2020
DOI: 10.1016/j.physa.2019.123655
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Earthquake clusters identification through a Markovian Arrival Process (MAP): Application in Corinth Gulf (Greece)

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Cited by 7 publications
(3 citation statements)
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“…Our results are consistent with what was found in these studies (e.g. (Michas et al, 2021), (Bountzis et al, 2020), (Papadimitriou et al, 2022): each step observed in our cumulative curves are indeed identified after the start of each crisis (Figure 10). We also compare our results to seismic clusters described in (Mesimeri et al, 2019) which contain a total of 1560 crisis events.…”
Section: Cumulative Curvessupporting
confidence: 94%
“…Our results are consistent with what was found in these studies (e.g. (Michas et al, 2021), (Bountzis et al, 2020), (Papadimitriou et al, 2022): each step observed in our cumulative curves are indeed identified after the start of each crisis (Figure 10). We also compare our results to seismic clusters described in (Mesimeri et al, 2019) which contain a total of 1560 crisis events.…”
Section: Cumulative Curvessupporting
confidence: 94%
“…Our main assumption is that each state corresponds to a distinct evolution phase of a seismic sequence, independently of its underlying mechanism. In this way, the model has the ability to approximate the temporal evolution of earthquake catalogs that incorporate both aftershock sequences and earthquake swarms [31], as well as datasets with non-stationary characteristics [34].…”
Section: Map As a Tool For The Detection Of Seismicity Rate Changesmentioning
confidence: 99%
“…The temporal distribution of the events is approximated essentially by a non-homogeneous Poisson process, N t , with a piece-wise constant intensity rate determined by the underlying Markov process, J t . Simulation studies and applications on real datasets showed that the model efficiently identifies the changes in the earthquake occurrence rates [31]. Recent works by Lu [32] and Benali et al [33] are based on non-stationary Poisson models whose rate is modulated by a hidden Markov process to determine a set of change-points for seismicity rate.…”
Section: Introductionmentioning
confidence: 99%