“…Sources of dissolved selenium in ground and surface water in the San Joaquin Valley were hypothesized to be sulfides in shale (the Moreno Formation of Cretaceous age) of the Coast Range of California (Presser and others, 1990) and sediments of the west-central San Joaquin Valley derived from Coast Range rocks (Deverel and others, 1984;Gilliom, 1989;Izbicki, 1989). Studies by Deverel and Millard (1988) and by Fujii and Deverel (1989) concluded that high concentrations of selenium in ground and surface water were a result of evaporative concentration of ground water, which was indicated by isotopic enrichment of oxygen and hydrogen stable isotopes and by correlation of elevated selenium concentrations with ground-water salinity. The hydrogeochemical processes involved in the immobilization of selenium from the aqueous phase has been the focus of several studies (Dubrovsky and others, 1990;Masscheleyn and others, 1991;Sposito and others, 1991;White and others, 1991).…”