Minglu Zhang, Zihao Cui, Yanjun Zhao, Nan Wang, Fojun Yao, Qiang Wang, Shengzhong Hu
{"title":"青海柴达木盆地米海矿区富钾、富锂卤水勘探方法","authors":"Minglu Zhang, Zihao Cui, Yanjun Zhao, Nan Wang, Fojun Yao, Qiang Wang, Shengzhong Hu","doi":"10.1002/gj.5215","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>The exploration and extraction of deep salt lake resources are of great significance for alleviating potassium and lithium resource shortages. However, large-scale industrial extraction has not been achieved due to technical challenges and cost constraints. This study focuses on the Mihai Mining District in Qaida Basin, Qinghai Province, investigating the exploration and development of deep confined brine enriched with potassium and lithium. The Mihai Mining Area boasts vast reserves of deep confined brine, however, they are not well-utilised because of their heterogeneity, low water yields, and extremely low mining efficiency. Previous studies have revealed that the high-yield wells in mining areas are located within fault zones. Therefore, based on the theoretical models of ‘brine circulation and potassium formation in fault zones’ and ‘storage of brine in steeply inclined water-collecting corridors’, an efficient exploration technique is proposed, which focuses on identifying active fault zones within areas with well-developed high-quality brine reservoirs as key target areas. This study employed radar remote sensing interpretation of pre- and post-seismic deformation intensity to infer fault zone development areas. Integrated with radon gas measurements, the results confirm the presence of a NE-striking active fault within the key target zone. Functioning as the sedimentary centre, this zone exhibits highly concentrated brine with co-enrichment of K<sup>+</sup> and Li<sup>+</sup> (both elements showing anomalously high concentrations), indicating high potential for K-Li-rich brine discovery. Guided by the exploration theory, verification drilling revealed brine with elevated K-Li concentrations (approximately double those in adjacent areas) and high-yield water flows in most boreholes, demonstrating significant exploration success. The distribution pattern of the discovered high-yield, water-rich areas and the exploration prediction method are of great significance for the development of deep brine in the Mihai Mining Area and have considerable potential for promotion in the Qaida Basin.</p>\n </div>","PeriodicalId":12784,"journal":{"name":"Geological Journal","volume":"60 8","pages":"1986-1997"},"PeriodicalIF":2.2000,"publicationDate":"2025-04-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Exploration Methods for Potassium-Rich and Lithium-Rich Brine in the Mihai Mining Area, Qaidam Basin, Qinghai\",\"authors\":\"Minglu Zhang, Zihao Cui, Yanjun Zhao, Nan Wang, Fojun Yao, Qiang Wang, Shengzhong Hu\",\"doi\":\"10.1002/gj.5215\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>The exploration and extraction of deep salt lake resources are of great significance for alleviating potassium and lithium resource shortages. However, large-scale industrial extraction has not been achieved due to technical challenges and cost constraints. This study focuses on the Mihai Mining District in Qaida Basin, Qinghai Province, investigating the exploration and development of deep confined brine enriched with potassium and lithium. The Mihai Mining Area boasts vast reserves of deep confined brine, however, they are not well-utilised because of their heterogeneity, low water yields, and extremely low mining efficiency. Previous studies have revealed that the high-yield wells in mining areas are located within fault zones. Therefore, based on the theoretical models of ‘brine circulation and potassium formation in fault zones’ and ‘storage of brine in steeply inclined water-collecting corridors’, an efficient exploration technique is proposed, which focuses on identifying active fault zones within areas with well-developed high-quality brine reservoirs as key target areas. This study employed radar remote sensing interpretation of pre- and post-seismic deformation intensity to infer fault zone development areas. Integrated with radon gas measurements, the results confirm the presence of a NE-striking active fault within the key target zone. Functioning as the sedimentary centre, this zone exhibits highly concentrated brine with co-enrichment of K<sup>+</sup> and Li<sup>+</sup> (both elements showing anomalously high concentrations), indicating high potential for K-Li-rich brine discovery. Guided by the exploration theory, verification drilling revealed brine with elevated K-Li concentrations (approximately double those in adjacent areas) and high-yield water flows in most boreholes, demonstrating significant exploration success. The distribution pattern of the discovered high-yield, water-rich areas and the exploration prediction method are of great significance for the development of deep brine in the Mihai Mining Area and have considerable potential for promotion in the Qaida Basin.</p>\\n </div>\",\"PeriodicalId\":12784,\"journal\":{\"name\":\"Geological Journal\",\"volume\":\"60 8\",\"pages\":\"1986-1997\"},\"PeriodicalIF\":2.2000,\"publicationDate\":\"2025-04-23\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geological Journal\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/gj.5215\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geological Journal","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/gj.5215","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Exploration Methods for Potassium-Rich and Lithium-Rich Brine in the Mihai Mining Area, Qaidam Basin, Qinghai
The exploration and extraction of deep salt lake resources are of great significance for alleviating potassium and lithium resource shortages. However, large-scale industrial extraction has not been achieved due to technical challenges and cost constraints. This study focuses on the Mihai Mining District in Qaida Basin, Qinghai Province, investigating the exploration and development of deep confined brine enriched with potassium and lithium. The Mihai Mining Area boasts vast reserves of deep confined brine, however, they are not well-utilised because of their heterogeneity, low water yields, and extremely low mining efficiency. Previous studies have revealed that the high-yield wells in mining areas are located within fault zones. Therefore, based on the theoretical models of ‘brine circulation and potassium formation in fault zones’ and ‘storage of brine in steeply inclined water-collecting corridors’, an efficient exploration technique is proposed, which focuses on identifying active fault zones within areas with well-developed high-quality brine reservoirs as key target areas. This study employed radar remote sensing interpretation of pre- and post-seismic deformation intensity to infer fault zone development areas. Integrated with radon gas measurements, the results confirm the presence of a NE-striking active fault within the key target zone. Functioning as the sedimentary centre, this zone exhibits highly concentrated brine with co-enrichment of K+ and Li+ (both elements showing anomalously high concentrations), indicating high potential for K-Li-rich brine discovery. Guided by the exploration theory, verification drilling revealed brine with elevated K-Li concentrations (approximately double those in adjacent areas) and high-yield water flows in most boreholes, demonstrating significant exploration success. The distribution pattern of the discovered high-yield, water-rich areas and the exploration prediction method are of great significance for the development of deep brine in the Mihai Mining Area and have considerable potential for promotion in the Qaida Basin.
期刊介绍:
In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited.
The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.