摘要
子尼铜矿规模已达中型铜矿床,其矿体主要呈似层状、透镜状赋存于近南北向的层间构造破碎带中,矿体围岩为三叠系上统哈工组三段的粉砂质板岩及含砾粉砂质板岩。成矿与断层、岩性及围岩蚀变强度有关,属与构造有关的中低温热液铜矿床。矿区深部和外围还有一定的找矿前景。
Zini Cu deposit is a middle scale Cu deposit. The main ore body is stratoid,lenticular in nearly NS interlayer structure fracture zone. The wall rock of ore body is Upper Permian Hagong Formation Member 3 silty slate and pebble-bearing silty slate. The metallogenesis is in relation with the fault,lithologic character and intensity of wal rock alteration. It belongs to the middle-low T hydrothermal Cu deposit. There is some prospecting potentiality in the deep and surrounding area.
出处
《云南地质》
2017年第1期34-38,共5页
Yunnan Geology
关键词
构造控矿
中低温热液矿床
云南香格里拉子尼
Ore Control of Structure
Middle-Low T Hydrothermal Deposit
Zini
Xianggelila
Yunnan
