GEOTHERMAL CHARACTERISTICS OF THE LIBIXIA ANTICLINE IN CHONGQING CITY

FAN Xin-qing; SHANG Ya-jun; HU Qian-chuan

2019 Vol. 28, No. 3

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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.

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

Received Date: 15 June 2018

Revised Date: 12 September 2018

Publish Date: 30 June 2019

Abstract

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.
- Libixia anticline /
- geothermal geology /
- hot spring /
- geothermal reservoir /
- Chongqing City

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References

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