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本文描述了产在乌克兰显生宙建造中的两个主要铀矿床类型。它们是由上石炭统到下三叠统的红层中的含铀地沥青和充填下第三系古河谷沉积物中的渗入(卷锋)型铀矿床。第一种矿床类型包括分别以氧碳沥青和氧硫沥青出现的浸染状到块状地沥青的黑色至深褐色层,这些层含铀和其他金属。这种铀矿化的年龄为195～200Ma。第二种类型是下第三系含煤沉积物中的渗入矿床,铀矿化出现在沉积序列的上部。沉积物产在侵蚀切入下伏的乌克兰地盾结晶基底及其风化壳的古河谷中,古河谷延深至70～90m。含煤沉积物被更新的沉积物所覆盖。已经发现几个第二种类型的铀矿床,包括几个已被确认有工业品位的矿床。
This article describes the two main types of uranium deposits produced in the Phanerozoic in Ukraine. They are uranium-bearing bitumen in the red beds of the Lower Triassic from the Upper Carboniferous and infiltration (volume feng shui) uranium deposits in the sediments of Tertiary paleo-valleys under filling. The first deposit type consists of a black to dark brown layer of disseminated, block-like bitumen appearing as oxycarbonated and oxysiluted, respectively, containing uranium and other metals. The age of this uranium mineralization is 195 ~ 200Ma. The second type is the infiltration of deposits in the Lower Tertiary coal-bearing deposits, uranium mineralization occurs in the upper part of the sedimentary sequence. Sediment production in the erosion into the underlying Ukraine shield crystalline basement and weathering the ancient valleys, the ancient valley deepened to 70 ~ 90m. Coal-bearing sediments are covered by newer sediments. Several second types of uranium deposits have been discovered, including several that have been identified as industrial grade.