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对苏联某些含铀矿区的热液铀矿床和硫化物-铀矿床氧化带矿物进行比较研究,使之有可能确定出在一般矿物成份和铀矿化性质方面彼此不同的氧化带的矿物类型。 鑑于这篇报告旨在阐述氧化带的类型,故有关具体的矿床这里并不加以探讨,仅提出研究工作的综合结果。作者的工作是根据C.C.斯米尔诺夫院士学派的传统分类进行的,他对硫化物矿床氧化带所提出的卓越的科学见解,在铀矿床氧化带内也得到了证实。一切经过研究的热液铀矿床氧化带均属于裂隙类型,即是说,在其他相同的条件下,其氧化带的发育取决
A comparative study of some uranium-bearing hydrothermal uranium deposits and sulfide-uranium oxide belt minerals in the Soviet Union made it possible to identify mineral types of oxide bands that differ from one another in general mineral composition and uranium mineralization. Since the purpose of this report is to describe the type of oxidation zone, the specific deposit concerned is not discussed here and only the comprehensive results of the research work are presented. The author’s work is based on the traditional classification of the academician C.C. Smirnov School and his excellent scientific insight into the oxidation zone of sulfide deposits has also been demonstrated in the oxidation zone of uranium deposits. All studied oxidation zones of hydrothermal uranium deposits belong to the fissure type, that is to say, under the same conditions, the development of the oxidation zone depends on