1887

Abstract

A layer replacement method for estimating and correcting seismic data for the variation in the velocity of sound in water not only overcomes some of the difficulties of a conventional method, it produces estimates of absolute rather than relative water ve

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/content/papers/10.3997/2214-4609.201400384
2009-06-08
2021-12-05
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400384
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