The migration of the multiples model is the data-domain, returning the multiple model that has to be artifact image we are looking for. For the case of internal subtracted from the original data. Here, we propose a multiple prediction the process is almost the same except method for estimating both surface-related and interbed for the first de-migration step: the data has to be multiple artifacts in the post-stack migrated domain, using reconstructed on an acquisition geometry with both sources as input the migrated section and the subsurface velocity and receivers at the depth of the interpreted horizon model. The proposed technique relies on the use of seismic involved in the interbed events generation; the application de-migration, it is faster than the conventional multiples of SRME and the further migration of the predicted events prediction methods, independent from the original returns the internal multiple artifacts in the image space.