Hydrogeochemical characteristics and genetic model of Oiga Graben geothermal waters system in Tibet

ZHANG Xu; HAO Hongbing; LIU Kanglin; MAO Wulin; XIAO Yao; ZHANG Wen

doi:10.12029/gc20200608

GEOLOGY IN CHINA > 2020 > 47(6): 1702-1714. > DOI: 10.12029/gc20200608

ZHANG Xu, HAO Hongbing, LIU Kanglin, MAO Wulin, XIAO Yao, ZHANG Wen. Hydrogeochemical characteristics and genetic model of Oiga Graben geothermal waters system in Tibet[J]. GEOLOGY IN CHINA, 2020, 47(6): 1702-1714. DOI: 10.12029/gc20200608

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Hydrogeochemical characteristics and genetic model of Oiga Graben geothermal waters system in Tibet

1.
Chengdu Center of Hydrogeology & Engineering Geology, Sichuan Bureau of Geology & Mineral Exploration & Development, Chengdu 610081, Sichuan, China
2.
Institute of Exploration Technology, CAGS, Chengdu 611734, Sichuan, China

Funds:

the Special Geological Survey Project of China Geological Survey 121201019000161305

More Information

Author Bio:
ZHANG Xu, male, born in 1987, engineer, master, mainly engages in hydrogeology and environmental geology; E-mail:497416206@qq.com
Corresponding author:
HAO Hongbing, male, born in 1975, senior engineer, master, mainly engages in hydrogeology and environmental geology. E-mail:704863847@qq.com
Received Date: September 14, 2019
Revised Date: March 19, 2020
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

Based on the study of hot water hydrogeochemical characteristics of the Oiga Graben Geothermal Waters, the authors carried out hot water heat storage temperature and recharge elevation calculation, and established the Oiga Thermal Spring mediumhigh temperature geothermal concept model. The results show that the Oiga hot spring is of medium-alkaline water with low TDS, and the water chemical types are mainly SO₄-Na type, SO₄-Cl-Na type and HCO₃^- SO₄-Na type. The hydrogeochemical characteristics of hot water indicate that the Oiga Springs are characterized by atmospheric rainfall recharge and shallow circulation groundwater in shallow geothermal systems. The hot water is heated by deep melting body and controlled by the Oiga semiinvisible controlled thermal fracture structure. but it is partially balanced or mixed with water in the Na-K-Mg triangle diagram due to the mixing effect by fissure diving or surface cold water. The mixed model is used to estimate the temperature before the influence of hot water and cold water mixing, the temperature range of the heat storage is 120-200℃, and the cold water mixing ratio is 70%-83%.
- Oiga hot spring,
- hydrogeochemistry,
- formation mechanism,
- Cona-Oiga rift,
- Oiga Graben,
- hydrogeological survey engineering,
- Tibet

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References (65)

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Hydrogeochemical characteristics and genetic model of Oiga Graben geothermal waters system in Tibet