摘要
金平县新发寨银多金属矿属碳酸盐岩型矿床,属构造、层位控矿,多物质来源、多期次成矿。矿床成因类型属中低温热液交代型银多金属矿床。
The silver polymetallic deposit located in Xin Fa-Zhai Yunnan China, belongs to carbonate deposits, and that belongs to the structural formation of ore control, multi sources, multi period mineralization.The genetic type of the deposit belongs to the low temperature hydrothermal silver polymetallic deposit.
出处
《世界有色金属》
2017年第10期242-244,共3页
World Nonferrous Metals
关键词
银多金属矿
中低温热液
新发寨金平云南
Silver Multimetallic
Low Temperature Xin Fa-Zhai
Jinping County
Yunnan province
China