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    中国百强科技报刊

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    Volume 49 Issue 2
    Feb.  2024
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    Article Contents
    Ding Bo, Liu Hongxu, Xu Deru, Qiu Linfei, Zhang Zilong, He Feng, 2024. Uranium Metallogenic Effect of Hydrothermal Fluid Transformation in Sandstone-Type Uranium Deposits in Northern Ordos Basin: Constraints from the Study of Biotite Chloritization Process. Earth Science, 49(2): 625-638. doi: 10.3799/dqkx.2022.336
    Citation: Ding Bo, Liu Hongxu, Xu Deru, Qiu Linfei, Zhang Zilong, He Feng, 2024. Uranium Metallogenic Effect of Hydrothermal Fluid Transformation in Sandstone-Type Uranium Deposits in Northern Ordos Basin: Constraints from the Study of Biotite Chloritization Process. Earth Science, 49(2): 625-638. doi: 10.3799/dqkx.2022.336

    Uranium Metallogenic Effect of Hydrothermal Fluid Transformation in Sandstone-Type Uranium Deposits in Northern Ordos Basin: Constraints from the Study of Biotite Chloritization Process

    doi: 10.3799/dqkx.2022.336
    • Received Date: 2022-12-25
    • Publish Date: 2024-02-25
    • Uranium (U)-concentrated areaof northern Ordos Basin is one of the most important sandstone-type U deposits in north China. In order to find out the Umetallogenic effect of hydrothermal fluid transformation in this area, the mineral-geochemical characteristics of biotite chloritization process were studied by thin section identification, scanning electron microscopy (SEM) and electron probe (EMPA). The results show that biotite in sandstone-type U deposits in north Ordos Basin mostly occurs chloritization, which is often altered and metasomatized along the cleavage and edge of biotite, accompanied by the release of Si, Fe, Ti, U and other elements. Hydrothermal fluid related to altered biotiteis basin brine with hydrocarbon and has the characteristics of alkaline–reducing and medium-low temperature (137.3~208.3 ℃). Moreover, U-rich source rocks were widely developed in the deep part of the Ordos Basin and the hydrocarbon expulsion and emigrated U can migrate along the faults and other channels with the geothermal brine in basin under the action of continuous burial and thermal events, which can theoretically provide deep U sources forsandstone-type U deposits in this area. When it migratedlaterally to ore-bearing layer, the U-rich hydrothermal fluid was formed by extracting U fromthe ore-bearing sandstones and dissolving the U minerals formed in the early stage. U is reactivated and migrated in the form of organic complexes or organic colloids in hydrothermal fluid and precipitated in the form of coffinite around pyrite, organic matter and calciteat the changing parts of reducing capacity, temperature, pressure and pH, resulting, which provides a basis for the Umetallogenic effect of hydrothermal fluid transformation in sandstone-type U deposits. In addition, the above fluid-rock reaction was easy to cause biotite chloritization, forminghydrothermal altered mineral assemblages, such aschloritized biotite-coffinite, chloritized biotite-pyrite-coffinite, chloritized biotite-anatase-coffinite, anatase-coffinite, which also provides direct evidence for the participation of hydrothermal fluid in sandstone type U deposits.

       

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