ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
四川盆地三叠系气田型深层富钾锂卤水勘探历程、进展与展望
  
关键词:Sichuan Basin  Triassic  deep brine of gas field type  genesis of brine  enrichment law
基金项目:中国地质调查局项目(编号: DD20160054);国家重点研发计划“川东北三叠纪岩相古地理研究”专题项目(编号: 2023YEC2906503-01)
作者单位E-mail
张兵 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
zhangb@cdut.edu.cn 
王绪本 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
 
郑绵平 中国地质科学院矿产资源研究所  
杨凯 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
 
张永生 中国地质科学院矿产资源研究所  
李倩 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
 
张赛民 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
 
温思宇 中国地质科学院矿产资源研究所  
林晓杨 成都理工大学地球勘探与信息技术教育部重点实验室
成都理工大学地球物理学院 
 
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摘要:
Exploration Process, Progress, and the Prospect of Deep Potassium-rich Lithium-rich Brine in Triassic Gas Field of Sichuan Basin
      The Triassic Jialingjiang and Leikoupo Formations in the Sichuan Basin are the key reservoirs of conventional natural gas. They also host brine resources rich in critical elements such as potassium and lithium. In this study, we reviewed and summarized the progress and current understanding of the exploration processes, genetic mechanisms, and enrichment patterns of deep brine in the Triassic gas fields of the Sichuan Basin while also identifying areas for future research. The concentrations of key metal elements, such as potassium and lithium, in the deep brine of the Triassic gas fields have reached industrial grade levels. With the increasing global demand for lithium resources, the initial focus on “gas potassium and exploration” gradually transitioned to a more comprehensive approach that includes “gas, potassium, and lithium comprehensive exploration”. The formation mechanisms of the Triassic deep potassium- and lithium-rich brines in the Sichuan Basin are largely similar. The evaporation and concentration of paleo-seawater under arid climatic conditions facilitated the enrichment of potassium and lithium in the brine. Subsequently, under conditions of high temperature and pressure, polyhalite/green bean rock containing potassium/lithium reacts with the buried brine, which further promotes the enrichment of potassium and lithium. Leaching is an important cause of K enrichment in brines. Deep brine is mainly stored in various dolomites and its enrichment is primarily controlled by faults, fracture development zones, and anticlines. The enrichment patterns can be summarized as “pore-fracture brine storage, fracture brine transport, and anticline brine enrichment”. Given the current status and challenges of exploring gas-field-type deep brines in the Sichuan Basin, future research should focus on the development of new integrated technologies for geophysical exploration, the optimization of resource evaluation methods and systems, exploration of new strata with high concentrations of associated elements, and the effective development and utilization of gas-field-type brines. These advancements are expected to lead to significant breakthroughs in the exploration of deep brine resources in the Sichuan Basin.
ZHANG Bing,WANG Xuben,ZHENG Mianping,YANG Kai,ZHANG Yongsheng,LI Qian,ZHANG Saimin,WEN Siyu,LIN Xiaoyang.2024.Exploration Process, Progress, and the Prospect of Deep Potassium-rich Lithium-rich Brine in Triassic Gas Field of Sichuan Basin[J].Acta Geoscientica Sinica,45(5):665-677.
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