GEOLOGY AND MINERALOGY OF THE DOGANHISAR CLAY BEDS (CENTRAL ANATOLIA, TURKEY)

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dc.contributor.authorAksoy, Rahmi
dc.contributor.authorInce, Ismail
dc.contributor.authorBozdag, Ali
dc.contributor.authorHuseyinca, M. Yavuz
dc.date.accessioned2020-03-26T17:26:58Z
dc.date.available2020-03-26T17:26:58Z
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 geology and the mineralogy of the clay beds (Doganhisar clays) located southeast of Doganhisar (central Anatolia, Turkey) were studied, Rock units found in and adjacent to the Doganhisar clay beds include metamorphic rocks of pre-Triassic age of the Sultandaglari Massif, the Miocene Ayaslar Formation and the Pliocene Doganhisar Formation as well as alluvium The Lower (?)-Middle Cambrian-Lower Ordovician Caltepe Formation forming the base of the metamorphic rocks is composed of recrystallized limestone and dolomite. The upper Cambrian-Lower Ordovician Sultandede Formation conformably overlies the Caltepe Formation. The Middle-Upper Devonian Engilli Formation unconformably overlies the Sultandede Formation and consists predominantly of metaquartzite. It is conformably overlain by the Lower-Middle Carboniferous Kirazli Formation. It is vertically and laterally graded upward in to the Lower-Middle Carboniferous Harlak Formation. Neogene cover units consist of alluvial fan and lacustrine deposits. Metamorphic rocks have undergone regional metamorphism under low grade metamorphic condition and three phases of deformation during the Alpine orogeny. X-ray diffraction (XRD) and chemical analysis were used to study the clay mineralogy. Illite and kaolinite, with lesser amount of chlorite dominate the mineral composition.en_US
dc.identifier.endpage90en_US
dc.identifier.isbn978-954-91818-1-4
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage83en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/22430
dc.identifier.wosWOS:000275795400012en_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.subjectSultandaglari Massifen_US
dc.subjectdeformationen_US
dc.subjectDoganhisar claysen_US
dc.subjectilliteen_US
dc.subjectkaoliniteen_US
dc.subjectTurkeyen_US
dc.titleGEOLOGY AND MINERALOGY OF THE DOGANHISAR CLAY BEDS (CENTRAL ANATOLIA, TURKEY)en_US
dc.typeConference Objecten_US

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