Magmatic origin of geothermal fluids constrained by geochemical evidence: Implications for the heat source in the northeastern Tibetan Plateau

• Published in: Journal of hydrology (Amsterdam) 2021-12, Vol.603, p.126985, Article 126985
• Main Authors: Pan, Sheng, Kong, Yanlong, Wang, Ke, Ren, Yaqian, Pang, Zhonghe, Zhang, Chao, Wen, Dongguang, Zhang, Linyou, Feng, Qingda, Zhu, Guilin, Wang, Jiyang
• Format: Article
• Language: English
• Subjects: Geothermal energy; Gonghe basin; Hydro-geochemistry; Northeastern Tibetan Plateau; Parent geothermal fluids; Partial melt zone
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2021.126985

[Display omitted] •High Cl, B, and Li concentrations are identified in the Geothermal fluids.•Geothermal fluids are found magmatic origin in northeastern Tibetan Plateau (NETP).•Parent geothermal fluid exists with temperature of 310 °C at depths of 6.8–7.8 km.•Partial melt zone exists and serves as additional heat source of Gonghe Basin.•Partial melt zone is ubiquitous in the middle to lower crust of the NETP. The northeastern Tibetan Plateau (NETP) represents the growth front of the Tibetan Plateau (TP) system. This region has long been recognized as a key in understanding the topographic response and crustal thickening of the entire TP. A heat flow anomaly (Gonghe Basin, 102 mW/m2) was found in the NETP. However, the heat-generation mechanism and the heat source of the Gonghe Basin are still debated as it is unclear whether they are related to magmatic melting activities. Herein, we provide systematic hydrogeochemical data of two types of geothermal waters (type I and II: geothermal waters sampled from within the basin and the mountainous regions, respectively) found in the region. Type I high δD (−85.0‰ to −59.0‰), δ18O (−11.1‰ to −8.0‰), Cl− (mostly range from 300 to 900 mg/L), and trace element, whereas type II has low δD (−97.1‰ to −89‰), δ18O (−13.0‰ to −11.8‰), Cl− (30 to 180 mg/L) and trace elements. Furthermore, we identified the existence of a high-temperature parent geothermal fluid based on the chloride – enthalpy model, it was estimated to possess a temperature of 310 °C and a circulation depth of 6.8–7.8 km. The parent geothermal fluid originated from snowmelt water, which later mixed with a magmatic fluid. The helium (He) ratios of geothermal gas ranged from 0.01 Ra to 0.18 Ra and indicated that the source of He was primarily from a crustal source. In addition to the heat flow analysis and magnetotelluric (MT) data, we suggested that the magmatic nature of the geothermal fluid is caused by a partial melt zone, which is ubiquitous in the middle to lower crust and serves as the heat source in the NETP. Finally, a conceptual model was built to illustrate the occurrence of magmatic fluid and its genesis. The findings will help to improve the understanding of the uplift of the TP and reveals the important role of deep groundwater circulation in the formation of high-temperature geothermal resources.