|
|
||||||||
Department of Earth Sciences University of Southern California, Los Angeles, California 90089-0740
U.S Geological Survey, MS 977, 345 Middlefield Rd., Menlo Park, California 94025-3591
Abstract
We perform two-dimensional plane-strain finite-difference calculations of dynamic rupture along an interface separating different elastic media. The calculations extend earlier results of Andrews and Ben-Zion (1997) who found a self-sustaining narrow slip pulse associated with dynamic reduction of normal stress along a material interface governed by constant friction, in agreement with Weertman (1980). The pulse propagates in a wrinklelike mode having remarkable dynamic properties that may be relevant to many geophysical phenomena. Here we examine the range of values of elastic parameters, friction coefficient, and strength heterogeneities allowing for the existence of the wrinklelike pulse. Rupture is initiated in the simulations by imposed slip in a limited space-time domain. Outside the region of the imposed slip, the pulse becomes narrower and higher with propagation distance along the interface. The strength of the wrinklelike pulse increases with S-wave velocity contrast up to a maximum at about 35% contrast. Beyond such a velocity contrast, there is no solution for a generalized Rayleigh wave along a material interface, and the strength of the pulse decreases. However, the wrinklelike pulse can still propagate in a self-sustaining manner for larger velocity contrasts. For a fixed S-wave velocity contrast, the strength has little dependence on density contrast or Poisson's ratio, but the pulse strength increases rapidly with increasing coefficient of friction. Stress and strength heterogeneities with small correlation length have little effect on the pulse, while long wavelength heterogeneities reduce the strength of the pulse. The high mechanical efficiency of the wrinklelike pulse suggests that earthquake ruptures may favor such mode of failure when possible.
This article has been cited by other articles:
![]() |
S. Ma and G. C. Beroza Rupture Dynamics on a Bimaterial Interface for Dipping Faults Bulletin of the Seismological Society of America, August 1, 2008; 98(4): 1642 - 1658. [Abstract] [Full Text] [PDF] |
||||
![]() |
S. Boutareaud, C. A. J. Wibberley, O. Fabbri, and T. Shimamoto Permeability structure and co-seismic thermal pressurization on fault branches: insights from the Usukidani fault, Japan Geological Society, London, Special Publications, January 1, 2008; 299(1): 341 - 361. [Abstract] [Full Text] [PDF] |
||||
![]() |
On the Self-Healing Fracture Mode Bulletin of the Seismological Society of America, December 1, 2003; 93(6): 2375 - 2388. |
||||
![]() |
The Three-Dimensional Dynamics of a Nonplanar Thrust Fault Bulletin of the Seismological Society of America, October 1, 2003; 93(5): 2222 - 2235. |
||||
![]() |
Predominance of Unilateral Rupture for a Global Catalog of Large Earthquakes Bulletin of the Seismological Society of America, December 1, 2002; 92(8): 3309 - 3317. |
||||
![]() |
Triggered Surface Slips in the Salton Trough Associated with the 1999 Hector Mine, California, Earthquake Bulletin of the Seismological Society of America, May 1, 2002; 92(4): 1300 - 1317. |
||||
![]() |
Dynamic Earthquake Ruptures in the Presence of Lithostatic Normal Stresses: Implications for Friction Models and Heat Production Bulletin of the Seismological Society of America, December 1, 2001; 91(6): 1765 - 1796. |
||||
![]() |
Simultaneous Determination of Site Responses and Source Parameters of Small Earthquakes along the Atotsugawa Fault Zone, Central Japan Bulletin of the Seismological Society of America, December 1, 2000; 90(6): 1430 - 1445. |
||||
![]() |
Rupture Pulse Characterization: Self-Healing, Self-Similar, Expanding Solutions in a Continuum Model of Fault Dynamics Bulletin of the Seismological Society of America, December 1, 2000; 90(6): 1480 - 1497. |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |