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Abstract

Reflection tomography produces reliable macro-models in depth for the velocity field of seismic waves and other geophysical properties, when complex 3-D structures are present. The well-known inversion ambiguities due to the null space can be avoided by fitting the grid to the distribution of the available ray paths.

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/content/papers/10.3997/2214-4609.201406860
1996-10-27
2021-06-13
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201406860
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