2022
DOI: 10.1785/0120210208
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The Effect of Seismic Sequences in Probabilistic Seismic Hazard Analysis

Abstract: Traditionally, probabilistic seismic hazard analysis (PSHA) considers only mainshock events and models their temporal occurrence through a homogeneous Poisson process. Thus, it disregards foreshocks and aftershocks, assuming they have a minor effect on PSHA. However, recent earthquake sequences, such as those in 2016–2017 in Central Italy and 2010–2011 in Christchurch, New Zealand, exposed the shortcomings of such a universally used but unconservative approach. Our efforts to quantify the bias in seismic hazar… Show more

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Cited by 11 publications
(3 citation statements)
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“…For this reason, the stochastic event sets in this study are considered acceptable. It is worth noting that other studies based on classical ETAS approaches also seem to provide a good description of the Italian seismicity, especially in the 5 < M W < 5.5 range (e.g., Šipčić et al., 2022).…”
Section: Case Studymentioning
confidence: 88%
“…For this reason, the stochastic event sets in this study are considered acceptable. It is worth noting that other studies based on classical ETAS approaches also seem to provide a good description of the Italian seismicity, especially in the 5 < M W < 5.5 range (e.g., Šipčić et al., 2022).…”
Section: Case Studymentioning
confidence: 88%
“…In addition, the Epidemic Type Aftershock Sequence (ETAS) model has also been used to study the spatio-temporal distribution of earthquakes in recent years (Ogata, 1988;Ogata, 1998;Zhuang et al, 2005;Ogata and Zhuang, 2006), and has been proposed or used by scientists as a means for probabilistic seismic hazard analysis (e.g., Xu et Wu, 2017;Pei et al, 2021;Šipčić et al, 2022). However, for seismic hazard analysis, more attention is paid to the temporal distribution of main shocks (Michael, 2011;Daub et al, 2012;Shearer and Stark, 2012;Beroza, 2012).…”
Section: Introductionmentioning
confidence: 99%
“…In addition, the Epidemic Type Aftershock Sequence (ETAS) model has also been used to study the spatio-temporal distribution of earthquakes in recent years (Ogata, 1988;Ogata, 1998;Zhuang et al, 2005;Ogata and Zhuang, 2006), and has been proposed or used by scientists as a means for probabilistic seismic hazard analysis (e.g., Xu et Wu, 2017;Pei et al, 2021;Šipčić et al, 2022). However, for seismic hazard analysis, more attention is paid to the temporal distribution of main shocks (Michael, 2011;Daub et al, 2012;Shearer and Stark, 2012;Beroza, 2012).…”
Section: Introductionmentioning
confidence: 99%