一、前言自十六世纪德人阿格利科拉提出成矿的概念,按形态进行了矿床分类以来,随着地质科学的发(?),特别是成矿理论的不断创新,于是各种矿床成因分类应运而生。至二十世纪前半期,在内生矿床方(?)明显分出两大派系:一 I. Preface Since the concept of metallogenesis was proposed by German Aglikkla in the 16th century, since the ore deposit was classified according to its morphology, with the continual innovation of geology (especially the mineralization theory) of geological science, Origin of the deposit classification came into being. By the first half of the twentieth century there were clearly two major factions in the endogenous deposits (?):