txt | & Ihlen 2004). The time of thrusting is not directly
dated: it is nevertheless younger than 1132 ±3 Ma, the
age of the Morkheia Monzonite Suite deformed along
the shear zone (Fig. 2; Heaman & Smalley 1994). Thrusting probably post-dates the peak of the most widespread
event of amphibolite-facies metamorphism recorded ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_996.txt | ":[{"#name":"author","$":{"id":"aut0030"},"$$":[{"#name":"given-name","_":"Richard E."},{"#name":"surname","_":"Ernst"},{"#name":"cross-ref","$":{"id":"crf0135","refid":"aff0030"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"f"}]},{"#name":"cross-ref","$":{"id":"crf0140","refid":"aff0035"},"$$":[{"#name":"sup","$":{"lo... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_160.txt | 63vmAs/8ga1cD0E3A7LEq6AXk1uXgsAAACTeyJvcmlnaW4iOiJodHRwczovL2dvb2dsZXN5bmRpY2F0aW9uLmNvbTo0NDMiLCJmZWF0dXJlIjoiRmxlZGdlQmlkZGluZ0FuZEF1Y3Rpb25TZXJ2ZXIiLCJleHBpcn | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_63.txt | 18a 220 129 89 76923 0.10720 0.44 4.713 2.31 0.3189 2.27 0.98 1752 8 1784 35 101.8 07a 98 74 42 127910 0.10770 0.61 4.795 2.33 0.3229 2.25 0.96 1761 11 1804 35 102.4 04a 124 106 54 18155 0.10935 0.66 4.876 2.33 0.3234 2.23 0.96 1789 12 1806 35 101.0 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_52.txt | m 1030 ±1 Romer and Smeds, 1996
Timmerhult rare-mineral pegmatite Clm 1039 ±3 Romer and Smeds, 1996
Skantorp rare-mineral pegmatite Clm 1041 ±2 Romer and Smeds, 1996
Sandsjön granite gneiss, 78140 Zrn 1210 +36/-34 Welin et al., 1981
Segmon granite, SWS9 Zrn 1249 +10/-7 Persson et al., 1983
Raufoss granite gne | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1152.txt | ":"2005"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"87"},{"#name":"last-page","_":"116"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0045"},"$$":[{"#name":"label","_":"Bingen et al., 2006"},{"#name":"reference","$":{"id":"sbref0045","refId":"9"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_56.txt | that all 208Pb in excess of blank, common-Pb, and spike is radiogenic (λ 232Th=4.9475 10-11 y-1). (5) Measured, uncorrected ratio. (6) Ratio corrected for fractionation, spike, blank, and initial
common-Pb (at the determined age from Stacey and Kramers, 1975). Pb fractionation correction = 0.094%/amu (±0.025% 1
σ); U f... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_492.txt | .74M84.59 9.18c0.17-0.17 1.29-0.46 1.98-0.46 2.48 0 3.76 0.53 3.86 3.43h-7.46C83.24 10.27 84.39 9.37 84.59 9.18zM103.9 1.98h-7.13v19.93h6.83c7.26 0 9.77-5.68 9.77-10.03C113.37 7.33 110. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_578.txt | -paragraph" href="#bib0275" name="bbib0275" data-sd-ui-side-panel-opener="true" data-xocs-content-type="reference" data-xocs-content-id="bib0275"><span class="anchor-text">Slagstad et al., 2013a</span></a>). Magmatism in this belt between 1060 and 1020<!-- --> <!-- -->Ma precedes and overlaps the main Sveconorwegi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_752.txt | ="nofollow"><span class="anchor-text">About ScienceDirect</span><svg focusable="false" viewBox="0 0 78 128" aria-label="Opens in new window" width="1em" height="1em" class="icon icon-arrow-up-right arrow-external-link"><path d="m4 36h57.07l-59.5 59.5 7.07 7.08 59.36-59.36v56.78h1e1v-74h-74z"></path></ | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_11.txt | commonly have an intermediate andesite-dacite composition. The best estimate
for the timing of magmatic activity in the Sauda supracrustals is provided by an augen gneiss layer giving an
age of 1496 ± 11 Ma (sample B00-106; Tables 1, 5; Fig.
