Continuous strain and tilt monitoring on the Trizonia Island, Rift of Corinth, Greece [Mesures continues de déformation et d'inclinaison dans l'̂le de Trizonia (golfe de Corinthe, Grèce)]

Bernard, P; Boudin, F; Sacks, S; Linde, A; Blum, P-A; Courteille, C; Esnoult, M-F; Castarede, H; Felekis, S; Billiris, H

dc.contributor.author	Bernard, P	en
dc.contributor.author	Boudin, F	en
dc.contributor.author	Sacks, S	en
dc.contributor.author	Linde, A	en
dc.contributor.author	Blum, P-A	en
dc.contributor.author	Courteille, C	en
dc.contributor.author	Esnoult, M-F	en
dc.contributor.author	Castarede, H	en
dc.contributor.author	Felekis, S	en
dc.contributor.author	Billiris, H	en
dc.date.accessioned	2014-03-01T01:20:03Z
dc.date.available	2014-03-01T01:20:03Z
dc.date.issued	2004	en
dc.identifier.issn	1631-0713	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/15825
dc.subject	Monitoring	en
dc.subject	Rift of Corinth	en
dc.subject	Silent earthquake	en
dc.subject	Strain	en
dc.subject	Tilt	en
dc.subject	Transient	en
dc.subject.classification	Geosciences, Multidisciplinary	en
dc.subject.other	crustal deformation	en
dc.subject.other	monitoring	en
dc.subject.other	rift zone	en
dc.subject.other	seismotectonics	en
dc.subject.other	strain measurement	en
dc.subject.other	tilt	en
dc.subject.other	Central Greece	en
dc.subject.other	Eurasia	en
dc.subject.other	Europe	en
dc.subject.other	Greece	en
dc.subject.other	Phocis	en
dc.subject.other	Southern Europe	en
dc.subject.other	Troizina	en
dc.title	Continuous strain and tilt monitoring on the Trizonia Island, Rift of Corinth, Greece [Mesures continues de déformation et d'inclinaison dans l'̂le de Trizonia (golfe de Corinthe, Grèce)]	en
heal.type	journalArticle	en
heal.identifier.primary	10.1016/j.crte.2003.11.015	en
heal.identifier.secondary	http://dx.doi.org/10.1016/j.crte.2003.11.015	en
heal.language	French	en
heal.publicationDate	2004	en
heal.abstract	Tilt and strain continuous monitoring started in October 2002 in the Trizonia Island, in the Gulf of Corinth, in order to detect possible strain transients in the rift. The hydrostatic tiltmeters, developed at IPGP, are 15 m long and buried in trenches at a depth of 2.5 m, with a few 10(-9)-radian noise level at short period. The strain is measured by a Sacks-Evertson dilatometer has cemented in a borehole at a depth of 148 m, with a few 10(-10) resolution at short period. A 1 h-lasting, 10(-7)-strain transient has been recorded on the dilatometer, possibly related to a seismic swarm that occurred 15 km away. To cite this article: R Bernard et al., C. R. Geoscience 336 (2004). (C) 2004 Academie des sciences. Published by Elsevier SAS. All rights reserved.	en
heal.publisher	EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	en
heal.journalName	Comptes Rendus - Geoscience	en
dc.identifier.doi	10.1016/j.crte.2003.11.015	en
dc.identifier.isi	ISI:000221265600009	en
dc.identifier.volume	336	en
dc.identifier.issue	4-5	en
dc.identifier.spage	313	en
dc.identifier.epage	323	en