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一、前言硫化铜镍矿床与分异的基性或基性-超基性侵入岩体有最密切的关系,并且多属岩浆熔离成因,这在目前已为广大学者所公认。可是,近几年来,在我国却发现了不少与未分异或分异不好的单独的超基性岩侵入体有关的铜镍矿床。这些矿床多半不只是岩浆熔离成因,也有岩浆晚期贯入或岩浆期后热液成因的。这是一个值得重视的问题。本文拟在王述平、刘若新、李万亨、周作侠等工作
I. Preface The copper sulphide-nickel deposit is most closely related to the differential basic or basic-ultrabasic intrusive rock mass and is mostly of the genesis of magma eroded, which is now widely recognized by scholars. However, in recent years, quite a few copper-nickel deposits related to the undivided or highly differentiated single ultrabasic intrusions have been discovered in our country. Most of these deposits are not only the cause of magmatic fission, but also the late magmatic penetration or magmatic hydrothermal genesis. This is a problem that deserves attention. This article intends to Wang Shu-ping, Liu Ruoxin, Li Wanheng, Zhou Zuoxia and other work