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

Koukis, G; Rozos, D

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