1887

Abstract

The coherent noise in seismic data consists mainly of surface waves propagating in the near surface from sources to receivers. The type and properties of surface waves depend on the elastic properties of the shallow subsurface, whose lateral variations an

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/content/papers/10.3997/2214-4609.201400330
2009-06-08
2021-10-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400330
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