MEASURING MULTIFRACTALITY IN SEISMIC SEQUENCES

dc.contributor.author	Telesca L.
dc.contributor.author	Lapenna V.
dc.date.accessioned	2025-04-19T06:19:39Z
dc.date.available	2025-04-19T06:19:39Z
dc.date.issued	2006
dc.identifier	https://elibrary.ru/item.asp?id=14731472
dc.identifier.citation	Tectonophysics, 2006, 423, 1-4, 115-123
dc.identifier.issn	0040-1951
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/48978
dc.description.abstract	We investigated the multifractal structure of the interevent times between successive earthquakes that occurred in Umbria-Marche, which is one of the most seismically active areas of central Italy. We used the Multifractal Detrended Fluctuation Analysis (MF-DFA), which permits detection of multifractality in nonstationary series. Analyzing the time evolution of the multifractal behaviour of the seismic sequence, a loss of multifractality during the aftershocks is revealed. © 2006 Elsevier B.V. All rights reserved.
dc.subject	EARTHQUAKES
dc.subject	MULTIFRACTAL DETRENDED FLUCTUATION ANALYSIS
dc.title	MEASURING MULTIFRACTALITY IN SEISMIC SEQUENCES
dc.type	Статья
dc.identifier.doi	10.1016/j.tecto.2006.03.023

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