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中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

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Volume 43 Issue 3
May  2024
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Article Contents
Article Navigation >  Bulletin of Geological Science and Technology  > 2024  >  43(3): 22-35
DU Xianli, WANG Hongbo, ZHAO Rongsheng, JI Hui, ZHU Huanlai, DAI Dengliang, WANG Ying, LI Yingjiu, XIAO Hongping. Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605
Citation: DU Xianli, WANG Hongbo, ZHAO Rongsheng, JI Hui, ZHU Huanlai, DAI Dengliang, WANG Ying, LI Yingjiu, XIAO Hongping. Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin[J]. Bulletin of Geological Science and Technology, 2024, 43(3): 22-35. doi: 10.19509/j.cnki.dzkq.tb20230605
shu

Geothermal chemical characteristics and genetic model of the Qingshankou Formation in the Daqingzijing area, southern Songliao Basin

doi: 10.19509/j.cnki.dzkq.tb20230605
  • 1.

    School of Earth Science, Northeast Petroleum University, Daqing Heilongjiang 163318, China

  • 2.

    College of Earth Science, Jilin University, Changchun 130061, China

  • 3.

    SINOPEC Shengli Oilfield Company Gudong Oil Extraction Plant, Dongying Shandong 257237, China

  • 4.

    PetroChina Jilin Oilfield Exploration and Development Research Institute, Songyuan Jilin 138000, China

  • 5.

    PetroChina Research Institute of Exploration and Development, Beijing 100083, China

More Information
  • Author Bio:

    DU Xianli, E-mail: duxl@nepu.edu.cn

  • Corresponding author: ZHAO Rongsheng, E-mail: zhaors@jlu.edu.cn
  • Received Date: 30 Oct 2023
  • Accepted Date: 23 Jan 2024
  • Rev Recd Date: 22 Jan 2024
    Abstract
  • Objective

    With high reservoir temperature, good lithology and high water content, the Qingshankou Formation is the best geothermal reservoir of Daqingzijing area, the saddle of the Changling Depression. Therefore, elucidating the genetic model of geothermal water is of great significance for the sustainable development and utilization of geothermal resources in this area.

    Methods

    In this study, the source and mixing process of geothermal water in a target area were studied by hydrochemical testing of geothermal water samples collected from 7 wells in the Qingshankou Formation, combined with 8 groups of hydrogen and oxygen isotope data, and a genetic model was established.

    Results

    The results show that the geothermal water of the Qingshankou Formation is mainly Cl-Na-type fluid, which is partially balanced. And the geothermal water is originated from the precipitation and primary sedimentary water in the Changbai Mountain area, with recharge elevation of 2 347-2 370 m. A geothermal fluid with a reservoir temperature of 81.25-112.80 ℃ was formed after the cyclic heat absorption process and was stored in the clastic rock reservoir of the Qingshankou Formation in a semi-open system.

    Conclusion

    In addition, the northeast-oriented and northwest-oriented fault systems in the study area are the main water conducting channels for geothermal fluid circulation. During the deep circulation, geothermal fluid reactions with surrounding rock minerals, resulting in the dissolution of carbonate and silicate minerals, forming geothermal water resources dominated by Na+, Cl- and HCO3- ions.

     

    • The authors declare that no competing interests exist.
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