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新疆北部的铜镍 (铂族元素 )硫化物矿床成矿系列形成于海西期 ,是世界上形成于显生宙的少数几个铜镍硫化物矿床成矿系列之一。它具有许多特殊性 ,如形成多个亚系列 (喀拉通克、黄山、箐布拉克 )、每个亚系列又包含多个岩体形成多个矿床、不同的亚系列及每个亚系列内部的各个岩体和矿体差别较大、成矿母岩低镁高铝富钾等等。海西期的地幔柱活动可能是形成该成矿系列的主要原因。目前对同一时期的箐布拉克亚系列及其它基性超基性岩带的研究程度较低 ,在今后的大调查中应加以注意
The copper-nickel (PGM) sulphide mineralization series in northern Xinjiang was formed in the Hercynian period and is one of the few copper-nickel sulphide mineralization series that formed in the Phanerozoic in the world. It has many special features, such as the formation of a number of sub-series (Kalatongke, Huangshan, Jubalak), each sub-series also contains a number of rock mass formation of multiple deposits, different sub-series and each sub-series within Of the rock and ore body vary greatly, the ore-forming mother rock low-magnesium high-aluminum potassium and so on. The Hercynian mantle plume activity may be the main reason for forming this metallogenic series. At present, the research on the 箐 Bulakya series and other basic ultrabasic rock belts in the same period is relatively low, and should be paid attention to in future major investigations