HR: 16:30h
AN: S34A-03    [Abstracts]
TI: Surface Breaking Dip-Slip Fault: Its Dynamics and Generation of Corner Waves
AU: * Uenishi, K
EM: uenishi@kobe-u.ac.jp
AF: Research Center for Urban Safety and Security, Kobe University, 1-1 Rokko-dai, Nada, Kobe, 657-8501 Japan
AU: Madariaga, R I
EM: madariag@geologie.ens.fr
AF: Laboratoire de Géologie, Département Terre-Atmosphère-Océan, Ecole Normale Supérieure, 24, rue Lhomond, Paris Cedex 05, 75231 France
AB: It is currently widespread to invert accelerograms for obtaining fault slip distribution and rupture history for large, shallow strike-slip earthquakes. For shallow dip-slip earthquake, however, the situation is different because only few events of this type have been well recorded in the near field and the physical properties still remain unexplored due to analytical difficulties (see Madariaga, PAGEOPH, 2003). Here, we study rupture dynamics associated with a dip-slip fault located in a two-dimensional, linear elastic half space. That fault, following a slip-weakening relation, dips either vertically or 45 degrees and is subjected to a loading static stress that increases linearly with depth. Using a finite difference technique, we investigate the seismic wave field radiated by rupture of this straight fault. The rupture propagates either spontaneously or at a constant speed. We show that in both vertical and inclined cases, when the rupture front reaches the free surface, four Rayleigh-type pulses are generated: two propagating along the free surface into the opposite directions to the far field, the other two moving back along the ruptured fault surfaces (interface) downwards into depth. If the fault is vertical, the problem is still symmetrical and the induced particle motions are symmetrical with respect to the rupturing fault, although the stopping phase of the dynamic rupture is largely controlled by the downward interface pulses. In the case the fault is inclined, the symmetry is broken: in the hanging wall, the downward-propagating interface pulse and the outward-moving Rayleigh surface pulse interact with each other, inducing a kind of shear wave (corner wave). This corner wave carries concentrated wave energy and propagates faster than the surface and interface pulses, generating extremely strong particle motions in the hanging wall before static equilibrium of the faulted medium is achieved. On the contrary, in the footwall, the ground motion is dominated simply by the weaker Rayleigh pulse propagating along the free surface and the interaction between this Rayleigh and the oppositely-moving interface pulse is also small. The generation of downward interface pulses and the corner wave has not been well recognized so far, partly because those waves are not expected for a fault that is located at depth and does not break the surface. However, the comparison of these fundamental numerical results with the seismological recordings of the 1999 Chi-Chi, Taiwan, and the 2004 Niigata-ken Chuetsu, Japan, earthquakes also suggests the need for more careful analytical treatment concerning the effects of the free surface on the strong motion near fault breakouts.
DE: 7209 Earthquake dynamics (1242)
DE: 7212 Earthquake ground motions and engineering seismology
DE: 7260 Theory
DE: 7290 Computational seismology
SC: Seismology [S]
MN: Fall Meeting 2005