Comparison of ray-matrix and finite-difference methods in a simple 1-D velocity model /

The ray-matrix method can extend the applicability of ray methods to 3-D heterogeneous velocity models containing thin stacks of fine isotropic or anisotropic layers. Ray-matrix synthetic seismograms are compared with finite-difference synthetic seismograms in a simple 1-D velocity model, consisting...

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Document type: Article
Language: English
ISSN: 0039-3169
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Online Access: Plný text

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