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.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.date.accessioned2025-01-27T18:53:18Z
dc.date.available2025-01-27T18:53:18Z
dc.date.issued2019
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
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. © 2019, Springer Nature Switzerland AG.
dc.identifier.doi10.1007/s42990-019-00006-4
dc.identifier.endpage53
dc.identifier.issn2661-863X
dc.identifier.issue1
dc.identifier.scopus2-s2.0-85108615787
dc.identifier.scopusqualityQ2
dc.identifier.startpage45
dc.identifier.urihttps://doi.org/10.1007/s42990-019-00006-4
dc.identifier.urihttps://hdl.handle.net/20.500.12428/12668
dc.identifier.volume1
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer Science and Business Media B.V.
dc.relation.ispartofMediterranean Geoscience Reviews
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_Scopus_20250125
dc.subjectBeachrock; MIS7; Mt. Keldağ; Penultimate interglacial; Raised stream gravels; Turkey
dc.titleRaised braided stream gravels on Mount Keldağ, Hatay (Eastern Mediterranean coast, Turkey): implications of transformation to beachrock and ensuing tectonic uplift
dc.typeArticle

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