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Perama Hill deposit, Alexandroupoli (Alexandroupolis), Évros Prefecture, Thraki Department (Thrace; Thracia), Greece
High-sulfidation Au-Ag-Te-Se epithermal system hosted in silicic- and argillic altered andesitic rocks and overlying sandstones.Early stage silica-pyrite rock and argillic alteration were followed by the deposition of sulfide-, sulfosalt- and telluride-bearing quartz-barite veins and stockworks.
Discovered by Thracean Gold Mining S.A. in 1995.
Mineral List
29 entries listed. 26 valid minerals.
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References
Voudouris & Skarpelis (1998)
McAlister et al. (1999)
Skarpelis et al. (1999)
Lescuyer et al. (2003)
Panagiotis Christos Voudouris, Vasilios Melfos, Paul G. Spry, Robert Moritz, Constantinos Papavassiliou und George Falalakis (2011): Mineralogy and geochemical environment of formation of the Perama Hill high-sulfidation epithermal Au-Ag-Te-Se deposit, Petrota Graben, NE Greece. Mineralogy and Petrology 103, 79-100.
Vodouris, P. C. (2011): Conditions of formation of the Mavrokoryfi high-sulfidation epithermal Cu–Ag–Au–Te mineralization (Petrota Graben, NE Greece). Mineralogy and Petrology 101, 97-113.
McAlister et al. (1999)
Skarpelis et al. (1999)
Lescuyer et al. (2003)
Panagiotis Christos Voudouris, Vasilios Melfos, Paul G. Spry, Robert Moritz, Constantinos Papavassiliou und George Falalakis (2011): Mineralogy and geochemical environment of formation of the Perama Hill high-sulfidation epithermal Au-Ag-Te-Se deposit, Petrota Graben, NE Greece. Mineralogy and Petrology 103, 79-100.
Vodouris, P. C. (2011): Conditions of formation of the Mavrokoryfi high-sulfidation epithermal Cu–Ag–Au–Te mineralization (Petrota Graben, NE Greece). Mineralogy and Petrology 101, 97-113.
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Updated Mineral Entry: CombarbaliteFrom David Von Bargen, 19th Jun 2013 16:43:01