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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_362.txt | 100% - 23px)}#onetrust-pc-sdk.ot-btn-container button{max-width:none;letter-spacing:.01em}#onetrust-pc-sdk #close-pc-btn-handler{top:10px;right:17px}#onetrust-pc-sdk p{font-size:.7em}#onetrust-pc-sdk #ot-pc-hdr{margin:10px 10px 0 5px;width:calc(100% - 15px)}# | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_4.txt | Zrn U-Pb 1325 ±18 Andersson, 2001
Kärra granite, pegmatite, DC200020 Zrn U-Pb 1325 ±8 Austin Hegardt et al., 2007
Chalmers gabbro, felsic facies, DC9723 Zrn U-Pb 1333 ±8 Kiel et al., 2003
Hästefjorden granite Zrn U-Pb 1334 +7/-3 Piontek et al., 1998
Askim granite, Lindome, DC9913 Zrn | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1265.txt | of complex sheeted zones during recycling of older magmatic units into younger: Sawmill Canyon area, Tuolumne batholith, Sierra Nevada, California"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"J. Volcanol. Geotherm. Res."}]},{"#name":"volume... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_15.txt | plating beneath the Oslo rift? Terra Nova
17, 129-134.
Eliasson, T. & Schöberg, H. 1991: U-Pb dating of the post-kinematic
Sveconorwegian (Grenvillian) Bohus granite, SW Sweden: evidence
of restitic zircon. Precambrian Research 51, 337-350.
Eliasson, T., Ahlin, S. & Petersson, J. 2003: Emplacement mechanism
and thermob... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_2.txt | of any model, the presence of Palaeoproterozoic and Archaean zircon populations in all clastic
sediment sequences deposited between c. 1500 and 1060
Ma in the Telemarkia, Bamble and Kongsberg Terranes
implies that these terranes were situated at the margin of
an evolved craton during the Mesoproterozoic (Fig. 10).
A f... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1463.txt | 2">These cookies allow us to count visits and traffic sources so we can measure and improve the performance of our site. They help us to know which pages are the most and least popular and see how visitors move around the site.</p><div class="ot-hlst-cntr"><button class="ot-link-btn category-host-list-handler" aria-lab... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_7.txt | ., Marker, M., Sigmond, E. M. O., Nordgulen, Ø., Ragnhildstveit, J., Mansfeld, J., Tucker, R. D. & Liégeois, J.-P.: Timing of continental building in the Sveconorwegian orogen, SW Scandinavia. Norwegian Journal of Geology, Vol. 85, pp. 87-116. Trondheim 2005. ISSN 029-196X.
The timing of continental building in the Sve... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1331.txt | ":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"J."},{"#name":"surname","_":"Vander Auwera"}]},{"#name":"author","$$":[{"#name":"given-name","_":"O."},{"#name":"surname","_":"Bolle"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Dupont"}]},{"#name":"author","$$":... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_31.txt | in some metasediment
samples suggest a continental margin setting with sources
in the volcanic arc itself and in an evolved Palaeoproterozoic continent, probably Fennoscandia, behind the
arc (Andersen et al. 2004). The Idefjorden terrane is
interpreted as a composite and increasingly mature arc
formed between 1.66 and... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_100.txt | window.addEventListener(e, t, a(r, n));
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1455.txt | p class="ot-acc-grpdesc ot-category-desc" id="ot-desc-id-1">These cookies are necessary for the website to function and cannot be switched off in our systems. They are usually only set in response to actions made by you which amount to a request for services, such as setting your privacy preferences, logging in or fill... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_2.txt | -Pb geochronological data are reported for 21
samples of magmatic and metasedimentary rocks in the
previously poorly investigated western part of the
Sveconorwegian orogen. These data are combined with
published data (e.g. Åhäll et al. 2000; Söderlund et al.
