Perama Hill epithermal gold deposit
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)
dataset
GR.IGME
:
GRC-00733
English
Geoscientific information
European Geoscience Registry - Projects:
INSPIRE code list register ,:
25.83,
40.695,
26.352,
40.959
publication: 2010-05-25
Institute of Geology and Mineral Exploration (IGME)
Eliopoulos Dimitrios
Athens,
13677,
Greece
tel: 2131337313
email:
eliopoulos@igme.gr
Role: principal investigator
Data Quality
Perama Hill deposit was discovered in 1995 by the Company Thrace Gold Mines. Most of each database contain coordinates that are usable for map applications.
Constraints
conditions unknown
Metadata about metadata
55b880b9-0618-40fc-80f7-682c0a010851
Institute of Geology and Mineral Exploration (IGME)
Eliopoulos Dimitrios
1 Spirou Loui Street,
Acharnae,
13677,
Greece
tel: 2131337313
email:
eliopoulos@igme.gr
Role: point of contact
2021-11-04