摘要
文章通过对云南省麻栗坡县三板桥多金属矿地质特征进行分析,认为矿区矿体主要赋存于早元古界猛硐岩群南秧田岩组二段矿化蚀变矽卡岩带内,矿床成因严格受地层、岩性、区域变质作用、岩浆期后及地下水热液叠加等因素的控制,矿床成因较为复杂。
The article through to the yunnan province malipo SanBanQiao polymetallic deposit geological characteristics were analyzed,and think mine ore bodies occur mainly in early proterozoic,fierce adit suite south seedling bed rock group 2 mineralized alteration in the skarn zone,deposit genesis strictly by strata,lithology,regional metamorphism,and groundwater after the magmatic hydrothermal superimposed factors such as control of ore deposit formation is more complicated.
作者
蒲兴明
PU Xing-ming(Wenshan Malipo Zijin Mining Group Co.,LTD.,Wenshan 663602,China)
出处
《世界有色金属》
2022年第20期110-112,共3页
World Nonferrous Metals
关键词
麻栗坡
多金属矿
成因浅析
Malipo
Polymetallic ore
genetic analysis
