The Trepca Belt of Pb-Zn-Ag mineralization is located in the NNW-SSE trending Vardar zone, and extends for over 80 km. It supports five mines during the period 1930-2010, and contains several other Pb-Zn occurrences. The replacement and vein type mineralisation is hosted primarily by Mesozoic carbonates, but also occasionally by amphibolites. It displays a clear structural control. Mineralisation is spatially and genetically related to Neogene andesite-dacite extrusive and sub volcanic intrusive.
References
- Sommerlatte, H. (1939): The ore deposits of the Trepca Mines Limited in Jugoslavia and the dressing of these ores. Metall und Erz 36, 95-100.
- Schumacher, F. (1950): Die Lagerstätte der Trepca und ihre Umgebung. Izdavacko Preduzece Sareta za Energetiku i Ekstraktirnu Ind. Vlade Fnrj., Belgrade, Serbia, 65 pp.
- Schumacher, F. (1951): Ore deposits of Trepca (Jugoslavia), a geologic and mineralogical phenomenon. Zeitschrift für Erzbergbau und Metallhüttenwesen 4, 419-423.
- Gluscevic, B. (1956): Mining techniques at the lead-zinc mines at "Trepca" in Yugoslavia. Zeitschrift für Erzbergbau und Metallhüttenwesen 9, 373-382.
- Der Aufschluss 1975(6):225-235
- Mineralogy and Petrology 52:197-208 (1995)
- The Mineralogical Record: 4: 55-61.
- Hyseni, Sylejman; Durmishaj, Bedri; Rama, Mursel; Zabeli, Muharrem (2010): Trepca ore Belt and Beloberdo mineral deposit-geological overview and interpretation, Kosovo. Journal of International Environmental Application & Science 5, 258-263.
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