CaltechAUTHORS
  A Caltech Library Service

Continuum of earthquake rupture speeds enabled by oblique slip

Weng, Huihui and Ampuero, Jean-Paul (2020) Continuum of earthquake rupture speeds enabled by oblique slip. . (Unpublished) https://resolver.caltech.edu/CaltechAUTHORS:20200331-090901094

[img] PDF (July 29, 2020) - Submitted Version
Creative Commons GNU LGPL (Software).

1843Kb

Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20200331-090901094

Abstract

Earthquake rupture speed can affect ground shaking and thus seismic hazard. Seismological observations show that large earthquakes span a continuum of rupture speeds, from slower than Rayleigh waves up to P wave speed, and include speeds that are predicted to be unstable by 2D theory. This discrepancy between observations and theory has not yet been reconciled by a quantitative model. Here we present numerical simulations that show that long ruptures with oblique slip (both strike-slip and dip-slip components) can propagate steadily at various speeds, including those previously suggested to be unstable. The obliqueness of slip and the ratio of fracture energy to static energy release rate primarily control the propagation speed of long ruptures. We find that the effects of these controls on rupture speed can be predicted by extending the 3D theory of fracture mechanics to long ruptures with oblique slip. We propose that this model provides a quantitative framework to interpret supershear earthquakes, to constrain the energy ratio of faults based on observed rupture speed and rake angle, and to relate the potential rupture speed and size of future earthquakes to the observed slip deficit along faults.


Item Type:Report or Paper (Discussion Paper)
Related URLs:
URLURL TypeDescription
https://doi.org/10.31223/osf.io/tw4juDOIDiscussion Paper
https://geodynamics.org/cig/software/specfem3dRelated ItemSPECFEM3D Cartesian
ORCID:
AuthorORCID
Weng, Huihui0000-0002-2936-2342
Ampuero, Jean-Paul0000-0002-4827-7987
Alternate Title:Oblique slip on long faults enables a continuum of earthquake rupture speeds
Additional Information:License: GNU Lesser General Public License (LGPL) 2.1. Submitted: March 30, 2020; Last edited: July 29, 2020. The open-source software SPECFEM3D used in our 3-D dynamic rupture simulations is available from the Computational Infrastructure for Geodynamics at https://geodynamics.org/cig/software/specfem3d/. This work was supported by the French government through the Investments in the Future project UCAJEDI (ANR-15-IDEX-01) managed by the French National Research Agency (ANR). We thank Diego Molina for providing the central Andes coupling model in digital form. Author contributions: H.W. designed and carried out the numerical experiments, and analysed the numerical results. H.W. and J.-P.A. developed the theoretical model, interpreted the results, and wrote the paper. Competing Interests: The authors declare that they have no competing interests.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
Agence Nationale pour la Recherche (ANR)ANR-15-IDEX-01
Subject Keywords:Physical Sciences and Mathematics; Earth Sciences; Geophysics and Seismology
Record Number:CaltechAUTHORS:20200331-090901094
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20200331-090901094
Official Citation:Weng, H., & Ampuero, J. (2020, March 31). Oblique slip on long faults enables a continuum of earthquake rupture speeds. https://doi.org/10.31223/osf.io/tw4ju
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:102192
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:31 Mar 2020 16:16
Last Modified:29 Jul 2020 17:00

Repository Staff Only: item control page