Abstract One of the benefits of dual-sensor (hydrophone and geophone) recordings in ocean bottom cable (OBC) experiments is that hydrophone data and geophone data can be combined to attenuate receiver-side reverberations in both data types or combined to split geophone data into upgoing P-and S-waves, albeit after applying appropriate scaling filters. Most of the formulae currently used to compute these scaling filters assume, sometimes implicitly, that the sea floor is horizontally flat. We present a generalization of these formulae to cases where the sea floor is arbitrarily heterogeneous. Heterogeneities can be due to the topography of the sea floor as well as laterally varying medium parameters along the sea floor. The novelty here is that our derivations are based on the elastodynamic representation theorem instead of plane wave decomposition. For the particular case where the medium parameters are constant along the receiver spread at a dipping sea floor, the resulting scaling filters are explicit and identical to those obtained by plane wave decomposition analysis. The results of our formulation can be used either for multiple attenuation or P/S splitting or both.
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