DETERMINATION OF THE EPICENTRAL DISTANCE OF AN IMPENDING EARTHQUAKE FROM THE RISE TIME OF SEISMIC ELECTRIC SIGNALS

dc.contributor.author	Varotsos P.
dc.contributor.author	Sarlis N.
dc.contributor.author	Skordas E.
dc.contributor.author	Lazaridou M.
dc.date.accessioned	2022-02-28T03:34:42Z
dc.date.available	2022-02-28T03:34:42Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=17277611
dc.identifier.citation	Issledovanie Zemli iz Kosmosa, 2003, , 5, 3-6
dc.identifier.issn	0205-9614
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/35799
dc.description.abstract	An earthquake with magnitude 4.7 occurred on June 13,2003 with an epicenter almost 65 km North of Athens. This was preceded by Seismic Electric Signals recorded at a station lying approximately 30 km ESE of Athens. Beyond other parameters of the impending earthquake, its epicentral distance has been determined well in advance. This paper explains the procedure on which the latter determination was based. The essence of this procedure lies in the fact that the transmission of low frequency electric signals in a weakly conductive medium like the earth, follows diffusion type equations.
dc.title	DETERMINATION OF THE EPICENTRAL DISTANCE OF AN IMPENDING EARTHQUAKE FROM THE RISE TIME OF SEISMIC ELECTRIC SIGNALS
dc.type	Статья
dc.subject.udc	528.873

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