Trepça Ore Belt and Stan Terg mine - Geological overview and interpretation, Kosovo (SE Europe)

Authors

  • Sylejman Hyseni
  • Bedri Durmishaj
  • Bislim Fetahaj
  • Ferat Shala
  • Avdullah Berisha
  • Duncan Large

DOI:

https://doi.org/10.5474/geologija.2010.006

Abstract

The Trepça Belt of Pb-Zn-Ag mineralization is located within the NNW-SSE trending Vardar zone. The Belt extends for over 80 km, and supported five mines during the period 1930-2008. It contains a number of the other Pb-Zn occurrences too. The replacement and vein type mineralization is hosted primarily by Mesozoic carbonates, but also occasionally by amphibolites, and displays a clear structural control. Mineralization is spatially and genetically related to Neogene andesite-dacite extrusives and sub-volcanic intrusives. Only Stan Terg mine is presented in this paper.

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How to Cite

Hyseni, S., Durmishaj, B., Fetahaj, B., Shala, F., Berisha, A., & Large, D. (2010). Trepça Ore Belt and Stan Terg mine - Geological overview and interpretation, Kosovo (SE Europe). Geologija, 53(1), 87–91. https://doi.org/10.5474/geologija.2010.006

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