四支沟钼矿床地质特征及成因初探  

Geological property and formation cause of Sizhigou molybdenum ore deposit

作　　者：卢清月[1] 魏远[1] 刘登锋[1] 

机构地区：[1]河南省地质矿产勘查开发局第一地质勘查院,河南南阳473000

出　　处：《矿业工程》2012年第6期13-15,共3页Mining Engineering

摘　　要：通过对内蒙古四支沟钼矿床的矿体特征、矿物组合以及矿化蚀变分带等研究,表明该矿床属斑岩型钼矿床,它的形成与区域上构造和岩浆活动密切相关,该区矿床赋存于花岗斑岩岩体内,具有明显的矿化蚀变分带现象。Orebody properties, mineral composition and mineralization alteration zoning of Sizhigou molybdenum ore deposit in Inner- Mongolia are studied. The study shows the molybdenum ore deposit belongs to porphyry type. The formation of the deposit is well related with region＇s geological structure and magmatic activity. The deposit is embedded in granite mass, having obvious mineralization alteration zoning.

关 键 词：四支沟矿床 钼矿 地质特征 矿床成因 

分 类 号：P611[天文地球—矿床学]