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对苏联铀矿床的研究表明,它们的物质成分是多种多样的。在对矿床中的矿物和矿物综合体的生成次序研究后查明,矿床中的铀矿化居于一定的位置。与铀矿物同时沉积有为数不多的其它矿物。这一矿物组在本文中称为共生矿物组。铀矿床中铀矿物的共生组合的分析,既表明了其中每一种共生体的特点,也表明了多数矿床铀成矿时期所固有的一般特点。共生组合的描述是按铀的化学化合物的类型进行的。按习惯上的分类,可分出铀的氧化物共生和铀的硅酸盐共生。前一种共生非常广泛,它又可分为一系列的共生组合,这些共生组合是根据主要铀矿物及与
Studies of Soviet uranium deposits show that their material composition is diverse. After studying the sequence of formation of the mineral and mineral complexes in the deposit, it has been found that the uranium mineralization in the deposit lives in a certain position. There are also a few other minerals deposited simultaneously with uranium minerals. This group of minerals is referred to herein as the group of symbiotic minerals. The analysis of the symbiotic assemblages of uranium minerals in uranium deposits not only indicates the characteristics of each of these symbionts, but also shows the general characteristics inherent in uranium mineralization in most deposits. The description of symbiotic combinations is based on the type of chemical compound of uranium. By convention, uranium oxide symbiosis and uranium silicate symbiosis can be separated. The former is a very broad symbiosis, which can be divided into a series of symbiotic combinations based on the combination of major uranium minerals and