The Anwangshan Gold Polymetallic Deposit is located in the middle part of the North Qinling metallogenic belt.Three NW trending strong deformation zones have been found in the deposit,among which 7 ore bodies have been delineated.The ore types are mainly structural alteration type and gold-bearing quartz vein type.The wall rock alteration closely related to mineralization is silicification,sericitization,early carbonatization,pyritization and so on.Ore bodies are found in the NW strong deformation zone,and reconstructed by quartz syenite vein and sulfide-bearing quartz vein controlled by NE fracture.The preliminary analysis is that the genesis of the mineral deposit is magmatic hydrothermal type.The NW strong deformation zone,the quartz syenite vein and the "red zone" composed of intense surface alteration can be used as important prospecting criteria.The composite anomalies formed by the elements such as Au,Ag,As,Pb,Zn,and Cu can be used as geochemical prospecting criteria.