深断裂带与多金属矿地质特征及矿床成因  

Geological characteristics and genesis of deep fault zone and polymetallic deposit

作　　者：雷自强 康维良 赵振东 LEI Zi-qiang;KANG Wei-liang;ZHAO Zhen-dong(Oansu fourth Bureau of Geology and mineral exploration,bureau of Geology and mineral resources exploration,Jiuquan 735000,China)

机构地区：[1]甘肃省地质矿产勘查开发局第四地质矿产勘查院,甘肃酒泉735000

出　　处：《世界有色金属》2018年第12期148-149,共2页World Nonferrous Metals

摘　　要：多金属矿也是我国矿区的一个典型特点,且不同的金属矿体类型,其地质特征和矿床成因也不尽相同。因此文章结合某深断裂带构造控制条件下的多金属矿实例,对其地质特征和矿床成因等进行了详细的分析,以供参考。Polymetallic ore is also a typical feature of China＇s mining area, and the geological characteristics and ore genesis of different metal ore bodies are different. Therefore, this paper makes a detailed analysis of the geological characteristics and the genesis of the deposit, which is based on the structural control of a deep fault zone, for reference.

关 键 词：深断裂带 多金属矿 地质特征 矿床成因 

分 类 号：P618.2[天文地球—矿床学]