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The document describes the geology of the Lavrion mining district in Attica, Greece. It discusses two main tectonic units separated by a detachment fault, with an upper marble unit and lower schist unit. Metals were transported via the detachment fault from an underlying granodiorite intrusion. World-class lead-silver deposits formed through the replacement of marble by massive sulfide ore bodies along contacts with the overlying schists. Primary sulfide minerals included pyrite, galena and sphalerite. Gang

Author

PETROS TZEFERIS

Language

EN