This paper is in Portuguese. Reverse Time Migration is an in-depth migration method that implements a solution of the full wave equation. The methodology of work is developed from the application of RTM pre-stacked to synthetic and real data. The components of RTM are presented and analysed modelling the acoustic wave, contour conditions and image condition. For wave modeling, a high order Finite Differences (DF) method was implemented in the space-time domain, based on an alternating grid scheme. In the extrapolation process an adaptive space operator of variable length was applied in the calculation of the spatial derivatives to reduce the computational cost effectively, with little reduction in the accuracy of the numerical solution. A hybrid ABC boundary condition was established that combines two of the most common solutions to the problem of boundary conditions: the predictive method and the attenuation method. RTM images were obtained from a Cross-Correlated Image Condition with Field Separation. The algorithm was applied to synthetic data obtained from the modeling of a complex geological structure, having control of the velocity model. On real data, an image of a complex structure was obtained that allowed to know the real location of the reflection events. The obtained seismic image presents better seismic events in comparison to the conventional methods of migration.