Mineralne parageneze Pb-Zn ležišta Babe-Kosmaj (Srbija)

Mineral paragenesis of the ore deposit Babe-Kosmaj (Serbia)

  • Biljana Zrnić University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
  • Ljubomir Cvetković University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
  • Ljuban Obradović University of Belgrade, Faculty of Mining and Geology, Đušina 7, 11000 Belgrade, Serbia.
Keywords: galena, sphalerite, mineral parageneses, Babe-Kosmaj, Serbia

Abstract

The complex polymetallic sulphide mineralization of Pb, Zn and Cu as major and Ni, Co, Bi and U as minor constituents in the Babe ore deposit was investigated. By using the ore microscopy method a relatively complex mineral composition, including textural and fabric relationships was determinated. Four mineral stages are outlined: contact metamorphic, pneumatolytic, hydrothermal and supergene. The sulphide mineralization has been formed during the hidrothermal stage and in domain of that the several mineral paragenses were estabished. The possible crystallization sequences of minerals and paragenses are presented on the sheme of succession.

 

Published
1998-12-19
How to Cite
Zrnić, B., Cvetković, L. and Obradović, L. (1998) “Mineralne parageneze Pb-Zn ležišta Babe-Kosmaj (Srbija)”, Geološki anali Balkanskoga poluostrva, 62(1), pp. 267-285. Available at: https://gabp.rgf.rs/index.php/gabp/article/view/357 (Accessed: 22December2024).
Issue
Vol 62 No 1 (1998): Geološki anali Balkanskoga poluostrva
Section
Original Scientific Paper

Copyright (c) 1998 Geološki anali Balkanskoga poluostrva

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