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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1011.txt | name":"hsp"},{"#name":"__text__","_":"Ma) in the Bolivian Precambrian shield – SW portion of the Amazonian Craton. The identical ca. 1110–1112"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma ages obtained for each (about 500"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"km apart) suggest ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1142.txt | "}]},{"#name":"author","$$":[{"#name":"given-name","_":"W.J."},{"#name":"surname","_":"Davis"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M.A."},{"#name":"surname","_":"Hamilton"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.K."},{"#name":"surname","_":"Engvik"}]},{"#name":"author","$$":[{"#name":"g... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_47.txt | Norges geologiske undersøkelse Bulletin 440, 5-18.
Andersen, T., Griffin, W.L. & Pearson, N.J. 2002b: Crustal evolution in
the SW part of the Baltic Shield: the Hf isotope evidence. Journal of
Petrology 43, 1725-1747.
Andersen, T., Sylvester, A.G. & Andresen, A. 2002c: Age and petrogenesis of the Tinn granite, Telemar... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_0.txt | layered intrusion (Rogaland, Southwest Norway). Journal of Structural Geology 22, 647-667.
Bolle, O., Demaiffe, D. & Duchesne, J. C. 2003a: Petrogenesis of jotunitic and acidic members of an AMC suite (Rogaland anorthosite
province, SW Norway): a Sr and Nd isotopic assessment. Precambrian Research 124, 185-214.
Bolle, ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_14.txt | ±17 Andersen et al., 2004
Hisingen suite, Eggsjö granodiorite Zrn U-Pb 1578 ±7 Åhäll & Connelly, 2008
Idala tonalite Zrn U-Pb 1584 ±15 Åhäll et al., 1995
Gabbro, granitic contact melt ASCH9801 Zrn U-Pb 1585 ±4 Ahlin et al., 2006
Bjørkelangen granodiorite, TA118 Zrn U-Pb 1585 ±18 Andersen | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_159.txt | ZXJ2ZXIiLCJleHBpcnkiOjE3MTkzNTk5OTksImlzU3ViZG9tYWluIjp0cnVlLCJpc1RoaXJkUGFydHkiOnRydWV9"><meta http-equiv="origin-trial" content="A6OdGH3fVf4eKRDbXb4thXA4InNqDJDRhZ8U533U/roYjp4Yau0T3YSuc | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_19.txt | yield
ages of 1498 ± 8 Ma and 1499 ± 12 Ma (samples B02-
022 and B02-027; Tables 1, 4; Figs. 9C, D). They provide
an estimate for the timing of plutonic activity in the
gneiss complex.
The Suldal sector displays a 1.27-1.21 Ga bimodal volcanic
suite associated with metasediments (Sæsvatn-Valldal
supracrustal sequence;... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_24.txt | 2.1 0.2714 1.8 0.84 1548 25 1713 21 9.7
23 10545 0.10220 1.0 3.930 1.6 0.2789 1.3 0.78 1586 18 1664 19 4.7
05 26493 0.10598 1.3 4.140 1.9 0.2833 1.3 0.71 1608 19 1731 24 7.1
17 15579 0.10224 1.0 3.995 1.9 0.2834 1.6 0. | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_65.txt | al Byklom granite Zrn U-Pb 970 +14/-18 Andersen et al., 2002
Telemark Høvring granite Zrn U-Pb 971 +63/-34 Andersen et al., 2002
Rogaland Granulite-facies leucosome, Ørsdalen, 3 samples Moly Re-Os 973 ±4 Bingen & Stein, 2003
Telemark Torsdalsfjell granite, 080396-1 Zrn U-Pb 990 ±14 Andersen et al., 2007
Suldal | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_489.txt | .82 6.57M72.12 9.01c0.23-0.13 0.69-0.26 1.72-0.26 1.72 0 2.41 0.3 2.41 1.58h2.38c0-0.36 0-0.79-0.03-1.09 -0.23-1.98-2.15-2.67-4.88-2.67 -3 0-6.7 2.31-6.7 7.76 0 5.22 2. | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_561.txt | .2l28.42-15.28c4.04 4.58 9.92 7.48 16.48 7.48 12.14 0 22-9.86 22-22s-9.86-22-22-22-22 9.86-22 22c0 1.98 0.28 3.9 0.78 5.72l-28.64 15.38c-4.02-4.34-9.76-7.1-16.14-7.1-12.14 0-22 9.86 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_43.txt | Baltic Shield; a review addressing the tectonic characteristics of Svecofennian, TIB 1 -related, and Gothian events. GFF
122, 193-206.
