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In a fine layered media of cyclic sedimentation,
the first arrival is attenuated very quickly
due to the transmission loss. As a result, the seismic
information is
carried by the short path multiples(O'Doherty and Anstey, 1971).
In this note, I studied the average effect of many thin isotropic layers by
simulating the impulse response in one dimensional random sequences of
two states.
Stanford Exploration Project
11/17/1997