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    郑绵平, 邢恩袁, 张雪飞, 黎明明, 车东, 卜令忠, 韩佳欢, 叶传永. 全球锂矿床的分类、外生锂矿成矿作用与提取技术[J]. 中国地质, 2023, 50(6): 1599-1620. DOI: 10.12029/gc20231025002
    引用本文: 郑绵平, 邢恩袁, 张雪飞, 黎明明, 车东, 卜令忠, 韩佳欢, 叶传永. 全球锂矿床的分类、外生锂矿成矿作用与提取技术[J]. 中国地质, 2023, 50(6): 1599-1620. DOI: 10.12029/gc20231025002
    ZHENG Mianping, XING Enyuan, ZHANG Xuefei, LI Mingming, CHE Dong, BU Lingzhong, HAN Jiahuan, YE Chuanyong. Classification and mineralization of global lithium deposits and lithium extraction technologies for exogenetic lithium deposits[J]. GEOLOGY IN CHINA, 2023, 50(6): 1599-1620. DOI: 10.12029/gc20231025002
    Citation: ZHENG Mianping, XING Enyuan, ZHANG Xuefei, LI Mingming, CHE Dong, BU Lingzhong, HAN Jiahuan, YE Chuanyong. Classification and mineralization of global lithium deposits and lithium extraction technologies for exogenetic lithium deposits[J]. GEOLOGY IN CHINA, 2023, 50(6): 1599-1620. DOI: 10.12029/gc20231025002

    全球锂矿床的分类、外生锂矿成矿作用与提取技术

    Classification and mineralization of global lithium deposits and lithium extraction technologies for exogenetic lithium deposits

    • 摘要:
      研究目的 为明确锂矿的找矿方向与勘查部署重点工作,矿床类型的合理划分非常重要。
      研究方法 本文按照锂资源赋存性质,对其详加厘定和划分,尝试把锂矿床(资源)按内、外生成因进行划分。
      研究结果 将全球锂矿床按照内外生成因划分为10种类型和5个亚类。
      结论 国外已查明新生代外生锂矿床的形成与分布主要受控于板块碰撞带,主要物质来源与深部洋壳重熔岩浆有关,形成时代主要在中新世和古近纪后期;具有偏酸性的岩浆专属性,盐湖型、地热型、火山沉积型锂矿与含锂凝灰岩和热水密切相关,且锂盐湖具有趋低性迁聚,超常富集机制,但对晚古生代黏土亚型和深部卤水物质来源,有待进一步查明;由于锂矿床(资源)类型多,成因复杂,它们是在多圈层相互作用形成的,建议要用构造地球化学、古大气环流和盐类学相结合研究的路线,开展外生锂矿床(资源)成矿作用研究。

       

      Abstract:
      This paper is the result of mineral exploration engineering.
      Objective A reasonable classification of deposits holds great significance for identifying prospecting targets and deploying exploration. The world's keen demand for lithium resources has expedited the discovery of numerous novel lithium resources.
      Methods Given the presence of varied classification criteria for lithium resources presently, this study further ascertained and classified the lithium resources according to their occurrence modes.
      Results The global lithium deposits are divided into 10 types and 5 subtypes of lithium deposits (resources) based on endogenetic and exogenetic factors.
      Conclusion As indicated by surveys of Cenozoic exogenetic lithium deposits in China and abroad, the formation and distribution of the deposits are primarily determined by plate collision zones, their primary material sources are linked to the anatectic magmas in the deep oceanic crust, and they were formed primarily during the Miocene and Late Paleogene. The researchers ascertained that these deposits, especially those of the salt lake, geothermal, and volcanic deposit types are closely related to lithium tuff and geothermal water, which have magmatic exclusivity of acidic nature, and the salt lake deposit types tend to migrate and accumulate toward low-lying areas, and display supernormal enrichment. However, the material sources of lithium deposits (resources) of the Neopaleozoic clay subtype and the deep brine type are yet to be further identified. Given the various types and complex origins of lithium deposits (resources), which were formed due to the interactions of multiple spheres, it is recommended that the mineralization of exogenetic lithium deposits (resources) be investigated by integrating tectono-geochemistry, paleoatmospheric circulation, and salinology. So far, industrialized lithium extraction is primarily achieved in lithium deposits of the salt lake, clay, and hard rock types. The lithium extraction employs different processes, with lithium extraction from salt lake-type lithium deposits proving the most energy-saving and cost-effective.

       

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