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dc.contributor.authorBayrak Yusuf
dc.contributor.authorÖztürk, Serkan
dc.contributor.authorÇınar, Hakan
dc.contributor.authorKoravos, G. Ch.
dc.contributor.authorTsapanos, T. M.
dc.date.accessioned2014-09-11T09:32:29Z
dc.date.available2014-09-11T09:32:29Z
dc.date.issued2008
dc.identifier.urihttps://hdl.handle.net/20.500.12440/136
dc.identifier.urihttps://link.springer.com/content/pdf/10.1007/s00024-008-0359-z.pdf
dc.description.abstractComplete data set of earthquakes in Turkey and the adjacent areas has been used in order to compute the x values in 24 seismic regions of Turkey. The parameter is obtained through Gumbel’s third asymptotic distribution of extreme values and is well known as upper bound magnitude. This is an interpretation that no earthquake magnitude greater than x can occur in a region. The results also estimate the most probable magnitude for a time period of 100 years. The estimates of x exceed the value of 7.00 in 20 of the 24 seismic regions. An effort is also made to find a relation between the magnitude and the length of a fault in the complicated tectonics of Turkey and the surrounding area. Earthquake hazard revealed as tables and maps are also considered for Turkey and the surrounding area.en_US
dc.language.isoengen_US
dc.publisherPure and Applied Geophysicsen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectx-valuesen_US
dc.subjectTurkeyen_US
dc.subjectmagnitude-rupture relationshipen_US
dc.subjectearthquake hazarden_US
dc.subjectGumbel’s distribution.en_US
dc.titleRegional variation of the ? - upper bound magnitude of GIII distribution in and around Turkey: Tectonic implications for earthquake hazardsen_US
dc.typearticleen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.departmentFakülteler, Mühendislik ve Doğa Bilimleri Fakültesi, Jeofizik Mühendisliği Bölümüen_US
dc.contributor.institutionauthorÖztürk, Serkan


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