TY - GEN
T1 - Globally optimized finite-difference extrapolator for strongly VTI media
AU - Zhang, Jin Hai
AU - Yao, Zhen Xing
N1 - Publisher Copyright:
© 2012 SEG.
PY - 2012
Y1 - 2012
N2 - The finite-difference (FD) migration is unconditionally stable and is popular in handling strong velocity variations, but its extension to strongly VTI media is difficult. Traditional local optimizations generate the optimized coefficients for each pair of Thomsen anisotropy parameters independently, which can degrade results substantially for large anisotropy variations and lead to a huge table. In this paper, we obtain an implicit FD method using the analytic Taylor-series expansion and present a global optimization scheme to improve its accuracy for wide phase angles. Compared with traditional local optimization, our scheme does not need any table and table lookup. For each order of the FD method, only one group of optimized coefficients is enough to handle strong variations in both velocity and anisotropy. More importantly, our global optimization scheme guarantees the accuracy for various possible ranges of anisotropy parameters, no matter how strong the anisotropy is. For the globally optimized 2nd-order FD method, the accurate phase angle is up to 58° and the increase is about 18°~22°. For the 4th-order FD method, the accurate phase angle is up to 77° and the increase is about 22°~27°.
AB - The finite-difference (FD) migration is unconditionally stable and is popular in handling strong velocity variations, but its extension to strongly VTI media is difficult. Traditional local optimizations generate the optimized coefficients for each pair of Thomsen anisotropy parameters independently, which can degrade results substantially for large anisotropy variations and lead to a huge table. In this paper, we obtain an implicit FD method using the analytic Taylor-series expansion and present a global optimization scheme to improve its accuracy for wide phase angles. Compared with traditional local optimization, our scheme does not need any table and table lookup. For each order of the FD method, only one group of optimized coefficients is enough to handle strong variations in both velocity and anisotropy. More importantly, our global optimization scheme guarantees the accuracy for various possible ranges of anisotropy parameters, no matter how strong the anisotropy is. For the globally optimized 2nd-order FD method, the accurate phase angle is up to 58° and the increase is about 18°~22°. For the 4th-order FD method, the accurate phase angle is up to 77° and the increase is about 22°~27°.
UR - https://www.scopus.com/pages/publications/85059176767
U2 - 10.1190/segam2012-0315.1
DO - 10.1190/segam2012-0315.1
M3 - 会议稿件
AN - SCOPUS:85059176767
SN - 9781622769452
T3 - Society of Exploration Geophysicists International Exposition and 82nd Annual Meeting 2012, SEG 2012
SP - 261
EP - 266
BT - Society of Exploration Geophysicists International Exposition and 82nd Annual Meeting 2012, SEG 2012
PB - Society of Exploration Geophysicists
T2 - Society of Exploration Geophysicists International Exposition and 82nd Annual Meeting 2012, SEG 2012
Y2 - 4 November 2012 through 9 November 2012
ER -