铜山岭矿田形成于地洼发展阶段产于亲硫构造地球化学区。矿田内碳酸盐岩层分布广泛。为形成Cu-(Mo)rrrrrrrrn-Pb、Zn-Ag多种类型的矿床组合提供了有利条件。本文根据实际资料,运用陈国达教授提出的地洼学说。对铜山rrrrrrrrn岭矿田成矿组合的特征、形成条件及成矿机制进行了初步分析。 Tongshanling ore field formed in the depression during the development stage pro-sulfur tectonogeochemical zone. Carbonate rock in the orefield is widely distributed. It provides favorable conditions for the formation of Cu- (Mo) r r r r r r n-Pb and Zn-Ag deposit types. Based on the actual data, this article uses the theory of diwa proposed by Professor Chen Guoda. The characteristics, forming conditions and metallogenetic mechanism of the metallogenic assemblage in Tongshan area are analyzed preliminarily.