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Abstract

The proposed migration procedure is performed in the double Radon transfonned frequency domain. The main advantages of the procedure are that it does not require a detailed input velocity model, does not need decomposition to up- and downgoing waves, and does not assume laterally invariant geology.

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/content/papers/10.3997/2214-4609.201411040
1991-05-28
2024-04-25

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