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Geochemical Characteristics of Hot Spring Fluids in Eryuan Region and Their Relationship with Seismic Activity
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Can YOU1, 2, Zihan TAI1, 2, Qilin LI1, 2, *, Xiaoping HAI1, 2, Xiang ZHANG1, 2, Hua RAN1, 2, Jiankun CHEN1, 2
Journal of Geodesy and Geodynamics | 2026, 46(5) : 530 - 540
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Journal of Geodesy and Geodynamics | 2026, 46(5): 530-540
Geochemical Characteristics of Hot Spring Fluids in Eryuan Region and Their Relationship with Seismic Activity
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Can YOU1, 2, Zihan TAI1, 2, Qilin LI1, 2, *, Xiaoping HAI1, 2, Xiang ZHANG1, 2, Hua RAN1, 2, Jiankun CHEN1, 2
Affiliations
  • 1 Yunnan Earthquake Agency, Kunming 650224, China
  • 2 Kunming Institute of Earthquake Prediction, CEA, Kunming 650201, China
Published: 2026-05-15 doi: 10.14075/j.jgg.2025.07.255
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We analyze the geochemical characteristics of five hot spring fluids in Eryuan and its surrounding areas, and explore the relationship among geothermal distribution, mantle-derived fluid degassing, hydrochemical anomalies, and seismic activity. The results show that hydrochemical type of hot springs in the study area include HCO3·SO4-Na·Ca, HCO3·SO4-Na, HCO3·Cl-Na, SO4-Ca·Na, and SO4·Cl-Na·Ca. The main sources of hot spring gases are atmospheric saturated water and air, with contributions from volatile components in the crust and mantle. The heat storage temperatures of hot springs in the study area ranges from 164 to 275 ℃, and circulation depths is from 6 369.78 to 11 143.98 meters. The content of He is from 12.90 to 821.62 ppm. Large-scale deep faults in Eryuan area provide favorable channels for the upward migration of deep-sourced fluids, and the deep-sourced fluids are the direct sources of geothermal energy and He. There is a correlation between the geochemical characteristics of hot spring fluids and seismic activities, which is characterized by the deeper the circulation depth, the higher the geothermal reservoir temperature, and the stronger the seismic activity. Moreover, most of the M≥4 earthquakes are located in the transition zone between high and low geothermal reservoir temperatures. The Cl- and SO42- concentrations of Wenmiao hot spring show abnormal increases before and after earthquakes, mainly due to the contribution of the mixing of deep-sourced fluids and different aquifers. The temperature at spring outlet shows an abnormal decrease, which may be related to the fact that multiple fractures provide heat dissipation channels after the earthquake. The hydrochemical values of hot springs were restored after the earthquake, indicating that the deep-sourced fluid activity in Eryuan area weakened.

Eryuan area  /  hot spring  /  fluid geochemistry  /  hydrochemical characteristics anomalies  /  earthquake
游灿, 台梓含, 李其林, 海潇平, 张翔, 冉华, 陈建坤. 洱源地区温泉流体地球化学特征及与地震活动的关系. 大地测量与地球动力学, 2026 , 46 (5) : 530 -540 . DOI: 10.14075/j.jgg.2025.07.255
Can YOU, Zihan TAI, Qilin LI, Xiaoping HAI, Xiang ZHANG, Hua RAN, Jiankun CHEN. Geochemical Characteristics of Hot Spring Fluids in Eryuan Region and Their Relationship with Seismic Activity[J]. Journal of Geodesy and Geodynamics, 2026 , 46 (5) : 530 -540 . DOI: 10.14075/j.jgg.2025.07.255
Year 2026 volume 46 Issue 5
35
13
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doi: 10.14075/j.jgg.2025.07.255
  • Receive Date:2025-07-18
  • Online Date:2026-10-29
  • Published:2026-05-15
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  • Received:2025-07-18
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    1 Yunnan Earthquake Agency, Kunming 650224, China
    2 Kunming Institute of Earthquake Prediction, CEA, Kunming 650201, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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