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FAN Xin-qing, SHANG Ya-jun, HU Qian-chuan. GEOTHERMAL CHARACTERISTICS OF THE LIBIXIA ANTICLINE IN CHONGQING CITY[J]. Geology and Resources, 2019, 28(3): 305-308.
Citation: FAN Xin-qing, SHANG Ya-jun, HU Qian-chuan. GEOTHERMAL CHARACTERISTICS OF THE LIBIXIA ANTICLINE IN CHONGQING CITY[J]. Geology and Resources, 2019, 28(3): 305-308.
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GEOTHERMAL CHARACTERISTICS OF THE LIBIXIA ANTICLINE IN CHONGQING CITY

  • No. 208 Team of Hydrogeology and Engineering Geology, Chongqing Bureau of Geology and Mineral Exploration, Chongqing 400700, China

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  • Received Date: June 14, 2018
  • Revised Date: September 11, 2018
  • Available Online: December 28, 2022
  • Published Date: June 29, 2019
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    • Abstract

  • With experiential summary and literature research, through systematic study on the exploration data of hot springs and geothermal wells in Libixia geothermal reservoir structure, it is found that the Libixia anticline has the characteristics of typical layered thermal reservoir structure. The geothermal water is dominated by calcium sulfate type, with the presently lowest water temperature drilled in Huaying Mountain anticlinorium. The currently known geothermal wells and hot springs are generally lower than 37℃ in water temperature, with obvious attenuation in water amount. It is suggested that the low geothermal water temperature be related to the structure.

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    • References (2)
  • [1]
    张润甲.重庆喀斯特槽谷土地利用模式的探讨[D].重庆: 西南大学, 2009. http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y1461185
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    李东升, 刘东升.重庆地热水资源热储构造与径流补给[J].河海大学学报:自然科学版, 2011, 39(4):19-23. http://d.old.wanfangdata.com.cn/Periodical/hhdxxb201104004
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