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Figure 11 | SpringerPlus

Figure 11

From: S-wave attenuation in northeastern Sonora, Mexico, near the faults that ruptured during the earthquake of 3 May 1887 Mw 7.5

Figure 11

Comparison of the nonparametric attenuation functions obtained with station OAX (continuous lines) with expected attenuation calculated using equation ( 4) with geometric spreading G ( r )=r-b(dotted lines) and theoretical geometric spreading G(r)=r- 1(dashed lines). The circles are the observed horizontal spectral amplitudes used to obtain the attenuation functions.

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