Perama Hill epithermal gold deposit
Description
Perama Hill is a high sulphidation deposit hosted by tertiary sandstones (Lescuyer J.L.et.al. 2003) and is located on the east margin of Petrota graben.Perama gold mineralisation is related the late Eocene-Oligocene volcanism in the Rhodope massif.Gold mineralisation is associated with a series of wide (>1,5m) to narrow (few cm) milky quartz-barite veins and stockwork veining in the vuggy silica block.Gold in microsized was also found disseminated in the surrounding altered (oxide mineralisation) epiclastic sandstones (Lescuyer J.L.et.al. 2003)
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