摘要
从矿体的产状、形态、矿石组成和组构特征等方面,论述了铜山岭乡金属矿床的地质特征。在此基础上,讨论了成矿作用的性质、成矿物质来源和控矿条件。作者认为,铜山岭多金属矿床应属同生沉积-岩浆热液叠加改造型层控矿床。
Based on the studies of occurrence, shap, composition and fabric fcatureof ore bodies as well as some other characteristics of the Tongshanlingpolymetallic deposit, this paper discusses the nature, material source and ore-control conditions of metallization. The author considers that the Tongshanlingpolymetallic deposit should belongto syndepositional--magma tic-hydrothermalsuperimposed reworked ore deposit.
关键词
多金属
矿床
地质特征
成矿
polymetallic deposit
stratabound ore deposit
ore formation
metallogeny
Hunan
Tongshanling
