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Geoscience ›› 2022, Vol. 36 ›› Issue (02): 484-493.DOI: 10.19657/j.geoscience.1000-8527.2021

• Water Resources and Environmental Research • Previous Articles     Next Articles

Geothermal Hydrogeochemical Characteristics and Genetic Analysis of the Seda-Songpan Fault Block

HU Zexiang1(), ZHAO Xueqin1, LI Song1, LI Junya2, WANG Yujue2, YANG Luo1   

  1. 1. School of Environment and Resources,Southwest University of Science and Technology, Mianyang, Sichuan 621010, China
    2. 405 Geological Brigade of Sichuan Bureau of Geology & Mineral Resources, Chengdu, Sichuan 611830, China
  • Received:2020-05-09 Revised:2021-10-29 Online:2022-04-10 Published:2022-06-01

Abstract:

To determine the geothermal resource occurrence and source in the Sedar-Songpan fault block, three hot springs(namely Reshuitang, Shangdagu and Kalonggou) in Heishui County of Sichuan Province were taken sampled, and analyzed for their water chemistry and isotopes, and the recharge source and heat storage temperature of geothermal water were discussed. The results show that the groundwater chemistry types of the Heishui hot springs are HCO3-Ca or HCO3-Na, and the replenishing water came mainly from atmospheric precipitation. The replenishment elevation of the Reshuitang, Shangdagu and Kalonggou is 5,121 m, 3,890 m and 3,921 m, respectively. Considering mineral saturation, SiO2 geothermometer was used to calculate the hot spring thermal storage temperature, yielding 119.036 ℃, 49.034 ℃ and 30.215 ℃, respectively. Based on the genetic analysis of the local geothermal water, we concluded that the underground hot water was formed by: the infiltration of meteoric water into the reservoir through the alpine recharge area, which absorbed heat from deep underground conducts and interacted with the wallrocks, forming the underground hot water. In the better developed parts of faults, cracks and joints, the hot water ascended along fault zones, and finally emerged as hot spring on the surface.

Key words: Seda-Songpan block, hot springs, hydrochemistry, isotope, geothermal reservoir

CLC Number: