Polygenic uranium-thorium-rare earth mineralization of the Nether-Polar Urals: discovery history and genesis

IF 0.2 Q4 FORESTRY
Sfen Karagodin, V. Karagodin, G. Khasanova
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Abstract

The research relevance is determined by the need to analyze various sources and author's observations to form ideas about the genesis of an unusual polygenic uranium-thorium-rare earth mineralization of the Nether-Polar Urals to assess the prospects and directions for subsequent mining and processing. The research results will aid in a more rational and efficient geological research. The research objective is to interpret the results, determine mineralization genesis features and show its future prospects against the background of the discovery history and using data from a complex analysis of uranium-thorium-rare-earth mineralization in conglomerates of the regional structural-stratigraphic unconformity zone. Results. The geological position of rare-metal conglomerates has been clarified, their belonging not to the Precambrian, but to the Early Paleozoic era has been determined. The absence is considered of a genetic connection between the gold mineralization recorded in the zone of structural-stratigraphic unconformity and polygenic uranium-thorium-rare earth mineralization. The shortage of rare earth elements determines the industrial significance of uranium-rare-earth complex ores, the extraction of which is possible using modern heap leaching technologies. Conclusions. The history of the study of uranium-thorium-rare-earth mineralization of the NetherPolar Urals is considered. According to the authors, it has a polygenic genesis and forms into the successive stages of sedimentary, metamorphogenic and hydrothermal processes. A hypothesis of hydrogenous hydrothermal ore formation under regional metamorphism is proposed as an alternative to the magmatogenic origin of hydrothermal ore melts. It determines the need for new approaches to mineralization assessment. The industrial value of mineralization lies in the presence of metamict, hydrated, easily soluble minerals, carriers of uranium and rare earth elements, which implies the possibility of using modern mining technologies.
乌拉尔下极多源铀钍稀土矿化:发现历史与成因
研究的相关性取决于需要分析各种来源和作者的观察,以形成关于下极乌拉尔地区不寻常的多源铀-钍-稀土矿化成因的想法,以评估后续开采和加工的前景和方向。研究结果将有助于更合理、更有效地开展地质研究。结合区域构造-地层不整合带砾岩中铀-钍-稀土矿化的发现历史和复杂分析资料,对结果进行解释,确定成矿成因特征,并展望其未来前景。结果。明确了稀有金属砾岩的地质位置,确定其不属于前寒武纪,而属于早古生代。认为构造-地层不整合带记录的金矿化与多成因铀-钍-稀土矿化之间存在成因联系。稀土元素的短缺决定了铀-稀土复合矿石的工业意义,利用现代堆浸技术可以提取铀-稀土复合矿石。结论。回顾了下极乌拉尔地区铀钍稀土矿化研究的历史。认为其成因是多成因的,形成于沉积作用、变质作用和热液作用的连续阶段。提出了区域变质作用下的含氢热液成矿假说,作为热液矿熔体岩浆成因的替代假说。这决定了需要新的矿化评价方法。矿化的工业价值在于存在变质岩、水合易溶矿物、铀和稀土元素的载体,这意味着利用现代采矿技术的可能性。
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