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Barnaby Fryer

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Articles

Foreshock-induced slip transients set mainshock nucleation timing

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By Dmitry I. Garagash, Mathias Lebihain, François Passelègue, Barnaby Fryer
| Nature Verified
Abstract Foreshocks are sometimes observed before earthquakes1,2,3,4,5,6,7,8,9,10,11,12,13, yet their role in controlling rupture nucleation remains unclear1,11,14. Classical models often assume that nucleation arises from slow, quasi-static slip governed primarily by fault weakening15,16,17,18,19,20,21, typically neglecting impulsive precursory events.
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