摘要
卡尔却卡铜多金属矿床多分布于柴达木盆地的西南边界,这种矿床是近些年在昆仑祁漫塔格矿床地带东部所发现的一种中型的矿床。这些金属矿物质主要来源于大洋板块运动过程所带来的一些地壳物质和部分熔岩浆。
Carl but copper polymetallic deposits are more distributed in the Southwest border of Qaidam Basin, which is a medium-sized deposit found in the eastern part of the Kunlun Qi Man Dhak deposit in recent years. These metals are mainly derived from some crustal substances and partially molten magma brought about by the process of oceanic plate movement.
出处
《世界有色金属》
2017年第10期44-44,46,共2页
World Nonferrous Metals
关键词
卡尔却卡铜
矿床特征
成因分析
Carl but copper
Deposit characteristics
Cause analysis
