Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2787
AuthorsLombardi, A. M.* 
Marzocchi, W.* 
TitleEvidence of clustering and nonstationarity in the time distribution of large worldwide earthquakes
Issue Date2007
Series/Report no./ 112 (2007)
DOI10.1029/2006JB004568
URIhttp://hdl.handle.net/2122/2787
KeywordsETAS model
cluster
Subject Classification04. Solid Earth::04.06. Seismology::04.06.02. Earthquake interactions and probability 
Abstract1The purpose of this paper is to characterize the statistical distribution of worldwide largest earthquakes. We analyze the distribution of worldwide shallow events with Ms 7.0+ since 1900, by following the Occam’s razor philosophy; we start from the simplest possible model (stationary Poisson process), and we inspect more complicated models only if the data show significant departures from the simplest one. The results show two important characteristics; first, worldwide Ms 7.0+ earthquakes tend to cluster in time and space, with features similar to smaller events. Second, for some seismic regions there is evidence in favor of long-term fluctuations of the earthquake rate. These results support the hypothesis of universality, suggesting that an ETAS model with a background varying with time can be considered reliable to describe the seismicity distribution over a wide space-time-magnitude window. From a practical point of view, our findings suggest that the paradigm that seismic zones are stationary systems, implicitly assumed in seismic hazard assessment, should be regarded with caution.
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