NEOTECTONIC FEATURES OF THE CAVUSCUGOL GRABEN (CENTRAL ANATOLIA, TURKEY)

dc.contributor.authorHuseyinca, M. Yavuz
dc.contributor.authorAksoy, Rahmi
dc.contributor.authorInce, Ismail
dc.date.accessioned2020-03-26T17:27:18Z
dc.date.available2020-03-26T17:27:18Z
dc.date.issued2008
dc.departmentSelçuk Üniversitesien_US
dc.description8th International Scientific Conference on Modern Management of Mine Producing, Geology and Environmental Protection -- JUN 16-20, 2008 -- Sofia, BULGARIAen_US
dc.description.abstractThe 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.en_US
dc.identifier.endpage164en_US
dc.identifier.isbn978-954-91818-1-4
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage157en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22527
dc.identifier.wosWOS:000275795400021en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherINT SCIENTIFIC CONFERENCE SGEMen_US
dc.relation.ispartofSGEM 2008: 8TH INTERNATIONAL SCIENTIFIC CONFERENCE, VOL I, CONFERENCE PROCEEDINGS: MODERN MANAGEMENT OF MINE PRODUCING GEOLOGY AND ENVIRONMENTAL PROTECTIONen_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectCavuscugol grabenen_US
dc.subjectneotectonicen_US
dc.subjectoblique-slip normal faultsen_US
dc.subjectCentral Anatoliaen_US
dc.titleNEOTECTONIC FEATURES OF THE CAVUSCUGOL GRABEN (CENTRAL ANATOLIA, TURKEY)en_US
dc.typeConference Objecten_US

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