f Seismic pulse propagation in randomly layered media: kinematic generalisation of the O'Doherty-Anstey result

itted wave can be a useful tool in applied seismics because of several reasons: • In forward modelling problems the transmitted signal can be computed very fast . • In inverse problems some overall quantities like the correlation length can be evaluated easily. In the case of large layered structures, where the typical size of a single lager is beyond resolution, the processing algorithms can be improved .