Åhäll, K.I. & Connelly, J.N. 2008: Long-term convergence along SW
Fennoscandia: 330 m.y. of Proterozoic crustal growth. Precambrian
Research 161, 452-474.
Ahlin, S., Austin Hegardt, E.... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_48.txt | high-temperature granulite-facies assemblages
(Möller et al. 2003) links the osumilite and pigeonite isograds with intrusion of the Rogaland AMC complex (932
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
62
±3 to 920 ±3 Ma; Fig. 8f; Schärer et al. 1996). (5) Monazite in... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_121.txt | #onetrust-banner-sdk #onetrust-close-btn-container{top:50%;margin:auto;transform:translate(-50%, -50%);position:absolute;right:0}#onetrust-banner-sdk #onetrust-close-btn-container button{right:-12px}#onetrust-banner-sdk #onetrust-policy{margin-left:2em}#onetrust-banner-sdk.vertical-align-content #onetrust-button-group-... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_594.txt | h2 class="section-title u-h4 u-margin-l-top u-margin-xs-bottom">Depth of crystallization of SMB granites</h2><p id="par0305">Mineral composition data, acquired by microprobe, were obtained from different parts of the SMB (black triangles in Fig. 1a) in order to determine the pressure and temperature (<em>P</em>–<em>T</... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_549.txt | 93s6.78-0.98 9.42-2.93l40.24-30.7v-10.34h-102zm92 56.48l-18.06-22.74-8.04 5.95 17.38 21.89h-64.54l18.38-23.12-8.04-5.96-19.08 24.02v-37.58l-1e1 -8.46v61.1h102v-59.18l-1e1 8. | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1442.txt | xi) {var _0xj = _0xi.createElement('script');_0xj.innerHTML = js;_0xi.getElementsByTagName('head')[0].appendChild(_0xj);}}if (document.readyState!== 'loading') {handler();} else if (window.addEventListener) {document.addEventListener('DOMContentLoaded', handler);} else {var prev = document.onreadystatechange || functio... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_45.txt | towards the base
of the Rjukan group. As a result, the nature of the base
of the group is uncertain. The amphibolite-facies Gøyst
metasupracrustal complex was regarded as a possible
basement to the Rjukan group by Sigmond et al.
(1997). However, detrital zircons in a sample collected
in a bedded metasandstone sequence... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1304.txt | ","$$":[{"#name":"given-name","_":"T.S."},{"#name":"surname","_":"Røhr"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H."},{"#name":"surname","_":"Schiellerup"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"A non-collisional, accretionary Sveconorwegian orogen"}]}]},{"#name":"host","$$":[{"#name":"issue"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1302.txt | -nr","_":"25"}]},{"#name":"date","_":"2013"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"169"},{"#name":"last-page","_":"171"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0280"},"$$":[{"#name":"label","_":"Slagstad et al., 2013b"},{"#name":"reference","$":{"id":"sbref0280","refId":"56"},"$$":[{"#name":"contr... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_48.txt | ", [this.#t(e), (0, g.z)(),!0], void 0, r.D.jserrors, this.ee);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_107.txt | JSONP_NODE: () => p,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_18.txt | ar zone, Koster islands, SW Sweden.
Bulletin of the Geological Society of Denmark 34, 151-197.
