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Sökning: id:"swepub:oai:DiVA.org:ltu-3483" > Time constraints on...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00005022naa a2200529 4500
001oai:DiVA.org:ltu-3483
003SwePub
008160929s2016 | |||||||||||000 ||eng|
009oai:DiVA.org:uu-297775
024a https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-34832 URI
024a https://doi.org/10.1016/j.precamres.2016.03.0112 DOI
024a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-2977752 URI
040 a (SwePub)ltud (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Kampmann, Tobiasu Luleå tekniska universitet,Geovetenskap och miljöteknik,Lulea Univ Technol, Dept Civil Environm & Nat Resources Engn, Div Geosci, SE-97187 Lulea, Sweden.4 aut0 (Swepub:ltu)tobkam
2451 0a Time constraints on magmatism, mineralisation and metamorphism at the Falun base metal sulphide deposit, Sweden, using U-Pb geochronology on zircon and monazite
264 1b Elsevier,c 2016
338 a electronic2 rdacarrier
500 a Validerad; 2016; Nivå 2; 20151014 (tobkam)
520 a U–Th–Pb (zircon and monazite) ion probe data have provided constraints on the timing of emplacement and metamorphism of magmatic rocks close to the Palaeoproterozoic, Falun base metal sulphide deposit in the Bergslagen lithotectonic unit, Fennoscandian Shield, Sweden, and, thereby the timing of mineralisation. Hydrothermal alteration and mineralisation at Falun are constrained to a short interval of several million years between a 207Pb/206Pb weighted average age of 1894 ± 3 Ma for a rhyolitic sub-volcanic rock in the felsic volcanic to sub-volcanic host rock suite, and a 207Pb/206Pb weighted average age of 1891 ± 3 Ma for a post-sulphide, porphyritic dacite dyke. Magmatism also included the emplacement of granite plutons with igneous crystallization ages of 1894 ± 3, 1894 ± 2 Ma and 1893 ± 3 Ma. The felsicsub-volcanic to volcanic activity and the emplacement of dacite dykes and granite plutons overlap in age within their respective analytical uncertainties, indicating hydrothermal alteration and sulphide mineralisation inside a narrow time span of intense magmatic activity, and burial of the supracrustal rocks.Two distinct patchy and homogeneous metamorphic monazite types in a felsic volcanic rock around and hydrothermally altered rocks at the Falun deposit yield 207Pb/206Pb weighted average ages of 1831 ± 8 Ma and 1822 ± 5 Ma, respectively. These ages fall well within the temporal range of a younger1.84–1.81 Ga (M2) metamorphic episode during the 2.0–1.8 Ga Svecokarelian orogeny, with the older episode (M1) inside the Bergslagen lithotectonic unit at around 1.86 Ga. This shows the major influence of the M2 event in the north-western part of this unit, leading to a complete resetting of the U–Th–Pb isotopesystem in monazite.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Multidisciplinär geovetenskap0 (SwePub)105032 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geosciences, Multidisciplinary0 (SwePub)105032 hsv//eng
653 a Falun deposit
653 a Fennoscandian Shield
653 a SIMS U–Pb geochronology
653 a Zircon
653 a Monazite
653 a Svecokarelian orogeny
653 a Ore Geology
653 a Malmgeologi
700a Stephens, Michaelu Luleå tekniska universitet,Geovetenskap och miljöteknik,Sveriges Geologiska Undersökning,Lulea Univ Technol, Dept Civil Environm & Nat Resources Engn, Div Geosci, SE-97187 Lulea, Sweden.;Geol Survey Sweden, Box 670, SE-75128 Uppsala, Sweden.4 aut0 (Swepub:ltu)micste
700a Ripa, Magnusu Sveriges Geologiska Undersökning,Geol Survey Sweden, Box 670, SE-75128 Uppsala, Sweden.4 aut
700a Hellström, Fredriku Sveriges Geologiska Undersökning,Geol Survey Sweden, Box 670, SE-75128 Uppsala, Sweden.4 aut
700a Majka, Jaroslawu Uppsala universitet,Mineralogi, petrologi och tektonik,AGH Univ Sci & Technol, Fac Geol Geophys & Environm Protect, Al Mickiewicza 30, PL-30059 Krakow, Poland.4 aut0 (Swepub:uu)jarma730
710a Luleå tekniska universitetb Geovetenskap och miljöteknik4 org
773t Precambrian Researchd : Elsevierg 278, s. 52-68q 278<52-68x 0301-9268x 1872-7433
856u https://doi.org/10.1016/j.precamres.2016.03.011y Fulltext
856u https://ltu.diva-portal.org/smash/get/diva2:976341/FULLTEXT01.pdfx primaryx Raw objecty fulltext:print
856u http://ltu.diva-portal.org/smash/get/diva2:976341/FULLTEXT01
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-3483
8564 8u https://doi.org/10.1016/j.precamres.2016.03.011
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-297775

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