http://www.cnr.it/ontology/cnr/individuo/prodotto/ID206271
Investigating the time-scaling behavior of the 2004-2010 seismicity of Aswan area (Egypt) by means of the Allan factor statistics and the detrended fluctuation analysis (Articolo in rivista)
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- Investigating the time-scaling behavior of the 2004-2010 seismicity of Aswan area (Egypt) by means of the Allan factor statistics and the detrended fluctuation analysis (Articolo in rivista) (literal)
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- 2012-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.5194/nhess-12-1267-2012 (literal)
- Alternative label
Telesca L., Lovallo M., Amin Mohamed AE-E., Elgabry M., El-Hady S., Abou Elenean KM., Elshafey Fat Elbary R. (2012)
Investigating the time-scaling behavior of the 2004-2010 seismicity of Aswan area (Egypt) by means of the Allan factor statistics and the detrended fluctuation analysis
in Natural hazards and earth system sciences (Print); Copernicus Gesellschaft MBH, Gottingen (Germania)
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- Telesca L., Lovallo M., Amin Mohamed AE-E., Elgabry M., El-Hady S., Abou Elenean KM., Elshafey Fat Elbary R. (literal)
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- CNR-IMAA, Consiglio Nazionale Delle Ricerche, Istituto di Metodologie per l'Analisi Ambientale, C.da S.Loja, 85050 Tito (PZ), Italy.
Agenzia Regionale per la Protezione dell'Ambiente di Basilicata, 85100 Potenza, Italy.
National Research Institute of Astronomy and Geophysics NRIAG, 11421 Helwan, Cairo, Egypt.
Aswan Seismological Research Institute, Egypt. (literal)
- Titolo
- Investigating the time-scaling behavior of the 2004-2010 seismicity of Aswan area (Egypt) by means of the Allan factor statistics and the detrended fluctuation analysis (literal)
- Abstract
- The time dynamics of seismicity of Aswan area (Egypt) from 2004 to 2010 was investigated by means of the (i) Allan Factor, which is a powerful tool allowing the capture of time-clusterized properties of temporal point processes; and the (ii) detrended fluctuation analysis, which is capable of detecting scaling in nonstationary time series. The analysis was performed varying the depth and the magnitude thresholds. The 2004-2010 Aswan seismicity is characterized by significant three-fold time-clustering behaviors with scaling exponents ~0.77 for timescales between 10 4.16 s and 10 5.14 s, ~0.34 for timescales between 10 5.14 s and 10 6.53 s, and ~1 for higher timescales. The seismic interevent times and distances are characterized by persistent temporal fluctuations for most of the magnitude and depth thresholds. (literal)
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