| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4695014 | Tectonophysics | 2006 | 9 Pages |
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.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Luciano Telesca, Vincenzo Lapenna,