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Abstract

Most of the seismic data recorded in the field are P-wave reflection data for waves travelling very close to vertical. Therefore, it is assumed that these waves will not be affected by lateral variation of earth's subsurface i.e.,transverse isotropy.

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/content/papers/10.3997/2214-4609.201408787
1996-06-04
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408787
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