The mineralization is located in the Kargi Ophiolite. Mineralization is observed in the meta-alkaline rocks in gray tones. Mineralization is observed generally in a way to follow the fracture and fissure systems, in hydrothermal process, with disseminated pyrites, chalcopyrites, pyritines and sphalerite minerals in low amounts and sometimes as plastings. Pyrites are found as large pieces though rare. There are serpentines in the wall rock of the mineralization and no mineralization was encountered in the wall rock.


Ahmet Aga Outcrop (4.8% Cu)