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John G. Anderson
Seismic energy and stress-drop parameters for a composite source model
Bulletin of the Seismological Society of America (February 1997), 87(1):85-96

Abstract:
This article examines relationships among radiated energy and several stress-drop parameters that are used to describe earthquake faulting. This is done in the context of a composite source model that has been quite successful in its ability to reproduce statistical characteristics of strong-motion accelerograms. The main feature of the composite source model is a superposition of subevents with a fractal distribution of sizes, but all with the same subevent stress drop (Delta sigma (sub delta ) ) that is independent of the static stress drop (Delta sigma s ). In the model, Delta sigma (sub delta ) is intended to represent the effective dynamic stress, and it does this well when Delta sigma (sub delta ) >2Delta sigma s . The radiated energy in the S wave is E CS S = 0.233 C E (Delta sigma d /mu ) M 0 , where M 0 is the seismic moment of the earthquake, mu is shear modulus, and C E is a dimensionless parameter that equals unity when Delta sigma d >2Delta sigma s . The apparent stress (sigma a ) is sigma a = 0.243 C E Delta sigma d . The effective stress is sigma e nearly equal C0.44C E Delta sigma d . The Orowan stress drop (Delta sigma 0 ) is Delta sigma 0 = 0.486 Delta sigma d . The root-mean-square (rms) stress drop (Delta sigma rms ) is Delta sigma rms = Delta sigma d I (super 1/2) (sub theta ) M 0 /M OS (R max ) (super 1/2) (f c /f 0 ) (super 1/2) , where f 0 is corner frequency of the earthquake, M OS (R max ) and f c are the moment and corner frequency of the largest subevent, and I (super 1/2) (sub theta ) is a dimensionless constant approximately equal to 1.7. Finally, the Savage-Wood ratio (SWR) is given by SWR nearly equal C E Delta sigma d /2Delta sigma s . These results clarify the relationships among all of these stress parameters in the context of a complex fault, showing the critical role of the subevent stress drop. They also provide an additional tool for energy, stress, and Savage-Wood ratio estimation. Since the process of modeling strong motion with the composite source uses realistic Green's functions, estimates of energy and stress parameters using this model are expected to have a good correction for wave propagation.

Index Terms/Descriptors:
applications; earthquakes; elastic waves; faults; focal mechanism; Green function; models; propagation; seismic moment; seismic waves; seismicity; stress; stress drops

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