Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones

Author:

Aben F. M.12,Doan M.-L.12,Mitchell T. M.3,Toussaint R.4,Reuschlé T.4,Fondriest M.5,Gratier J.-P.12,Renard F.126

Affiliation:

1. University Grenoble Alpes, ISTerre; Grenoble France

2. CNRS, ISTerre; Grenoble France

3. Department of Earth Sciences; University College London; London UK

4. Institut de Physique du Globe de Strasbourg; University of Strasbourg/EOST; Strasbourg France

5. School of Earth, Atmospheric and Environmental Sciences; University of Manchester; Manchester UK

6. PGP, Department of Geosciences; University of Oslo; Oslo Norway

Funder

European Union's Seventh Framework Programme for Research, Technological Development and Demonstration

Labex OSUG@2020

NERC

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference64 articles.

1. Self-excited oscillations of two elastic half-spaces sliding with a constant coefficient of friction;Adams;J. Appl. Mech.,1995

2. Ampuero , J.-P. 2014 Physical limits on damaged fault zone thickness: The role of seismogenic depth AGU Fall Meeting 2014

3. Cracks, pulses and macroscopic asymmetry of dynamic rupture on a bimaterial interface with velocity-weakening friction;Ampuero;Geophys. J. Int.,2008

4. Rupture dynamics with energy loss outside the slip zone;Andrews;J. Geophys. Res.,2005

5. Wrinkle-like slip pulse on a fault between different materials;Andrews;J. Geophys. Res.,1997

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