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The Sambhar playa in Rajasthan, India, located at the eastern fringe of the Thar Desert, records multiple phases of clastic- and evaporite-dominated deposition as revealed from a ∼23 m deep core drilled in the center of the playa. Seven evaporite facies, identified from the mineralogical data, reflect variable brine chemistry throughout the history of the playa. The complete absence of gypsum-rich...
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