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过去几十年,成矿学有很大的进展,这种说法虽然不会有人反对。取得这种进展的原因是,我们在苏联领域上,研究了以内生矿床为主矿床的分布规律,发现了若干新的矿区和矿省,并且取得了成就。但是,在过去几年,对成矿学研究的兴趣略有减少,这也是显而易见的,原因可能很多,其中至少三个原因是大家都知道的。第一个原因是:我们曾制定出区域成矿分析的一般理论原则,后来在50—60年代末对其作了改进,根据这些原则编了成矿规律
In the past few decades, great progress has been made in mineralogy, though no one will object. The reason for this progress is that we studied the distribution of endogenic deposits in the Soviet Union, discovered several new mines and mines, and achieved success. However, it is also obvious that there has been a slight decrease in interest in mineralogical research over the past few years for many reasons, at least three of which we all know. The first reason is that we have devised the general theoretical principles of regional metallogenic analysis and later improved it in the late 1950s and 1960s, according to which the principles of mineralization were codified