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2018 Vol. 45, No. 6
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Article navigation > Geology in China > 2018 > 45(6): 1087-1102
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ZHANG Senqi, YAN Weide, LI Dunpeng, JIA Xiaofeng, ZHANG Shengsheng, LI Shengtao, FU Lei, WU Haidong, ZENG Zhaofa, LI Zhiwei, MU Jianqiang, CHENG Zhengpu, HU Lisha. 2018. Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province[J]. Geology in China, 45(6): 1087-1102. doi: 10.12029/gc20180601
Citation: ZHANG Senqi, YAN Weide, LI Dunpeng, JIA Xiaofeng, ZHANG Shengsheng, LI Shengtao, FU Lei, WU Haidong, ZENG Zhaofa, LI Zhiwei, MU Jianqiang, CHENG Zhengpu, HU Lisha. 2018. Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province[J]. Geology in China, 45(6): 1087-1102. doi: 10.12029/gc20180601
shu

Characteristics of geothermal geology of the Qiabuqia HDR in Gonghe Basin, Qinghai Province

  • 1.

    Center for Hydrogeology and Environmental Geology Survey, China Geological Survey, Baoding 071051, Hebei, China

  • 2.

    Department of Land and Resources of Qinghai, Xining 810002, Qinghai, China

  • 3.

    School of Zijin Mine, Fuzhou University, Fuzhou 350116, Fujian, China

  • 4.

    Institute of Hydrogeology, Engineering Geology and Environmental Geology Survey of Qinghai, Xining 810008, Qinghai, China

  • 5.

    School of Resources and Environment, Jilin University, Changchun 130026, Jilin, China

  • 6.

    State Key Lab of Geodesy and Geodynamics, Chinese Academy of Sciences, Wuhan 350116, Hubei, China

  • 7.

    Geophysical Exploration Institute of China Metallurgical Geology Bureau, Baoding 071000, Hebei, China

    • Fund Project: Supported by China Geological Survey Program (No. DD20160192, DD20179033, DD20179621)
More Information
  • Author Bio: ZHANG Senqi, male, born in 1962, master, professor, mainly engages in the study of geothermal geology, hydrogeology, and environmental geology survey and research; E-mail: senqizhang@126.com
  • Corresponding author: FU Lei, male, born in 1986, master, engineer, majors in the study of geothermal geology, hydrogeology, and environmental geology survey and research; E-mail:pengyou0808@163.com 
Received Date:  28 March 2018
Revised Date:  10 June 2018
Publish Date:  25 December 2018
    Abstract

  • Based on regional geology, geothermal geology and integrated geophysical exploration results, the GR1 hot dry rock exploration well was completed in the central part of Qiabuqia Town in the Gonghe basin. The GR1 well is the highest temperature hot-dry rock exploration well in China, which has laid an important foundation for China's first EGS demonstration project. The temperature measurement results show that the temperature at the depth of 2500 m is 150℃, entering into the hot dry rock section. The temperature of the bottom hole at the depth of 3705 m is 236℃. The average geothermal gradient of 2500-3705 m is 71.4℃/km, which is higher than that of the other 3 hot dry rock exploration wells. At 2800-3705 m of GR1 well the geothermal gradient is higher than 80℃/km. The exploration results show that the depth of the hot dry rock is 2104.31-2500 m, which is oval-shaped in the east-west direction, with an area of 246.90 km2. The evaluation results show that the total theoretical resources of the Qiabuqia hot dry rock is 1638.16EJ in the depth of 3-5 km, equivalent to 55.909 billion tons of standard coal.

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