Fluid pressure and shear zone development over the locked to slow slip region in Cascadia
Author:
Affiliation:
1. Department of Earth and Environmental Sciences, University of Ottawa, Ottawa, Canada.
Abstract
Funder
Alfred P. Sloan Foundation
Natural Sciences and Engineering Research Council of Canada
Publisher
American Association for the Advancement of Science (AAAS)
Subject
Multidisciplinary
Reference39 articles.
1. Downward landward limit of Cascadia great earthquake rupture;Hyndman R. D.;J. Geophys. Res.,2013
2. Invited review paper: Some outstanding issues in the study of great megathrust earthquakes—The Cascadia example;Wang K.;J. Geodyn.,2016
3. Central Cascadia subduction zone creep;Schmalzle G. M.;Geochem. Geophys. Geosyst.,2014
4. Episodic Tremor and Slip on the Cascadia Subduction Zone: The Chatter of Silent Slip
5. Cascadia subducting plate fluids channelled to fore-arc mantle corner: ETS and silica deposition
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