Hansen, B.T., Persson, P.O., Söllner, F. & Lindh, A. 1989: The influence
of recent lead loss on the interpretation of disturbed U–Pb systems
in zircons from metamorphic rocks in southwest Sweden. Lithos 23,
123-136.
Hansen, B... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1007.txt | -mantle plume event in SW Amazonia."}],"$":{"view":"all","id":"par0010"},"#name":"para"}],"$":{"id":"lsti0010"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0015"},"#name":"para","_":"The LIP-mantle plume event is potentially linked with an evolving Grenville margin."}],"$":{"id":"l... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_53.txt | 09307 5 3.32695 501 0.25925 40 1489.4 1.1
R94-66, Aurdal granite, Fig. 8G
1 3gr,+75,cl,c,eu,pr 9 30.4 115 2 0.28 6874 0.09383 8 3.36778 497 0.26033 37 1504.6 1.5
2 10gr,+75,cl,eu,l-pr 18 57.1 217 2 0.24 40063 0.09386 5 3.38663 4 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_272.txt | icon svg{display:block;height:10px;width:10px}#onetrust-pc-sdk #clear-filters-handler{margin-top:20px;margin-bottom:10px;float:right;max-width:200px;text-decoration:none;color:#3860be;font-size:.9em;font-weight:bold;background-color:rgba(0,0,0,0);border-color:rgba(0,0,0,0);padding:1px | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_577.txt | --><span>km magmatic belt, the Sirdal Magmatic Belt (SMB). Previously mapped as granitic gneisses in many areas, the existence of this large, commonly undeformed and unmetamorphosed granitoid <a href="/topics/earth-and-planetary-sciences/batholith" title="Learn more about batholith from ScienceDirect's AI-generated To... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_17.txt | age estimate.
Zircon from one sample of the Flå granite pluton was
analysed by isotope dilution - thermal ionisation mass
spectrometry (ID–TIMS) at Washington University following the procedures outlined in Tucker et al. (1999;
Table 2). Ages were derived with the following decay constants: λ238U = 1.55125 10-10 y-1; ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_49.txt | group. A depositional age younger than 1.51 Ga is
nevertheless possible.
The Telemark sector displays a voluminous continental
1.19-1.13 Ga bimodal plutonic and volcanic suite associated with clastic sediments (Fig. 2; Laajoki et al. 2002;
Bingen et al. 2003). This suite is overlain by a cover of
sediments younger than... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_670.txt | the coeval paleomagnetic data from Laurentia do not support the traditionally envisaged Meso- to Neoproterozoic Baltica-Laurentia relationship either. Overall, the new data do not lend any support to the close connection between the two continents during the proposed Rodinia tenure but instead emphasize the problems w... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_701.txt | f–O isotopic data indicate that the 1050–930 Ma Sveconorwegian magmas show little isotopic fingerprint that are expected in an active subduction setting, as their formation witnessed significantly less input of sedimentary components and juvenile mantle-derived magmas than arc magmas generated in typical accretionary m... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_68.txt | 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 the Kongsberg and
Bamble sector. In Tobi, A.C. & Touret, J.L. (eds.), The deep Proterozoic crust in the north Altantic pro... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_21.txt | formation
are not discussed in this paper (Tucker et al. 1990;
Bingen et al. 2001b; Skår & Pedersen 2003). Continental
domains in the Sveconorwegian orogen are referred to
as sectors, segments or terranes in the literature. We use
the term terrane, in the sense recommended by the
glossary of the American Geological Ins... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_18.txt | :!0
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_834.txt | orogen. Local anatexis also may be important in other pegmatite provinces."}],"$":{"view":"all","id":"as010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab010","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstracts"},"pdf":{"urlType":"download","url":"/sci... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_44.txt | irine in SW Sweden: a record of Sveconorwegian (-Grenvillian) late-orogenic tectonic exhumation. Journal
of Metamorphic Geology 17, 127-141.
