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Deposition of the Palaeogene to early Neogene calcareous and siliceous deep-water sediments of the Lefkara Formation in Cyprus was successively dominated by pelagic, turbidity current, a return to pelagic and then bottom-current processes. Sedimentation occurred on the distal parts of a carbonate slope-apron to basin plain setting located in the western arm of the Tethys Ocean. The early phase of...