1887

Abstract

We show that seismic waves travelling in the subsurface are subject to two physically different processes, namely propagation inside smoothly inhomogeneous layers and reflection and transmission at internal reflectors. We propose a new approach to modelin

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/content/papers/10.3997/2214-4609.201400098
2009-06-08
2020-08-06
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400098
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