Exciting news! We're transitioning to the Statewide California Earthquake Center. Our new website is under construction, but we'll continue using this website for SCEC business in the meantime. We're also archiving the Southern Center site to preserve its rich history. A new and improved platform is coming soon!

Kinematic Ground Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations

Robert W. Graves, & Arben Pitarka

Published August 23, 2016, SCEC Contribution #6226

We describe a methodology for generating kinematic earthquake ruptures for use in 3D ground motion simulations over the frequency band 0 to 5 Hz. Our approach begins by specifying a spatially random slip distribution that has a roughly wavenumber-squared falloff. Given a hypocenter, the rupture speed is specified to average about 75-80% of the local shear wave speed and the prescribed slip-rate function has a Kostrov-like shape with a fault-averaged rise time that scales self-similarly with seismic moment. Both the rupture time and rise time include significant local perturbations across the fault surface specified by spatially random fields that are partially correlated with the underlying slip distribution. We represent velocity-strengthening zones in the shallow (< 5 km) and deep (> 15 km) crust by decreasing rupture speed and increasing rise time in these regions. Additional refinements to the approach include the incorporation of geometric perturbations to the fault surface, 3D stochastic correlated perturbations to the velocity structure, and a “damage zone” surrounding the shallow fault surface characterized by a 30% reduction in seismic velocity. We demonstrate the approach using a suite of simulations for a hypothetical Mw 6.45 strike-slip earthquake embedded in a generalized hard-rock velocity structure. The simulation results are compared with the median predictions from the 2014 NGA GMPEs and show very good agreement over the frequency band 0.1 to 5 Hz for distances out to 25 km from the fault. Additionally, the newly added features act to reduce the coherency of the radiated higher frequency (f > 1 Hz) ground motions, and homogenize radiation pattern effects in this same bandwidth, which move the simulations closer to the statistical characteristics of observed motions as illustrated by comparison with recordings from the 1979 Imperial Valley earthquake.

Citation
Graves, R. W., & Pitarka, A. (2016). Kinematic Ground Motion Simulations on Rough Faults Including Effects of 3D Stochastic Velocity Perturbations. Bulletin of the Seismological Society of America, 106(5), 2136-2153.