Geodetic investigation of the 13 May 1995 Kozani - Grevena (Greece) earthquake

Clarke, PJ; Paradissis, D; Briole, P; England, PC; Parsons, BE; Billiris, H; Veis, G; Ruegg, J-C

dc.contributor.author	Clarke, PJ	en
dc.contributor.author	Paradissis, D	en
dc.contributor.author	Briole, P	en
dc.contributor.author	England, PC	en
dc.contributor.author	Parsons, BE	en
dc.contributor.author	Billiris, H	en
dc.contributor.author	Veis, G	en
dc.contributor.author	Ruegg, J-C	en
dc.date.accessioned	2014-03-01T01:12:57Z
dc.date.available	2014-03-01T01:12:57Z
dc.date.issued	1997	en
dc.identifier.issn	0094-8276	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/12288
dc.subject	Monte Carlo Method	en
dc.subject	Sar Interferometry	en
dc.subject.classification	Geosciences, Multidisciplinary	en
dc.subject.other	Distance measurement	en
dc.subject.other	Earthquakes	en
dc.subject.other	Geodesy	en
dc.subject.other	Geologic models	en
dc.subject.other	Global positioning system	en
dc.subject.other	Monte Carlo methods	en
dc.subject.other	Tectonics	en
dc.subject.other	Hybrid simplex method	en
dc.subject.other	Triangulation networks	en
dc.subject.other	Seismology	en
dc.subject.other	focal mechanism	en
dc.subject.other	GPS	en
dc.subject.other	Kozani-Grevena earthquake 1995	en
dc.subject.other	SAR interferometry	en
dc.subject.other	Greece, Macedonia	en
dc.title	Geodetic investigation of the 13 May 1995 Kozani - Grevena (Greece) earthquake	en
heal.type	journalArticle	en
heal.identifier.primary	10.1029/97GL00430	en
heal.identifier.secondary	http://dx.doi.org/10.1029/97GL00430	en
heal.language	English	en
heal.publicationDate	1997	en
heal.abstract	The M(s) = 6.6 13 May 1995 Kozani - Grevena earthquake struck a region of low historical seismic activity which includes a 10-year-old triangulation network in northern Greece. After the earthquake, monuments from this network were occupied with GPS to measure co-seismic displacements. Inversion of the co-seismic displacement field to yield a source mechanism is achieved by use of a hybrid simplex - Monte-Carlo method which requires no a priori constraints. The model focal mechanism agrees well with the global CMT solution and locally observed aftershocks, but implies a significantly higher scalar moment than do seismological or SAR interferometry studies, and has a longer fault length than the model based on SAR interferometry.	en
heal.publisher	AMER GEOPHYSICAL UNION	en
heal.journalName	Geophysical Research Letters	en
dc.identifier.doi	10.1029/97GL00430	en
dc.identifier.isi	ISI:A1997WN97200022	en
dc.identifier.volume	24	en
dc.identifier.issue	6	en
dc.identifier.spage	707	en
dc.identifier.epage	710	en