Wushan skarn copper deposit is associated with Wushan granodiorite in genesis. In this paper, the authors petrographic and mineralogical characteristics of the biotites in Wushan granodiorite are investigated, and its forming conditions and the significance for petrogenesis and mineralization are discussed. The crystallization conditions indicate that Wushan granodiorite, which was formed in high temperature and oxygen fugacity, has a large mineralization potentiality and is benefit for the formation of Wushan copper deposit.xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />