ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
青藏高原柴达木盆地盐湖K、Li、B等盐类资源研究进展
  
关键词:Qaidam Basin  salt lake  salt resource  enrichment genesis  material source  mineralization mechanism  isotope
基金项目:陕西省杰出青年基金项目(编号: 2022JC-16);青海省“昆仑英才?高端创新创业人才”计划项目、青海省地质矿产勘查开发局高层次人才培养项目(编号: 2023-3-18)
作者单位E-mail
饶辉辉 中国科学院地球环境研究所, 黄土与第四纪地质国家重点实验室 18379237324@163.com 
潘彤 青海省地质矿产勘察开发局 hemy@ieecas.cn 
贺茂勇 中国科学院地球环境研究所, 黄土与第四纪地质国家重点实验室  
侯殿保 中国科学院青海盐湖研究所, 盐湖资源绿色高值利用重点实验室  
陈建洲 青海省第四地质勘查院青海省页岩气资源重点实验室  
周江迪 中国科学院地球环境研究所, 黄土与第四纪地质国家重点实验室长安大学地球科学与资源学院  
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摘要:
Progress in the Study of Potassium, Lithium, and Boron Salt Resources in Salt Lakes of the Qaidam Basin on the Qinghai-Tibet Plateau
      The Qaidam Basin is the largest plateau-type inland basin in western China. It is renowned for its rich mineral resources in salt lakes, particularly its significant reserves of potassium (K), lithium (Li), and boron (B), which are of domestic and international importance. This review explores the factors that contribute to the enrichment of these resources, which are categorized into four aspects: geological structure, climate change, chemical weathering and deposition, and water recharge. The unique “alpine deep basin” environment of Qaidam Basin was shaped by geological tectonic movement, creating the initial conditions necessary for salt deposition. Climate change, especially the onset of arid climate, further promoted the evaporation and concentration of salts. Chemical weathering provided the source of minerals for the salt lakes, and the depositional process determined where these substances were enriched in the basin. The water recharge includes surface water, groundwater, hot springs, and deep oil field water, which plays a crucial role in the enrichment of K, Li, and B salts in the lake. In addition, isotope geochemical methods have been widely applied to reveal the sources of brine, recharge sources, and mineralization processes in salt lakes, thereby providing novel insights for a comprehensive and systematic understanding of the geochemical system of salt lakes. However, some unsolved problems remain, such as the evolution of the ancient lake of Qaidam and the mineralization of K salts under the mixing of calcium-chlorine (Ca-Cl) brines. Addressing these issues is vital for advancing our understanding of the enrichment and mineralization mechanisms of strategic salt lake resources.
RAO Huihui,PAN Tong,HE Maoyong,HOU Dianbao,CHEN Jianzhou,ZHOU Jiangdi.2025.Progress in the Study of Potassium, Lithium, and Boron Salt Resources in Salt Lakes of the Qaidam Basin on the Qinghai-Tibet Plateau[J].Acta Geoscientica Sinica,46(2):376-396.
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