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dc.contributor.authorEfe, Recep
dc.date.accessioned2019-10-17T11:15:38Z
dc.date.available2019-10-17T11:15:38Z
dc.date.issued2014en_US
dc.identifier.issn1877-0428
dc.identifier.urihttps://doi.org/10.1016/j.sbspro.2014.02.143
dc.identifier.urihttps://hdl.handle.net/20.500.12462/8541
dc.description.abstractDuring the 1999, the northwestern part of Turkey experienced two major earthquakes (Golcuk and Duzce) along the North Anatolian Fault Zone. The Golcuk Earthquake occurred on August 17, and caused damage in a zone extending from Duzce to Istanbul. The Duzce Earthquake struck on November 12, 1999 and caused damage in Duzce, Kaynash and Bolu. These two earthquakes caused significant changes in natural environment such as; surface rupture, cracks, landslides, offsets in the riverbeds, discharge of subsurface water from underground, liquefaction and coastal collapse. The surface rupture, which is 168 km long, extending from Kaynash to Golcuk, is the most significant. The changes after the earthquakes were identified from field measurements and assembling the existing maps at 1:25,000 and 1:100,000 scales. (C) 2013 The Authors. Published by Elsevier Ltd.en_US
dc.language.isoengen_US
dc.publisherElsevier Science Bven_US
dc.relation.isversionof10.1016/j.sbspro.2014.02.143en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectTurkeyen_US
dc.subjectGolcuk Earthquakeen_US
dc.subjectDuzce Earthquakeen_US
dc.subjectGeomorphic Effecten_US
dc.subjectSurface Ruptureen_US
dc.titleEarthquake hazard assessment in Turkey: the Mw=7.4, Golcuk (August 17, 1999) and the Mw=7.1, Duzce (November 12, 1999) earthquakesen_US
dc.typeconferenceObjecten_US
dc.relation.journal3rd International Geography Symposium, Geomed2013en_US
dc.contributor.departmentFen Edebiyat Fakültesien_US
dc.identifier.volume120en_US
dc.identifier.startpage629en_US
dc.identifier.endpage636en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US


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