PATTERNS OF URANIUM-ORE LOCALIZATION IN THE DONO-DNIPROVSKA POTENTIAL URANIUM-ORE METALLOGENIC PROVINCE IN ASSOCIATION WITH LITHOSPHERE'S DEEP STRUCTURE

G. Kalashnyk, А. Кuzmin
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Abstract

The objective of the study is to identify the main patterns of uranium-ore localization in the Dono-Dniprovska potential uranium-ore province in association with lithosphere's deep structure. The analysis of geophysical, geological, petrological, radiogeochemical information on the features of the formation, placement of uranium occurrences of the different genetic types in the Dnieper-Donets aulacogen in close connection with the features of the deep structure of the lithosphere, asthenosphere, fault tectonics was carried out. The features of the deep structure of the lithosphere and their physical parameters that affect the conditions of intensive uranium ore genesis in the formation of the main geological industrial types of uranium deposits in the research area were revealed. According to analysis of geological materials (uranium bearing, features of sedimentary-volcanogenic and, to a lesser extent, crystalline rocks occurrence, variety of breaking tectonics at various levels of the geological section, groundwater circulation conditions, etc.) the most perspective for discovering of new uranium deposits horizons and strata assigned to uranium-bearing geological formation in this region were identified. Based on a joint analysis of the geological conditions of localization of uranium deposits, ore occurrences and manifestations of uranium mineralization, geological uranium-bearing formations, their prevalence and depth occurrence in the Dnieper-Donets aulacogen, the four most perspective for this region industrial types of uranium deposits have been identified. The practical significance of this research is to increase the efficiency of metallogenic forecasts by expanding the deep factors and regional criteria for uranium ore genesis of various genetic types specified to the study area. This makes it possible to reasonably determine the prospects of the territories for the possibility of forming uranium industrial ore concentration with the allocation of areas of their most probable localization.
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多诺-德涅普罗夫斯卡铀矿成矿潜力区铀矿定位模式与岩石圈深部构造的关系
研究的目的是结合岩石圈深部构造,确定多诺-德涅普洛夫斯卡铀矿潜力省铀矿定位的主要模式。结合岩石圈、软流圈、断裂构造等深部构造特征,对第聂伯河-顿涅茨断陷槽内不同成因类型铀的形成特征、赋存位置进行了地球物理、地质、岩石学、放射地球化学等方面的资料分析。揭示了研究区主要铀矿床地质工业类型形成过程中影响铀矿成矿条件的岩石圈深部结构特征及其物性参数。通过对地质资料(含铀、沉积—火山特征及少量结晶岩产状、地质剖面各层次破碎构造的多样性、地下水循环条件等)的分析,确定了该区新铀矿层位和含铀地质构造层位最有发现前景。通过对第聂伯-顿涅茨断陷槽铀矿定位地质条件、铀矿赋存状态和矿化表现、含铀地质构造、分布及产状深度的综合分析,确定了该地区铀矿工业类型的4种最具前景。本研究的现实意义在于通过扩大研究区各种成因类型铀矿成因的深层因素和区域标准,提高成矿预测的效率。这就有可能合理地确定有可能形成铀工业矿砂集中的领土的前景,并分配其最可能定位的地区。
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