Acoustic VTI modeling and pre-stack reverse-time migration based on the time–space domain staggered-grid finite-difference method
Reverse-time migration (RTM) is based on seismic numerical modeling algorithms, and the accuracy and efficiency of RTM strongly depend on the algorithm used for numerical solution of wave equations. Finite-difference (FD) methods have been widely used to solve the wave equation in seismic numerical...
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| Published in | Journal of applied geophysics Vol. 90; pp. 41 - 52 |
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| Main Authors | , |
| Format | Journal Article |
| Language | English |
| Published |
Elsevier B.V
01.03.2013
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| Subjects | |
| Online Access | Get full text |
| ISSN | 0926-9851 1879-1859 |
| DOI | 10.1016/j.jappgeo.2012.12.008 |
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| Abstract | Reverse-time migration (RTM) is based on seismic numerical modeling algorithms, and the accuracy and efficiency of RTM strongly depend on the algorithm used for numerical solution of wave equations. Finite-difference (FD) methods have been widely used to solve the wave equation in seismic numerical modeling and RTM. In this paper, we derive a series of time–space domain staggered-grid FD coefficients for acoustic vertical transversely isotropic (VTI) equations, and adopt these difference coefficients to solve the equations, then analyze the numerical dispersion and stability, and compare the time–space domain staggered-grid FD method with the conventional method. The numerical analysis results demonstrate that the time–space domain staggered-grid FD method has greater accuracy and better stability than the conventional method under the same discretizations. Moreover, we implement the pre-stack acoustic VTI RTM by the conventional and time–space domain high-order staggered-grid FD methods, respectively. The migration results reveal that the time–space domain staggered-grid FD method can provide clearer and more accurate image with little influence on computational efficiency, and the new FD method can adopt a larger time step to reduce the computation time and preserve the imaging accuracy as well in RTM. Meanwhile, when considering the anisotropy in RTM for the VTI model, the imaging quality of the acoustic VTI RTM is better than that of the acoustic isotropic RTM.
► Deriving staggered-grid FD coefficients with time-space domain dispersion relation. ► Acoustic VTI modeling and RTM with the time-space domain staggered-grid FD method. ► Obtaining high-precision numerical modeling and accurate imaging. |
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| AbstractList | Reverse-time migration (RTM) is based on seismic numerical modeling algorithms, and the accuracy and efficiency of RTM strongly depend on the algorithm used for numerical solution of wave equations. Finite-difference (FD) methods have been widely used to solve the wave equation in seismic numerical modeling and RTM. In this paper, we derive a series of time–space domain staggered-grid FD coefficients for acoustic vertical transversely isotropic (VTI) equations, and adopt these difference coefficients to solve the equations, then analyze the numerical dispersion and stability, and compare the time–space domain staggered-grid FD method with the conventional method. The numerical analysis results demonstrate that the time–space domain staggered-grid FD method has greater accuracy and better stability than the conventional method under the same discretizations. Moreover, we implement the pre-stack acoustic VTI RTM by the conventional and time–space domain high-order staggered-grid FD methods, respectively. The migration results reveal that the time–space domain staggered-grid FD method can provide clearer and more accurate image with little influence on computational efficiency, and the new FD method can adopt a larger time step to reduce the computation time and preserve the imaging accuracy as well in RTM. Meanwhile, when considering the anisotropy in RTM for the VTI model, the imaging quality of the acoustic VTI RTM is better than that of the acoustic isotropic RTM.
► Deriving staggered-grid FD coefficients with time-space domain dispersion relation. ► Acoustic VTI modeling and RTM with the time-space domain staggered-grid FD method. ► Obtaining high-precision numerical modeling and accurate imaging. |
| Author | Yan, Hongyong Liu, Yang |
| Author_xml | – sequence: 1 givenname: Hongyong surname: Yan fullname: Yan, Hongyong email: yanhongyong@163.com – sequence: 2 givenname: Yang surname: Liu fullname: Liu, Yang |
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| CitedBy_id | crossref_primary_10_1088_1742_2132_12_1_108 crossref_primary_10_1016_j_soildyn_2014_10_009 crossref_primary_10_1071_EG17018 crossref_primary_10_1007_s11770_014_0463_z crossref_primary_10_1142_S0218396X16500168 crossref_primary_10_1093_gji_ggu024 crossref_primary_10_1111_1755_6724_14895 crossref_primary_10_1016_j_jappgeo_2021_104447 crossref_primary_10_1016_j_jappgeo_2024_105352 crossref_primary_10_1071_EG17088 crossref_primary_10_4028_www_scientific_net_AMM_518_220 crossref_primary_10_1016_j_jappgeo_2020_104058 |
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| Keywords | Vertical transversely isotropic (VTI) Time–space domain Staggered-grid Reverse-time migration (RTM) Finite-difference (FD) |
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| Snippet | Reverse-time migration (RTM) is based on seismic numerical modeling algorithms, and the accuracy and efficiency of RTM strongly depend on the algorithm used... |
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| SubjectTerms | Finite-difference (FD) Reverse-time migration (RTM) Staggered-grid Time–space domain Vertical transversely isotropic (VTI) |
| Title | Acoustic VTI modeling and pre-stack reverse-time migration based on the time–space domain staggered-grid finite-difference method |
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