Depth-dependent Time-clustering Behaviour in Seismicity of Southern California

Details Depth-dependent Time-clustering Behaviour in Seismicity of Southern California Depth-dependent Time-clustering Behaviour in Seismicity of Southern California

Nov 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001georl..28.4323t&link_type=abstract

Geophysical Research Letters, Volume 28, Issue 22, p. 4323-4326

Physics

Geophysics

15

Mathematical Geophysics: Nonlinear Dynamics, Seismology: Earthquake Parameters

Scientific paper

Temporal fluctuations in seismicity of southern California have been investigated by means of two methods, the Allan Factor Analysis and the Detrended Fluctuation Analysis, which are used to detect the scaling behaviour of an nonstationary observational time series. Performing the time-clustering analysis varying the depth of the events, we found that the seismicity of the area reveals a tendency toward Poissonian behaviour near the depth ranges 14-16 km.

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