岩浆型铜镍硫化物矿床研究进展

The Research Advancement of the Magmatic Ni-Cu Sulfide Deposit

岩浆型铜镍硫化物矿床是铜矿石的重要来源,也是世界镍金属的主要来源。综述了岩浆铜镍硫化物矿床的分类、成岩成矿背景、矿床成矿过程及控制因素等方面。结合最新的研究成果,以我国东天山地区的一系列岩浆型铜镍硫化物矿床为例,对比了产于造山带环境和稳定克拉通地区的该类矿床的特征。

Magmatic Ni-Cu sulfide deposit is an important source for copper ore and the main hosts for world nickel metal.In this paper,the classification,ore-forming background,mineralization process and controlling factors of the magmatic Ni-Cu deposit have been discussed.With the combination of the recent studies to the magmatic Ni-Cu deposit in the Eastern Tianshan region in China,the features of these deposits occurred in the orogenic belt and Cratonarea have been compared.