Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/686
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dc.contributor.authorallTsapanos, T. M.; Aristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.authorallGalanis, O. C.; Aristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.authorallKoravos, G. C.; Aristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.authorallMusson, R. M. W.; British Geological Survey,Edinburgh,U.K.en
dc.date.accessioned2006-02-14T08:19:49Zen
dc.date.available2006-02-14T08:19:49Zen
dc.date.issued2002en
dc.identifier.urihttp://hdl.handle.net/2122/686en
dc.description.abstractSeismic hazard in terms of probability of exceedance of a given intensity in a given time span,was assessed for 12 sites in Japan.The method does not use any attenuation law.Instead,the dependence of local intensity on epicentral intensity I 0 is calculated directly from the data,using a Bayesian model.According to this model (Meroni et al., 1994),local intensity follows the binomial distribution with parameters (I 0 ,p ).The parameter p is considered as a random variable following the Beta distribution.This manner of Bayesian estimates of p are assessed for various values of epicentral intensity and epicentral distance.In order to apply this model for the assessment of seismic hazard,the area under consideration is divided into seismic sources (zones)of known seismicity.The contribution of each source on the seismic hazard at every site is calculated according to the Bayesian model and the result is the combined effect of all the sources.High probabilities of exceedance were calculated for the sites that are in the central part of the country,with hazard decreasing slightly towards the north and the south parts.en
dc.format.extent1016539 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameINGVen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries5/45 (2002)en
dc.subjectBayesian estimationen
dc.subjectlocal intensityen
dc.subjectrandom variable pen
dc.subjectprobabilities of exceedanceen
dc.titleA method for Bayesian estimation of the probability of local intensity for some cities in Japanen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.description.journalTypeJCR Journalen
dc.description.fulltextopenen
dc.contributor.authorTsapanos, T. M.en
dc.contributor.authorGalanis, O. C.en
dc.contributor.authorKoravos, G. C.en
dc.contributor.authorMusson, R. M. W.en
dc.contributor.departmentAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.departmentAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.departmentAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greeceen
dc.contributor.departmentBritish Geological Survey,Edinburgh,U.K.en
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greece-
crisitem.author.deptAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greece-
crisitem.author.deptAristotle University of Thessaloniki,School of Geology,Geophysical Laboratory,Thessaloniki,Greece-
crisitem.author.deptBritish Geological Survey-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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