1887

Abstract

From the P-wave traveltime measurements over a spherical shale sample at 40 MPa we find the symmetry axis. We transform the ray velocities from the measurement coordinate system to the symmetry axis coordinate system. Assuming transverse isotropy symmetry

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/content/papers/10.3997/2214-4609.201400117
2009-06-08
2021-12-09
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201400117
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