1887

Abstract

Transmission effects in the overburden are important for amplitude-versus-offset studies and for tree-amplitude imaging of seismic data. Thin layers produce transmission effects which depend on frequency and slowness. O'Doherty and Anstey (1971) derived a remarkable formula for the transmission response for a plane wave at normal incidente in a stack of homogeneous layers taking into account the direct pulse and short-period multiples.

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/content/papers/10.3997/2214-4609.201406733
2001-04-30
2020-11-24
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