摘要
内蒙古阿拉善盟叠布斯格金多金属矿处于华北陆块北缘西段,新太古代活动大陆边缘裂谷带。通过对该矿床地质特征及矿体特征分析,认为该矿床是以铜、金、锌等少量金属矿物为主的中低温热液型矿床。
The Dibusige gold polymetallic deposit in Alashan League, Inner Mongolia, is located in the western part of the northern margin of North China Block and the Neoarchean active continental margin rift zone. Based on the analysis of the geological characteristics and orebody characteristics of the deposit, it is considered that the deposit is a medium-low temperature hydrothermal deposit with a small amount of metallic minerals such as copper, gold and zinc.
作者
李长才
苟小军
姚世恒
LI Chang-cai;GOU Xiao-jun;YAO Shi-heng(First Institute of Geological and Mineral Exploration and Development of Inner Mongolia Autonomous Region, Hohhot 010020,China)
出处
《世界有色金属》
2019年第4期90-91,共2页
World Nonferrous Metals
关键词
叠布斯格金多金属矿床
地质特征
矿床成因
Dubusige gold polymetallic deposit
geological characteristics
genesis of the deposit