Publisher： John Wiley & Sons Inc
E-ISSN： 2156-2202|96|B4|6291-6302
ISSN： 0148-0227
Source： Journal Of Geophysical Research, Vol.96, Iss.B4, 1991-04, pp. : 6291-6302
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Abstract
The high‐frequency falloff ω−γ of earthquake displacement spectra and the b value of aftershock sequences are attributed to the character of spatially varying strength along fault zones. I assume that the high frequency energy of a main shock is produced by a self‐similar distribution of subevents, where the number of subevents with radii greater than R is proportional to R−D, D being the fractal dimension. In this model, an earthquake is composed of a hierarchical set of smaller earthquakes. The static stress drop is parameterized to be proportional to Rη, and strength is assumed to be proportional to static stress drop. I find that a distribution of subevents with D = 2 and stress drop independent of seismic moment (η = 0) produces a main shock with an ω−2 falloff, if the subevent areas fill the rupture area of the main shock. By equating subevents to “islands” of high stress of a random, self‐similar stress field on a fault, I relate D to the scaling of strength on a fault, such that D = 2 − η. Thus D = 2 corresponds to constant stress drop scaling (η = 0) and scale‐invariant fault strength. A self‐similar model of aftershock rupture zones on a fault is used to determine the relationship between the b value, the size distribution of aftershock rupture zones, and the scaling of strength on a fault. The b value for aftershock sequences on a fault is found to equal (3 − 1.5η)/(3 + η). Therefore this model indicates that the typically observed spectral falloffs of ω−2 and b values of 1 can be entirely caused by scale‐invariant strength (η = 0) along fault zones.
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