Huseyinca, M. YavuzAksoy, RahmiInce, Ismail2020-03-262020-03-262008978-954-91818-1-4https://hdl.handle.net/20.500.12395/225278th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection -- JUN 16-20, 2008 -- Sofia, BULGARIAThe aim of this study is to elucidate the neotectonic characteristics of the Cavuscugol graben. The Cavuscugol graben is 3-8 km wide 28 km long. It is a N-S trending actively evolving extensional structure containing infills of fluvial sediments of Pliocene-Quaternary age. The Cavuscugol graben is bounded on both sides by oblique-slip normal faults. These faults trend N-S and named as Ilgin Fault on the west and Tekeler Fault on the east. The footwall side of the faults are composed of the pre-Late Cretaceous metamorphic rocks and the Miocene-Pliocene fluviolacustrine sediments. Field studies indicated that the graben has been developed as a result of E-W extension since Upper Pliocene.eninfo:eu-repo/semantics/closedAccessCavuscugol grabenneotectonicoblique-slip normal faultsCentral AnatoliaConference Object157164N/AWOS:000275795400021N/A