内蒙古镁铁质—超镁铁质岩型铜镍矿床成矿条件与找矿远景分析  

METALLOGENIC CONDITIONS AND PROSPECTING FOR COPPER-NICKEL TYPE DEPOSITS IN MAFIC-ULTRAMAFIC ROCKS IN INNER MONGOLIA

作　　者：刘国军 王建平 

机构地区：[1]内蒙古自治区有色地质勘查局,呼和浩特010010

出　　处：《地质与勘探》2004年第1期17-20,共4页Geology and Exploration

摘　　要：按构造环境控岩控矿特点,划分区内铜镍型矿成矿(岩)带,分析成矿条件,研究了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,提出了找矿方向和建议。According to characteristics of geological environments, mineralizing belts are classified for Cu-Ni type deposit in Inner Mongolia. Based on the study of metallogenic conditions, distribution factors of mafic-ultramafic rocks, metallogenic characteristics of Cu-Ni sulfide type deposits, and prospecting targets are discussed.

关 键 词：镁铁质岩 超镁铁质岩 铜镍硫化物矿 成矿 找矿 

分 类 号：P618.41[天文地球—矿床学] P618.63[天文地球—地质学]