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3-D results

To apply RIP to 3-D data, we chose to change our migration operator from downward-continuation migration to common azimuth migration Biondi and Palacharla (1996). This helps to keep our computational needs relatively low for a 3-D imaging problem. It also means that we will only be handling the inline offsets, so geophysical RIP will only be acting along the inline offset ray parameter.