[1] We present an attempt to describe the scaling law of the slip weakening rate at the onset of instability using a two-dimensional fault model. A fault consists of a series of weak patches under slip weakening friction, separated by unbreakable barriers. A first group of faults contains an even distribution of patches of different scales conserving the same total slipping length, while a second group consists of various fractal Cantor sets. The global behavior of rupture is described by the exponential growth rate l. For an infinite homogeneous fault, the coefficient l is governed by the weakening rate of the friction law. We estimate the weakening rate of each individual fault in an heterogeneous fault system such that the rate of exponential growth l of this fault network is identical to that of a single homogeneous fault. Using this homogenization procedure, we compute the weakening rate on the weak patches for faults with different scales of heterogeneity and a given l. At large scales, the weakening rate is scale-independent, the initiation process on a long patch being similar to the case of an infinite fault. At small scales and for all the different geometries considered here, the weakening rate varies as a = b * 0 /a, where a is the scale or half length of each elementary fault and b * 0 ' 1.158. We discuss the physical implications of our results on the value of the slip weakening distance D c and give a possible explanation of the scale dependence of this parameter. Citation: Perfettini, H., M. Campillo, and I. Ionescu, On the scaling of the slip weakening rate of heterogeneous faults,
CITATION STYLE
Perfettini, H., Campillo, M., & Ionescu, I. (2003). On the scaling of the slip weakening rate of heterogeneous faults. Journal of Geophysical Research: Solid Earth, 108(B9). https://doi.org/10.1029/2002jb001969
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