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大兴安岭北部地区金属矿成矿地质特征及深部勘查方向

Metallogenic geological features and deep exploration direction of metal ore in northern Greater Khingan Range
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摘要 大兴安岭北部地区是我国矿区中较大的一个多金属集中矿区,其依靠自身的地质条件及岩浆的活动作用,形成不同种类的金属矿床。为了更好地开发和利用此矿区的金属矿产资源,对其成矿地质研究变得非常重要。在此对大兴安岭北部地区金属矿成矿地质特征、成矿条件及深部勘查方向进行分析和研究,并取得了很大的成果。 The northern part of Greater Khingan Range is a large polymetallic concentrating mining area in China's mining area, which relies on its own geological conditions and magmatic activities to form different kinds of metal deposits. In order to better develop and utilize the metal mineral resources in this mining area, it is very important for the study of its metallogenic geology. The metallogenic geological characteristics, metallogenic conditions and deep exploration direction of metal deposits in northern Greater Khingan Range are analyzed and studied, and great achievements have been made.
作者 朱大龙 ZHU Da-long(College of Geoscience, Jilin University,Changchun 130061,China)
出处 《世界有色金属》 2018年第3期92-92,94,共2页 World Nonferrous Metals
关键词 大兴安岭 多金属集中矿区 成矿地质特征 深部勘查方向 Greater Khingan Range polymetallic concentrated mining area metallogenic geological characteristics deep exploration direction
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