Processamento de dados GPR registrados na Lagoa do Abaeté pelo método de empilhamento CRS

The Common Reflection Surface (CRS) stack method is suite to simulate a zero-offset section with high quality and high signal-to-noise ratio from multi-coverage reflection seismic data. This seismic imaging method is fully automatic and it may be applied to irregular geometry data. We present the first results of the application of the Common Reflection Surface (CRS) method based on global optimization to simulate a zero offset stacked section from multi-coverage Ground Penetrating Radar (GPR) real data. We lso present a comparison of the results of the CRS processing with the conventional NMO processing. The results show that the CRS processing provided a zero-offset stacked section with better resolution.