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一、前言从十九世纪九十年代起,岩浆硫化铜镍矿床的成因观点先后有岩浆的、热液的、硫化作用的、变质的与陨石冲击的……等五、六种之多。但国内绝大多数研究者则持岩浆成因观点,即岩浆就地结晶熔离成矿的传统理论。二十余年来,在这一理论的影响下,所述岩体被认为系单式岩体,其矿床则认为是岩浆晚期“熔离分凝矿床”与“熔离贯入矿床”(王述平,1962),或“熔离矿床”与“熔离贯入矿床”(鲍世强,1963),还有人认为是“岩浆残余矿床”(刘若新,1963)……等,七十年代后,又提出“岩浆深部熔离矿床”(吉冶607队等,1974)。
I. Preface From the 1990’s onwards, the origin of the magma copper sulphide nickel deposit has been followed by magmatic, hydrothermal, sulfidation, metamorphic and meteorite impact ... and many other five or six. However, the vast majority of researchers in China hold the view of magmatism, that is, the traditional theory of in-situ crystallization and magmatic mineralization of magma. For more than two decades, under the influence of this theory, the rock mass is considered to be a unitary rock mass, and its deposit is considered as the late stage of “magmatic segregation ore deposit” and “melted-penetrated ore deposit” (Wang Siping , 1962), or “melting from the ore deposit” and “melting into the ore deposit” (Bao Shiqiang, 1963), and others considered “magmatic remnant deposit” (Liu Ruoxin, 1963) ...... After the 1970s, Magmatic deep melt deposit "(Jiye 607 team, etc., 1974).