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对独联体各国热液金矿床分布的分析表明,晚太古代、元古代、古生代、中生代和新生代成矿期金矿化的强度不相上下。对独联体各国的含金性图进行了整理。评价金矿化发育强度的基础主要是大型(>100t)金矿床总储量(开采余下的储量)数据。将热液金矿床划分了16个地质成因类型;其形成与不同种类的成矿系统有关。评价了各种系统的极限产矿力,普通系统其值可以达到4000t 金。讨论了岩浆系统和变质系统的概念。得出了大型矿床的形成是由于地幔作用与地壳作用相互间发生非常复杂作用的结果的结论。
The analysis of the distribution of hydrothermal gold deposits in various countries of the Commonwealth of Independent States shows that the strength of gold mineralization in late Archean, Proterozoic, Paleozoic, Mesozoic and Cenozoic mineralization stages is comparable. The gold charts of the Commonwealth of Independent States have been sorted out. The basis for assessing the strength of gold mineralization is mainly the total (> 100t) gold deposit total reserves (remaining reserves) data. The hydrothermal gold deposit is divided into 16 geologic types; its formation is related to different types of metallogenic systems. Evaluation of the various systems of the limit of mineral production, the value of the ordinary system can reach 4000t gold. Discuss the concept of magma system and metamorphic system. It is concluded that the formation of a large deposit is the result of a very complex interaction between the mantle and the crust.