Mineralogically the geological units outcropping, trenching and tunneling which is along the Toroud-Chahshirin magmatic arc comprise of Eocene Tuffes and Lavas intersected by the Eocene Granitoid masses and shows Hydrothermal alteration on the Chah Faragh property consisting native copper, primary and secondary copper sulfide minerals, and copper oxide minerals including Coveline, Malachite, Chrysocolla in the presence of the Calcic veins.

Based on the ancient tunneling and diamond core drilling prospect work the mineralization zone continues to around 200 meter depth.

Mineralization on the mining area is a structured controlled type and was formed along the Toroud and Bagho faults( mainly trending East-West).