摘要
新疆巴里坤膨润土矿是该地区一处大型膨润土矿床,无论在质量上还是在规模上都令人瞩目,对该矿床进行系统合理的研究和开发,对当地矿产经济发展具有非常重要的意义。本文从该矿床成矿区域地质特征进行研究,分析了该矿床成因,该矿属火山沉积型矿床,主要岩性为中-酸性火山碎屑。
The Balikun bentonite deposit in Xinjiang is a large bentonite deposit in this area. It is of great significance for the development of local mineral economy to study and develop the deposit systematically and reasonably, both in quality and in scale. Based on the study of the regional geological characteristics of the deposit, the genesis of the deposit is analyzed. The deposit belongs to volcanic-sedimentary type, and its main lithology is medium-acid pyroclastic.
作者
肖仁文
林泽华
XIAO Ren-wen;LIN Ze-hua(First Regional Geological Survey Brigade of Xinjiang Geological and Mineral Bureau,Urumchi 830013,China)
出处
《世界有色金属》
2019年第4期284-284,286,共2页
World Nonferrous Metals
关键词
巴里坤
坤膨润土矿
地质特征
矿床成因
Barikun
Kunbentonite deposit
geological characteristics
genesis of the deposit
