POLYGENIC EXOGENOUS FORMATION OF URANIUM DEPOITS IN DNIEPER DONETSK DEPRESSION

Abstract

The mechanism of forming of the Adamovskoie, Krasnooskolskoie, Berekskoie poligenous uranium – bitumenous fields being attributed to the local stratigraphical disconformities of the Systems of the Carboniferous and Permian, has been considered. The synchroneity of all the following named – the dynamical activity of fractures, the forming of anticlinal structures, the input of hydrothermic ore – bearing solutions, the destruction of hydrocarbon pools, the forming of U-bitumenous mineralization in hydrogeologically opened structures has been strongly paid attention. The U-bearing metallizations being accompanied by that of polymetallization-present