Characterizations of geothermal springs along the Moxi deep fault in the western Sichuan plateau, China

• Published in: Physics of the earth and planetary interiors 2017-02, Vol.263, p.12-22
• Main Authors: Qi, Jihong, Xu, Mo, An, Chengjiao, Wu, Mingliang, Zhang, Yunhui, Li, Xiao, Zhang, Qiang, Lu, Guoping
• Format: Article
• Language: English
• Subjects: Aqueous chemistry; Daily variation; Deep fault; Geothermal water; Solid tide
• ISSN: 0031-9201; 1872-7395
• DOI: 10.1016/j.pepi.2017.01.001

•The studied geothermal springs occur in a typical deep fault region where the Tibet Plateau subducts beneath the Yangtze craton.•Cyclical variation of flows with solid tides is used to study the geothermal water.•The study shows that the geothermal waters have deep heat sources, with heat flow being the most intensified and centered around Laoyulin in Kangding. Abundant geothermal springs occur along the Moxi fault located in western Sichuan Province (the eastern edge of the Qinghai-Tibet plateau), highlighted by geothermal water outflow with an unusually high temperature of 218°C at 21.5MPa from a 2010-m borehole in Laoyulin, Kangding. Earthquake activity occurs relatively more frequently in the region and is considered to be related to the strong hydrothermal activity. Geothermal waters hosted by a deep fault may provide evidence regarding the deep underground; their aqueous chemistry and isotopic information can indicate the mechanism of thermal springs. Cyclical variations of geothermal water outflows are thought to work under the effect of solid earth tides and can contribute to understanding conditions and processes in underground geo-environments. This paper studies the origin and variations of the geothermal spring group controlled by the Moxi fault and discusses conditions in the deep ground. Flow variation monitoring of a series of parameters was performed to study the geothermal responses to solid tides. Geothermal reservoir temperatures are evaluated with Na-K-Mg data. The abundant sulfite content, dissolved oxygen (DO) and oxidation-reduction potential (ORP) data are discussed to study the oxidation-reduction states. Strontium isotopes are used to trace the water source. The results demonstrate that geothermal water could flow quickly through the Moxi fault the depth of the geothermal reservoir influences the thermal reservoir temperature, where supercritical hot water is mixed with circulating groundwater and can reach 380°C. To the southward along the fault, the circulation of geothermal waters becomes shallower, and the waters may have reacted with metamorphic rock to some extent. Our results provide a conceptual deep heat source model for geothermal flow and the reservoir characteristics of the Moxi fault and indicate that the faulting may well connect the deep heat source to shallower depths. The approach of hot spring variation research also has potential benefits for earthquake monitoring and prediction.