Titlebook: Scattering and Attenuations of Seismic Waves, Part I; Keiiti Aki,Ru-Shan Wu Book 1988 Springer Basel AG 1988 Manuscript.modeling.numerical

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,Multiple Scattering and Energy Transfer of Seismic Waves—Separation of Scattering Effect from Intritenuation be expressed as an exponential decay form. One is the . case, i.e., when .. ≫ 0.5, where .. = .. /.. + ..) is the seismic albedo, ŋ. is the scattering coefficient, .. is the absorption coefficient. In this case the absorption is dominant, the apparent attenuation . can be approximated by t

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Vector-Scattering of Elastic Waves by Directional Structural Space Gradients,z formalism, opens new ways to calculate the scattered fields due to various structural inhomogeneities applicable to exploration and earthquake seismology. The theoretical results of this study point to the conclusion that the scalar wave approximation may not always be valid for the propagation of

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Seismic Energy Partitioning and Scattering in Laterally Heterogeneous Ocean Crust,eous models..‘Random’ incoherent secondary scattering generally increases as . (wavenumber, ., and correlation length, .) approaches one. Deterministic secondary scattering from larger heterogeneities is the dominant effect in the models as . increases above one. Secondary scattering also shows up a

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Observations of Teleseismic , Wave Coda for Underground Explosions,ucca Flat events. This may result from systematic variations between the spectra of direct signals and coda arrivals caused by . interference for the largest events, all of which were detonated at Pahute Mesa. Another possible explanation is a frequency-dependent propagation effect on the direct sig

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Spatial Variation of Crustal Coda , in California,way between (.. = 900). These are extremely large variations compared to measures of seismic velocities of comparable resolution, demonstrating the exceptional sensitivity of the high frequency coda . measurement to regional geology. In addition, the frequency trend of the results is opposite to tha