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Abstract

itted wave can be a useful tool in applied seismics because of several reasons: • In forward modelling problems the transmitted signal can be computed very fast . • In inverse problems some overall quantities like the correlation length can be evaluated easily. In the case of large layered structures, where the typical size of a single lager is beyond resolution, the processing algorithms can be improved .

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/content/papers/10.3997/2214-4609.201410571
1992-06-01
2020-10-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410571
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