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Abstract

Traditional ray tracing methods for seismic modelling become prohibitively difficult to implement for complex media, and are inappropriate for models where sub-wavelength scatterers domïnate the seismic response.

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/content/papers/10.3997/2214-4609.201408291
1998-06-08
2024-11-11
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/content/papers/10.3997/2214-4609.201408291
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