Group B, Poster #198, Earthquake Forecasting and Predictability (EFP)
Testing Rate-and-State Predictions of Aftershock Decay with Distance
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Poster Presentation
2024 SCEC Annual Meeting, Poster #198, SCEC Contribution #13618 VIEW PDF
t to measure, as it often reflects short-term catalog incompleteness rather than a true saturation in aftershock rate.
We explore the dependence of the Omori c-value on the distance to the mainshock by applying the “a-positive” method (van der Elst and Page, 2023). This method is insensitive to short-term aftershock incompleteness and allows resolution of the true aftershock rate deep into the mainshock coda. For aftershocks of the Ridgecrest mainshock and stacked M5-6 mainshocks, we observe systematic differences in early aftershock rates, relative to mainshock distance, consistent with the predictions of rate-and-state friction. Furthermore, for the larger Ridgecrest dataset, we observe that aftershocks nearer to the mainshock start earlier, and we resolve a flattening of the Omori curve consistent with a larger Omori c-value for the farthest aftershocks, as predicted by Dieterich (1994).
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We explore the dependence of the Omori c-value on the distance to the mainshock by applying the “a-positive” method (van der Elst and Page, 2023). This method is insensitive to short-term aftershock incompleteness and allows resolution of the true aftershock rate deep into the mainshock coda. For aftershocks of the Ridgecrest mainshock and stacked M5-6 mainshocks, we observe systematic differences in early aftershock rates, relative to mainshock distance, consistent with the predictions of rate-and-state friction. Furthermore, for the larger Ridgecrest dataset, we observe that aftershocks nearer to the mainshock start earlier, and we resolve a flattening of the Omori curve consistent with a larger Omori c-value for the farthest aftershocks, as predicted by Dieterich (1994).
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