Geological characteristics and analysis of hydrothermal genesis in the Suijiang-1 well in Yunnan Province, China

SHU Qin-feng; WEI Liang-shuai; LI Xiao

doi:10.19637/j.cnki.2305-7068.2019.01.005

Volume 7 Issue 1

Mar. 2019

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Article Navigation > Journal of Groundwater Science and Engineering > 2019 > 7(1): 53-60

SHU Qin-feng, WEI Liang-shuai, LI Xiao. 2019: Geological characteristics and analysis of hydrothermal genesis in the Suijiang-1 well in Yunnan Province, China. Journal of Groundwater Science and Engineering, 7(1): 53-60. doi: 10.19637/j.cnki.2305-7068.2019.01.005

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Geological characteristics and analysis of hydrothermal genesis in the Suijiang-1 well in Yunnan Province, China

doi: 10.19637/j.cnki.2305-7068.2019.01.005

1 Institude of Exploration Technology, CAGS, Chengdu 611734, China.2Chengdu University of Technology, Chengdu 610059, China.

Publish Date: 2019-03-28

Abstract

Abstract

The geothermal water hydrochemistry and isotopic characteristics of boreholes in the Suijiang-1 well in Yunnan Province were studied based on the actual drilling geology, regional geological structure and hydrogeological conditions. The analysis results show that the geothermal water is SO4-Ca?Mg type, the recharge elevation is 1 381-1 646 m, the recharge source is atmospheric precipitation, the geothermal reservoir temperature is 42-45 ℃, and the geothermal water is controlled by lithology and geological structure conditions of study area. Atmospheric precipitation enters the groundwater circulation system through the surface karst form of the Wujiaobao anticline, northwest-southeast tensile faults, fissures and karst depression, and geothermal water formed through the rising deep cycle water temperature, then blocked by the double rivers’ fault zone and drilling explosion.
- Geothermal water,
- Hydrochemistry,
- Origin analysis of hot spring

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References(16)

References

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