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    Si Qinghong, Zhu Qiang, Miao Peisen, Li Jianguo, Zhao Hualei, Wang Zhixiang. 2024. Alteration characteristics and implication to uranium metallogenetic fluids of faded sandstones in Luohe Formation, Pengyang area, Ordos Basin[J]. Geology in China, 51(5): 1455−1468. DOI: 10.12029/gc20210416001
    Citation: Si Qinghong, Zhu Qiang, Miao Peisen, Li Jianguo, Zhao Hualei, Wang Zhixiang. 2024. Alteration characteristics and implication to uranium metallogenetic fluids of faded sandstones in Luohe Formation, Pengyang area, Ordos Basin[J]. Geology in China, 51(5): 1455−1468. DOI: 10.12029/gc20210416001

    Alteration characteristics and implication to uranium metallogenetic fluids of faded sandstones in Luohe Formation, Pengyang area, Ordos Basin

    Funds: Supported by the Key Program of the National Science Foundation of China (No.92162212), National Key Research and Development Program (No.2023YFC2906700, No.2018YFC0604200), International Geoscience Program (No.IGCP675) and the project of China Geological Survey (No.DD20221678).
    More Information
    • Author Bio:

      SI Qinghong, male, born in 1986, senior engineer, mainly engaged in study of geochemistry and fluid alteration; E-mail: sqinghongcgs@163.com

    • Corresponding author:

      ZHU Qiang, male, born in 1987, senior engineer, mainly engaged in the investigation of sandstone type uranium deposits and fluid alteration; E-mail: zhuq1987@163.com.

    • Received Date: April 15, 2021
    • Revised Date: October 03, 2022
    • This paper is the result of mineral exploration engineering.

      Objective 

      The faded alteration of uranium−bearing rock series in the redbed is closely related to reductive alteration, and the analysis of the characteristics of faded alteration and its genetic fluid is of great significance for understanding the uranium ore−forming fluids and ore−forming mechanism.

      Methods 

      This study is based on analyzing the sedimentary characteristics and faded alteration characteristics of sandstones in Luohe Formation by means of core logging, element geochemical test, electron microscope scanning, electron probe analysis, XRF scanning and core infrared spectrum scanning.

      Results 

      The sandstones in the Luohe Formation are basically formed in aeolian sedimentary with oxidation conditions mineral assemblages enriched in uranium minerals, pyrite and gypsum but little trivalent iron oxides, and uranium and sulfur elements show obvious migration. Then, the redox state of sandstone and the correlation between uranium mineralization and faded alteration were discussed.

      Conclusions 

      The main body of Luohe Formation sandstone was formed in aeolian deposits under oxidation conditions, and its color, Fe2O3/FeO, Th/U and Cu/Zn reflect that the environment has been changed from oxidation to reduction with the increase of sandstone faded degree. The characteristics of the consistency between faded alteration and uranium mineralization in Luohe Formation in space, mineral association and redox state suggest that their genesis is related to the same reducing fluid.

      Highlights
      The multi−scale matching relationship between the faded alteration and uranium mineralization of the Luohe Formation sandstone in the Pengyang area was described by using multiple methods, and the redox indexes of the sandstones with different fading degrees were compared. The genesis of uranium mineralization and faded alteration is mainly reformed by reducing fluid by the same reducing fluid. This realization has an indicative effect on the fluid which has innovative significance for establishing and identifying metallogenic fluids of uranium.
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