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云南金平新发寨银多金属矿成矿地质条件

The metallogenic geological conditions of Ssilver multimetallic deposit in xinfazhai,jinping county,yunnan province,China
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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
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