1887
Volume 28, Issue 9
  • ISSN: 0263-5046
  • E-ISSN: 1365-2397

Abstract

Edward Jenner, ION Geophysical, expands previous work on how lateral velocity heterogeneity in the overburden could explain apparent azimuthal NMO at a target horizon on field data. Here, modelling studies show, among other things, that lateral variations in anisotropy are well resolved and do not distort the inverted interval anisotropy in deeper target layers if the vertical velocity is laterally homogeneous.

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/content/journals/0.3997/1365-2397.28.9.41393
2010-09-01
2024-04-23
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http://instance.metastore.ingenta.com/content/journals/0.3997/1365-2397.28.9.41393
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  • Article Type: Research Article
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