前言阿尔卑斯型铬铁矿的成岩成矿作用,是一个比较复杂的问题。对此,国内外学者已进行过大量研究,从欧美学者创立并发展的早期岩浆结晶堆积说(沃格特1894),到晚期岩浆分异—残浆成矿说(斯别尔1933),特别是六十年代我国学者王恒升等提出熔离成矿说, Introduction The diagenesis and mineralization of alpine chromite is a complicated issue. In this regard, scholars at home and abroad have carried out a large number of studies, from the early magma depositional accumulation (Vogt 1894) founded and developed by European and American scholars to late magmatic differentiation - the remnant mineralization (Speyer 1933), especially Is the sixties scholars such as Wang Hengsheng proposed fusion from mineralization that,