ABSTRACT
Estimation of elastic specular reflectivity from seismic reflection data
is important in that it may provide crucial information about
subsurface physical
properties related to lithology, rock physics, pore-fluid content, and
physical states. I derive a generalized least-squares solution for
elastic reflectivity in terms of local seismic wavefield displacement vectors.
Solutions for the local wavefields are derived as representation integrals
over surface source and receiver displacement fields, weighted by a
WKBJ approximate Green's tensor. The resulting integral solution is a
vector analogy of the Kirchhoff-Rayleigh-Sommerfeld integrals for scalar waves.
In particular, I give explicit formulas for the least-squares evaluation of the
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