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早就发现中西伯利亚的金矿床产于一定成分和相从属关系的变质岩发育区。H.B.彼得洛夫卡斯娅在40年代研究该区矿床的矿物学并否定矿化与变质作用的成因联系之后,仍然根据围岩的变质作用程度进行了金属矿床的分类。矿化与一定内生作用的关系目前尚未得到公认。有关矿化与岩浆作用、变质作用和交代作用的关系存在多种见解。在进行找矿工作时有必要考虑变质作用的类型和变质改造的程度。
It has long been discovered that the gold deposits in Central Siberia are produced in the metamorphic rock development zone of certain composition and phase subordination. H.B. Petrovka Kassa classified the metallogenic deposits according to the degree of metamorphism of the surrounding rock after studying the mineralogy and negating the genesis of mineralization and metamorphism in the area in the 1940s. The relationship between mineralization and certain endogenous effects has not yet been recognized. There are many insights into the relationship between mineralization and magmatism, metamorphism and metasomatism. It is necessary to consider the type of metamorphism and the degree of metamorphism and transformation when conducting prospecting.