摘要
刀公箐铜矿矿体呈复杂透镜状、豆荚状赋存于断裂构造破碎带中,矿体围岩为中二叠统羊八寨组(P_2y)绢云千枚岩及凝灰岩。属中低温热液矿床。
The ore body of Daogongqing Cu deposit is complicatedly lenticular, leguminous in the fault fracture zone. The wall rock of ore body is Middle Permian Yangbazhai Formation （P2Y） sericite phyllite, tuff. It is a middle -low T hydrothermal ore deposit.
出处
《云南地质》
2016年第1期40-43,共4页
Yunnan Geology
关键词
构造破碎带控矿
中低温热液矿床
云南景谷刀公箐
Ore control of Structure Fracture Zone
Middle - Low T Hydrothermal Deposit
Daogongqing, Jinggu, Yunnan
