Abstract: Situated in cat RidgeMaoling~and Wolongquan gold mineralization concentration area, Zhaojiapuzi gold deposit is is a typical mesothermal-of the epithermal deposits. Through Regional metamorphism of rocks activated metallogenic elements such as while Au, and Ag ore-forming elements such as activation, who migrated with metamorphic hydrotherm and enriched initially in favorable tectonic settingswith metamorphic hydrothermal favorable structural parts migrated preliminary enrichment. Under the effect of stress, Through stress, so that the plastic deformation of rocks, was aroused to forming a NW-trending ductile shear zone, whileand the ore-forming elements such as Au, and Ag again ore-forming elements such as remobilizationed again, and enrichmented;. Then through a large area of the late magmatic intrusion, forming formed a NW-trending ductile-brittle fracture and a NE-trending brittle fault superimposed on top of the ductile shear zones superimposed on top of the NW-trending ductile-brittle fracture and the North East to brittle fracture. Meanwhile, the while ambitiouenormouss heat sources formations gold acaused another gain activation, migration, and accumulation of the minerals, enriched and mineralized at favorable structural positions with a large number of metallogenic material brought by magma, whichtic minerals brought together into a large number of favorable structural positions in enrichment and mineralization, this area is a major stage of mainly intothe gold mineral phasedeposit mineralization in this area.