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混合法深度偏移及其吸收边界条件 被引量:9

Hybrid depth migraion and its absorbing boundary condition
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摘要 混合法偏移是一种将有限差分偏移和频率波数域偏移相结合进行偏移的方法,它兼有两者的优点,即既能适应较大横向变速情况,又节省内存和运算量。本文利用平方根算子的最佳逼近,导出了混合法偏移的一种新算法,其运算交替用ω-x域中的有限差分法和f-k是域中的相移法来完成。同时,还提出了一种新的吸收边界条件,它通过在边界外附加一个很薄的具有强吸收作用的边界层,并与衰减型吸收边界条件相结合,有效地消除了边界反射。该方法既适用于规则区域,又适用于不规则区域,其离散方程具有统一形式,易于编程。较多的模型计算和实际资料试算表明,该方法是一种计算量适中、处理精度高、稳定性好、吸收效果明显的偏移方法。 The hybrid migration is a metfor that combines the finite-difference migration with thefrequency-wavenumber migration. It has advantages of these two migration methed simultanansly, i.e., it can not ony handle large lateral velocity variations, but also save computer run time and memories. In the paper a new algorithm for the hybrid migration is derived, which is based on an optimizedapprpaching to the square-root opertor. The migration is completed alternatively with the phare-shiftmethod in f-k doman and the finite-difference mehed in ω-x domain. Also, a new absorbing boundarycondittion is proposed. After adding a thin layer with strong absorbing ability along the boundary, andcombining it with the attenuative absorbing boundary condition, we find that boundary reflections can beavoided effectively. The absorbing condition is suitable to both regular area and irregular area and its discrete equation has a united form and can be programmed easily. The comutations of theoretical modelsand field data show that the depth migration method is stable, accurate and efficient.
出处 《石油物探》 EI CSCD 北大核心 1999年第3期1-7,13,共8页 Geophysical Prospecting For Petroleum
基金 中国博士后科学基金
关键词 混合法 深度偏移 吸收边界条件 地震勘探 hybrid method, depth migration, finite-difference method, phase-shift method, absorbing boundary condition
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参考文献5

  • 1贺振军 王才经 等.反射地震资料偏移处理与反演方法[M].重庆:重庆大学,1989..
  • 2郝现军 张关泉 等.速度横向剧变介质的波场延拓与偏移成像.98'CPS/SEG/EAEG北京国际地球物理研讨会论文摘要[M].,1998.502-504.
  • 3郝现军,’98 CPSA/SEG/EAEG北京国际地球物理研讨会论文摘要,1998年,502页
  • 4贺振华,反射地震资料偏移处理与反演方法,1989年,56页
  • 5Zhang Guanquan,J Comput Math,1985年,3卷,1期,90页

同被引文献37

  • 1李振春,张凯,张建磊,陈士军,王延光.共聚焦点偏移成像方法研究[J].石油物探,2003,42(1):16-21. 被引量:11
  • 2张关泉.波动方程的上行波和下行波的耦合方程组[J].应用数学学报,1993,16(2):251-263. 被引量:46
  • 3张关泉,侯唯健.三维叠后差分偏移的因子分解法[J].地球物理学报,1996,39(3):382-391. 被引量:2
  • 4同济大学海洋地质与地球物理系编.反射地震学论文集[M].上海:同济大学出版社,2000..
  • 5李录明,罗省贤.相移加校正叠前深度偏移及偏移速度分析[J].石油地球物理勘探,1997,32(1):57-67. 被引量:9
  • 6Gazdag J. Wave equation migration with the phase-shift method. Geophysics, 1978, 43(12):1342-1351.
  • 7Stoffa P L, Forkema J T, de Luna Freire B M, et al. Split-step Fourier migration. Geophysics, 1990, 55(4) : 410 - 421.
  • 8Ristow D, Ruhl T. Fourier finite-difference migration. Geophysics,1995, 59(12) : 1882 - 1893.
  • 9Haddow C M. Hybrid migration by finite-difference and phase shift.62th Ann. Internat. Mtg., Soc. Expl. Geophys.. Expanded Abstracts , 1992. 893 - 896.
  • 10Claerbout J F. Multidimensional recursive filters via a helix with application to velocity estimated and 3-D migration. 68th Annual Internat. Mtg. Soc. Expl. Geophys.. Expanded Abstracts, 1998.1995 - 1998.

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