| dc.contributor.author | Andráš, Peter | |
| dc.contributor.author | Chovan, Martin | |
| dc.contributor.author | Dirner, Vojtech | |
| dc.contributor.author | Král, Ján | |
| dc.contributor.author | Bachlinski, Robert | |
| dc.date.accessioned | 2010-11-22T12:48:38Z | |
| dc.date.available | 2010-11-22T12:48:38Z | |
| dc.date.issued | 2010 | |
| dc.identifier.citation | Carpathian Journal of Earth and Environmental Sciences. 2010, vol. 5, no. 2, p. 71-80. | en |
| dc.identifier.issn | 1842-4090 | |
| dc.identifier.uri | http://hdl.handle.net/10084/83450 | |
| dc.description | Článek je přístupný po bezplatné registraci na webu vydavatele. | |
| dc.description.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. | en |
| dc.language.iso | Neuvedeno | en |
| dc.publisher | North University of Baia Mare, Faculty of Mineral Resources and Environment | en |
| dc.relation.ispartofseries | Carpathian Journal of Earth and Environmental Sciences | en |
| dc.relation.uri | http://www.ubm.ro/sites/CJEES/viewTopic.php?topicId=92 | |
| dc.subject | stibnite | en |
| dc.subject | gudmundite | en |
| dc.subject | galena | en |
| dc.subject | Pb-isotopes | en |
| dc.subject | model ages | en |
| dc.subject | orogenic lead | en |
| dc.subject | crustal lead | en |
| dc.title | Pb-isotope study in Sb-mineralisation from Western Carpathian (Slovakia) | en |
| dc.type | article | en |
| dc.identifier.location | Není ve fondu ÚK | en |
| dc.identifier.wos | 000283618800008 | |