Imaging tilted transversely isotropic media with a generalised screen propagator
Autor: | Sung Il Shin, Soon Jee Seol, Joongmoo Byun |
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Rok vydání: | 2015 |
Předmět: |
Physics
010504 meteorology & atmospheric sciences Wave propagation business.industry Seismic migration Propagator Geology Geometry 010502 geochemistry & geophysics Wave equation 01 natural sciences symbols.namesake Geophysics Optics Transverse isotropy Taylor series symbols Anisotropy business Slowness 0105 earth and related environmental sciences |
Zdroj: | Exploration Geophysics. 46:349-358 |
ISSN: | 1834-7533 0812-3985 |
DOI: | 10.1071/eg14113 |
Popis: | One-way wave equation migration is computationally efficient compared with reverse time migration, and it provides a better subsurface image than ray-based migration algorithms when imaging complex structures. Among many one-way wave-based migration algorithms, we adopted the generalised screen propagator (GSP) to build the migration algorithm. When the wavefield propagates through the large velocity variation in lateral or steeply dipping structures, GSP increases the accuracy of the wavefield in wide angle by adopting higher-order terms induced from expansion of the vertical slowness in Taylor series with each perturbation term. To apply the migration algorithm to a more realistic geological structure, we considered tilted transversely isotropic (TTI) media. The new GSP, which contains the tilting angle as a symmetric axis of the anisotropic media, was derived by modifying the GSP designed for vertical transversely isotropic (VTI) media. To verify the developed TTI-GSP, we analysed the accuracy of wave propagation, especially for the new perturbation parameters and the tilting angle; the results clearly showed that the perturbation term of the tilting angle in TTI media has considerable effects on proper propagation. In addition, through numerical tests, we demonstrated that the developed TTI-GS migration algorithm could successfully image a steeply dipping salt flank with high velocity variation around anisotropic layers. |
Databáze: | OpenAIRE |
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