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已有许多文献探讨过内生矿化和交代岩之间的成因联系和恃征。鲍格达萨罗夫等人把交代岩分为近矿蚀变岩石和区域交代岩石。根据这些作者的意见,第一种岩石是在“与矿源同一种溶液作用下形成的,而且,成矿作用是在同时期或者在作用的最后阶段产生”。他们将与区域性交代岩有关的金属矿床分为同生矿床和次生交代矿床。他们认为,次生交代矿床的特点之一是,矿化前,
Much literature has been explored about the genesis and association between endogenous mineralization and metasomatism. Bogdarsarov and others divided the metasomatic rocks into near-alteration rocks and areas to account for rocks. According to these authors, the first type of rock is formed “under the same solution as the source and the mineralization is produced at the same time or at the final stage of the action.” They divide the metal deposits related to the regional metasomatism into syngenetic deposits and secondary replacement deposits. In their view, one of the characteristics of secondary replacement deposits is that before mineralization,