The Shenggongshan gold polymetallic deposit,Qingyang has long been regarded as a single,magmatic hydrothermal type deposit. Exploration in recent years indicates that the gold polymetallic mineralization is also widely developed in the granodiorite porphyry and wall rock fractures,mainly as disseminated,stringer or stockwork ore bodies in the NE-trending faults and their secondary feather fractures,shear fractures,and the fissures and fractures formed by the fluid,exhibiting the binary spatial structure of a porphyry deposit. The existing ore bodies have not been fully controlled. The gold metal resource is predicted to be medium-sized in quantity in the subsurface of 0～-250 m using volumetric method. Further work is encouraged.
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