Analyses of seismic deformation at the Kibyra Roman stadium, southwest Turkey

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dc.authorid0000-0003-2581-7984
dc.authorid0000-0002-1926-6410
dc.authorid0000-0002-3522-2987
dc.authorid0000-0003-0470-303X
dc.authorid0000-0001-9485-2017
dc.contributor.authorKarabacak, Volkanen_US
dc.contributor.authorYönlü, Önderen_US
dc.contributor.authorDökü, Feyzullah Erayen_US
dc.contributor.authorGüneç Kıyak, Nafiyeen_US
dc.contributor.authorAltunel, Erhanen_US
dc.contributor.authorÖzüdoǧru, Şükrüen_US
dc.contributor.authorYalçıner, Cahit Çağlaren_US
dc.contributor.authorAkyüz, Hüsnü Serdaren_US
dc.date.accessioned2015-01-15T23:02:16Z
dc.date.available2015-01-15T23:02:16Z
dc.date.issued2013-11
dc.departmentIşık Üniversitesi, Fen Edebiyat Fakültesi, Fizik Bölümüen_US
dc.departmentIşık University, Faculty of Arts and Sciences, Department of Physicsen_US
dc.description.abstractThe ancient city of Kibyra in southwest Turkey has the potential to reveal the location and date of historical earthquakes. The most compelling evidence for earthquake faulting is observed in the city's Roman stadium. Damage related to seismic shaking is characterized by systematically collapsed columns, dilated and collapsed walls, and by rotated and displaced blocks in the stadium. Detailed archaeoseismological observations suggest that Kibyra was affected by earthquakes that were also recorded in historical earthquake catalogs. Although there is no historical record of a large earthquake after the 5th century A.D., Optically stimulated luminescence (OSL) dating of deposits under the collapsed blocks suggests a later seismic event. OSL results indicate that another large event occurred in southwest Turkey, probably around the 10-11th century A.D., and caused extensive damage (I-o = VIII-IX) to the Kibyra stadium.en_US
dc.description.versionPublisher's Versionen_US
dc.identifier.citationKarabacak, V., Yönlü, Ö., Dökü, E., Güneç Kıyak, N., Altunel, E., Özüdoğru, Ş., Yalçıner, C. Ç. & Akyüz, H. S. (2013). Analyses of seismic deformation at the kibyra roman stadium, southwest Turkey. Geoarchaeology, 28(6), 531-543. doi:10.1002/gea.21456en_US
dc.identifier.doi10.1002/gea.21456
dc.identifier.endpage543
dc.identifier.issn0883-6353
dc.identifier.issn1520-6548
dc.identifier.issue6
dc.identifier.scopus2-s2.0-84885083070
dc.identifier.scopusqualityQ1
dc.identifier.startpage531
dc.identifier.urihttps://hdl.handle.net/11729/474
dc.identifier.urihttp://dx.doi.org/10.1002/gea.21456
dc.identifier.volume28
dc.identifier.wosWOS:000325256600002
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.indekslendigikaynakScience Citation Index Expanded (SCI-EXPANDED)en_US
dc.indekslendigikaynakArts & Humanities Citation Index (A&HCI)en_US
dc.institutionauthorGüneç Kıyak, Nafiyeen_US
dc.language.isoenen_US
dc.peerreviewedYesen_US
dc.publicationstatusPublisheden_US
dc.publisherWiley-Blackwellen_US
dc.relation.ispartofGeoarchaeologyen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectStimulated luminescenceen_US
dc.subjectArchaeological relicsen_US
dc.subjectDead-seaen_US
dc.subjectSitesen_US
dc.subjectEarthquakesen_US
dc.subjectSedimentsen_US
dc.subjectGreeceen_US
dc.subjectBasinen_US
dc.subjectFaulten_US
dc.titleAnalyses of seismic deformation at the Kibyra Roman stadium, southwest Turkeyen_US
dc.typeArticleen_US
dspace.entity.typePublication

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