1887

Abstract

Cross-dipole acoustic logging is used to measure formation shear-wave anisotropy around the borehole. The phase velocities of the flexural modes are dispersive, and reach the formation fast and slow shear velocities at low frequencies. Their dispersion pr

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/content/papers/10.3997/2214-4609.201400353
2009-06-08
2024-04-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400353
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