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对矿脉中铀矿化分布规律性的研究具有重要的意义,但是到目前为止,地质人员对控制铀矿化的因素尚无一致的意见,而对铀从热液中沉淀的条件更无统一的见解。第一种人认为,铀是由于热液与含二价铁、钙、镁、钠的化学性活泼的围岩相互作用而从热液中沉淀出来的(别雷姆斯基,1959);第二种人否认围岩对热液中铀沉淀过程的影响,仅承认构造因素的作用(别捷赫京,1959);第三种人认为,化学性活泼的围岩和构造变动对矿脉中铀从溶液中的沉淀均有影响(鲁金,索纽什金,1958;纳乌莫夫,1959;雅尼舍夫斯基,康斯坦丁诺夫,1960)。
Research on regularity of uranium mineralization distribution in veins is of great significance, but so far there is no consensus among geologists on the factors that control uranium mineralization, and there is no uniform condition for uranium precipitation from hydrothermal fluids opinion. The first believed that uranium precipitated from hydrothermal fluids due to the interaction of hydrothermal fluids with chemically active rock containing ferrous, calcium, magnesium and sodium (Beremski 1959); Two kinds of people deny the impact of wall rock on hydrothermal uranium precipitation, only recognize the role of tectonic factors (Beijjegen, 1959); the third kind of people think that the chemical activity of the surrounding rock and structural changes of uranium in the veins The precipitation from the solution has an effect (Rukin, S0nushkin, 1958; Numomov, 1959; Janishevsky, Konstantinov, 1960).