2020
DOI: 10.1007/s00477-020-01798-w
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Modelling background seismicity components identified by nearest neighbour and stochastic declustering approaches: the case of Northeastern Italy

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Cited by 13 publications
(7 citation statements)
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“…The obtained results highlight non-stationarity of seismic activity, at a time-scale of several years and up to decades, in agreement with earlier findings by Benali et al (2020), an element that should be taken into account for improving local seismic hazard assessment. The regions and time intervals identified in this study, which display homogeneous features of seismic activity, may supply valuable information toward timedependent seismic hazard assessment (e.g., Kossobokov et al, 2015 and references therein), while providing new constraints for earthquakes forecasting in Northeastern Italy.…”
Section: Discussionsupporting
confidence: 90%
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“…The obtained results highlight non-stationarity of seismic activity, at a time-scale of several years and up to decades, in agreement with earlier findings by Benali et al (2020), an element that should be taken into account for improving local seismic hazard assessment. The regions and time intervals identified in this study, which display homogeneous features of seismic activity, may supply valuable information toward timedependent seismic hazard assessment (e.g., Kossobokov et al, 2015 and references therein), while providing new constraints for earthquakes forecasting in Northeastern Italy.…”
Section: Discussionsupporting
confidence: 90%
“…Although the temporal pattern of activity rate changes identified in this study reflects trends at the sub-regions scale, this result appears compatible with the observation of a period of rather low background seismicity rate (i.e. for the declustered catalog) ongoing since more than a decade, detected by Benali et al (2020) for the whole FVG region.…”
Section: Discussionsupporting
confidence: 89%
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“…The global features of the resulting background seismicity and earthquake clusters turn out to be consistent between the two approaches, though the partitions are slightly different (Benali et al., 2020). Specifically, the statistics of clusters, singles, and fore/aftershocks are quite comparable (Table 1).…”
Section: Discussionmentioning
confidence: 92%
“…Notably the two methods, as applied in this study, have a different definition of background events: while NN assigns to the background seismicity the largest event from each cluster (i.e., the mainshock), SD assigns to it the first event of the cluster (not necessarily the mainshock). Therefore, the declustered catalogs resulted from these two methods may differ, particularly when foreshocks are identified (Benali et al., 2020).…”
Section: Declustering Algorithms Under Examinationmentioning
confidence: 99%