Water bottom multiple


Water-bottom multiples are those multiples whose raypaths lie entirely within the water layer (Figure 6a). Since the sea floor usually has a higher reflectivity than.

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Multiples from the water bottom (the interface of the base of water and the rock or sediment beneath it) and the air-water interface are common in marine seismic.

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Description:This underscores the need for their removal. These approaches include the linear, slant-stack or tau-P, hyperbolic and parabolic Radon transform. This is particularly true, on hard water-bottom areas where sediments are compacted and well consolidated. Multiples give rise to false seismic events and if they are not eliminated in processing, they can make interpretations of the final processed seismic sections difficult and give false results. The time difference between the primary and its first multiple is, every where, equal to the time through the water layer. Import into RefWorks 1. In essence, the data are summed along a series of parabolas in the frequency-space domain; whereas, the primaries map to the zero residual moveout while multiples map to the positive residual moveout zone.

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