Quasi-shear wave ray tracing by wavefront construction in 3-D, anisotropic media |
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| Authors: | Hung-Liang Lai Richard L Gibson Jr Kyoung-Jin Lee |
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| Institution: | aFormerly Texas A&M University, Department of Geology and Geophysics, College Station, Texas; presently Seismic Micro-Technology, Inc., 8584 Katy Freeway, Suite 400, Houston, TX 77024, United States;bDepartment of Geology and Geophysics, Texas A&M University, College Station, TX 77843, United States;cBP America, Inc., 501 Westlake Park Boulevard, Houston, TX 77079, United States |
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| Abstract: | Wavefront construction (WFC) methods provide robust tools for computing ray theoretical traveltimes and amplitudes for multivalued wavefields. They simulate a wavefront propagating through a model using a mesh that is refined adaptively to ensure accuracy as rays diverge during propagation. However, an implementation for quasi-shear (qS) waves in anisotropic media can be very difficult, since the two qS slowness surfaces and wavefronts often intersect at shear-wave singularities. This complicates the task of creating the initial wavefront meshes, as a particular wavefront will be the faster qS-wave in some directions, but slower in others. Analogous problems arise during interpolation as the wavefront propagates, when an existing mesh cell that crosses a singularity on the wavefront is subdivided. Particle motion vectors provide the key information for correctly generating and interpolating wavefront meshes, as they will normally change slowly along a wavefront. Our implementation tests particle motion vectors to ensure correct initialization and propagation of the mesh for the chosen wave type and to confirm that the vectors change gradually along the wavefront. With this approach, the method provides a robust and efficient algorithm for modeling shear-wave propagation in a 3-D, anisotropic medium. We have successfully tested the qS-wave WFC in transversely isotropic models that include line singularities and kiss singularities. Results from a VTI model with a strong vertical gradient in velocity also show the accuracy of the implementation. In addition, we demonstrate that the WFC method can model a wavefront with a triplication caused by intrinsic anisotropy and that its multivalued traveltimes are mapped accurately. Finally, qS-wave synthetic seismograms are validated against an independent, full-waveform solution. |
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| Keywords: | Anisotropy Ray tracing Wavefront construction Quasi-shear wave |
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