Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/861
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dc.contributor.authorallTsapanos, T. M.; Aristotle University of Thessaloniki, School of Geology, Geophysical Laboratory, Thessaloniki, Greeceen
dc.contributor.authorallMäntyniemi, P.; Institute of Seismology, University of Helsinki, Finlanden
dc.contributor.authorallKijko, A.; Council for Geoscience, Pretoria, South Africaen
dc.date.accessioned2006-02-22T10:20:46Zen
dc.date.available2006-02-22T10:20:46Zen
dc.date.issued2004en
dc.identifier.urihttp://hdl.handle.net/2122/861en
dc.description.abstractA probabilistic approach was applied to map the seismic hazard in Greece and the surrounding region. The procedure does not require any specification of seismic sources or/and seismic zones and allows for the use of the whole seismological record, comprising both historical and instrumental data, available for the region of interest. The new seismic hazard map prepared for Greece and its vicinity specifies a 10% probability of exceedance of the given Peak Ground Acceleration (PGA) values for shallow seismicity and intermediate soil conditions for an exposure time of 50 years. When preparing the map, the new PGA attenuation relation given by Margaris et al. (2001) was employed. The new map shows a spatial distribution of the seismic hazard that corresponds well with the features of shallow seismicity within the examined region. It depicts the level of seismic hazard in which the exceedance of the PGA value of 0.25 g may be expected to occur within limited areas. The highest estimated levels of seismic hazard inside the territory of Greece are found in the Northern Sporades Islands, where PGA values in excess of 0.50 g are reached at individual sites, and in the Zante Island in Western Greece, where PGA values in the range of 0.35 g to 0.40 g are obtained at more numerous localities. High values are also observed in the sea between the Karpathos and Rhodes islands, near the Island of Amorgos (Cyclades Archipelago) and in the Southwestern Peloponnesus. The levels of seismic hazard at the sites of seven Greek cities (Athens, Jannena, Kalamata, Kozani, Larisa, Rhodes and Thessaloniki) were also estimated in terms of probabilities that a given PGA value will be exceeded at least once during a time interval of 1, 50 and 100 years at those sites. These probabilities were based on the maximum horizontal PGA values obtained by applying the design earthquake procedure, and the respective median values obtained were 0.24 g for Athens, 0.28 g for Jannena, 0.30 g for Kalamata, 0.21 g for Kozani, 0.24 g for Larisa, 0.43 g for Rhodes and 0.35 g for Thessaloniki. The probabilities of exceedance of the estimated maximum possible PGA value were also calculated for the cities to illustrate the uncertainty of maximum PGA assessment.en
dc.format.extent2793454 bytesen
dc.format.mimetypeapplication/pdfen
dc.language.isoEnglishen
dc.publisher.nameINGVen
dc.relation.ispartofAnnals of Geophysicsen
dc.relation.ispartofseries6/47 (2004)en
dc.subjectseismicity of Greeceen
dc.subjectprobabilistic seismicen
dc.subjecthazarden
dc.subjectpeak ground accelerationen
dc.subjectdesign earthquake procedureen
dc.titleA probabilistic seismic hazard assessment for Greece and the surrounding region including site-specific considerationsen
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.authorMäntyniemi, P.en
dc.contributor.authorKijko, A.en
dc.contributor.departmentAristotle University of Thessaloniki, School of Geology, Geophysical Laboratory, Thessaloniki, Greeceen
dc.contributor.departmentInstitute of Seismology, University of Helsinki, Finlanden
dc.contributor.departmentCouncil for Geoscience, Pretoria, South Africaen
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.deptInstitute of Seismology, University of Helsinki, Finland-
crisitem.author.deptCouncil for Geoscience, Pretoria, South Africa-
crisitem.classification.parent04. Solid Earth-
Appears in Collections:Annals of Geophysics
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