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2023 Vol. 50, No. 4
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Article navigation > Geology in China > 2023 > 50(4): 1149-1162
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GAO Nan'an, WANG Xinwei, LIANG Haijun, DU Li, MAO Xiang, LUO Lu. 2023. Genetic mechanism of geothermal system in Daming Sag, Linqing Depression in the junction of Hebei, Shandong and Henan Provinces and its exploration potential[J]. Geology in China, 50(4): 1149-1162. doi: 10.12029/gc20201230002
Citation: GAO Nan'an, WANG Xinwei, LIANG Haijun, DU Li, MAO Xiang, LUO Lu. 2023. Genetic mechanism of geothermal system in Daming Sag, Linqing Depression in the junction of Hebei, Shandong and Henan Provinces and its exploration potential[J]. Geology in China, 50(4): 1149-1162. doi: 10.12029/gc20201230002
shu

Genetic mechanism of geothermal system in Daming Sag, Linqing Depression in the junction of Hebei, Shandong and Henan Provinces and its exploration potential

  • 1.

    SINOPEC Star Petroleum Co., Ltd., Beijing 100083, China

  • 2.

    Key Laboratory of Geothermal Exploitation and Utilization, Sinopec, Beijing 100083, China

    • Fund Project: Supported by Science and Technology Project of Sinopec Corporation (No. JP19002)
More Information
  • Author Bio: GAO Nan'an, female, born in 1989, Ph.D., engineer, mainly engaged in basin analysis and geothermal geology research; E-mail: nanan.gao96@gmail.com
  • Corresponding author: WNG Xinwei, male, born in 1968, Ph.D., senior engineer, mainly engaged in structural geology and geothermal geology research; E-mail: wangxinwei.xxsy@sinopec.com 
Received Date:  30 December 2020
Revised Date:  19 January 2021
Publish Date:  25 August 2023
    Abstract

  • This paper is the result of geothermal survey engineering.

     Objective

    Building genetic model of the geothermal system plays an important guiding role in the evaluation of the geothermal resources of the geothermal field and the later selection of favorable zones. Daming Sag is a secondary structural unit at the southern of Guantao Uplift in Linqing Sag, Bohai Bay Basin. The sandstone thermal reservoir of Guantao Formation can form a complete geothermal system.

     Methods

    Combining previous research results and regional geothermal drilling data, through analysis and research on the main geological factors of the "source, reservoir, migration, and cover", the conceptual model of the geothermal system was established in Daming Sag, Linqing Depression. On this basis, a evaluation of geothermal resources was carried out.

     Results

    The thermal reservoirs of the Guantao Formation are uniformly distributed in the area, the floor depth is between 1550-2000 m, the thickness of the reservoir is between 268-324m, the porosity is between 14%-32%, and the reservoir-thickness ratio can reach up to 70%. The geothermal wells drilled into the Guantao Formation in the area, its water temperature is about 54-60℃, and the water chemistry type is mainly Cl×SO4-Na. The upper Quaternary and Minghuazhen Formation strata have a geothermal gradient between 22-60℃/km, forming a good cap layer. The heat source comes from the high geothermal value background of the Cenozoic rift basin, about 52-57 mW/m2. The Linzhang-Daming fault in the south and the Guanxian fault in the east are favorable channels for the upward transportation of deep heat. The geothermal system receives the atmospheric precipitation replenishment from the Taihang Mountains in the west and the southwestern Luxinan uplift in the east. After being warmed by deep heat conduction and local heat convection, it is enriched in the reservoir.

     Conclusions

    The evaluation results of the geothermal resources in the Damingci Depression show that the sandstone geothermal system resources of the Guantao Formation are more than 127.42×108 GJ, the annual geothermal resources that can be exploited are 31.86×106 GJ equivalent to 1.09×106 t of standard coal. The annual exploitation of geothermal resources can meet the heating area over 3.14×107 m2, and the development potential is great.
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