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This sedimentological and sequence-stratigraphic study focuses on the late Miocene deposits in one of the largest periMediterranean basins of southern Turkey, the Adana Basin, which formed as a Tauride foreland depression accumulating molasse deposits. The Tortonian–Messinian shallow-marine Handere Formation, previously interpreted as a regressive succession, appears to have recorded several relative sea-level changes. | Messinian forced regressions in the Adana Basin: A near-coincidence of tectonic and eustatic forcing
