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The influence of the brittle-ductile transition zone on aftershock and foreshock occurrence

Giuseppe Petrillo, Eugenio Lippiello (), François P. Landes and Alberto Rosso
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Giuseppe Petrillo: University of Campania “L. Vanvitelli”
Eugenio Lippiello: University of Campania “L. Vanvitelli”
François P. Landes: Univ. Paris-Sud, CNRS, INRIA, Université Paris-Saclay
Alberto Rosso: CNRS, Univ. Paris-Sud, Université Paris-Saclay

Nature Communications, 2020, vol. 11, issue 1, 1-10

Abstract: Abstract Aftershock occurrence is characterized by scaling behaviors with quite universal exponents. At the same time, deviations from universality have been proposed as a tool to discriminate aftershocks from foreshocks. Here we show that the change in rheological behavior of the crust, from velocity weakening to velocity strengthening, represents a viable mechanism to explain statistical features of both aftershocks and foreshocks. More precisely, we present a model of the seismic fault described as a velocity weakening elastic layer coupled to a velocity strengthening visco-elastic layer. We show that the statistical properties of aftershocks in instrumental catalogs are recovered at a quantitative level, quite independently of the value of model parameters. We also find that large earthquakes are often anticipated by a preparatory phase characterized by the occurrence of foreshocks. Their magnitude distribution is significantly flatter than the aftershock one, in agreement with recent results for forecasting tools based on foreshocks.

Date: 2020
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:11:y:2020:i:1:d:10.1038_s41467-020-16811-7

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DOI: 10.1038/s41467-020-16811-7

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