Seismic Wave Propagation and Scattering in the Heterogeneous Earth

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Constraints on the shallow elastic and anelastic structure of Mars from InSight seismic data (2020, background): “Indeed, the scattering pattern is strongly frequency dependent and tends to become isotropic as the frequency decreases (Sato et al., 2012).”
Seismic Wave Propagation and Scattering in the Heterogeneous Earth : Second Edition (2012, background): “As summarized well in a recent book by Sato and Fehler (1998), the acceptance of coda waves in the data set is needed for the acceptance of small-scale seismic heterogeneity of the lithosphere.”
Frequency‐Bessel Transform Method for Effective Imaging of Higher‐Mode Rayleigh Dispersion Curves From Ambient Seismic Noise Data (2019, background): “According to previous studies (e.g., Sanchezsesma & Campillo, 2006; Sato et al., 2012), the Fourier transform of the CCF of ambient seismic noise data between two points is approximate to the imaginary part of Green's function between these points, that is, C̃(r, 𝜔) ≈ A · Im { G̃zz(r, z = 0, ;𝜔)…”
Depth sensitivity of seismic coda waves to velocity perturbations in an elastic heterogeneous medium (2013, background): “We know that regions that show tectonic and/or volcanic activity are highly heterogeneous (Abubakirov et al. 1990; Aki et al. 1975, 2000; Sato and Fehler 1998).”