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Abstract

Seismic wave propagation in random media yields complex wavefield fluctuations and apparent attenuation by scattering. Both can be observed and analyzed in VSPs and cross-hole data .

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/content/papers/10.3997/2214-4609.201410424
1992-06-01
2024-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410424
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