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Nummulitic facies of the Crimean-Caucasian Region
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The nummulitic limestones of Crimea and the southwestern Caucasus, often interpreted as “nummulite banks”, formed carbonate platforms throughout most of the Ypresian–Lutetian. Such deposits were accumulated in shallow warm-water basins of Crimea and the Caucasus, which differed from each other by the structure of the basement and the hydrodynamic regime.
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