摘要
羊场铜矿位于内蒙古自治区赤峰市巴林右旗,赋矿地层为二叠系下统大石寨组,含矿岩石为凝灰岩断裂中充填的石英脉。矿体呈脉状产出,产状稳定。通过对含矿岩系及矿体的地质特征进行分析,确定了矿床类型,并指出了找矿标志。
Yangchang copper mine is located in Bairin Right Banner of Chifeng City,Inner Mongolia Autonomous Region,ore hosting strata occured in the Permian Dashizhai group,the ore-bearing rocks occured in the tuff fracture filling quartz veins.Orebody was occured in vein,with stable occurrence.According to analyzing the mineral evolving and the geological characteristics,the deposit type was determined,andprospecting criteria was pointed out.
出处
《有色矿冶》
2010年第3期2-5,共4页
Non-Ferrous Mining and Metallurgy
关键词
羊场铜矿
地质特征
成因分析
找矿标志
Yangchang copper mine
geological characteristics
genetic analysis
prospecting criteria
