USGS Deposit Model for Lithium Brines

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USGS Deposit Model for Lithium Brines ( usgs-deposit-model-lithium-brines )

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Examples of Li-Brine Systems and Their Tectonic Settings All closed-basin lithium-brine deposits that are of present economic interest are of Quaternary age. Basins that contain lithium-enriched brines have a number of different tectonic origins (fig. 2). Quantities of Li in million metric tons (Mt) in the following discussion are from Kesler and others (2012). Clayton Valley, Nevada, (0.2 Mt of Li) is located within the Basin and Range extensional province of the western United States; in detail, it is hosted in an extensional half-graben system between a young metamorphic core complex and its breakaway zone (Oldow and others, 2009). The Salar de Atacama (6.3 Mt of Li) and Salar de Uyuni (10.2 Mt of Li) are located on the Altiplano of Chile and Bolivia, a high, internally drained plateau along the crest of the Andean convergent-margin orogen that includes a number of closed basins; the basin of the Salar de Atacama itself is a contractional intrarc basin. The Salton Sea, California, is a strike-slip basin located at a releasing bend along an intracontinental segment of the San Andreas transform fault. Zabuye Lake (1.5 Mt of Li) is one of a family of closed basins in the Tibetan plateau on the upper plate of the Himalayan-Tibetan collisional orogen; in detail, it is a Neogene graben at high angles to the structural grain of the orogen. Curiously, and due partly to extreme aridity, most of these example deposits are in globally exceptional tectonic settings: the Basin and Range is the world’s widest extensional province, the Altiplano is the highest sector of a continental-margin arc, and Tibet is the largest and highest syncollisional plateau. Figure 2. (A) World map of lithium brine deposits (red dots). (B) Detail in South America. (C) Histogram showing the bimodal latitudinal distribution of Li brine deposits in northern and southern arid belts. 3

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