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Azimuthal Anisotropy Resolved By Tilted Orthorhombic Tomography
2018
First EAGE/PESGB Workshop on Velocities
unpublished
This paper explains a qualitative and quantitative approach to identify and resolve P wave TTI and HTI variations in the depth migration velocity model building process. The combination of these effects can be represented by an orthorhombic model with three mutually orthogonal planes of mirror symmetry; the P-waves in each symmetry plane can be described kinematically as an independent TI model (Song and Alkhalifah, 2013). Orthorhombic velocity model building and imaging tools are required to
doi:10.3997/2214-4609.201800002
fatcat:3tx2qb2effap5mfxmtphvl6dja