摘要
打花儿金矿床位于内蒙古白云鄂博大型稀土-铁矿东约12 km处,属于中低温热液型金矿,断裂构造是矿床最主要的控矿因素,成矿物质来源于隐伏的斑岩体。
The Dahuaer gold deposit,is about 12 Kilometers away from the east of the Baiyunebo large rare earth-iron ore deposit in Inner Mongolia,belongs to the middle-low hydrothermal type,controlled by the fault structure,and the ore-forming materials was enriched from the deep porphyry.
出处
《甘肃冶金》
2015年第3期112-114,共3页
Gansu Metallurgy
关键词
金矿床
成因初探
找矿前景
打花儿
gold deposit
genesis discussion
prospecting potential
Dahuaer
