Temporal patterns in southern Aegean seismicity revealed by the multiresolution wavelet analysis

dc.contributor.author	Telesca, Luciano	it
dc.contributor.author	Χλούπης, Γεώργιος Π.	el
dc.contributor.author	Νικολήνταγα, Μαρία-Ειρήνη	el
dc.contributor.author	Βαλλιανάτος, Φίλιππος	el
dc.date.accessioned	2015-06-07T13:10:44Z
dc.date.available	2015-06-07T13:10:44Z
dc.date.issued	2015-06-07
dc.identifier.uri	http://hdl.handle.net/11400/15465
dc.rights	Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/3.0/us/	*
dc.source	http://www.elsevier.com/	en
dc.subject	Earthquakes
dc.subject	Wavelet
dc.subject	Multiresolution analysis
dc.subject	σεισμοί
dc.subject	κυμάτιο
dc.subject	ανάλυση πολλαπλών αναλύσεων
dc.title	Temporal patterns in southern Aegean seismicity revealed by the multiresolution wavelet analysis	en
heal.type	journalArticle
heal.classification	Technology
heal.classification	Environmental technology
heal.classification	Τεχνολογία
heal.classification	Περιβαλλοντική τεχνολογία
heal.classificationURI	http://id.loc.gov/authorities/subjects/sh85133147
heal.classificationURI	http://lod.nal.usda.gov/5857
heal.classificationURI	N/A-Τεχνολογία
heal.classificationURI	N/A-Περιβαλλοντική τεχνολογία
heal.identifier.secondary	DOI: 10.1016/j.cnsns.2005.12.005
heal.language	en
heal.access	campus
heal.publicationDate	2007-12
heal.bibliographicCitation	TELESCA, L., HLOUPIS, G.P., NIKOLINTAGA, M.-I. & VALLIANATOS F. (2007). Temporal patterns in southern Aegean seismicity revealed by the multiresolution wavelet analysis. Communications in Nonlinear Science and Numerical Simulation. [online] 12 (8). p. 1418-1426. Available from: http://www.elsevier.com/[Accessed 07/03/2006]	en
heal.abstract	We applied multiresolution wavelet analysis to the sequence of times between earthquakes occurred between 1970 and 2003 in the southern Aegean area, one of the most seismically active area in the Mediterranean. We observed a twofold features in the wavelet-coefficient standard deviation σwav: (i) at low scales it decreases in correspondence with the occurrence of the strongest earthquake, mainly due to the aftershock activation mechanism; (ii) at high scales it is characterized by oscillating behaviour, which is a typical background seismicity.	en
heal.publisher	Elsevier	en
heal.journalName	Communications in Nonlinear Science and Numerical Simulation	en
heal.journalType	peer-reviewed
heal.fullTextAvailability	true