Möller, C., Andersson, J., Lundqvist, I. & Hellström, F.A. 2007: Linking
deformation, migmatite formation and zircon U-Pb geochronology in polymetamorphic gneisses, Sveconorwegian... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_241.txt | word;word-wrap:break-word}#onetrust-pc-sdk #no-results p span{font-weight:bold}#onetrust-pc-sdk #ot-fltr-modal{width:100%;height:auto;display:none;-moz-transition:.2s ease;-o-transition:.2s ease;-webkit-transition:2s ease;transition:.2s ease;overflow:hidden;opacity:1;right:0}#onetrust-pc | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_73.txt | Metamorphic Geology
23, 201-215.
Torsvik, T.H., Smethurst, M.A., Meert, J.G., Van der Voo, R., Mc Kerrow, W.S., Brasier, M.D., Sturt, B.A. & Walderhaug, H.J. 1996: Continental break up and collision in the Neoproterozoic and Paleozoic
- A tale of Baltica and Laurentia. Earth-Science Reviews 40, 229-
258.
Touret | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1206.txt | author","$$":[{"#name":"given-name","_":"A.C."},{"#name":"surname","_":"Tobi"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R.P.E."},{"#name":"surname","_":"Poorter"}]},{"#name":"author","$$":[{"#name":"given-name","_":"C."},{"#name":"surname","_":"Maijer"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":" | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_28.txt | 0.0719 0.0022 1.60 0.07 0.161 0.005 0.68 983 62 963 26 98.0
9 0.0726 0.0019 1.86 0.07 0.186 0.004 0.66 1004 54 1097 24 109.3
13 0.0727 0.0012 1.89 0.05 0.188 0.004 0.76 1005 34 1112 20 110.7
2 0.0733 0.0064 1.66 0.15 0.165 0 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1145.txt | "},{"#name":"last-page","_":"42"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0035"},"$$":[{"#name":"label","_":"Bingen et al., 2008b"},{"#name":"reference","$":{"id":"sbref0035","refId":"7"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-na... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_792.txt | "},"_":"The Late Mesoproterozoic Sirdal Magmatic Belt, SW Norway: Relationships between magmatism and metamorphism and implications for Sveconorwegian orogenesis"}],"floats":[],"footnotes":[],"attachments":[]},"vol-first":"265","vol-iss-suppl-text":"Volume 265","userSettings":{"forceAbstract":false,"creditCardPurchaseA... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_3.txt | ; Bingen et al. 2001a; Andersen et
al. 2004a; Åhäll & Connelly 2008). Lithologies show an
average younging towards the west. From east to west,
these are the 1660-1640 Ma Horred metavolcanic rocks,
the 1630-1590 Ma Åmål Formation and coeval Göteborg
granite suite, and the 1590-1520 Ma Stora Le-Marstrand
Formation and c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_234.txt | 0px}#onetrust-pc-sdk #ot-host-lst.ot-acc-txt{overflow:hidden;width:95%}#onetrust-pc-sdk.ot-host-hdr{position:relative;z-index:1;pointer-events:none;width:calc(100% - 125px);float:left}#onetrust-pc-sdk.ot-host-name,#onetrust-pc-sdk.ot-host-desc{display:inline-block;width: | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1295.txt | langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"M.W."},{"#name":"surname","_":"Schmidt"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A.B."},{"#name":"surname","_":"Thompson"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Epidote in calc-alkaline magmas: ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_30.txt | pegmatite dyke Zrn Pb-Pb 1409 ±20 Söderlund, 1996
South Särdal granite, pegmatite dyke, 3 Zrn U-Pb 1426 +9/-4 Christoffel et al., 1999
South Gåsanabbe mafic orthogneiss, paleosome, 5 Zrn U-Pb 1438 +12/-8 Christoffel et al., 1999
PZ Tåghusa streaky granite, CJA46 Zrn U-Pb 1442 ±9 Cec | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_10.txt | (.8); transform: scaleX(.8)}
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_457.txt | -child(odd),.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) tr:nth-child(odd) a{background:#f6f6f4}.ot-sdk-cookie-policy:not(#ot-sdk-cookie-policy-v2) td{border:none;border-bottom:1px solid #eee;position:relative;padding-left:50%}.ot-sdk-cookie-policy:not(#ot-sdk-cookie | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_593.txt | to assess the spatial (to identify from older granites) and temporal range of SMB magmatism. Data from 28 of these samples are previously unpublished (see Table 1). Several different techniques have been used to analyze these samples, including Laser-Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) at... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_398.txt | }
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background-color: #FFFFFF;
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_103.txt | neiss, paleosome, 1, T2 Am 207Pb/206Pb 2 934 c. Christoffel et al., 1999
South Gåsanabbe mafic orthogneiss, paleosome, 5 Am 207Pb/206Pb 2 935 ±5 Christoffel et al., 1999
South Garnet amphibolite, 9007 Am 206Pb/238U 3 945 ±2 Wang et al., 1998
South Titanite in garnet, eclogite boudin, Lilla Hammås, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_27.txt | ±3 and 880 ±3 Ma (Mulch et al.
