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dc.contributor.authorPolymeris, George S.en_US
dc.contributor.authorErginal, Ahmet Evrenen_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.date.accessioned2015-01-15T23:02:05Z
dc.date.available2015-01-15T23:02:05Z
dc.date.issued2012
dc.identifier.citationPolymeris, G. S., Erginal, A. E. & Güneç Kıyak, N. (2012). A comparative morphological, compositional and TL study of tenedos (bozcaada) and Sile aeolianites, Turkey. Mediterranean Archaeology and Archaeometry, 12(2), 117-131.en_US
dc.identifier.issn1108-9628
dc.identifier.issn2241-8121
dc.identifier.urihttps://hdl.handle.net/11729/460
dc.description.abstractAeolianites are carbonate-cemented deposits of coastal dune sands, mostly of Quaternary age. Even though aeolianite exposures on the coasts of the Mediterranean Sea are frequent, very few records have been documented from the coasts of either the Aegean or the Black Sea. The present study deals with evaluating and comparing both compositions and thermoluminescence (TL) ages of two recently reported samples of coastal aeolianites. Both were recovered at the Turkish coasts of Tenedos (Bozcaada) island, Aegean Sea and Şile, Western Black Sea. In the latter case, being the first record for the specific coastal area, the oldest age obtained was dated at 158±25 ka while the youngest age yielded was 108±14 ka. These values imply that both deposition and cementation occurred during the high sea stand of marine isotope stage 5 (MIS 5). In the case of Tenedos, the aeolianites were deposited between the early stage of the oxygen isotope stage 2 period (OIS 2) and the very late phase of the oxygen isotope stage 3 period (OIS 3). These latter TL results are in excellent agreement with a previous study of the same complex after applying OSL. Besides the ages, a number of luminescent features and properties in conjunction with compositional data suggest the dissimilarity for the quartz samples extracted from the aeolianites recovered at these two sampling sites, excluding thus any transport from one sampling site to the other, despite the short distance of the two sampling sites and the meteorological data regarding the preferable wind directions between them.en_US
dc.language.isoengen_US
dc.publisherUniv Ageanen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectAeolinitesen_US
dc.subjectArchaeologyen_US
dc.subjectAustraliaen_US
dc.subjectBahamasen_US
dc.subjectCaveen_US
dc.subjectCoastal-plainen_US
dc.subjectDatingen_US
dc.subjectGeologyen_US
dc.subjectIslanden_US
dc.subjectIsraelen_US
dc.subjectKarsten_US
dc.subjectLuminescenceen_US
dc.subjectQuartzen_US
dc.subjectSea levelen_US
dc.subjectSouth-Africaen_US
dc.subjectTenedos (Bozcaada)en_US
dc.subjectTLen_US
dc.titleA comparative morphological, compositional and tl study of tenedos (Bozcaada) and Sile aeolianites, Turkeyen_US
dc.typearticleen_US
dc.description.versionPublisher's Versionen_US
dc.relation.journalMediterranean Archaeology and Archaeometryen_US
dc.contributor.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.contributor.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.contributor.authorID0000-0002-9972-429X
dc.identifier.volume12
dc.identifier.issue2
dc.identifier.startpage117
dc.identifier.endpage131
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.contributor.institutionauthorPolymeris, George S.en_US
dc.contributor.institutionauthorGüneç Kıyak, Nafiyeen_US
dc.relation.indexWOSen_US
dc.relation.indexScopusen_US
dc.relation.indexArts & Humanities Citation Index (A&HCI)en_US
dc.description.wosidWOS:000314325100009


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