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Geotechncial aspects of the 1995 Aegion, Greece, earthquake

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dc.contributor.author Bouckovalas, GD en
dc.contributor.author Gazetas, G en
dc.contributor.author Papadimitriou, AG en
dc.date.accessioned 2014-03-01T02:48:45Z
dc.date.available 2014-03-01T02:48:45Z
dc.date.issued 1999 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/34082
dc.relation.uri http://www.scopus.com/inward/record.url?eid=2-s2.0-0033508505&partnerID=40&md5=5d192c9e93efc26afde617902dfe21a6 en
dc.subject.other earthquake damage en
dc.subject.other earthquake mechanism en
dc.subject.other earthquake rupture en
dc.subject.other failure mechanism en
dc.subject.other geotechnical property en
dc.subject.other seismicity en
dc.subject.other structural response en
dc.subject.other Greece en
dc.subject.other Mediterranean Sea en
dc.title Geotechncial aspects of the 1995 Aegion, Greece, earthquake en
heal.type conferenceItem en
heal.publicationDate 1999 en
heal.abstract Results are presented from multidisciplinary studies regarding the M(S)=6.2, 15 June, 1995 Aegion Earthquake (Gulf of Corinth, Greece). From a seismological point of view this event deserves attention since it is the first well documented earthquake resulting from low angle (33°) normal faulting. From a geotechnical point of view, attention is focused upon the high acceleration (0.54g), long period (0.40-50s) ground motion recorded in the city of Aegion, which is attributed to the coincidence of a number of independent factors: directivity of rupture, soil amplification and topography effects. In addition, the analysis of structural damage within the city of Aegion and ground failures along both coasts of the Gulf provides new insight to earthquake-induced failure mechanisms. en
heal.publisher A.A.Balkema en
heal.journalName Earthquake geotechnical engineering. Proceedings of the 2nd international conference on earthquake geotechnical engineering, Lisbon, June 1999. (3 vols.). en
dc.identifier.spage 739 en
dc.identifier.epage 748 en


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