Depositional environment characteristics of UlukA +/- AYla Evaporites, Central Anatolia, Turkey

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dc.contributor.authorKeskin, Şeref
dc.contributor.authorŞener, Mehmet
dc.contributor.authorŞener, Mehmet Furkan
dc.contributor.authorÖztürk, Muhammed Zeynel
dc.date.accessioned2020-05-01T09:11:17Z
dc.date.available2020-05-01T09:11:17Z
dc.date.issued2017
dc.departmentDÜ, Mühendislik Fakültesi, Çevre Mühendisliği Bölümüen_US
dc.descriptionOzturk, Muhammed Zeynel/0000-0002-9834-7680en_US
dc.descriptionWOS: 000400272000010en_US
dc.description.abstractThis paper examines evaporated deposits of gypsum known as the UlukA +/- AYla Evaporites located in the UlukA +/- AYla Basin, central Anatolia, Turkey. The Late Eocene compression between the Eurasian and Afro-Arabian plates formed numerous shallow epicontinental basins in SE central Anatolia. During this period, the UlukA +/- AYla Basin was a shallow marine environment. The composition of the UlukA +/- AYla Basin indicates that gypsum and stromatolite were deposited due to an arid climate and sea level oscillation between 37.25 and 38.52 Ma. Oxygen, sulfur, and strontium isotopes and the geochemistry of the evaporated rocks were measured to understand the paleoenvironment of this formation. Trace element analyses of Fe, K, Mg, Na, Mn, Sr, Ni, and Cu from the gypsum samples showed very high variability. The average K/Na, Sr/Ca, and Mg/Na were measured to be 0.4, 2.35, and 2.9 %, respectively, which indicates that the UlukA +/- AYla gypsum lies in a formerly hypersaline environment. Sr-87/Sr-86, O-18, and S-34 isotope ratios indicate that the gypsum was deposited in marine water then mixed with fresh continental water.en_US
dc.description.sponsorshipNigde University Research Found (NUAF) [FEB 2008/22]en_US
dc.description.sponsorshipFinancial support for this study by Nigde University Research Found (NUAF) (Project No: FEB 2008/22) is gratefully acknowledged.en_US
dc.identifier.doi10.1007/s13146-016-0292-7en_US
dc.identifier.endpage241en_US
dc.identifier.issn0891-2556
dc.identifier.issn1878-5212
dc.identifier.issue2en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage231en_US
dc.identifier.urihttps://doi.org/10.1007/s13146-016-0292-7
dc.identifier.urihttps://hdl.handle.net/20.500.12684/5475
dc.identifier.volume32en_US
dc.identifier.wosWOS:000400272000010en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringeren_US
dc.relation.ispartofCarbonates And Evaporitesen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectCentral Anatoliaen_US
dc.subjectUlukisen_US
dc.subjectla basinen_US
dc.subjectSedimentologyen_US
dc.subjectGeochemistryen_US
dc.subjectIsotopeen_US
dc.subjectEvaporatesen_US
dc.titleDepositional environment characteristics of UlukA +/- AYla Evaporites, Central Anatolia, Turkeyen_US
dc.typeArticleen_US

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