摘要
按构造环境控岩控矿特点,划分区内铜镍型成矿(岩)带,分析成矿条件,研究与该类矿床成矿有关的镁铁质岩、超镁铁质岩分布规律及铜镍硫化物成矿特征,指出找矿方向和建议。
According to the rock control and ore control characteristics of tectonic environment, the Cu -Ni metallogenesis is divided into metallogenetic zone in this area. We have an analysis of the metallogenetic conditions, a study on the distribution rule of mafic-uhramafic rocks in relation to this metallogenesis and the metallogenetic characteristics of Cu-Ni sulfide and put forward the ore-prospecting direction and suggestion.
出处
《云南地质》
2008年第1期12-19,共8页
Yunnan Geology
关键词
铜镍成矿区
镁铁-超镁铁岩
两大构造环境
岩相分异差别
金平云南
Cu- Ni Metallogenetic Province
Ferruginous rocks
2 Tectonic environments
difference of Lithofacies Differentiation
Jinping,Yunnan
