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矿床成因学——是地貭学的年青分支之一,它是矿床学的一个方面,专门研究矿化分布規律和控制这种分布的地貭因素。成矿研究主要涉及的問題是矿化作用在地壳某一个地段内的空间分布和以地貭条件为轉移的矿化作用在地壳的发展史中的发生时間。当然这就涉及到矿床的成因問题,即矿床生成的原因和形成的过程。但是对于这些問題也是从矿化分布的观点来研究的。从以上的論述可以知道,矿床成因研究在提高找矿效率上该有多么重大的意义。苏联矿床成因学的奠基人——斯米尔諾夫、毕利賓創立了这門学科来研究錫,鎢,金等矿床的区域分布規律并不是
Genesis of deposit - is one of the young branches of geology, it is an aspect of depositology, specializing in the distribution of mineralization rules and control of this distribution of factors. The main problems involved in metallogenetic research are the spatial distribution of mineralization in one part of the crust and the occurrence of mineralization in the development of the earth’s crust as a result of the 地 conditions. Of course, this involves the genesis of the deposit, that is, the cause of deposit formation and the process of formation. However, these issues are also studied from the perspective of mineralization. It can be seen from the above discussion that the significance of the research on deposit genesis in improving the efficiency of prospecting is of great significance. The founder of the Soviet Union deposit genesis - Smirnov, Bi Li Bin founded the discipline to study tin, tungsten, gold and other deposits of the regional distribution is not