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Implications of a composite source model and seismic-wave attenuation for the observed simplicity of small earthquakes and reported duration of earthquake initiation phase

Instituto de Geofísica UNAM, C.U., 04510 Mexico D.F., Mexico
Instituto de Ingeniería UNAM, C.U., 04510 Mexico D.F., Mexico
National Geophysical Research Institute, Hyderabad 500007, India

Abstract

An examination of P waves recorded on near-source, velocity seismograms generally shows that most small earthquakes (M_w < 2 to 3) are simple. On the other hand, larger earthquakes (M_w 4) are most often complex. The simplicity of the seismograms of M_w < 2 to 3 events may reflect the simplicity of the source (and, hence, may imply that smaller and larger earthquakes are not self-similar) or may be a consequence of attenuation of seismic waves. To test whether the attenuation is the cause, we generated synthetic P-wave seismograms from a composite circular source model in which subevent rupture areas are assumed to follow a power-law distribution. The rupture of an event is assumed to initiate at a random point on the fault and to propagate with a uniform speed. As the rupture front reaches the center of a subevent patch (all of which are circular), a P pulse is radiated that is calculated from the kinematic source model of Sato and Hirasawa (1973). Synthetic P-wave seismograms, which are all complex, are then convolved with an attenuation operator for different values of t*. The results show that the observed simplicity of small events (M_w < 2 to 3) may be entirely explained by attenuation if t* 0.02 sec.

The composite source model predicts that the average time delay between the initiation of the rupture and the rupture of the largest patch, , scales as M₀^1/3, such that log = (1/3) log M₀ – 8.462. This relation is very similar to that reported by Umeda et al. (1996) between M₀ and the observed time difference between the initiation of the rupture and the rupture of the "bright spot." It roughly agrees with the relation between M₀ and the duration of the initiation phase reported by Ellsworth and Beroza (1995) and Beroza and Ellsworth (1996). The relation also fits surprisingly well the data on duration of slow initial phase, tsip, and M₀, reported by Iio (1995). One possible explanation of this agreement may be that the composite source model, which is essentially the "cascade" model, successfully captures the evolution of the earthquake source process and that the rupture initiation and the abrupt increase in the velocity amplitude observed on seismograms by previous researchers roughly corresponds to the rupture of the first subevent and the breaking of the largest subevent in the composite source model.