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Abstract

Seismic anisotropy is widespread in sedimentary basins. Vertical transverse isotropy associated with shale deposition and horizontal layering may give errors in "seismic depth", as well as reduced stack power and mispositioning of dipping events.

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/content/papers/10.3997/2214-4609.201408272
1998-06-08
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408272
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