1887

Abstract

This paper studies the azimuthal anisotropy of PS-converted waves recorded in the horizontal radial and transverse components in HTI media. Due to converted wave splitting, the horizontal radial and transverse components contain two types of converted wave: the fast P-SV1 and the slow P-SV2 that propagate along the directions parallel and perpendicular to the fracture strike, respectively. The NMO velocity variations of both the P-SV1 and P-SV2 waves are close to two different ellipses. Therefore it is necessary to analyse and compensate individually for the azimuthal anisotropy of each of the P-SV1 and P-SV2 waves. By applying two NMO-velocity ellipses to the synthetic and field data, the NMO correction results are improved.

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/content/papers/10.3997/2214-4609.20148522
2012-06-04
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20148522
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