摘要
卡特里西铜锌矿成矿类型属于海相火山沉积型硫化物矿床,被首次发现于东昆仑地区,托库孜达坂群(下石炭统)火山岩是该矿的主要赋矿地层,该矿层控特征非常突出。东昆仑下石炭统托库孜达坂群地层中海相火山岩带分布有众多铜多金属矿点,为一较有前景的海相火山岩型铜矿成矿带,卡特里西铜锌矿在该去的找矿发现,为区内同类型矿床的寻找提供了重要的指引作用,同时使得该区此类矿床类型的空白彻底被打破。因此,加强对该矿地质特征及其成因进行研究具有非常重要的意义。
The metallogenic type of the cupric copper zinc deposit belongs to the marine volcanic deposit type sulfide deposit, which was first found in the East Kunlun area. The tkurzaka group （Lower Carboniferous） volcanic rocks are the main ore bearing strata of the ore, and the control characteristics of the ore layer are very prominent. There are numerous copper polymetallic ore spots in the lower Carboniferous tkurzaka group formation in the lower Carboniferous strata of Eastern Kunlun. It is a promising marine volcanic type copper ore belt. The discovery of the cktcn copper zinc deposit in this area provides an important guiding role for the search for the same type of deposit in the area, and the blank of the type of this type of deposit has been completely broken. Therefore, it is very important to strengthen the research on the geological characteristics and genesis of the mine.
作者
范旭东
FAN Xu-dong(The Xinjiang Uygur Autonomous Region geological and mineral exploration and Development Bureau ninth Geological Brigade, Urumchi 830000,Chin)
出处
《世界有色金属》
2018年第4期143-144,共2页
World Nonferrous Metals
关键词
卡特里西铜锌矿
地质特征
成因分析
Khatri Si copper zinc deposit
geological characteristics
cause analysis
