摘要
安定铜镍矿均产于安定基性岩体中。矿床类型属于岩浆熔离—热液硫化铜镍矿床,矿体呈似层状、透镜状、脉状产出。
Anding Cu-Ni deposit is in Anding basic rock Body. It belongs to the magmatic immiscible hydro- therma sulfide Cu-Ni deposit. The orebody is stratoid, lenticular and veined.
出处
《云南地质》
2014年第4期550-554,共5页
Yunnan Geology
关键词
铜镍矿
矿产成因
云南富宁县安定
Cu-Ni Deposit
Genesis of Ore Deposit
Anding, Funing, Yunnan