Episodic Tremor and Slip Explained by Fluid‐Enhanced Microfracturing and Sealing

Abstract Episodic tremor and slow‐slip events at the deep extension of plate boundary faults illuminate seismic to aseismic processes around the brittle‐ductile transition. These events occur in volumes characterized by overpressurized fluids and by near failure shear stress conditions. We present a...

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Bibliographic Details
Main Authors: M. Bernaudin, F. Gueydan
Format: Article
Language:English
Published: Wiley 2018-04-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2018GL077586
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