盘山冲铅锌矿地质特征及矿床成因

Geological characteristics and genesis of panshanchong lead zinc deposit

湖南省江华县盘山冲铅锌多金属矿属于岩浆期后热液型多金属矿,在其形成过程中,各种地质因素影响并制约着矿体的分布、形态、规模、品位及矿物组合。通过论述该矿床的地质特征、控矿因素,总结成矿地质特征及矿床成因。

The Panshanchong Pb-Zn polymetallic deposit in Jianghua Yao Autonomous County,Hunan Province,is a post-magmatic hydrothermal polymetallic deposit.During its formation,various geological factors affect and restrict the distribution,shape,scale,grade and mineral assemblage of the deposit.The geological characteristics and ore-controlling factors of the deposit are discussed,and the ore-forming geological characteristics and genesis are summarized.