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截止到1997年，对俄罗斯境内地台和叠置造山盆地的盖层含铀性的实际资料进行了综合研究。对这些盖层的含铀性取得了一些认识。这些认识是在编制一系列1：5000000的成矿预测图件的基础上获得的。对该区主要工业类型铀矿化的分布和形成规律进行了描述，提出了前中生代、中生代和新生代铀成矿期的区划和分类。对传统的、非传统的以及新的铀矿化类型，首先是呈局部和区域分布的与层间和潜水氧化带有关的矿化类型进行了预测，指出了在俄罗斯亚洲地区发现可地浸开采铀矿化地区是西西伯利亚地台的南部和外贝加尔地区的叠置盆地。
As of 1997, a comprehensive study was carried out on the actual uranium-bearing data of the overburden and overburden in Russia. Some understanding of the uranium-bearing properties of these cap rocks has been made. These understandings are based on the preparation of a series of 1: 5000000 map of mineralization. The distribution and formation regularity of uranium mineralization in major industrial areas in this area are described. The division and classification of pre-Mesozoic, Mesozoic and Cenozoic uranium mineralization stages are proposed. Prediction of traditional, unconventional and new types of uranium mineralization, first and foremost local and regional mineralization associated with interlayer and subduction oxidation zones, indicates the availability of sub-leachable mining in the Russian region of Asia The uranium mineralization is a superimposed basin of southern Siberia and Outer Baikal.