摘要
南坡铜矿产于中生界白垩系曼宽河组浅色砂岩中,是一种典型的砂岩型铜矿床。本区铜矿成矿受地层、岩性、构造及围岩蚀变等多重因素控制。本文在分析控矿因素的基础上,对矿床成因进行了探讨,为下一步在矿区开展成矿预测工作提供指导。
Nanpo Copper Deposit occurs in sandstone of Mankuanhe formation,cretaceous system,Mesozoic erathem.It is a typical sandstone-type copper deposit.The metallogenic factors of copper in this area include stratum,lithology,structure,wall-rock alteration,etc.Based on analysis of ore-controlling factors,the deposit genesis has been discussed and the direction for further prospecting is put forward.
出处
《有色金属（矿山部分）》
2012年第1期20-23,共4页
NONFERROUS METALS(Mining Section）
关键词
南坡铜矿
控矿因素
物质来源
矿床成因
Nanpo Copper Deposit
ore-controlling factors
material source
deposit genesis
