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Engineering geological characteristics of the 1981 earthquakes in the eastern corinthian gulf, Greece

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dc.contributor.author Koukis, G en
dc.contributor.author Rozos, D en
dc.date.accessioned 2014-03-01T01:38:45Z
dc.date.available 2014-03-01T01:38:45Z
dc.date.issued 1985 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/22351
dc.title Engineering geological characteristics of the 1981 earthquakes in the eastern corinthian gulf, Greece en
heal.type journalArticle en
heal.identifier.primary 10.1007/BF02594770 en
heal.identifier.secondary http://dx.doi.org/10.1007/BF02594770 en
heal.publicationDate 1985 en
heal.abstract Summary  The 1981 seismic paroxysm of the Corinthian gulf was well inside the framework, of the geodynamic evolution of this graben with its successive enlargement. The serious damage, the surface rupture and the secondary effects defined a seismic area of an E-W general direction, which coincides with the main tectonic axes. The contribution of the tectonics, lithology and particular ground foundation en
dc.identifier.doi 10.1007/BF02594770 en


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