1887

Abstract

Seismic images below a seafloor with complex topography are always distorted due to (1) lateral velocity contrast between the water and sediments and (2) lateral velocity variations within shallow sediments caused by the variable water depth. Normally, co

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/content/papers/10.3997/2214-4609.201400372
2009-06-08
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400372
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