Raised braided stream gravels on Mount Keldağ, Hatay (Eastern Mediterranean coast, Turkey): Implications of transformation to beachrock and ensuing tectonic uplift

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dc.authorid0000-0002-3112-5258
dc.authorid0000-0001-8704-4935
dc.contributor.authorErginal, Ahmet Evren
dc.contributor.authorPolymeris, Georgios S.
dc.contributor.authorKarataş, Atilla
dc.contributor.authorGiannoulatou, Valeria
dc.contributor.authorŞahiner, Eren
dc.contributor.authorMeriç, Niyazi
dc.contributor.authorErenoğlu, Oya
dc.contributor.authorSelim, Hamit Haluk
dc.contributor.authorKarabıyıkoğlu, Mustafa
dc.date.accessioned2024-10-12T19:47:14Z
dc.date.available2024-10-12T19:47:14Z
dc.date.issued2019
dc.departmentİstanbul Ticaret Üniversitesi, Mühendislik ve Tasarım Fakültesi, Mücevherat Mühendisliği Bölümüen_US
dc.description.abstractOn the seaward northwest slopes of Mount Keldağ, Hatay, the combination of an unconformably overlapping sequence of cemented gravels on a wave-cut platform, and a raised notch and irregular pits left by grazing molluscs on the walls of this notch, carved in an NE-trending high-angle fault plane, retain the record of raised braided stream gravels transformed into beachrock. From the OSL ages, this study reveals that deposition of this sequence occurred between 232.30 ± 31.62 and 214.01 ± 27.42 ka during the penultimate interglacial. The four distinct facies identified are massive matrix-supported conglomerate, massive to crudely stratified gravel, cross-stratified gravel, and clast-supported open-work gravel. Extending to the paleo-coastline during the MIS7 highstand, this sequence was cemented by carbonate and iron-oxide cements and records an uplift of around 0.1 mm/year up to the present. en_US
dc.identifier.citationErginal, A. E., Polymeris, G. S., Karataş, A., Giannoulatou, V., Şahiner, E., Meriç, N., ... & Karabıyıkoğlu, M. (2019). Raised Braided Stream Gravels on Mount Keldağ, Hatay (Eastern Mediterranean coast, Turkey): Implications of Transformation to Beachrock and Ensuing Tectonic Uplift. Mediterranean Geoscience Reviews, 1, 45-53.
dc.identifier.doi10.1007/s42990-019-00006-4
dc.identifier.endpage53en_US
dc.identifier.issn2661-863X
dc.identifier.issue1en_US
dc.identifier.scopus2-s2.0-85108615787en_US
dc.identifier.scopusqualityN/Aen_US
dc.identifier.startpage45en_US
dc.identifier.urihttps://doi.org/10.1007/s42990-019-00006-4
dc.identifier.urihttps://hdl.handle.net/11467/8845
dc.identifier.volume1en_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSpringer Science and Business Media B.V.en_US
dc.relation.ispartofMediterranean Geoscience Reviewsen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectRaised Stream Gravelsen_US
dc.subjectBeachrocken_US
dc.subjectMIS7en_US
dc.subjectPenultimate Interglacialen_US
dc.subjectMt. Keldağen_US
dc.subjectTurkeyen_US
dc.titleRaised braided stream gravels on Mount Keldağ, Hatay (Eastern Mediterranean coast, Turkey): Implications of transformation to beachrock and ensuing tectonic upliften_US
dc.typeArticleen_US

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