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The inverse problem
Laterally heterogeneous models
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amplitude anelastic application associated assumed asymptotic attenuation average band body boundary layer calculations complex consider constant convection core corresponding crust defined density dependence depth determined diffusion discussed displacement distribution Earth earthquake effect eigenfrequencies elastic energy equation estimates example fault field flow fluid force frequency function Geophys given heat heat flow important increase integral inverse J. R. Astron lateral linear lithosphere lower mantle material mean measured mechanism method modes motion multiplet observed obtained oceanic parameters perturbation phase plane plate possible present pressure problem propagation properties reference region relation relative relaxation represents response scale seismic shear shown solid solution spectrum spherical stress structure surface temperature theory thermal thickness upper vector velocity viscosity wave