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A Late Pliocene - Quaternary pinched crustal wedge in NW central Anatolia, Turkey: A Neotectonic structure accommodating the internal deformation of the Anatolian plate

Crustal WedgeEngineeringStructural GeologyNw Central AnatoliaQuaternary Tectonic DeformationGeologyRegional TectonicsGeochronologyOrogenyNeotectonicsInternal DeformationRegional GeologyTectonics