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Simple Physical Model for the Probability of a Subduction‐ Zone Earthquake Following Slow Slip Events and Earthquakes: Application to the Hikurangi Megathrust, New Zealand
Author(s) -
Kaneko Yoshihiro,
Wallace Laura M.,
Hamling Ian J.,
Gerstenberger Matthew C.
Publication year - 2018
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2018gl077641
Subject(s) - subduction , seismology , geology , episodic tremor and slip , slip (aerodynamics) , foreshock , interplate earthquake , tectonics , slow earthquake , earthquake prediction , tsunami earthquake , aftershock , engineering , aerospace engineering
Slow slip events (SSEs) have been documented in subduction zones worldwide, yet their implications for future earthquake occurrence are not well understood. Here we develop a relatively simple, simulation‐based method for estimating the probability of megathrust earthquakes following tectonic events that induce any transient stress perturbations. This method has been applied to the locked Hikurangi megathrust (New Zealand) surrounded on all sides by the 2016 Kaikoura earthquake and SSEs. Our models indicate the annual probability of a M ≥7.8 earthquake over 1 year after the Kaikoura earthquake increases by 1.3–18 times relative to the pre‐Kaikoura probability, and the absolute probability is in the range of 0.6–7%. We find that probabilities of a large earthquake are mainly controlled by the ratio of the total stressing rate induced by all nearby tectonic sources to the mean stress drop of earthquakes. Our method can be applied to evaluate the potential for triggering a megathrust earthquake following SSEs in other subduction zones.