1887

Abstract

Variations in water-layer travel time caused by changes in temperature and salinity must be accounted for when processing 3D and 4D seismic surveys in deep water. The current industry “water column statics” solutions are not sufficient when rapid lateral

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/content/papers/10.3997/2214-4609.201400427
2009-06-08
2024-04-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400427
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