2005). This estimate is consistent with two titanite ages
at 913 ±5 and 901 ±7 Ma and three amphibole 40Ar/39Ar
age spectra ranging from 893 ±14 to 861 ±36 Ma, giving
evidence for late-Sveconorwegian cooling between 910
and 860 Ma in the Telemarkia foot wall of the shear zone
(Heaman & S... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_464.txt | .ot-sdk-cookie-policy table tr:last-child td:last-child{border-bottom:0px}}
#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy h5,
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_46.txt | mode at 1508 ± 10 Ma (7 out
of 20 crystals) and minor modes at 1.98, 1.83, 1.80,
1.75, 1.63 Ga (sample B98-43; Tables 1, 3; Figs. 3, 9A).
The 1508 ± 10 Ma mode demonstrates that the sediment
was partly sourced in a catchment coeval to the Rjukan
group and thus can not represent a basement to this
group. The sediments ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1020.txt | name":"organization","_":"Department of Geology, Lund University"},{"#name":"address-line","_":"Sölvegatan 12"},{"#name":"city","_":"Lund"},{"#name":"postal-code","_":"SE-223 62"},{"#name":"country","_":"Sweden"}]}]},{"#name":"affiliation","$":{"id":"aff0010"},"$$":[{"#name":"label","_":"b"},{"#name":"textfn","_":"Depa... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1040.txt | ":"author","$":{"id":"au025","author-id":"S0301926816300146-e6b96f96cd0f079e6d83bc35a292fc43"},"$$":[{"#name":"given-name","_":"Liang"},{"#name":"surname","_":"Liu"},{"#name":"cross-ref","$":{"refid":"af005","id":"c0105"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"author","$":{"id":" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_47.txt | s) in the Pb/U and 207Pb/206Pb ratios calculated following Ludwig (1980)
Table 2. ID-TIMS U-Pb data on zircon, Flå granite pluton
Fig. 2. Simplified geologic map of a portion of the Sveconorwegian belt, east of the Oslo rift, following Nordgulen (1999). The map shows the location
of granitoid samples FUN26, 33, and 38.... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_127.txt | ...a,
jsAttributes: {
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no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir7.txt | part7 -------------------
Production[edit]
To obtain the contents of the oil reservoir, it is usually necessary to drill into the Earth's crust, although surface oil seeps exist in some parts of the world, such as the La Brea Tar Pits in California and numerous seeps in Trinidad. Factors that affect the quantity of rec... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1079.txt | id":"crf0165","refid":"cor0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"⁎"}]},{"#name":"e-address","$":{"id":"eadd0005","type":"email"},"_":"spenchristoph@gmail.com"},{"#name":"e-address","$":{"id":"eadd0010","type":"email"},"_":"chriss@bgs.ac.uk"}]},{"#name":"author","$":{"id":"aut0010"},"$$":[{"#name":"given-na... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_806.txt | encedirectassets.com/prod/258cbf7ffb0f544990f7288c6b5a2362d06486df/image/elsevier-non-solus.png","logoAltText":"Elsevier"},"publicationCoverImageUrl":"https://ars.els-cdn.com/content/image/1-s2.0-S0301926815X00088-cov150h.gif"},"useEnhancedReader":true,"volRange":"265","features":["keywords","references","preview"]," | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_66.txt | Research 124, 215-241.
