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Rupture modes in laboratory earthquakes: Effect of fault prestress and nucleation conditions

Lu, Xiao and Rosakis, Ares J. and Lapusta, Nadia (2010) Rupture modes in laboratory earthquakes: Effect of fault prestress and nucleation conditions. Journal of Geophysical Research B, 115 . Art. No. B12302. ISSN 0148-0227. https://resolver.caltech.edu/CaltechAUTHORS:20110104-111925811

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Abstract

Seismic inversions show that earthquake risetimes may be much shorter than the overall rupture duration, indicating that earthquakes may propagate as self-healing, pulse-like ruptures. Several mechanisms for producing pulse-like ruptures have been proposed, including velocity-weakening friction, interaction of dynamic rupture with fault geometry and local heterogeneity, and effect of bimaterial contrast. We present experimental results on rupture mode selection in laboratory earthquakes occurring on frictional interfaces, which were prestressed both in compression and in shear. Our experiments demonstrate that pulse-like ruptures can exist in the absence of a bimaterial effect or of local heterogeneities. We find a systematic variation from crack-like to pulse-like rupture modes with both (1) decreasing nondimensional shear prestress and (2) decreasing absolute levels of shear and normal prestress for the same value of nondimensional shear prestress. Both pulse-like and crack-like ruptures can propagate with either sub-Rayleigh or supershear rupture speeds. Our experimental results are consistent with theories of ruptures on velocity-weakening interfaces, implying that velocity-weakening friction plays an important role in governing the dynamic behavior of earthquake ruptures. We show that there is no measurable fault-normal stress decrease on the fault plane due to the nucleation procedure employed in experiments, and hence, this is not a factor in the rupture mode selection. We find that pulse-like ruptures correspond to the levels of nondimensional shear prestress significantly lower than the static friction coefficient, suggesting that faults hosting pulse-like ruptures may operate at low levels of prestress compared to their static strength.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/2009JB006833DOIArticle
ORCID:
AuthorORCID
Rosakis, Ares J.0000-0003-0559-0794
Lapusta, Nadia0000-0001-6558-0323
Additional Information:© 2011 American Geophysical Union. Received 9 September 2009; revised 25 May 2010; accepted 6 August 2010; published 1 December 2010. Nadia Lapusta gratefully acknowledges the support of NSF grant EAR 0548277 for this study. Ares J. Rosakis also gratefully acknowledges the support of NSF grants EAR 0207873 and EAR 0911723, the U.S. Department of Energy grant DE‐FG52‐06NA-26209, and MURI grant N000140610730 (Y.D.S. Rajapakse, Program Manager).
Group:GALCIT
Funders:
Funding AgencyGrant Number
NSFEAR-0548277
NSFEAR-0207873
NSFEAR-0911723
Department of Energy (DOE)DE-FG52-06NA 26209
Office of Naval Research (ONR)N000140610730
Subject Keywords:earthquake physics; velocity-dependent friction; pulse-like rupture; supershear speed; rupture mode; nucleation
Record Number:CaltechAUTHORS:20110104-111925811
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20110104-111925811
Official Citation:Lu, X., A. J. Rosakis, and N. Lapusta (2010), Rupture modes in laboratory earthquakes: Effect of fault prestress and nucleation conditions, J. Geophys. Res., 115, B12302, doi:10.1029/2009JB006833
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:21574
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:05 Jan 2011 20:01
Last Modified:09 Mar 2020 13:19

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