湖北铁山矿床是“大冶式”铁矿床的重要代表。解放后,黄懿和裴荣富等曾以勘探工作时所获成果为基础,论述了“大冶式”铁矿的特征,提出矽卡岩和热液成因的看法。六十年代注意了闪长岩钠长石化析出铁质,七十年代演变为接触交代论点;这一阶段还强调了三叠纪膏盐层促进闪长岩钠化而成矿的意义。 The Tieshan deposit in Hubei is an important representative of the “Daye type” iron deposit. After the liberation, Huang Yi and Pei Rongfu had based on the achievements obtained during the exploration work, discussed the characteristics of the “Daye-type” iron ore and put forward the views on the genesis of skarn and hydrothermal fluids. In the 1960s, attention was paid to the diorite precipitation of diorite, which became the contact conformation in the seventies. This stage also emphasized the significance of Triassic gypsum saltification to promote the sodiumification of diorite and mineralization.