期刊文献+

能量约束下的高斯射线束法地震波场正演 被引量:11

Seismic wave field modeling by energy controlled Gaussian beam method
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摘要 高斯射线束法同时考虑波的运动学和动力学特征,并且无需两点试射追踪,因此运算速度快、精度较高。Zoeppritz方程反映了地层界面上反射波和透射波的能量。本文将高斯射线束正演与Zoeppritz方程联系起来,将高斯射线束正演得到的波场记录赋予能量信息,并利用模型对波动方程、常规射线法和本文方法的计算精度和效率进行了对比,验证了本文方法的可行性和有效性。 Gaussian beam method is an improvement of the traditional ray tracing method in seismic modeling.It simultaneously involves characteristics of both kinematics and dynamics without the trial ray tracing between two points.So it is more efficient and accuracy.However,its energy of wave field is not enough compared with wave equation methods.Zoeppritz's equations can give the conversion information and decide energy distribution about P-and S-waves when reflection and transmission occurs at layer interfaces.By combination of Zoeppritz's equations and Gaussian beam forward modeling,we realize ray beams endowed energy information and achieve a fast and efficient wave field modeling method.Several models are tested with wave equation methods,conventional ray tracing methods and our method.The results show the feasibility and effectiveness of this new method.
出处 《石油地球物理勘探》 EI CSCD 北大核心 2011年第6期856-861,1012+830,共6页 Oil Geophysical Prospecting
基金 国家重点基础研究发展计划(2007CB209605) 教育部自主创新科研计划(09CX04009A)联合资助
关键词 射线追踪 地震正演 高斯射线束 ZOEPPRITZ方程 ray tracing,seismic modeling,Gaussian beam,Zoeppritz's equations
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参考文献13

  • 1Alterman Z,KaralF C Jr.Propagation of elastic wavesin layered media by finite difference methods.Bulle-tin of the Seismological Society of America,1968,58(1):367~398.
  • 2Kelly K R,Ward R W,Treitel S et al.Synthetic se-imograms:a finite difference approach.Geophysics,1976,41(1):2~27.
  • 3Virieux J.SH wave propagation in heterogeneous fi-nite-difference method.Geophysics,1984,49(12):1933~1942.
  • 4Cerveny V.Seismic rays and ray intensities in inho-mogeneous anisotropic media.Geophys J R AstronSoc,1972,29(1):1~13.
  • 5Chander R.On tracing rays with specified end points.JGeophys,1975,41(2):173~177.
  • 6Cerveny V,Nolotkov I A and Psencik I.Ray Methodsin Seismology.Praque:Charles University Press,1977.
  • 7Chander R.On tracing seismic rays with specifiedend points in layers of constant velocity and plane in-terface.Geophys Prosp,1977,25(1):120~124.
  • 8Cerveny V.Synthetic body wave seismograms for lat-erally varying structures by the Gaussian beam meth-od.Geophys J R Astr Soc,1983,73(3):389~426.
  • 9吴立明,许云,乌达巴拉.高斯束射线法在二维非均匀介质复杂构造中的应用[J].地球物理学报,1995,38(A01):144-152. 被引量:11
  • 10刘学才,周熙襄,沙椿.三维高斯射线束法合成三分量VSP记录[J].石油地球物理勘探,1995,30(5):669-680. 被引量:8

二级参考文献19

  • 1周熙襄,刘学才,蒋先艺.二维高斯射线束地震模型[J].石油地球物理勘探,1991,26(4):452-464. 被引量:12
  • 2徐涛,徐果明,高尔根,朱良保,蒋先艺.三维复杂介质的块状建模和试射射线追踪[J].地球物理学报,2004,47(6):1118-1126. 被引量:75
  • 3刘学才,周熙襄.二维非均匀介质移动网格的射线追踪算法[J].物探化探计算技术,1994,16(1):34-38. 被引量:3
  • 4刘学才,周熙襄,沙椿.三维高斯射线束法合成三分量VSP记录[J].石油地球物理勘探,1995,30(5):669-680. 被引量:8
  • 5袁慰平 张令敏 黄新芹 等.计算方法与实习[M].南京:东南大学出版社,1997..
  • 6Cerveny V. Synthetic body wave seismograms for laterally varying structures by the Gaussian beam method [J] . Geophys, 1983, 73 : 389-426.
  • 7Cerveny V, Psencik I. Gaussian beams and paraxial ray approximation in three-dimensional elastic in homogeneous media [ J] . Geophys, 1983, 53: 1-15.
  • 8Cerveny V. Gaussian beams synthetic seismograms [ J ]. Geophys, 1985, 58: 44-72.
  • 9Cerveny V. Ray Synthetic Seismograms for complex two-dimensional and three-dimensional structures [J] . Geophys, 1985, 58: 24-26.
  • 10Cerveny V, Hron F. The ray-series method and dynamic ray tracing for three-dimensional in inhomogeneous media [ R] . Bull, 1980, 70 : 47-77.

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