1887

Abstract

OBC data is usually processed assuming normal incidence and ignoring angular variations in the geophone response, water bottom reflectivity and reverberation period. A z-p domain decomposition allows the angular variations within the data to be separated and handled. An approach to handling the ghost attenuation is described

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/content/papers/10.3997/2214-4609.201408120
1998-06-08
2021-06-14
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408120
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