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Genetic model of uranium mineralization in the Permo-Triassic sedimentary rocks of the Stara Planina eastern Serbia
Authors:Jovan Kova evi&#x;  Zoran Niki&#x;  Petar Papi&#x;
Institution:aGeological Institute of Serbia, 11000 Belgrade, Rovinjska 12, Serbia;bDepartment of Ecological Engineering, Faculty of Forestry University of Belgrade, 11030 Belgrade, Kneza Višeslava 1, Serbia;cFaculty of Mining and Geology University of Belgrade, 11000 Belgrade, Đušina 7, Serbia
Abstract:One deposit and four occurrences of uranium minerals in the Permo-Triassic sedimentary rocks of the Stara Planina in eastern Serbia were ascertained using data from years of multidisciplinary geological research. The minerals are the fissure-filling type, and were assigned to the exogenic mineralization group, being mostly epigene in nature. Relevant geological information was used to derive a genetic model of uranium mineralization in the Permo-Triassic sedimentary rocks of the Stara Planina. The model explains the formation of Permo-Triassic rocks and three stages of the complex process of U mineralization. The genetic model treats: (1) the primary sources of the uranium; (2) the mobility of uranium; and (3) accessory metals from the parent rocks to their deposition in host rocks and the postmineral change in ore bodies. A geochemical barrier zone was identified in the sedimentary rocks that contained uranium mineral ore. This geochemical barrier area included crescent-shaped, flat-lens, or vein-like ore bodies. The U-containing mineral described is comparable with those from the relatively common fissure-filling uranium minerals found around the world.
Keywords:Uranium minerals  Permo-Triassic  Sedimentary rocks  Groundwater  Eastern Serbia
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