Sedimentology and geochemistry of the middle Miocene playa lake evaporites in the Gurun Basin (S of Sivas), Central Anatolia, Turkey

Basit Öğe Kaydı
dc.authorwosidTekin, Erdogan/AAH-9614-2020
dc.contributor.authorOnal, Mehmet
dc.contributor.authorHelvaci, Cahit
dc.contributor.authorTekin, Erdogan
dc.contributor.authorAyyildiz, Turhan
dc.date.accessioned2024-08-04T20:30:53Z
dc.date.available2024-08-04T20:30:53Z
dc.date.issued2008
dc.departmentİnönü Üniversitesien_US
dc.description.abstractThe Gurun basin is a half graben filled by alluvial, fluvial and playa-lake deposits of the Gurun Formation accumulated under the N-S direction extensional tectonic regime and volcanic rocks. The Gurun Formation is divided into four members such as the Kavak, Gokpinar, Cayboyu and Terzioglu members, and the Cayboyu Member has two different evaporitic occurrences such as selenitic and satin spar. During the first phase of evaporite deposition, selenitic gypsum crystals in 5 to 15 cm thick layer within the dolomitic mudstones were formed. The second evaporitic phase consists of four different levels of cavity filling within the sandstones and shale alternation at the upper part of sequence originated as 5 to 10 cm sized satin-spar gypsum crystals with white colored, partly orientated, fibrous-radial shaped. XRF major, minor and some rare elements analyses (La, Ce, Ta, W and U) and low Sr-87/Sr-86 (parts per thousand) and delta S-34 (CDT) values indicate that meteoric and volcanic solution occasionally mixed with the lake water. In addition, low delta O-18 (SMOW) values in the continental evaporate could be interpreted as mixing of fresh water with the playa lake environment. Selenitic gypsum in the Cayboyu Member of the Gurun Formation was precipitated from ground water-brine water rich in humic acid during periodic desiccations of in the shore-lake plain.en_US
dc.identifier.doi10.1007/BF03176248
dc.identifier.endpage20en_US
dc.identifier.issn0891-2556
dc.identifier.issn1878-5212
dc.identifier.issue1en_US
dc.identifier.scopus2-s2.0-46949090162en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage11en_US
dc.identifier.urihttps://doi.org/10.1007/BF03176248
dc.identifier.urihttps://hdl.handle.net/11616/94589
dc.identifier.volume23en_US
dc.identifier.wosWOS:000256935900002en_US
dc.identifier.wosqualityQ4en_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.subjectevaporiteen_US
dc.subjectgeochemistryen_US
dc.subjectsedimentologyen_US
dc.subjectisotopeen_US
dc.subjectGurun Basinen_US
dc.subjectCentral Anatoliaen_US
dc.titleSedimentology and geochemistry of the middle Miocene playa lake evaporites in the Gurun Basin (S of Sivas), Central Anatolia, Turkeyen_US
dc.typeArticleen_US

Dosyalar

Koleksiyon

WoS İndeksli Yayınlar Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu