“…In the second stage (main stage), mineralization in skarn is completed and enriched, porphyry copper-molybdenum deposit formed during several successive phases, pervasive alteration zones (pervasive, potatic, propelic, phyllic and argillic) Copper and molybdenum have been formed and mineralized, and in the final stage, after the formation of the deposit, the performance of selective chlorination-calcite, epidote-calcite, chlorite, calcite and hematite alterations with intensity And various weaknesses of all types of igneous rocks and infertile dykes have infiltrated the deposit (Rown et al, 1997).The consequence of the formation of four alteration zones, the occurrence of pervasive siliceous alteration, caused the overprinting of the section A large part of the ore zone is concentrated in the phyllite zone and the rest in the potasic zone and the type of mineralization in the deposit is diffused (ore zonc). Disseminated) Stock work The most important minerals identified in the deposit are: chalcopyrite, molybdenite, pyrite, rutile, ilmenite, pure copper, copper, calcite, colin, Ideait, Arsenopi Rite, burnite and minerals of Fahlor group (tenantite, tetrahydrite) (Xu et al, 2019). The supergen enriched zone in the deposit is not well formed, it is mostly concentrated in the eastern slope of the deposit and its most important minerals are pure copper, chalcopyrite, caprite and burnite.…”