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The Bor-Ulukışla Basin situated in the south-eastern part of the Tuz Gölü Basin, Central Anatolia, provide prominent example of lacu strine basins and varying assemblages of evaporite and detrital minerals. The evaporatic sedimentation formed in the central part of the basin as a shallow, saline lake syst em, where abundant ha lite and Ca-Na sulfate deposits. Sodium sulfates and also halite depos its have been explo ited from the recent salt-playa lakes in the basin. The evaporite s were deposited by related t...