摘要
辽西南青龙沟金矿矿体赋存在2条近东西向断裂中间的碳酸盐岩地层中,明显受前寒武系雾迷山组控制。已知矿床规模不大,但矿化稳定,金与铁矿物有关,是其特点。
The Qinglonggu Gold deposits occur in the carbonate formation between two fracture zones strikingnearly in a east west direction and are obviously controlled by the Pre-cambrian Wumishan Fcrmation.The known deposits are not big in scale,but stable in their mineralization.The gold ores are characte-rized by their association with iron ores.
出处
《地质与勘探》
CAS
CSCD
北大核心
1992年第4期18-20,共3页
Geology and Exploration
