ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
断裂控制型地热流体成因机制研究进展
  
关键词:fault-controlled geothermal resource  hydrochemistry  isotopes  water-rock interactions  reservoir temperature  genetic mechanism
基金项目:由深地国家科技重大专项(编号: 2024ZD1004103; 2025ZD1011107)和中国地质科学院基本科研业务费专项(编号: JKY202406; JKYZD202401; JKY202511)联合资助。
作者单位E-mail
刘凯 中国地质科学院
地质大学(北京)水资源与环境学院 
acancer@163.com 
张寿川 中国地质科学院 zhangsc@cags.ac.cn 
万力 中国地质大学(北京)水资源与环境学院 China University of Geosciences (Beijing) 
张垚垚 中国地质科学院  
史浙明 中国地质大学(北京)水资源与环境学院 China University of Geosciences (Beijing) 
贾伍慧 中国地质科学院  
闫金凯 中国地质科学院  
张秋兰 中国地质大学(北京)水资源与环境学院 China University of Geosciences (Beijing) 
王路瑶 中国地质科学院  
任天翔 中国地质科学院  
岳鑫蕊 中国地质科学院  
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摘要:
Research Progress on the Evolution Processes and Genetic Mechanism of Fault-controlled Geothermal Resource
      The characteristics of fracture-controlled geothermal resources are dominated by the channeling effect and heat-controlling role of deep-seated fault zones, involving complex deep fluid circulation and water-rock interaction processes. Research progress on the genetic mechanisms of fault-controlled geothermal fluids is reviewed based on recharge sources, circulation pathways, and geothermal reservoir characteristics of hydrothermal systems. Regarding the identification of recharge sources, the applications and limitations of isotope tracing technologies (e.g., hydrogen, oxygen, carbon, and noble gases) for identifying fluid recharge endmembers and discriminating sources are systematically reviewed. In terms of circulation pathways, hydrochemical diagrams and ion ratios are employed to investigate water-rock interactions, cation exchange, and mixing processes, thereby revealing dominant interaction processes and fluid migration patterns in fracture-controlled geothermal resources. For reservoir evaluation, the applicability of hydrochemical geothermometers, multi-mineral equilibrium approaches, the silica-enthalpy mixing model, and machine learning methods for estimating reservoir temperatures and circulation depths is compared and analyzed, clarifying error sources and correction approaches for different methods. Currently, research on the genetic mechanisms of fault-controlled geothermal fluids faces challenges such as multi-solutionality, insufficient quantitative characterization of complex water-rock interactions, and limited accuracy in estimating geothermal reservoir parameters. In the future, developing integrated multi-isotope tracing techniques, advancing multi-process coupled numerical simulation methods, and constructing interpretable machine learning models will provide key theoretical and technical support for precise characterization of the coupled “source-pathway-reservoir” evolution mechanism and the sustainable development of fracture-controlled geothermal resources.
LIU Kai,ZHANG Shouchuan,WAN Li,ZHANG Yaoyao,SHI Zheming,JIA Wuhui,YAN Jinkai,ZHANG Qiulan,WANG Luyao,REN Tianxiang,YUE Xinrui.2026.Research Progress on the Evolution Processes and Genetic Mechanism of Fault-controlled Geothermal Resource[J].Acta Geoscientica Sinica,47(1):31-48.
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