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dc.contributor.authorAndráš, Peter
dc.contributor.authorChovan, Martin
dc.contributor.authorDirner, Vojtech
dc.contributor.authorKrál, Ján
dc.contributor.authorBachlinski, Robert
dc.date.accessioned2010-11-22T12:48:38Z
dc.date.available2010-11-22T12:48:38Z
dc.date.issued2010
dc.identifier.citationCarpathian journal of earth and environmental sciences. 2010, vol. 5, no. 2, p. 71-80.en
dc.identifier.issn1842-4090
dc.identifier.urihttp://hdl.handle.net/10084/83450
dc.description.abstractThe article present the comparison of the Pb-isotope study of antimony-ores from important Sb-mineralisation of Western Carpathian: from Tatric unit (Pezinok, Kuchyňa, Pernek, Dúbrava, Magurka, Lom, Trangoška, Jasenie, Kriváň deposits and occurrences), Gemeric unit (Helcmanovce, Grexa and Poproč deposits) and from Eastern Slovakian neovolcanites (Zlatá Baňa). The study is compared with results of previous investigations of affiliated galena mineralisation. The lead is of a crustal origine. The lead from Taric and that from Gemeric unit (and Eastern Slovakian Neovolcanites) seems to be derived from different reservoirs.en
dc.language.isoNeuvedenoen
dc.publisherNorth University of Baia Mare, Faculty of Mineral Resources and Environmenten
dc.relation.ispartofseriesCarpathian journal of earth and environmental sciencesen
dc.subjectstibniteen
dc.subjectgudmunditeen
dc.subjectgalenaen
dc.subjectPb-isotopesen
dc.subjectmodel agesen
dc.subjectorogenic leaden
dc.subjectcrustal leaden
dc.titlePb-isotope study in Sb-mineralisation from Western Carpathian (Slovakia)en
dc.typearticleen
dc.identifier.locationNení ve fondu ÚKen
dc.identifier.wos000283618800008


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