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.
引文
[1]周怀鲲,瑞凯.内蒙古自治区阿拉善左旗巴彦乌拉山北部岩金矿成矿地质特征及成因初探[J].西部资源,2014(1):139-140.
[2]计新利,于广程,冠利民,等.阿拉善盟地区金属矿成矿规律分析[J].科技资讯,2016,14(10):152-153.