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金平镁铁质-超镁铁质岩铜镍矿床成矿条件
引用本文:盖春宽.金平镁铁质-超镁铁质岩铜镍矿床成矿条件[J].云南地质,2008,27(1):12-19.
作者姓名:盖春宽
作者单位:云南省有色地质勘查院滇南院,云南,个旧,661400
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。

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

THE METALLOGENETIC CONDITIONS OF MAFIC - ULTRAMAFIC CU - NI DEPOSITS IN JINPING
GAI Chun-kuan.THE METALLOGENETIC CONDITIONS OF MAFIC - ULTRAMAFIC CU - NI DEPOSITS IN JINPING[J].Yunnan Geology,2008,27(1):12-19.
Authors:GAI Chun-kuan
Institution:GAI Chun-kuan (South Yunnan Branch, Yunnan Nonferrous Geoexploration Institute, Gejiu 661400)
Abstract: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.
Keywords:Cu- Ni Metallogenetic Province  Ferruginous rocks  2 Tectonic environments  difference of Lithofacies Differentiation  Jinping  Yunnan
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