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WU Jian,YANG Haoyu,XU Yanyong,et al. Reservoir characteristics and development control factors of Benxi Formation bauxite in the Linxing area of Ordos Basin[J]. Bulletin of Geological Science and Technology,2025,44(5):1-12 doi: 10.19509/j.cnki.dzkq.tb20230657
Citation: WU Jian,YANG Haoyu,XU Yanyong,et al. Reservoir characteristics and development control factors of Benxi Formation bauxite in the Linxing area of Ordos Basin[J]. Bulletin of Geological Science and Technology,2025,44(5):1-12 doi: 10.19509/j.cnki.dzkq.tb20230657

Reservoir characteristics and development control factors of Benxi Formation bauxite in the Linxing area of Ordos Basin

doi: 10.19509/j.cnki.dzkq.tb20230657
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  • Author Bio:

    E-mail:ilcby@163.com

  • Corresponding author: E-mail:yhydaze@163.com
  • Received Date: 27 Nov 2023
  • Accepted Date: 02 Jan 2024
  • Rev Recd Date: 21 Dec 2023
  • Available Online: 05 Jan 2024
  • <p>In recent years, the bauxite gas exploration of the Taiyuan Formation in the Longdong area of Ordos Basin has made a breakthrough, which has attracted wide attention at home and abroad. During the same period, the bauxite rock gas of the Benxi Formation in the Linxing area has also made some progress; however, the characteristics and controlling factors of the bauxite reservoir in this area remain unclear, which restricts the exploration process. </p></sec><sec><title>Objective

    To identify the reservoir characteristics and influencing factors of Benxi Formation bauxite in the Linxing area,

    Methods

    the paper carried out XRD, cast sheet imaging, SEM-EDS, mercury intrusion porosimetry, nitrogen and carbon dioxide adsorption, and routine porosity measurements, coupled with seismic logging data, to characterize the mineral composition, pore structure, and physical properties of the bauxite reservoir and to discuss the controls on its development.

    Result

    The results show that the aluminum-bearing minerals in Benxi Formation bauxite in the Linxing area are dominated by dispore. Pore types are primarily intra-granular, intergranular, matrix, and microcrack pores, with occasional organic pores. Pore volume is mainly contributed by mesopores and macropores, with pore-size peaks mainly at 30−70, 80−130, 400013000 nm. The overall reservoir physical properties are modest, with an average porosity of 3.28% and an average permeability of 1.398×10−3 μm2. However, the lower part of the section, which has a higher diaspore content, exhibits relatively better properties. Finally, the development of the Linxing bauxite reservoir is controlled by palaeo-geomorphology, palaeo-sedimentary environment, and diagenesis. Specifically, accumulation and distribution of bauxite are controlled by the paleogeomorphology of depressions and troughs and by enclosed to semi-enclosed intermittent swamps and lagoons. Diagenesis determines the reservoir-space types and the resulting physical-property conditions within the sedimentary context.

    Conclusion

    The research results can provide theoretical guidance for the bauxite gas exploration.

     

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