Fault slip controlled by gouge rheology: a model for slow earthquakes
Author:
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/gji/article-pdf/159/1/347/5871565/159-1-347.pdf
Reference26 articles.
1. Earthquake slip on oceanic transform faults;Abercrombie;Nature,2001
2. Fluid conduits in carbonate-hosted seismogenic normal faults of central Italy;Agosta;J. geophys. Res.,2003
3. Slow rupture of an aseismic fault in a seismogenic region of Central Italy;Amoruso;Geophys. Res. Lett.,2002
4. Viscoelastic stress relaxation on deep fault sections as a possible source of very long period elastic waves;Bonafede;J. geophys. Res.,1983
5. The MEDNET program;Boschi;Ann. Geofis.,1994
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4. InSAR observations of aseismic slip associated with an earthquake swarm in the Columbia River flood basalts;Journal of Geophysical Research;2011-12-10
5. Slip localization and fault weakening as a consequence of fault gouge strengthening — Insights from laboratory experiments;Earth and Planetary Science Letters;2008-11
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