STRUCTURAL PROPERTIES OF THE NEOGENE EVAPORITE DEPOSITS IN THE SOUTH OF TUZGOLU BASIN, TURKEY

Basit Öğe Kaydı
dc.contributor.authorDelikan, Arif
dc.contributor.authorBozdag, Ayla
dc.contributor.authorKarakaya, Necati
dc.contributor.authorErcan, Hatice
dc.contributor.authorKarakaya, Muazzez Celik
dc.date.accessioned2020-03-26T19:42:42Z
dc.date.available2020-03-26T19:42:42Z
dc.date.issued2017
dc.departmentSelçuk Üniversitesien_US
dc.description3rd International Scientific Conference on Geobalcanica -- MAY 20-21, 2017 -- Skopje, MACEDONIAen_US
dc.description.abstractTuzgolu Basin located at the Central Anatolia is an inner enclosed basin and is bounded by Ankara uplift in the north, the Kirsehir massif from in the east and the Sivrihisar-Bozdag massif from the west. The Salt Lake is bordered by Tuzgolu, Aksehir and Nigde fault zones in NE-GW direction. Typical mechanical and sedimentary structures in the evaporitic sediments are observed in especially gypsum and anhydrite, partially glauberite and halite deposits. The most prominent structures observed in the investigated cores are usually sequential sedimentation or stratification, other primary structures are slump structures, sub-strata traces, mud cracks and flat conglomeratic gravel sediments. Stratification in the evaporites showed changes in the mineralogical and textural properties from the bed to the bed. There are also settlement/load structures, ripple cross lamination and cross stratification were determined. As a result of sedimentation, sedimentation-grade bedding and intercalation of clay or carbonate mud and salted mineral mud have been observed. The lacustrine sediments in the inner zones of the basin consist of Ca-Na-sulphate, Mg-sulphate sediments, claystone, carbonate alternation and partly laminated. Repeating the evaporitic sediments in mm and cm thickness provides a seasonal sedimentation view.en_US
dc.description.sponsorshipScientific and Technological Research Council of TurkeyTurkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK) [TUBITAK 114Y629]; Selcuk University Scientific Research ProjectsSelcuk University [16401034]en_US
dc.description.sponsorshipThe project was funded by The Scientific and Technological Research Council of Turkey (TUBITAK 114Y629) and the Selcuk University Scientific Research Projects (16401034) support program.en_US
dc.identifier.doi10.18509/GBP.2017.01en_US
dc.identifier.endpage8en_US
dc.identifier.startpage3en_US
dc.identifier.urihttps://dx.doi.org/10.18509/GBP.2017.01
dc.identifier.urihttps://hdl.handle.net/20.500.12395/35496
dc.identifier.wosWOS:000466905500001en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.language.isoenen_US
dc.publisherGEOBALCANICA SOCen_US
dc.relation.ispartof3RD INTERNATIONAL SCIENTIFIC CONFERENCE GEOBALCANICA 2017en_US
dc.relation.ispartofseriesInternational Scientific Conference Geobalcanica Proceedings
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectEvaporiteen_US
dc.subjecthaliteen_US
dc.subjectglauberiteen_US
dc.subjectTuzgoluen_US
dc.subjectTurkeyen_US
dc.titleSTRUCTURAL PROPERTIES OF THE NEOGENE EVAPORITE DEPOSITS IN THE SOUTH OF TUZGOLU BASIN, TURKEYen_US
dc.typeConference Objecten_US

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