2021
DOI: 10.1029/2021jb022566
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Spatio‐Temporal Evolution of Earthquake Static Stress Drop Values in the 2016–2017 Central Italy Seismic Sequence

Abstract: The estimation of earthquake static stress drop values over a wide range of magnitudes generates considerable recent interest due to the related implications for frictional models (e.g., Abercrombie, 1995), ground motion predictions (e.g., Baltay et al., 2013), and the physical differences between large and small earthquakes (e.g., Prieto et al., 2004). The average difference in shear stress on a fault (static stress drop) caused by an earthquake typically ranges between 0.1 and 100 MPa (e.g., Hanks, 1977). It… Show more

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Cited by 16 publications
(33 citation statements)
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References 120 publications
(260 reference statements)
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“…Priors for the corner frequency f c of each event depend on the event size but are assumed to follow a lognormal distribution derived from a corresponding stress drop prior with a median stress drop of 5 MPa and standard deviation of 0.4 in log10 units. These values are in line with recent work (Baltay et al., 2013; Bindi, Zaccarelli, & Kotha, 2020; Kemna et al., 2021; Oth et al., 2017; Trugman, 2020), though the final inversion results are insensitive to the precise values selected (within reason). Seismic moment M 0 is also assumed lognormal and centered on the catalog value.…”
Section: Background and Methodologysupporting
confidence: 90%
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“…Priors for the corner frequency f c of each event depend on the event size but are assumed to follow a lognormal distribution derived from a corresponding stress drop prior with a median stress drop of 5 MPa and standard deviation of 0.4 in log10 units. These values are in line with recent work (Baltay et al., 2013; Bindi, Zaccarelli, & Kotha, 2020; Kemna et al., 2021; Oth et al., 2017; Trugman, 2020), though the final inversion results are insensitive to the precise values selected (within reason). Seismic moment M 0 is also assumed lognormal and centered on the catalog value.…”
Section: Background and Methodologysupporting
confidence: 90%
“…Both the Ridgecrest (Trugman et al., 2020; X. Wang & Zhan, 2020) and the San Jacinto (Cheng et al., 2018; Ross, Rollins, et al., 2017) fault zones are structurally complex fault systems, yet differ in their source properties. Without any target events of note on the main strand of the San Andreas, it is difficult to fully assess the potential effects of fault geometry and maturity on source properties like stress drop (Chu et al., 2021; Kemna et al., 2021).…”
Section: Discussionmentioning
confidence: 99%
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“…The comparison of the results in terms of source spectra and source parameters (Figs 11 and 12) allows us to confirm the robustness of source parameter estimation, as well as to validate the coda calibration in this region. The consistency of source parameters estimated from analysis performed on different portions of seismic recordings is also a matter of debate for Central Italy (Kemna et al 2021). Figs 11 and 12 show that coda and S waves methodologies applied independently to a common data set compiled for central Apennines in Italy provide very similar source spectra, from which consistent scaling laws are extracted.…”
Section: Discussion a N D C O N C L U S I O N Smentioning
confidence: 98%
“…Andrews 1986;Castro et al 1990;Boatwright et al 1991;Edwards et al 2008;Malagnini et al 2011;Oth et al 2011;Picozzi et al 2017;Trugman & Shearer 2017). Despite so many different novel approaches, it is rare that results from different methods focusing on the same data set yield similar results, and as such, the question of absolute stress drop and its scaling remains quite ambiguous, especially over a broad range of magnitudes (Shearer et al 2019;Kemna et al 2021).…”
Section: Introductionmentioning
confidence: 99%