ISSN 1006-3021 CN11-3474/P
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鄂尔多斯盆地陕北盐盆东部盐下马四段富K、Li、Br油田水新发现
  
关键词:Ordos Basin  oil and salt exploration  lower member  fourth member of the Majiagou Formation  K-rich, Li-rich, and Br-rich oilfield water
基金项目:国家重点研发计划项目(编号: 2023YFE0104000)
作者单位E-mail
樊馥 中国地质科学院矿产资源研究所 自然资源部盐湖资源与环境重点实验室 383106448@qq.com 
马占荣 中国石油天然气股份有限公司长庆油田分公司勘探事业部 mazr_cq@petrochina.com.cn 
刘建平 中国石油天然气股份有限公司长庆油田分公司勘探事业部  
张永生 中国地质科学院矿产资源研究所 自然资源部盐湖资源与环境重点实验室  
包洪平 中国石油天然气股份有限公司长庆油田分公司勘探事业部  
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摘要:
Discovery of K-, Li-, and Br-rich Oilfield Water in the Ma4 Member under the Salt Formation in the Eastern Part of the Shanbei Salt Basin, Ordos Basin
      K and Li are key mineral resources required to ensure China’s agricultural food security and support the development of a new energy industry, allowing China to continue to maintain a high degree of foreign independence. Institute of Mineral Resources, Chinese Academy of Geological Sciences in collaboration with Changqing Oilfield Branch, Petrochina, upon “exploration of both oil and salt”, have made new discoveries of K-, Li-, and Rb-rich oilfield water in the fourth member of the lower member of the Majiagou Formation in the eastern salt basin of northern Shaanxi in the Ordos Basin, including Wells Mitan 6 and Yuyang 1. This water represents a newly discovered Li and K resource stratum in the Ordos Basin. Test results show that the KCl content of the brine in this layer is 1.798%–3.573%, and the LiCl content is 1 460.606–1 915.152 mg/L, both representing industrial grade concentrations; the contents of Rb2O and Br also reach industrial and comprehensive utilization standards. The fourth member of the Majiagou Formation is widely distributed in the basin. The discovery of K-, Li-, and Br-rich oilfield waters indicates good prospects for K and Li resources in the Ordos Basin.
FAN Fu,MA Zhanrong,LIU Jianping,ZHANG Yongsheng,BAO Hongping.2025.Discovery of K-, Li-, and Br-rich Oilfield Water in the Ma4 Member under the Salt Formation in the Eastern Part of the Shanbei Salt Basin, Ordos Basin[J].Acta Geoscientica Sinica,46(2):493-496.
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