2002; Andersen et al. 2004), to provide an overview of the
ma... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_270.txt | float:left;padding-bottom:10px;font-size:1em;width:100%}#onetrust-pc-sdk.ot-cat-grp{margin-top:10px}#onetrust-pc-sdk.ot-cat-item{line-height:1.1;margin-top:10px;display:inline-block;width:100%}#onetrust-pc-sdk.ot-btn-container{text-align:right}#onetrust-pc-sdk.ot-btn | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_36.txt | neiss strong B02-027 401374 6584548 Bt, Ttn SIMS 17 16 2.7 1499 12 intrusion 9D
Sauda Vanvik granite gneiss weak B00-149 349902 6604087 Bt, Ep, Ttn LA-ICPMS 11 11 0.51 1499 11 intrusion 10H
Suldal Sand augen gneiss medium B00-137 345552 6596393 Bt, Ttn LA-ICPMS 11 10 0.25 1501 11 intrusion 10E
Suldal | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_109.txt | ism is recorded east
of the Mylonite Zone, and fading away to the east. Secondary titanite at 976 ±4 to 956 ±6 Ma dates this deformation (Table 5; Söderlund et al. 1999).
The Eastern Segment south of lake Vänern shows penetrative amphibolite-facies metamorphism. Mafic boudins
display high-pressure granulite-facies and ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_16.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_56.txt | en and Telemarkia Terranes (Fig. 6). They can
thus result from interaction between these two terranes.
Cornell and Austin Hegardt (2004) observed that all
magmatic suites and metamorphic events older than c.
980 Ma in the Idefjorden Terrane are distinct from those
in the Eastern Segment. Consequently, they propose that... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_297.txt | nd-item>button:focus{outline:#000 solid 2px}#onetrust-pc-sdk.ot-vnd-item>button{position:absolute;cursor:pointer;width:100%;height:100%;margin:0;top:0;left:0;z-index:1;max-width:none;border:none}#onetrust-pc-sdk.ot-vnd-item>button[aria-expanded=false]~.ot-acc-txt{margin-top:0;max- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_12.txt |
University, MO 63130, St. Louis, USA; J. –P. Liégeois, Musée royal de l'Afrique centrale, B-3080 Tervuren, Belgium.
spectrometry (LA-ICPMS) at the Geological Survey of
Norway, Trondheim (Table 5). For the SIMS and
LA-ICPMS analyses, 20 to 60 zircon crystals were
mounted in epoxy and polished to approximately half
thic... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_54.txt | (Table 4; Christoffel et
al. 1999; Söderlund et al. 2002; Möller et al. 2007).
The intensity of Sveconorwegian reworking and metamorphism increases from north to south and from east
to west (Johansson et al. 1991; Söderlund et al. 1999).
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, S... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_92.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_28.txt | al monzodiorite-granite plutonism, local-scale decompression melting and a regionalscale drop in pressure (Vander Auwera et al. 2003; Tomkins et al. 2005; Bogaerts et al. 2006). The regional N-S
trending structural pattern and NE-SW trending lineation in a c. 960 Ma granite (Bolle et al. 2003b) suggest
a N-S to NE-SW d... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1282.txt | ":[{"#name":"given-name","_":"N.M.W."},{"#name":"surname","_":"Roberts"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T."},{"#name":"surname","_":"Slagstad"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R.R."},{"#name":"surname","_":"Parrish"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M.J." | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_68.txt | ärer et al., 1996
Hidra monzonorite, charnockite dyke R Zrn 931 ±10 Pasteels et al., 1979
Helleren anorthosite, 75-65 R Zrn 932 ±3 Schärer et al., 1996
Åna-Sira anorthosite, 92-21 R Zrn 932 ±3 Schärer et al., 1996
Vehuskjerringa granite T Zrn 934 ±5 Dahlgren et al., 1990 b
Vrådal granite, 081696- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_84.txt | Zrn 1428±9 Am Grey unveined orthogneiss, Dagsås U-Pb SIMS 6 Söderlund et al., 2002 PZ Zrn 1437±21 Am Åker metabasite U-Pb SIMS 4 Söderlund et al., 2004 South Zrn 1449±11 Am Veined granitic gneiss, Gällared N U-Pb SIMS 15 Söderlund et al., 2002 South Zrn 1464±8 Am Grey orthogneiss with veinlets, Gäll | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_47.txt | of the orogen,
and suggests closure of an ocean basin between
Telemarkia and the Idefjorden terrane. (3) As argued
earlier, the Bamble-Kongsberg sector contains lithologies characteristic of both the Idefjorden terrane and
Telemark sector and can thus be considered as a mixture of rocks of different origins (Fig. 2). ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1223.txt | thorne"}]},{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Kato"}]},{"#name":"author","$$":[{"#name":"given-name","_":"H.J."},{"#name":"surname","_":"Kisch"}]},{"#name":"author","$$":[{"#name":"given-name","_":"V.G."},{"#name":"surname","_":"Krivovichev"}]},{"#name":"author","$$":[{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1136.txt | _":"Weis"}]},{"#name":"author","$$":[{"#name":"given-name","_":"J."},{"#name":"surname","_":"Michot"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"K-rich calc-alkaline augen gneisses of Grenvillian age in SW Norway: mingling of mantle-derived and crustal components"}]}]},{"#name":"host","$$":[{"#name":"issue","... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_9.txt | Austin Hegardt, E. 2004: Abstract. When, where and
how did the Sveconorwegian terranes of Sweden meet? GFF 126,
20.
