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Monte Carlo simulation of peak-acceleration attenuation using a finite-fault uniform-patch model including isochrone and extremal characteristics

A. M. Rogers·D. M. Perkins
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Abstract

A finite-fault statistical model of the earthquake source is used to confirm observed magnitude and distance saturation scaling in a large peak-acceleration data set. This model allows us to determine the form of peak-acceleration attenuation curves without a priori assumptions about their shape or scaling properties. The source is composed of patches having uniform size and statistical properties. The primary source parameters are the patch peak-acceleration distribution mean, the distribution standard deviation, the patch size, and patch-rupture duration. Although our model assumes no scaling of peak acceleration with magnitude at the patch, the peak-acceleration attenuation curves, nevertheless, strongly scale with magnitude ( da p /dM ) ≠ 0, and the scaling is distance dependent ( da p /dM ) ∝ f ( r ).

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Bulletin of the Seismological Society of AmericaArticle

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A. M. Rogers, D. M. Perkins. 1996-02-01. Monte Carlo simulation of peak-acceleration attenuation using a finite-fault uniform-patch model including isochrone and extremal characteristics. https://doi.org/10.1785/bssa08601a0079

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