Estimating Fault Friction From Seismic Signals in the Laboratory

Abstract Nearly all aspects of earthquake rupture are controlled by the friction along the fault that progressively increases with tectonic forcing but in general cannot be directly measured. We show that fault friction can be determined at any time, from the continuous seismic signal. In a classic...

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Bibliographic Details
Main Authors: Bertrand Rouet‐Leduc, Claudia Hulbert, David C. Bolton, Christopher X. Ren, Jacques Riviere, Chris Marone, Robert A. Guyer, Paul A. Johnson
Format: Article
Language:English
Published: Wiley 2018-02-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1002/2017GL076708
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