Corti, G., Bonini, M., Conticelli, S., Innocenti, F., Manetti, P. & Sokoutis, D. 2003: Analogue modelling of continental extension: a review
focused on the relations between the patterns of deformation a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1006.txt | ":"par0005"},"#name":"para","_":"We obtained precise U–Pb baddeleyite ages for the Rincón del Tigre and the Huanchaca intrusions."}],"$":{"id":"lsti0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$$":[{"#name":"__text__","_":"The 1110–1112"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_134.txt | ed", e);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_58.txt | sdk-ten.ot-sdk-columns,#ot-sdk-cookie-policy.ot-sdk-ten.ot-sdk-columns{width:82.6666666667%}#onetrust-banner-sdk.ot-sdk-eleven.ot-sdk-columns,#onetrust-pc-sdk.ot-sdk-eleven.ot-sdk-columns,#ot-sdk-cookie-policy.ot-sdk-eleven.ot-sdk- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_950.txt | reim–Sokndal Layered Intrusion at ca. 930"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"Ma (see Bingen et al., 2008a, Bingen et al., 2008b and references therein). This picture, however, has become significantly more complicated recently with the proposed identification of a UHT event at ca. 1006"},{"#na... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1141.txt | page","_":"1440"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0030"},"$$":[{"#name":"label","_":"Bingen et al., 2008a"},{"#name":"reference","$":{"id":"sbref0030","refId":"6"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"B."},{"... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_18.txt | from the data. Only element and isotope ratios
are manipulated (Table 5). Concordia diagrams and age
calculations are generated with the ISOPLOT program
(Ludwig 2001). For the ten samples analysed in this
study, upper intercept ages and weighted mean
207Pb/206Pb ages are statistically equivalent. We choose
to quote th... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_95.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_746.txt | ><span class="pps-count">31</span></li></ul></div></div></div><div><div class="pps-branding pps-branding-bottom"><img alt="plumX logo" src="//cdn.plu.mx/3ba727faf225e19d2c759f6ebffc511d/plumx-logo.png" class="plx-logo"></div><a target="_blank" href="https://plu.mx/plum/a/?doi=10. | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_51.txt | oscandia: LAM-ICPMS
U-Pb and Lu-Hf isotope evidence from granites and gneisses in
Telemark, southern Norway. Lithos 93, 273-287.
Andersson, J., Söderlund, U., Cornell, D., Johansson, L. & Möller, C.
