1887

Abstract

Simple equations relating time lapse changes in seabed diffraction hyperbolas to changes in water layer velocity ant thickness are derived. We find that this method is more robust than using seabed reflection data for the same purpose. We point at two mai

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/content/papers/10.3997/2214-4609.201400423
2009-06-08
2021-11-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400423
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