KAUST DepartmentEarth Science and Engineering Program
Permanent link to this recordhttp://hdl.handle.net/10754/622096
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AbstractNear-surface normal faults can sometimes separate two distinct zones of velocity heterogeneity, where the medium on one side of the fault has a faster velocity than on the other side. Therefore, the slope of surface-wave arrivals in a common-shot gather should abruptly change near the surface projection of the fault. We present ray-map imaging method that migrates transmitted surface waves to the fault plane, and therefore it roughly estimates the orientation, depth, and location of the near-surface fault. The main benefits of this method are that it is computationally inexpensive and robust in the presence of noise.
CitationLi J, Schuster GT (2016) Ray-map migration of transmitted surface waves. Interpretation 4: SQ33–SQ40. Available: http://dx.doi.org/10.1190/INT-2016-0014.1.
SponsorsWe thank the 2016 sponsors of Center for Subsurface Imaging and Fluid Modeling (CSIM) at King Abdullah University of Science and Technology (KAUST) for their support.
PublisherSociety of Exploration Geophysicists