Titlebook: Digital Seismology and Fine Modeling of the Lithosphere; R. Cassinis,G. Nolet,G. F. Panza Book 1989 Springer Science+Business Media New Yo

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https://doi.org/10.1007/978-3-642-14840-8ing slabs can lead to compositional variations and to seismic velocities up to 10 percent higher than the surrounding mantle. These major sources of heterogeneity are known to have significant effects on the travel times and ray trajectories of waves travelling within them (e.g., Sleep, 1973; Davies

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Spencer G. Lucas,Lawrence H. Tannerpic, causal relaxation function . .(., .). Then, the wave equation operator is not necessarily symmetric (‘self-adjoint’), but the reciprocity property is still satisfied. The representation theorem contains a term proportional to the history of strain. The dual problem consists in solving the wave

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