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A standard imaging method in seismic data processing is the simulation of a zero offset section from seismic reflection data. In traditional imaging methods, e. g. NMO/DMO/stack, an accurate macro velocity model is needed. Common reflection surface (CRS) stack is a new data driven method, introduced in recent years which remove the necessity of making this model and just use the surface velocity to simulate zero offset section (2D) or volume (3D). In this article, we drive the CRS stacking on a synthetic data to o...