1887

Abstract

Seismic data moveout on a full azimuth land 3D dataset revealed strong spatially variant azimuthal anisotropy. It was interpreted as a result of short-wavelength heterogeneity and true azimuthal anisotropy for the interval velocity. Iterative depth-velo

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/content/papers/10.3997/2214-4609.201400150
2009-06-08
2021-12-04
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400150
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