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dc.contributor.authorALTINOK, Yıldız
dc.contributor.authorAlpar, Başak Işıl
dc.contributor.authorYALTIRAK, CENK
dc.date.accessioned2021-03-05T11:48:21Z
dc.date.available2021-03-05T11:48:21Z
dc.identifier.citationALTINOK Y., Alpar B. I. , YALTIRAK C., "Tsunami of Sarkoy-Mujrefte 1912 earthquake: Western Marmara, Turkey", NATO Advanced Research Workshop on Underwater Ground Failures on Tsunami Generation, Modeling, Risk and Mitigation, İstanbul, Türkiye, 23 - 26 Mayıs 2001, cilt.21, ss.33-42
dc.identifier.othervv_1032021
dc.identifier.otherav_aa08c31b-3232-4bb8-9fbe-02074c0ad2d4
dc.identifier.urihttp://hdl.handle.net/20.500.12627/113538
dc.description.abstractOne of the largest earthquakes in the Balkans is the 09.08.1912 (01:29:00 UTH) Sarkoy-Murefte Earthquake which occurred on the active Ganos fault zone (Ms=7.4). The eastern termination of the associated faulting is in the Marmara Sea. On the basis of archiving and library studies, geological field surveys and offshore investigations, the 1912 earthquake produced a tsunami. The mechanism of this co-seismic tsunami may be assigned to an underwater failure along the southern slopes of the Tekirdag Trough rather than a seabed dislocation.
dc.language.isoeng
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectJEOLOJİ
dc.subjectJeofizik Mühendisliği
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectJEOKİMYA VE JEOFİZİK
dc.titleTsunami of Sarkoy-Mujrefte 1912 earthquake: Western Marmara, Turkey
dc.typeBildiri
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume21
dc.contributor.firstauthorID5264


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