Cu Ni sulfide deposit is a typical magmaticoredeposit.
铜镍硫化物矿床是典型的岩浆矿床。
2
The comprehensive analyzing of the relationship among magmatic rocks, fault, wall rock condition and ore-body scale or enrichment style are used for explain the genesis of this deposit.
本文从矿区资料的综合研究入手，深入剖析了岩浆岩、断裂、围岩圈闭条件与矿体规模、富集程度的关系。
3
It has characteristics of polystage-magmatic intrusions, polystage metallogenetic evolution and zonal differentiation of the oredeposit.