摘要
卡特里西铜锌多金属矿是东昆仑区域内发现的一重要铜锌矿床,托库达坂群火山岩地层(下石炭统)是该矿的主要产出部位,区内地层对矿体控制非常明显。找矿潜力巨大。文中对卡特里西铜锌矿地质特征进行分析,并探讨其矿床成因,旨在对区内找矿提供指导作用。
Khatri Si copper zinc polymetallic ore is an important copper zinc deposit found in eastern Kunlun region,Tuokuda Osaka group volcano rock formation(Lower Carboniferous) is the main production site of the mine,strata of ore body control is very obvious.There is a great potential for ore prospecting.In this paper,the geological characteristics of the cupric copper zinc deposit are analyzed and the genesis of the deposit is discussed in order to provide guidance for the prospecting in the area.
出处
《世界有色金属》
2017年第24期162-162,164,共2页
World Nonferrous Metals
关键词
卡特里西铜锌矿
地质特征
矿床成因
Khatri Si copper zinc ore
geological characteristics
genesis of the deposit
