摘要
双步结热铜矿产于下白垩统比马组与始新世黑云母花岗闪长岩接触带形成的夕卡岩中,铜矿体以似层状、透镜状产出,矿石平均品位ω(Cu)=4.27％。矿区深部具有良好的找矿前景。
Shuangbujiere copper deposit occurs in skarn fromed at contact zone between the Lower Creta-ceous Bima Formation and Eocene biotite granodiorite. Ore bodies are layeroid or lenticular with average w(Cu)=4.27%. The deposit is potential to depth.
出处
《地质找矿论丛》
CAS
CSCD
2003年第z1期68-69,87,共3页
Contributions to Geology and Mineral Resources Research
