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You are here: Home » Past Issues » Volume 5, 2010 - Number 2 » Pb-ISOTOPE STUDY IN Sb-MINERALISATION FROM WESTERN CARPATHIAN (SLOVAKIA)


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Peter ANDRÁŠ1,2, Martin CHOVAN3, Vojtech DIRNER4, Ján KRÁĽ5 & Robert BACHLINSKI6
1Faculty of Natural Sciences,, Matej Bel University, Tajovského 40, 974 01 Banská Bystrica
2Geological Institute, Slovak Academy of Sciences, Ďumbierska 1, 974 01 Banská Bystrica, Slovakia, andras@savbb.sk
3Comenius University, Mlynská dolina G, 842 15 Bratislava, Slovakia, chovan@fns.uniba.sk
4State Geological Institute of Dionýz Štúr, Mlynská dolina 1, 842 15 Bratislava, Slovakia
5VŠB-Technical University of Ostrava, 17. listopadu, 15/2172, 708 33 Ostrava – Poruba; Vojtech.dirner@vsb.cz
6Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818, Warszawa, Poland

Pb-ISOTOPE STUDY IN Sb-MINERALISATION FROM WESTERN CARPATHIAN (SLOVAKIA)

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Abstract: The 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.

Keyword: stibnite, gudmundite, galena, Pb-isotopes, model ages, orogenic lead, crustal lead


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