Landslide phenomena related to major fault tectonics: rift zone of Corinth Gulf, Greece

Koukis, G; Sabatakakis, N; Ferentinou, M; Lainas, S; Alexiadou, X; Panagopoulos, A

dc.contributor.author	Koukis, G	en
dc.contributor.author	Sabatakakis, N	en
dc.contributor.author	Ferentinou, M	en
dc.contributor.author	Lainas, S	en
dc.contributor.author	Alexiadou, X	en
dc.contributor.author	Panagopoulos, A	en
dc.date.accessioned	2014-03-01T01:57:59Z
dc.date.available	2014-03-01T01:57:59Z
dc.date.issued	2009	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/28583
dc.subject	Active Fault	en
dc.subject	Heavy Rainfall	en
dc.subject	Structural Complexity	en
dc.title	Landslide phenomena related to major fault tectonics: rift zone of Corinth Gulf, Greece	en
heal.type	journalArticle	en
heal.identifier.primary	10.1007/s10064-008-0184-8	en
heal.identifier.secondary	http://dx.doi.org/10.1007/s10064-008-0184-8	en
heal.publicationDate	2009	en
heal.abstract	Landslides in the Gulf of Corinth rift zone, Greece, are mainly in the vicinity of major active faults. The current study reports a representative landslide in this structurally controlled region which periodically moved, triggered/reactivated by heavy rainfall and earthquake activity. The composite landslide developed on structurally complex formations including sheared and weathered flysch—the most landslide-prone geological formation in Greece. The	en
heal.journalName	Bulletin of Engineering Geology and The Environment	en
dc.identifier.doi	10.1007/s10064-008-0184-8	en