Bingen, B. & Stein, H.J. 2003: Molybdenite Re–Os dating of biotite
dehydration melting in the Rogaland high-temperature granulites,
S Norway. Earth and Planetary Science Letters 208, 181-195.
Bingen, B., Skår, Ø., Marker, M., Sigmond, E.M.O., Nordgulen, Ø.,
Ragnhildstveit, J., Mansfeld, J., Tuck... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1279.txt | ","$$":[{"#name":"given-name","_":"N.M.W."},{"#name":"surname","_":"Roberts"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Slagstad"}]}]},{"#name":"title","$$":[{"#name":"maintitle","$$":[{"#name":"__text__","_":"Continental growth and reworking on the edge of the Columbia and Rodin... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_38.txt | sillimanite-rich
gneiss, orthoamphibole-cordierite gneiss, and calc-silicate
gneiss (Modum, Kragerø and Nidelva complexes; Starmer
1985). Detrital zircon data constrain deposition of the
metagreywacke-metapelite complexes in Bamble to be
younger than 1.45 and 1.38 Ga (2 samples) and the
quartzite complexes to be young... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_102.txt | const n = (0, r(4402).Rl)();
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_779.txt | The orogenic evolution of SW Norway is characterized by emplacement of large volumes of granitic magma and more localized UHT metamorphism, which is quite different from the widespread, long-lasting metamorphic evolution observed in the Grenville Province, and may point to different tectonic regimes for the two provinc... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_4.txt | ova
1993). These include the Western Gneiss Complex, the
large basement window in Western Norway, and nappes
attributed to the Middle Allochthon, namely the Lindås,
Dalsfjord and Jotun Nappes (Tucker et al. 1990; Bingen et
al. 2001b; Corfu & Andersen 2002; Skår & Pedersen 2003;
Lundmark et al. 2007; Lundmark & Corfu 20... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_85.txt | d, (a = n, function () {
var e = this;
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_640.txt | </h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Rev. Mineral. Geochem.</h3></div><div class="series">(2003)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>P.G. </span>DeCelles</span><em> et al.</em></spa... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_9.txt | ...t
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_58.txt | s = /iPad|iPhone|iPod/.test(navigator.userAgent),
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_42.txt | : U-Pb
geochronological evidence for significant Grenvillian activity in
the Bamble area, Norway. Terra Abstracts, supplement to Terra Nova
3, 504.
Kullerud, L. & Dahlgren, S.H. 1993: Sm-Nd geochronology of Sveconorwegian granulite facies mineral assemblages in the Bamble
shear belt, south Norway. Precambrian Research ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_130.txt | F.length-2,2)}return k}function J(k){k=k.replace(/rn/g,"n");var d="";for(var F=0;F<k.length;F++){var x=k.charCodeAt(F);if(x<128){d+=String.fromCharCode(x)}else{if((x>127)&&(x<2048)){d+=String.fromCharCode((x>>6)|192);d+=String.fromCharCode((x&63)|128)} | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_67.txt | adsen, 2000
Rogaland Charnockite gneiss, Gyavatnet, NR19A Zrn U-Pb 1035 ±6 Möller et al., 2002
Telemark Fennefoss granodioritic augen gneiss, B613 Zrn U-Pb 1035 ±3 Bingen & van Breemen, 1998
Rogaland Rosskreppfjord granite Zrn U-Pb 1036 +23/-22 Andersen et al., 2002
Rogaland Charnockite gneiss, Gy |
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