Episodic Slow Slip Hosted by Talc‐Bearing Metasomatic Rocks: High Strain Rates and Stress Amplification in a Chemically Reacting Shear Zone
Author:
Affiliation:
1. University of Washington Seattle WA USA
2. University of California Santa Barbara CA USA
3. Amherst College Amherst MA USA
Funder
National Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL101083
Reference77 articles.
1. Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing
2. Semibrittle and cataclastic deformation of hornblende-quartz rocks in a ductile shear zone
3. Fracture and Weakening of Jammed Subduction Shear Zones, Leading to the Generation of Slow Slip Events
4. Strength of Strained Two‐Phase Mixtures: Application to Rapid Creep and Stress Amplification in Subduction Zone Mélange
5. Fluid flow and metasomatism in a subduction zone hydrothermal system: Catalina Schist terrane, California
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