Short Note Common-azimuth migration and Kirchhoff migration for 3-D prestack imaging: A comparison on North Sea data
نویسندگان
چکیده
Common-azimuth migration (CAM) is a 3-D prestack depth migration technique based on the wave equation (Biondi and Palacharla, 1996). It exploits the intrinsic narrow-azimuth nature of marine data to reduce its dimensionality and thus manages to cut the computational cost of 3-D imaging significantly enough to compete with Kirchhoff methods. Based on a recursive extrapolation of the recorded wavefield, CAM is potentially better able to handle multi-pathing problems induced by complex velocity structures.
منابع مشابه
3-D wave-equation imaging of a North Sea dataset: common-azimuth migration + residual migration
3-D prestack common-azimuth depth migration (CAM) has strong potential for accurately imaging complex media and correctly handling multi-pathing. Here, we apply the technique to a North Sea dataset recorded over a salt dome region. The results obtained demonstrate the suitability of the method for complex media, and illustrate important differences with Kirchhoff methods. A detailed analysis of...
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3-D prestack common-azimuth depth migration has strong potential for accurately imaging complex media and correctly handling multi-pathing. Here, we apply the technique to a North Sea real data containing a salt dome. The results obtained demonstrate the suitability of the method for complex media. A detailed analysis of associated angle-domain common-image gathers shows opportunities for impro...
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3-D prestack common-azimuth depth migration has a strong potential for imaging accurately complex media and handling multi-pathing. We apply the technique to North Sea real data for imaging a salt dome. The results obtained demonstrate the efficiency of the method in complex media. A detailed analysis of common-image gathers shows opportunities for improving the velocity model.
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Common-azimuth migration (CAM) is an attractive solution for 3-D prestack imaging. It reduces the full 5-D phase-shift operator to 4-D through the stationary-phase approximation, lowering the computational cost. However, this assumption yields constraints in the downward-continuation process that can limit accuracy. Those errors are estimated in this paper by comparison to other wave-equation m...
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