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At the southern end of the Salton Sea district, Cerro Prieto, Mexico contains equally hot, but much more dilute brine with a lithium content of 5– 100 ppm. Pilot plant solar ponds have been operated that concentrated the brine to about 400 ppm Li after a potash recovery process, but no attempt was made to recover the lithium (Garrett, 1996; Vine, 1980; Berthold and Baker, 1976). The origin of the Salton Sea geothermal brine is believed to be meteoric water (based upon dD and d18O values) from the nearby Chocolate Mountains flowing through fault lines deep into the earth, where it is heated by hot rocks or magma.
194 — — — — Geology 1; an average of 40 Salar de Uyuni samples, 2; a more detailed individual sample analysis, 3; an average of the eight highest-lithium samples, found in a narrow band in the southern half of the eastern lobe of the salar, 4 is an average of four Salar de Empexa or Coipasa samples. 2, p. 198, q 1998 by permission of Elsevier. a This salar is slightly southwest of Uyuni, in Bolivia. There is also a Pastos Grandes in Argentina. 3. c Adjacent to Uyuni. d All analyses as ppm. 18 Summary of stratigraphic units in Searles Lake evaporite sequence (Smith, 1979).
2002b,c). Other laboratory studies have been conducted on the leaching or adsorption of lithium from rocks obtained by the Nankai Trough drilling program. Some of the rock’s lithium began to be leached at a temperature of 1508C with considerable isotopic fractionation, and the leaching was nearly completely at temperatures over 3008C. At higher temperatures there was considerable albitization of calcic plagioclase (You and Gieskes, 2001). Various studies have also been made on the lithium Geology 45 isotopic distribution of unaltered island arc lavas and Mid Ocean Ridge basalt.