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A1.07 Ma Change from Persistent Lakes to Intermittent Flooding and Desiccationin the San Felipe Hills, Salton Trough, Southern California
Sedimentary rocks of Pliocene to Pleistocene age in the San Felipe Hills (SFH), Salton Trough, record an abrupt change from the older, perennial lake beds of the Borrego Formation to cyclic alluvial and marginal lacustrine deposits at 1.07 Ma. The ~1680-m-thick lacustrine claystone, mudstone and san
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