1999: Sveconorwegian (-Grenvillian) deformation, metamorphism
and leucosome formation in SW Sweden, SW Baltic Shield: con... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1285.txt | ","_":"523"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0245"},"$$":[{"#name":"label","_":"Romer, 1996"},{"#name":"reference","$":{"id":"sbref0245","refId":"49"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"R.L."},{"#name":"sur... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_117.txt | banner-sdk.ot-iab-2 #onetrust-policy,#onetrust-banner-sdk.ot-iab-2.banner-option{width:100%}#onetrust-banner-sdk.ot-iab-2 #onetrust-button-group #onetrust-accept-btn-handler,#onetrust-banner-sdk.ot-iab-2 #onetrust-button-group #onetrust-reject-all-handler,#onetrust-banner-sd | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1099.txt | data for the volcanosedimentary units in the Bandak succession record an episode of intracontinental extension, associated with formation of a series of intermontane basins. We hypothesize that these localized basins were formed at different stages of extensional collapse following a pulse of regional orogenesis. The ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1444.txt | pdf_bridge_https_www_sciencedirect_com" style="display: none; margin: 0; padding: 0; border: 0px none; overflow: hidden;" frameborder="0" border="0" scrolling="no" allowtransparency="true" tabindex="-1" hidden="true" title="" role="presentation" src="https://brxt-research.mendeley.com/"></iframe><div class="js-react-mo... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_32.txt | in the north Atlantic provinces,
NATO-ASI C158, 309-322. Reidel, Dordrecht.
Gorbatschev, R. & Bogdanova, S. 1993: Frontiers in the Baltic Shield.
Precambrian Research 64, 3-21.
Hageskov, B. 1985: Constrictional deformation of the Koster dyke
swarm in a ductile sinistral shear zone, Koster islands, SW Sweden.
Bulletin ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_443.txt | weight:bold}.ot-sdk-cookie-policy.ot-mobile-border{display:none}.ot-sdk-cookie-policy section{margin-bottom:2em}.ot-sdk-cookie-policy table{border-collapse:inherit}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy{font-family:inherit;font-size:1rem}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy h3, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_1.txt | Haas et al.
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia
Fig. 9. Schematic
model for orogenic
evolution of the
Sveconorwegian
orogeny.
64
1999; Bingen et al. 2001a; 2002; 2003; Andersen & Laajoki
2003). All detrital zircon populations can be accounted
for by felsic sou... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_84.txt | ._A.XMLHttpRequest = function (e) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_204.txt | rust-pc-sdk.ot-chkbox label::after{height:5px;width:9px;border-left:3px solid;border-bottom:3px solid;transform:rotate(-45deg);-o-transform:rotate(-45deg);-ms-transform:rotate(-45deg);-webkit-transform:rotate(-45deg);left:4px;top:5px}#onetrust-pc-sdk.ot-label-txt{display:none}#onetrust-pc-sdk | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_388.txt | #onetrust-consent-sdk #onetrust-pc-sdk #ot-host-lst.ot-host-name a,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_630.txt | ="title">Geol. Soc. Am. Mem.</h3></div><div class="series">(1983)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>B. </span>Bingen</span><em> et al.</em></span><h3 class="title">K-rich calc-alkaline augen gneisses of Grenvillian age in SW Nor... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_57.txt | areas = areas.slice(0, 5).join('>');
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1333.txt | Duchesne"}]},{"#name":"author","$$":[{"#name":"given-name","_":"N."},{"#name":"surname","_":"Mattielli"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Bogaerts"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Source-derived heterogeneities in the composite (charnockite-granite)... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_155.txt | HRwczovL2RvdWJsZWNsaWNrLm5ldDo0NDMiLCJmZWF0dXJlIjoiV2ViVmlld1hSZXF1ZXN0ZWRXaXRoRGVwcmVjYXRpb24iLCJleHBpcnkiOjE3MTk1MzI3OTksImlzU3ViZG9tYWluIjp0cnVlfQ=="><meta http-equiv="origin- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_961.txt | aut0015"},"$$":[{"#name":"given-name","_":"C.V."