MEASURING MULTIFRACTALITY IN SEISMIC SEQUENCES

dc.contributor.authorTelesca L.
dc.contributor.authorLapenna V.
dc.date.accessioned2025-04-19T06:19:39Z
dc.date.available2025-04-19T06:19:39Z
dc.date.issued2006
dc.description.abstractWe 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.identifierhttps://elibrary.ru/item.asp?id=14731472
dc.identifier.citationTectonophysics, 2006, 423, 1-4, 115-123
dc.identifier.doi10.1016/j.tecto.2006.03.023
dc.identifier.issn0040-1951
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48978
dc.subjectEARTHQUAKES
dc.subjectMULTIFRACTAL DETRENDED FLUCTUATION ANALYSIS
dc.titleMEASURING MULTIFRACTALITY IN SEISMIC SEQUENCES
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Tele_06.pdf
Размер:
355.41 KB
Формат:
Adobe Portable Document Format

Коллекции