摘要
通过对矿床地质特征、矿体特征和矿石质量特征的分析,初步探讨了矿床成因,认为该矿属于中低温热液交代叠加改造型铜钴矿床,指明了矿区找矿工作方向。
With the analysis of geological characteristics, orebody feature and ore quality characteristics, the preliminary deposits genesis was discussed, it is considered that the deposit was metasomatic transformation type Epi-Mesothernal copper-cobalt deposits, the paper points out next prospecting direction.
出处
《世界有色金属》
2017年第21期128-128,130,共2页
World Nonferrous Metals
关键词
矿床地质特征
矿床成因
中低温热液矿床
geological characteristics
ore genesis
Epi-Mesothernal deposit