Slow Slip as an Indicator of Fault Stress Criticality

Abstract Fault regions inferred to be slowly slipping are interpreted to accommodate much of tectonic plate motion aseismically and potentially serve as barriers to earthquake rupture. Here, we build on prior work using simulations of earthquake sequences with enhanced dynamic fault weakening to sho...

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Bibliographic Details
Published in:	Geophysical Research Letters
Main Author:	Valère Lambert
Format:	Article
Language:	English
Published:	Wiley 2024-06-01
Subjects:	slow slip fault stress enhanced dynamic weakening
Online Access:	https://doi.org/10.1029/2023GL107356

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