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Pure quasi-P wave equation and numerical solution in 3D TTI media

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Abstract

Based on the pure quasi-P wave equation in transverse isotropic media with a vertical symmetry axis (VTI media), a quasi-P wave equation is obtained in transverse isotropic media with a tilted symmetry axis (TTI media). This is achieved using projection transformation, which rotates the direction vector in the coordinate system of observation toward the direction vector for the coordinate system in which the z-component is parallel to the symmetry axis of the TTI media. The equation has a simple form, is easily calculated, is not influenced by the pseudo-shear wave, and can be calculated reliably when δ is greater than ε. The finite difference method is used to solve the equation. In addition, a perfectly matched layer (PML) absorbing boundary condition is obtained for the equation. Theoretical analysis and numerical simulation results with forward modeling prove that the equation can accurately simulate a quasi-P wave in TTI medium.

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Acknowledgments

We gratefully acknowledge all reviewers for their constructive comments and suggestions, and express our thanks also to AGED for their patience and tolerance.

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Correspondence to Bing-Shou He.

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This work is supported by the National Natural Science Foundation of China (No. 41674118), the national science and technology major project (No. 2016ZX05027-002).

Zhang Jian-Min is a graduate student of geophysical prospecting at the Ocean University of China. Her research interests are seismic wave theory, forward modeling, and reverse-time migration imaging.

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Zhang, JM., He, BS. & Tang, HG. Pure quasi-P wave equation and numerical solution in 3D TTI media. Appl. Geophys. 14, 125–132 (2017). https://doi.org/10.1007/s11770-017-0613-1

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  • DOI: https://doi.org/10.1007/s11770-017-0613-1

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