摘要
LUSHA SOUTH铜钴矿位于世界著名的加丹加弧形铜钴多金属成矿带上,带内分布有多个大型—超大型铜钴矿床。通过对以往地质工作资料的收集和整理,对矿区内的地质特征,矿体特征,矿床成因和下一步找矿方向做了简要分析。矿区内出露的地层主要为罗安群,矿床成因类型为沉积—热液改造的层控型铜钴矿床,矿区内找矿潜力巨大。
LUSHA SOUTH copper and cobalt mine is located in the world famous copper and cobalt polymetallic metallogenic belt of the world,and there are several large-super large copper and cobalt deposits in the belt.Through the collection and arrangement of geological work data in the past,the geological characteristics,the ore body characteristics,the genesis of the ore deposit and the next prospecting direction are briefly analyzed.The strata in the mining area are mainly luoan group,and the genetic type of the deposit is the layer controlled copper and cobalt deposit,which is transformed by sediment-hydrothermal transformation.The potential of prospecting in the mine is huge.
作者
翟鑫
Zhai Xin(Southwest Nonferrous Kunming Exploration Surveying and Desigining(institute)inc,Kunming 650000,China)
出处
《世界有色金属》
2018年第8期122-123,共2页
World Nonferrous Metals
关键词
刚果(金)
LUSHASOUTH
铜钴矿
地质特征
找矿方向
Congo(DRC)
LUSHA SOUTH
Copper and cobalt deposit
Geological characteristics Prospecting direction
