The AVO analysis is based in variation of amplitude of waves with offset, due mainly to elastic properties of rocks. The variables characterizing the elastic behavior ofrocks, licke velocity of s-waves and attenuation, can be estimated by AVO analysis. This can be considered cheap in case ofland acquisition and possible in case of maxime acquisition. This paper describes a different methodology to use AVO, analyzing the relative change ofthe amplitude use with frequency between two reflectors, recovering the last energy of wave due transmission are conversion of wares affected by the angle of incidence. The method was applica to synthetic data of models with homogeneus and isotropic layers separated by plan-paralled interfaces, models associated to maxime depositation environment with low tectonic activity, with stratigraphic features as seen in wt plans in Colombia.