早在1958年,就曾有人提出了白云鄂博铁矿属沉积成因的看法,此后在经过科学院地质所和贵阳地化所的研究,大多数人认为应属于沉积———热液交代变质铁矿,本文对前人有关资料略作归纳,以进一步论证白云鄂博铁矿的沉积———热液交代变质成因。 As early as 1958, some people had put forward the view of the genesis of the Baiyunebo iron deposit, and after that, after the research by Institute of Geology and Guiyang Institute of Geography, most people think that it belongs to the sedimentary-hydrothermal metamorphic iron ore This article summarizes the relevant data of the predecessors in order to further demonstrate that the deposition of the Baiyunebo Iron Deposit is the cause of metamorphism of hydrothermal fluids.