Transient electric variations associated with large intermediate-depth earthquakes in South Aegean

dc.contributor.author	Νομικός, Κωνσταντίνος Δ.	el
dc.contributor.author	Βαλλιανάτος, Φίλιππος	el
dc.date.accessioned	2015-06-12T09:28:42Z
dc.date.available	2015-06-12T09:28:42Z
dc.date.issued	2015-06-12
dc.identifier.uri	http://hdl.handle.net/11400/15795
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.sciencedirect.com/science/article/pii/S0040195196001576#	el
dc.subject	Greece
dc.subject	Preseismic electric variations
dc.subject	Προσεισμικές ηλεκτρικές παραλλαγές
dc.subject	Ελλάδα
dc.title	Transient electric variations associated with large intermediate-depth earthquakes in South Aegean	en
heal.type	journalArticle
heal.classification	Physics
heal.classification	Environmental technology
heal.classification	Φυσική
heal.classification	Περιβαλλοντική τεχνολογία
heal.classificationURI	http://skos.um.es/unescothes/C02994
heal.classificationURI	http://zbw.eu/stw/descriptor/15774-3
heal.classificationURI	N/A-Φυσική
heal.classificationURI	N/A-Περιβαλλοντική τεχνολογία
heal.keywordURI	http://zbw.eu/stw/descriptor/17184-0
heal.identifier.secondary	doi:10.1016/S0040-1951(96)00157-6
heal.language	en
heal.access	campus
heal.publicationDate	1997-01
heal.bibliographicCitation	Nomikos, K. and Vallianatos, F. (1997). Transient electric variations associated with large intermediate-depth earthquakes in South Aegean. "Tectonophysics", 269(1-2), January 1997. pp. 171-177. Available from: http://www.sciencedirect.com/science/article/pii/S0040195196001576#. [Accessed 05/06/1998]	en
heal.abstract	A telluric station was installed on Crete in the South Aegean in order to investigate the existence of transient electric variations before large near intermediate-depth earthquakes. During the experiment, two transient electric variations (not correlated with geomagnetic variations) were recorded and associated with two time isolated intermediate-depth earthquakes with local magnitude ML 5.8 and 4.8, respectively. Finally a qualitative discussion on the form of the electric signal, based on the charge dislocation model, is presented.	en
heal.journalName	Tectonophysics	en
heal.journalType	peer-reviewed
heal.fullTextAvailability	true