Efecto de la rugosidad del terreno en las secciones sísmicas: modelamiento por elementos finitos.

The foothills areas are characterized by low velocity shallow layers and rugged topopgraphy. Inside these stratas a coherent noise named back scattering is produced, that noise overlaps the waves comming from the deeper reflectors. In seismic sections of the colombian foothills this signal is observed, obscuring the subsurface image. A method to attenuate this signal is presented in this paper, the approach is based in the prediction of this noise and the posterior remotion from the seismic records. The shallow layer response is simulated through the numerical modeling in finite elements of the acustic wave propagation in a subsurface model. Lately, the shallow layer response is subtracted trace by trace from the synthetic record, getting a high noise's attenuation in the shot. We present results obtained by synthetic data modeling. [ABSTRACT FROM AUTHOR]