摘要
艾家坪-水城地区是贵州重要的铅锌矿化集中区,铅锌矿赋存于石炭系碳酸盐岩中,威水背斜近轴部高角度逆冲断层是主要控矿构造。北西向逆冲断层、层间剥离构造和石炭系碳酸盐化灰岩是本区铅锌矿的重要找矿标志。
The aijiaping Shuicheng area is an important lead-zinc mineralization concentration area in Guizhou Province.The lead-zinc deposits occur in Carboniferous carbonate rocks,and the high angle thrust near the axis of Weishui anticline is the main ore controlling structure.The NW thrust,interlayer detachment structure and Carboniferous carbonated limestone are the important prospecting indicators of lead-zinc deposits in this area.
作者
朱华
杨光龙
ZHU Hua;YANG Guang-long(Geological Brigade 106 of Guizhou Geological and mineral exploration and Development Bureau,Zunyi 563000,China)
出处
《世界有色金属》
2019年第23期103-103,105,共2页
World Nonferrous Metals
关键词
铅锌矿
控矿因素
找矿标志
艾家坪-水城地区
贵州
lead zinc ore
ore controlling factors
prospecting indicators
aijiaping Shuicheng area
Guizhou