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Geology, Geochemistry, and Hydrogeology of Lithium Brines

机译:锂盐水地质,地球化学和水文地质

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Global demand for lithium has been increasing since the mid-1900s. In particular, the past few decades have shown that the demand for lithium has been elevated because it is a critical and technologically important element used extensively in the production of batteries for electric cars and portable electronic devices. Lithium is found in three main deposit types: 1) pegmatites, 2) continental brines, and 3) clays. Continental brines provide approximately three-fourths of the world's produced lithium due to the relatively low production cost, and are becoming even more important with the development of new extraction technologies. Understanding the genesis of Li-brine deposits is essential to improving exploration models for discovery of new deposits. This short paper will summarize the geology, geochemistry and hydrogeology of these systems.
机译:自190年代中期以来,全球对锂的需求已经增加。特别是,过去几十年表明,锂的需求已经提升,因为它是一种批判性和技术重要的元素,其在电动汽车和便携式电子设备的电池生产中广泛使用。锂在三种主要沉积类型中发现:1)Pegmatites,2)欧洲盐水和3)粘土。由于生产成本相对较低,欧式​​盐水提供了大约四分之三的世界生产的锂,并且随着开发新的提取技术而变得更加重要。了解李林氏矿床的起源对于改善发现新存款的勘探模型至关重要。本短文将总结这些系统的地质,地球化学和水文地质。

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