Sedimentological characteristics of Quaternary Aydincik tufa (Mersin-Turkiye)

Basit Öğe Kaydı
dc.contributor.authorOrhan, Hukmu
dc.contributor.authorKalan, Fethiye
dc.date.accessioned2020-03-26T19:07:00Z
dc.date.available2020-03-26T19:07:00Z
dc.date.issued2015
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractThe Aydincik tufa crops out in an area of approximately 1 km(2) along the Mediterranean coast of AydA +/- ncA +/- k town (Mersin-Turkey) located at the southern flank of the central Taurus mountain belt comprising clastics and carbonates ranging from Late Proterozoic to middle Eocene and several NE-SW aligned faults. It comprises seven texturally different facies: phytoherm framestone facies, phytoherm boundstone facies, micritic tufa facies, crossbedded carbonate sandstone facies, carbonate-coated conglomerate facies, pebbly carbonate sandstone facies, and tufa breccias facies. Of these, the phytoherm framestone facies and the phytoherm boundstone facies were deposited at the peripheral part of lake, whereas the micritic tufa facies toward the lake depocenter. Tufa breccias facies and crossbedded carbonate sandstone facies were resulted from erosion and redeposition of fragments from previously formed units such as phytoherm framestone and boundstone by fluvial activities developed within the environment. The tufa samples are composed of low-Mg calcite, and the terrigenous material in all tufa facies is generally very low. C and O isotop data show that the deposition of the AydA +/- ncA +/- k tufa took place under cold water condition. The sedimentological and mineralogical characteristics of the facies points that the AydA +/- ncA +/- k tufa was deposited in a fluvio-lacustrine environment in which the terrigen input was very low and was feeded by water from springs developed along the faults close to the Aydincik tufa.en_US
dc.description.sponsorshipSelcuk University Research FundSelcuk University [SU-BAP-08201009]en_US
dc.description.sponsorshipWe are grateful to the Selcuk University Research Fund for their support (Project No: SU-BAP-08201009) for the financial support. Special thanks go to Prof. Dr. Levent ZOROGLU from Department of Archeology, Selcuk University for introducing us the Aydincik Tufa and for his logistic support in the field studies. This article is produced from Master Thesis of Fethiye (KOSE) KALAN supervised by Hukmu ORHAN.en_US
dc.identifier.doi10.1007/s13146-015-0244-7en_US
dc.identifier.endpage459en_US
dc.identifier.issn0891-2556en_US
dc.identifier.issn1878-5212en_US
dc.identifier.issue4en_US
dc.identifier.scopusqualityQ3en_US
dc.identifier.startpage451en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s13146-015-0244-7
dc.identifier.urihttps://hdl.handle.net/20.500.12395/32530
dc.identifier.volume30en_US
dc.identifier.wosWOS:000365094000007en_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.selcuk20240510_oaigen_US
dc.subjectAydinciken_US
dc.subjectTufaen_US
dc.subjectQuaternaryen_US
dc.subjectPhytoherm framestone faciesen_US
dc.subjectPhytoherm boundstone faciesen_US
dc.subjectMicritic tufa faciesen_US
dc.titleSedimentological characteristics of Quaternary Aydincik tufa (Mersin-Turkiye)en_US
dc.typeArticleen_US

Dosyalar

Koleksiyon

WoS İndeksli Yayınlar Koleksiyonu
Scopus İndeksli Yayınlar Koleksiyonu