10B) and a weakly-deformed granodiorite gneiss boudin giving an age of 1497 ±... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1208.txt | name":"first-page","_":"51"},{"#name":"last-page","_":"74"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0140"},"$$":[{"#name":"label","_":"Holland and Blundy, 1994"},{"#name":"reference","$":{"id":"sbref0140","refId":"28"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"a... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_32.txt | ”. These are the Telemark, Hardangervidda, Suldal and Rogaland-Vest Agder Sectors
B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
61
(Fig. 1; Bingen et al. 2005). The boundaries between them
are generally transitional, except along the N-S trending
Mandal-Ustaoset Fault and Shear Zone (Fig. 1; Sigmond
1985). The four sec... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_382.txt | pc-lst.back-btn-handler p,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_15.txt | pler. Analyses were performed following Bingen
et al. (2005). The laser beam was rastered over an area of
c. 40 x60 μm at the surface of selected crystals presented
on double-sided tape. Two to three analyses were made at
the same position to ensure progressive ablation from the
surface to the core of the crystal. Mass... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1049.txt | , China"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Institute of Geology and Geophysics"},{"#name":"organization","_":"Chinese Academy of Sciences"},{"#name":"city","_":"Beijing"},{"#name":"postal-code","_":"100029"},{"#name":"country","_":"China"}]}]},{"#name":"affiliation","$":{"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1379.txt | isOpenVirtualSpecialIssueLink":false,"isOpenRecommendations":true,"isOpenSubstances":true,"citingArticles":[false,false,false,false,false,false],"recommendations":[false,false,false,false,false,false]},"seamlessAccess":{},"specialIssueArticles":{},"substances":{},"supplementaryFilesData":[],"tableOfContents":{"outlineT... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_721.txt | class="sub-heading u-padding-xs-bottom"><h3 class="related-content-panel-list-entry-outline-padding text-s u-font-serif" id="special-issue-articles-article2-title"><a class="anchor u-clamp-2-lines anchor-default" href="/science/article/pii/S0301926815001023" title="Multiple reactivation and strain localization along a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_134.txt | if ("string" == typeof e || null === e) return b("application.version", e, "setApplicationVersion",!1);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_309.txt | ot-lst-cnt.ot-vnd-info-cntr{border:1px solid #d8d8d8;padding:.75rem 2rem;padding-bottom:0;width:auto;margin-top:.5rem}#onetrust-pc-sdk #ot-lst-cnt.ot-vnd-info{margin-bottom:1rem;padding-left:.75rem;padding-right:.75rem;display:flex;flex-direction:column}#onetrust-pc | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_78.txt | urmen, E.A.T. 1980: On the thermal stability of Rb-Sr and K-Ar biotite systems: evidence from
coexisting Sveconorwegian (ca 870 Ma) and (ca 400 Ma) biotites
in SW Norway. Contributions to Mineralogy and Petrology 74, 245-
252.
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavi... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_774.txt | –930"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma, and an anorthosite–mangerite–charnockite–granite (AMCG) suite at 930"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma. New detailed mapping and geochronology in the area reveal a very different and much more complex evolution, and requ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_54.txt | ogenic extensional deformation after c. 985 Ma.
Exotic vs. indigenous models
The three largest lithotectonic units in the Sveconorwegian
belt, the Eastern Segment, the Idefjorden Terrane and the
Telemarkia Terrane are characterized by distinct events
of continental growth (in the sense of the oldest event
of widespread... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_862.txt | orogenic activity and externally (as opposed to gravitationally) driven extension suggest that the RAP formed in a continental back-arc setting."}],"$":{"view":"all","id":"as010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab010","lang":"en","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1405.txt | A4258E4D7FB42E5CDA3EC3BE1A2AD34978E6E467FBA88B160B471687035859AC27543FBA44D1BD4E4F2EB0469A67597464825D387A21AFA2E514&utt=eed1-faed0787e81b5ba7af5-e6f50c45e22cf1ff" tabindex="-1"></iframe>
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1153.txt | ","$$":[{"#name":"given-name","_":"B."},{"#name":"surname","_":"Bingen"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H.J."},{"#name":"surname","_":"Stein"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Bogaerts"}]},{"#name":"author","$$":[{"#name":"given-name","_":"O."},{"#n... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1074.txt | italic","_":"P"},{"#name":"__text__","_":" rocks in the Phanerozoic continental collisional orogens. It seems to indicate that the thermal regimes and tectonic mechanisms of Paleoproterozoic probably differ from those of Phanerozoic eons, and these H"},{"#name":"italic","_":"T"},{"#name":"__text__","_":"–H"},{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_166.txt | 62 : 'Search - Result Types'
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