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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