摘要
In this paper, tin-copper polymetallic deposit in western low of the east part of Gejiu is studied through a systematic analysis of its geological setting,geological characteristics of the deposit, characteristics of alterations zoning, geochemical component of altered granite, and deep exploration experience. The results show that the deposit is a part of diverse magmatic hydrothermal mineralization system, which often occurs in the inner altered granite, especially the edge and transition facies. It is a high-temperature magmatic hydrothermal deposit combining with the post-gas-liquid mineralization by the decomposition and gasification of magma in early stage and the alteration of magma intrusion in later stage. The deposit has close relationship with wall-rock alteration, especially potash feldspathization,pyritization, fluoritization and tourmalinization.