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Power spectra of random heterogeneities in the solid earth

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Figure

Figure 1. (a) Log–log plot of PSDF vs. wavenumber m in 3-D space (von Kármán type, κ = 0.1, 0.5, and 1; Henyey–Greenstein type, HG,κ = 0; Gaussian type, G)
Figure 2a shows estimated 1-D PSDFs, where the wavenum-ber range is on the order of 1 mm−1
Figure 2. (a) 1-D PSDF vs. wavenumber for rock samples and acoustic well logs. (b) Converted 3-D PSDF vs
Figure 3. 3-D PSDF vs. wavenumber for (a) the lithosphere (the crust and uppermost mantle), (b) strong heterogeneities and array dataanalyses in the lithosphere
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