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Clearly, the methodology described in this paper is only weakly supported
by the simple 2-D example presented here. The challenge lies in the
implementation of the non-linear inversion process capable of computing the
optimum source and receiver positions given all the geophysical, logistical
and financial constraints for 3-D data.
The sensitivity of the acquisition geometry to the accuracy of the initial
structural and velocity model is also clearly an important issue to be
analyzed in detail. Extensive research will have to be done before clear
guidelines can be established in that respect.
Next: Curry: : REFERENCESMulti-scale PEFs
Up: Prucha and Biondi: STANFORD
Previous: Summary and conclusions
Stanford Exploration Project
6/7/2002