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Source properties of dynamic rupture pulses with off-fault plasticity

Gabriel, A.-A. and Ampuero, J.-P. and Dalguer, L. A. and Mai, P. M. (2013) Source properties of dynamic rupture pulses with off-fault plasticity. Journal of Geophysical Research. Solid Earth, 118 (8). pp. 4117-4126. ISSN 2169-9313. https://resolver.caltech.edu/CaltechAUTHORS:20131101-135955675

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Abstract

Large dynamic stresses near earthquake rupture fronts may induce an inelastic response of the surrounding materials, leading to increased energy absorption that may affect dynamic rupture. We systematically investigate the effects of off-fault plastic energy dissipation in 2-D in-plane dynamic rupture simulations under velocity-and-state-dependent friction with severe weakening at high slip velocity. We find that plasticity does not alter the nature of the transitions between different rupture styles (decaying versus growing, pulse-like versus crack-like, and subshear versus supershear ruptures) but increases their required background stress and nucleation size. We systematically quantify the effect of amplitude and orientation of background shear stresses on the asymptotic properties of self-similar pulse-like ruptures: peak slip rate, rupture speed, healing front speed, slip gradient, and the relative contribution of plastic strain to seismic moment. Peak slip velocity and rupture speed remain bounded. From fracture mechanics arguments, we derive a nonlinear relation between their limiting values, appropriate also for crack-like and supershear ruptures. At low background stress, plasticity turns self-similar pulses into steady state pulses, for which plastic strain contributes significantly to the seismic moment. We find that the closeness to failure of the background stress state is an adequate predictor of rupture speed for relatively slow events. Our proposed relations between state of stress and earthquake source properties in the presence of off-fault plasticity may contribute to the improved interpretation of earthquake observations and to pseudodynamic source modeling for ground motion prediction.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1002/jgrb.50213 DOIArticle
http://onlinelibrary.wiley.com/doi/10.1002/jgrb.50213/abstractPublisherArticle
ORCID:
AuthorORCID
Ampuero, J.-P.0000-0002-4827-7987
Additional Information:© 2013 American Geophysical Union. Received 12 February 2013; revised 4 May 2013; accepted 6 May 2013; published 5 August 2013. This work was supported by PG&E, NSF (grant EAR-0944288), and SCEC (funded by NSF EAR-0106924 and USGS 02HQAG0008 cooperative agreements). This is SCEC contribution number 1655. We acknowledge the research computing facilities at King Abdullah University of Science and Technology and J. Ruiz for providing Figure 7. We thank the Editor and the editorial team, E.M. Dunham, and an anonymous reviewer for their improvements of the manuscript.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
PG&EUNSPECIFIED
NSFEAR-0944288
Southern California Earthquake Center (SCEC)UNSPECIFIED
NSFEAR-0106924
USGS02HQAG0008
Subject Keywords:rupture dynamics; off-fault plasticity; slip pulse; ground motion; seismology
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Southern California Earthquake Center1655
Issue or Number:8
Record Number:CaltechAUTHORS:20131101-135955675
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20131101-135955675
Official Citation:Gabriel, A.-A., J.-P. Ampuero, L. A. Dalguer, and P. M. Mai (2013), Source properties of dynamic rupture pulses with off-fault plasticity, J. Geophys. Res. Solid Earth, 118, 4117–4126, doi:10.1002/jgrb.50213
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42198
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:01 Nov 2013 21:39
Last Modified:03 Oct 2019 05:56

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