An Inversion Method for Elastic Wave Fields , by Robert W. Clayton

The inversion of two-demensional elastic displacement fields can be handled in a very similar manner to the way the acoustic problem is handled. The Born approximation of the Lippman-Schwinger equation yields a simple relationship in the Fourier-transform domain between the observed horizontal and vertical displacement fields, and the scattering potential. Basically, the observaticons are a liner combination of the scattering potential evaluated along four different shells. The four shells may be interpreted P to P, P to S, S to P, and S to S scattering. If the source is either purely compressional or purely shear, then one experiment will suffice to invert the forward equation. If the source is a (known) mixture of P and S components, then twon experiments with different combinations of P and S components are necessary for the inversion.


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