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刍议内蒙古阿拉善盟叠布斯格金多金属矿地质特征与找矿规律 被引量:1

Discussion on Geological Characteristics and Prospecting Rules of the Dibusige Gold Polymetallic Deposit in Alxa League,Inner Mongolia
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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
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  • 1内蒙古第八地质矿产勘查开发院.内蒙古自治区阿拉善左旗巴彦乌拉山北部岩金矿详查报告[R],20109.
  • 2王金龙,尹忠,黄志全,等.内蒙古阿拉善地区成矿规律及找矿方向探讨[C]//中国西部地区金矿地质学术讨论会,2001.

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