Um novo algorítimo para implementação do método de empilhamento SRC 3-D e modelagem sísmica da Bacia do Amazonas

Abstract

The Common Reflection Surface Stack (CRS) is a seismic reflection imaging technique that is independent of velocity model to simulate Zero-Offset (ZO) seismic section or volume. This technique have been used, alternatively, in seismic reflection processing and many works have been demonstrate that the CRS method shows results with better signal to noise rate and lateral resolution in comparison with conventional methods, e. g., NMO/DMO stack. The CRS stack provides some attributes or wavefield parameters that could be used in many applications, e.g., velocity models estimation, AVO and AVA analysis, geometric spread factor estimation, projected Fresnel zone, and others. The CRS technique has a second order hyperbolic traveltimes approximation in central ray vicinity. In the 3-D case, for a normal central ray or ZO, the CRS operator depends on eight parameters, estimating by coherency analysis from seismic data. In this work, the 3-D ZO CRS operator is analyzed for both reflection and diffraction events with respect the traveltimes obtained from straight modeling. I present a new CRS stack algorithm to simulate ZO sections or volume. I still present, in this work, a 3-D seismic modeling of the sedimentary Amazon Basin with SW3D consortium packages. The geologic model was based in true geologic and geophysics data.