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- W2015948680 abstract "Observational data on the attenuation of short-period Rayleigh waves in North America east of the Rocky Mountains yield the following average values for the coefficient of anelastic attenuation: γ = 0.07 deg−1 for 1-sec-period waves and γ = 0.10 deg−1 for waves with a maximum particle velocity in the period range 3–12 sec. By way of comparison, the amplitude data that form the basis of Richter's empirical local magnitude scale for southern California give γ = 0.60 deg−1. Differences in γ values are sufficient to explain the observation that earthquakes in the eastern United States have a radius of perceptibility as much as 10 times larger than that of earthquakes of the same magnitude in the western United States. Theoretical curves of log A/T versus log Δ are not linear. Thus magnitude formulas of the type M = B + C (log Δ) + log A/T are valid only over a limited range of distance, for which the curve can be approximated by a straight line. Formulas of this kind, which give mb and Ms from short-period Rayleigh waves, are proposed for eastern North America." @default.
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- W2015948680 date "1973-02-10" @default.
- W2015948680 modified "2023-10-14" @default.
- W2015948680 title "Seismic wave attenuation and magnitude relations for eastern North America" @default.
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- W2015948680 doi "https://doi.org/10.1029/jb078i005p00876" @default.
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