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3-D results

To apply RIP to 3-D data, I chose to change my migration operator from the downward-continuation migration described in Chapter 2 to common azimuth migration (). This helps to keep my computational needs relatively low for a 3-D imaging problem. It also means that I will only be handling the inline offsets, so geophysical RIP will only be acting along the inline offset ray parameter. I have chosen to apply only geophysical RIP on this 3-D problem.