},{"#name":"surname","_":"Spaggiari"},{"#name":"cross-ref","$":{"id":"crf0060","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"affiliation","$":{"id":"aff0005"},"$$":[{"#name":"label","_":"a"},{"#name":"textfn","_":"Geological Survey of W... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1098.txt | a mantle source that had been previously enriched through subduction, and variable contamination from older continental crust, or melts derived from it (i.e. the Dalaå Formation). The mafic lithologies reveal decreasing amounts of crustal contamination higher in the section, compatible with increasing amounts of exten... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_60.txt | 96 15 1512 30 101.1 08a 81 161 35 18836 0.09349 0.75 3.362 2.36 0.2608 2.24 0.95 1498 14 1494 30 99.8 20a 76 83 27 29121 0.09359 0.80 3.263 2.37 0.2529 2.23 0.94 1500 15 1453 29 96.9 05a 162 112 54 87260 0.09376 0.63 3.353 2.32 0.2594 2.23 0.96 1503 12 14 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_133.txt | e, t) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1226.txt | author","$$":[{"#name":"given-name","_":"D.C."},{"#name":"surname","_":"Smith"}]},{"#name":"author","$$":[{"#name":"given-name","_":"N.C.N."},{"#name":"surname","_":"Stephenson"}]},{"#name":"author","$$":[{"#name":"given-name","_":"L."},{"#name":"surname","_":"Ungaretti"}]},{"#name":"author","$$":[{"#name":"given-name"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_833.txt | Thus, the Grenville peak postdates the Sveconorwegian Group 1 peak by about 30 Ma. These pegmatites formed in similar orogenic settings, implying that similar tectono-metamorphic developments along the Grenville–Sveconorwegian orogenic belt were diachronous."},{"$":{"view":"all","id":"sp0025"},"#name":"simple-para","_... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_77.txt | -Pb 1205 ±9 Heaman & Smalley, 1994
Telemark Vråvatn Co, Granodioritic gneiss, Kviteseid, TA01-14 Zrn U-Pb 1205 ±8 Andersen et al., 2007
Telemark Vråvatn Co, Granitic gneiss, Kviteseid, TA01-15 Zrn U-Pb 1208 ±6 Andersen et al., 2007
Telemark Vråvatn Co, Granitic gneiss, Fossø | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_377.txt | onetrust-pc-sdk h4,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_63.txt | grain
Pb evaporation dating of complex zircons from a pegmatite in the
high-grade gneisses of southwestern Sweden. Lithos 38, 93-105.
Söderlund, U., Jarl, L.G., Persson, P.O., Stephens, M.B. & Wahlgren,
C.H. 1999: Protolith ages and timing of deformation in the eastern,
marginal part of the Sveconorwegian orogen, south... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_89.txt | ’Nions & Baadsgaard, 1971
Bamble Hovdefjell charnockite gneiss Zrn U-Pb 1168 ±2 Råheim unpublished
Bamble Tromøy gabbro-tonalite complex, Hisøy tonalite, HGG Zrn U-Pb 1178 ±9 Andersen et al., 2004
Bamble Tromøy gabbro-tonalite complex, 4 samples Zrn U-Pb 1198 ±13 Knudsen & Andersen, 1999
Kongs | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_48.txt | to metarhyolite of the Rjukan group. Norges geologiske undersøkelse Bulletin 440, 19-26.
Andersen, T. & Laajoki, K. 2003: Provenance characteristics of Mesoproterozoic metasedimentary rocks from Telemark, South Norway:
a Nd-isotope mass-balance model. Precambrian Research 126, 95-
122.
Andersen, T., Griffin, W.L., Jac... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_31.txt | um metapluton forms a
foliated boudin parallel to the regional NW-SE structural
trend. It ranges in composition from diorite to tonalite
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 91
Fig. 4. Geological sketchmap of the Sauda-Suldal area with a summary of sampling and result... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_126.txt | )|(F&(~k))}function p(d,F,k){return(d^F^k)}function n(d,F,k){return(F^(d|(~k)))}function u(G,F,aa,Z,k,H,I){G=K(G,K(K(r(F,aa,Z),k),I));return K(L(G,H),F)}function f(G,F,aa,Z,k,H,I){G=K(G, | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_590.txt | u-h4 u-margin-l-top u-margin-xs-bottom">Field description and petrography of the Sirdal Magmatic Belt</h2><p id="par0080">In the following section we describe the different lithologies that constitute the SMB, and also the nature of xenoliths and host rocks found within and around the batholith. Determination of rock ... | |
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