Beachrock formation on the coast of Gokceada Island and its relation to the active tectonics of the region, northern Aegean Sea, Turkey

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dc.authoridAVCIOGLU, MUSTAFA/0000-0002-1590-0832
dc.contributor.authorAvcioglu, Mustafa
dc.contributor.authorYiğitbaş, Erdinç
dc.contributor.authorErginal, Ahmet Evren
dc.date.accessioned2025-01-27T20:17:07Z
dc.date.available2025-01-27T20:17:07Z
dc.date.issued2016
dc.departmentÇanakkale Onsekiz Mart Üniversitesi
dc.description.abstractThere are beachrock formations in 5 different sections of the south coast of Gokceada, Turkey's largest Aegean island. These beachrocks form two different groups in terms of layering characteristics, delta O-18 and delta C-13 stable isotope compositions, consecutive cementation structures, and C-14 dating. The West Group beachrocks, to the west, were dated to 4010-5830 BP, while the East Group beachrocks were dated to 620-2390 BP. The beachrock formations in both groups are separated by the NE-SW-trending Ugurlu Fault. The Ugurlu Fault is a right lateral, strike slip with reverse component oblique fault, and is an active fault within the North Anatolian Fault Zone. In the period between the formation of the two beachrock groups (2390-4010 BP), an earthquake was responsible for the destruction of Gokceada Yenibademli mound and the development of two generations of beachrock. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
dc.description.sponsorshipResearch Fund of the Canakkale Onsekiz Mart University (COMU-BAP) [2012/008]
dc.description.sponsorshipThe findings obtained from this study comprise a portion of the doctorate of the 1st author ( M.A.) and were partially supported by supported by Research Fund of the Canakkale Onsekiz Mart University (COMU-BAP, Project Number: 2012/008). Muhammed Zeynel Ozturk and Ismail Onur Tunc are thanked for their contribution to field studies and sample preparation, and we are grateful to Mustafa Bozcu for his help with petrographic determinations.
dc.identifier.doi10.1016/j.quaint.2015.10.108
dc.identifier.endpage152
dc.identifier.issn1040-6182
dc.identifier.issn1873-4553
dc.identifier.scopus2-s2.0-84963779311
dc.identifier.scopusqualityQ1
dc.identifier.startpage141
dc.identifier.urihttps://doi.org/10.1016/j.quaint.2015.10.108
dc.identifier.urihttps://hdl.handle.net/20.500.12428/21492
dc.identifier.volume401
dc.identifier.wosWOS:000374478500012
dc.identifier.wosqualityQ2
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherPergamon-Elsevier Science Ltd
dc.relation.ispartofQuaternary International
dc.relation.publicationcategoryinfo:eu-repo/semantics/openAccess
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WoS_20250125
dc.subjectBeachrock formation
dc.subjectActive tectonics
dc.subjectC-14 dating
dc.subjectNorth Aegean Sea
dc.subjectTurkey
dc.titleBeachrock formation on the coast of Gokceada Island and its relation to the active tectonics of the region, northern Aegean Sea, Turkey
dc.typeArticle

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