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Abstract

Several methods for processing hydrophone and geophone ocean-bottom acquisitions have been proposed in recent years. The aim of this paper is to examine the way in which these methods address the peg-leg attenuation problem, and compare with streamer data peg-leg attenuation methods. The main conclusion is that the peg-leg attenuation problem is basically the same for ocean-bottom as for streamer acquisitions, and that we should take advantage of our experience in peg-leg attenuation of streamer data far ocean-bottom processing.

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/content/papers/10.3997/2214-4609.201408175
1998-06-08
2024-11-04
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/content/papers/10.3997/2214-4609.201408175
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