金平镁铁质-超镁铁质岩铜镍矿床成矿条件  

THE METALLOGENETIC CONDITIONS OF MAFIC-ULTRAMAFIC CU-NI DEPOSITS IN JINPING

作　　者：盖春宽 

机构地区：[1]云南省有色地质勘查院滇南院,云南个旧661400

出　　处：《云南地质》2008年第1期12-19,共8页Yunnan Geology

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.

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 

分 类 号：F618.63[经济管理—产业经济]