< p >添加Sabre牙齿的总结:< / p > < p >除了风化长英质的火山岩作为圣描述,另一个方面,多年来一直受到关注直接输入工资(或河岸)温泉来源。这个想法是,锂在岩浆,不仅仅是大气水。毫无疑问,温泉通常与锂卤水——但由于因果关系还不是结论性的,会有一个潜在的混杂变量。< / p > < p > Daisuke Araoka最近发表的一篇论文(2013),特别是一样覆盖在内华达州的霍夫斯特拉(2013),发现同位素证据源长英质的火山岩风化的温泉。所以辩论并不是结束。李有一些异常高水平的金银脉矿化毗邻克莱顿山谷。我不确定如何适合——Ag-Au矿化是有点老,但仍能与更大的故事。我不知道乌尤尼地区以及阿根廷发工资,但是我不认为那里的温泉模式已经被太多的虽然我做头发偶尔提到在阿根廷。< / p > < p >一个好的地球化学讨论提供了来源在安第斯山脉Risacher (2003)。他的工作也在开发勘探技术中的应用。的研究(即资金),进入斑岩矿床成因和勘探方法小矮人的数量进入锂卤水。 And much of the work that has been done has been by a few companies that have had no motivation to publish their work in the way that the academic groups researching porphyries have. Consequently there is still work to be done in this area. Risacher's paper, and others by him on the same subject are readable and interesting examples of applied geochemistry in genetic models and potential exploration methods. Araoka, D., Kawahata, H., Takagi, T., Watanabe, Y., Nishimura, K., Nishio, Y., 2013, Lithium and strontium isotopic systematics in playas in Nevada, USA: constraints on the origin of lithium, Mineralium Deposita, v, 49, is. 3, pp 371-379
Risacher, F., Alonso, H., Salazar, C., 2003, The origin of brines and salts in Chilean salars—A hydrochemical review: Earth-Science Reviews, v. 63, nos. 3–4, p. 249–293.