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相射线Maslov求和法:一个完全的有限频率射线法 被引量:2

Phase-ray Maslov summation:a complete finite-frequency ray method.
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摘要 现有的有限频率射线方法,包括Maslov射线求和法和相射线法,只能部分地模拟菲涅耳干涉和介质非均匀性散射这两个影响有限频率波在非均匀介质传播的基本物理过程。为克服这些局限性,提出了一种新的有限频率射线方法。该方法融合了Maslov射线求和法和相射线法两者的长处,可以同时精确地模拟由菲涅耳干涉及介质非均匀性散射产生的有限频率波动现象,因此是一个完全的有限频率方法。此外,由于精确地描述了波场在焦散区附近由散射引起的波场平滑过程,也从根本上解决了渐近射线理论的奇异性问题。 The existing finite-frequency ray methods,including the Maslov ray summation and phase-ray method,can only partially simulate the basic physical process during which the finite-frequen- cy wave affected by Fresnel interference and medium heterogeneity scattering propagates.Aiming at such limitations of these finite- frequency ray methods,we have proposed a new finite-frequency ray method which combines the advantages of both Maslov ray summation and phase-ray methods.The new method can simulate the finite-frequency wave phenomena arising from both Fresnel in- terference and medium heterogeneity scattering.Hence,it is a complete finite-frequency ray method.Moreover,being able to de- scribe accurately the wave field smoothing process at a caustic due to the scattering,the method satisfactorily eliminates the singulari- ty problem of asymptotic ray theory.
作者 朱天飞
机构地区 CGGVeritas 公司
出处 《石油物探》 EI CSCD 2007年第6期630-632,共3页 Geophysical Prospecting For Petroleum
关键词 有限频率射线方法 相射线法 Maslov射线求和法 菲涅耳干涉 介质非均匀性散射 finite-frequency ray methods phase-ray method Maslov ray summation method Fresnel interference medium heterogeneity scattering
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参考文献5

  • 1Zhu T F, Chun K Y. Understanding finite-frequency wave phenomena: phase-ray formulation and inhomogeneity scattering[J]. Geophysical Journal International, 1994,119(1) : 78-90 被引量:1
  • 2Chapman C H,Drummond R. Body-wave seismograms in inhomogeneous media using Maslov asymptotic theory[J]. Bulletin of Seismological Society of America, 1982,72(6b) :S277-S317 被引量:1
  • 3Cerveny V, Popov M M, Psencik I. Computation of wave fields in inhomogeneous media - Gaussian beam approach[J]. Geophysical Journal of the Royal Astronomical Society, 1982,70(1) : 109-128 被引量:1
  • 4Zhu T F. A ray-Kirchhoff method for body-wave calculations in inhomogeneous media: theory[J]. Geophysical Journal International, 1988,92 (1) : 181-193 被引量:1
  • 5Kendall J M, Thomson C J. Maslov ray summation, pseudo-caustics, Lagrangian equivalence and transient seismic waveforms[J]. Geophysical Journal International,1993,113(1):186-214 被引量:1

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  • 1王华忠,方正茂,匡斌,马在田.任意介质中的动态规划法地震波三维走时计算[J].地球物理学报,2001,44(z1):179-189. 被引量:7
  • 2Bevc D. Flooding the topography:wave equation datuming of land data with rugged acquisition topography[J].Geophysics,1997,(01):1586-1595. 被引量:1
  • 3Raiaskaran S,McMechan G A. Prestack processing of land data with complex topography[J].Geophysics,1995,(06):1875-1886.doi:10.1190/1.1443919. 被引量:1
  • 4Liu S Y,Wang H Z. An effective 3D Kirchhoff PSDM and MVA procedure from rugged topography[A].2011.378. 被引量:1
  • 5Capon J,Goodman N. Probability distributions for estimates of the frequency-wavenumber spectrum[J].Proceedings of the IEEE,1970,(10):1785-1786. 被引量:1
  • 6Ozbek A. Adaptive beamforming with generalized linear constraints[A].2000.2081-2084. 被引量:1
  • 7Wang H Z,Li W B,Zhang Y Q. Beam ray gather stacking for attenuating non-coherent noises and PSTM from rugged topography[A].2007.2635-2639. 被引量:1
  • 8Brandsberg-Dahl S,Etgen J. Beam-wave migration[A].2003.977-980. 被引量:1
  • 9Cerveny V,Hron F. The ray series method and dynamic ray tracing for three dimensional in inhomogeneous media[J].Bulletin of the Seismological Society of America,1980,(01):47-77. 被引量:1
  • 10Cerveny V. Gaussian beam synthetic seismograms[J].Journal of Geophysics,1985,(01):44-72. 被引量:1

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