Dynamic rupture on an interface between a compliant fault zone layer and a stiffer surrounding solid

[1] We use two-dimensional plane strain finite difference calculations to study dynamic rupture on a material discontinuity interface between a compliant elastic layer and a stiffer elastic medium. Previous works established that rupture along a material interface governed by Coulomb friction propagates as a unidirectional narrow pulse associated with self-sharpening and divergent behavior. These effects are generated by coupling between spatial variations of slip along a material interface and local changes of normal stress. The simulations here employ a regularized friction law with a fading memory dependence of frictional strength on normal stress rather than the instantaneous Coulomb-type response. We find that the self-sharpening and divergent behavior found earlier with Coulomb friction exists also with regularized friction for large enough propagation distance. The parameters of regularized friction have to be fine tuned to produce apparent stability for a given propagation distance. However, eventually, the pulse always either diverges or dies. For cases with a single material interface the pulse strength increases with increasing contrast of shear wave velocity up to a maximum at ∼30% contrast, beyond which the generalized Rayleigh wave does not exist. This is similar to earlier results with Coulomb friction. For models having layer width comparable to or somewhat larger than the imposed source size, there is strong dependence of the pulse strength and shape on the layer width and velocity. The pulse amplitude is modulated by regular oscillations with period proportional to the layer width and is amplified for a range of layer widths. The results suggest that rupture along an interface between a compliant layer and a stiffer surrounding medium, initiated by a failure of an asperity with size not larger than the layer width, can become a self-sustaining wrinkle-like pulse.

[1]  A. Lachenbruch,et al.  Heat flow from Cajon Pass, fault strength, and tectonic implications , 1992 .

[2]  A. Schallamach How Does Rubber Slide , 1971 .

[3]  Paul G. Richards,et al.  Quantitative Seismology: Theory and Methods , 1980 .

[4]  Yehuda Ben-Zion,et al.  Wrinkle-like slip pulse on a fault between different , 1997 .

[5]  T. Nakata,et al.  Large slip velocity of the surface rupture associated with the 1990 Luzon Earthquake , 1994 .

[6]  John R. Rice,et al.  Fault rupture between dissimilar materials: Ill-posedness, regularization, and slip-pulse response , 2000 .

[7]  W. Mooney,et al.  Seismic measurements of the internal properties of fault zones , 1986 .

[8]  J. Brune Tectonic stress and the spectra of seismic shear waves from earthquakes , 1970 .

[9]  Joint inversion of fault zone head waves and direct P arrivals for crustal structure near major faults , 1992 .

[10]  Y. Ben‐Zion Dynamic ruptures in recent models of earthquake faults , 2001 .

[11]  Allan M. Rubin,et al.  Aftershock asymmetry/rupture directivity among central San Andreas fault microearthquakes , 2000 .

[12]  D. J. Andrews,et al.  Properties and implications of dynamic rupture along a material interface , 1998, Bulletin of the Seismological Society of America.

[13]  A. Michael,et al.  Relations Among Fault Behavior, Subsurface Geology, and Three-Dimensional Velocity Models , 1991, Science.

[14]  W. T. Parry,et al.  Fracturing and hydrothermal alteration in normal fault zones , 1994 .

[15]  J. Brune,et al.  Heat Flow, Stress, and Rate of Slip along the San Andreas Fault, , 1969 .

[16]  John R. Rice,et al.  Slip dynamics at an interface between dissimilar materials , 2001 .

[17]  T. Heaton Evidence for and implications of self-healing pulses of slip in earthquake rupture , 1990 .

[18]  Steven M. Day,et al.  Effects of a low-velocity zone on a dynamic rupture , 1997, Bulletin of the Seismological Society of America.

[19]  Vikas Prakash,et al.  Frictional Response of Sliding Interfaces Subjected to Time Varying Normal Pressures , 1998 .

[20]  George G. Adams,et al.  Self-excited oscillations of two elastic half-spaces sliding with a constant coefficient of friction , 1995 .

[21]  J. Weertman,et al.  Unstable slippage across a fault that separates elastic media of different elastic constants , 1980 .

[22]  F. Chester,et al.  Ultracataclasite structure and friction processes of the Punchbowl Fault , 1998 .

[23]  James N. Brune,et al.  Wrinkle-like Weertman pulse at the interface between two blocks of foam rubber with different velocities , 1999 .