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井间地震观测数据模拟和偏移的有限单元法 被引量:4

The finite unit method of cross-hole seismic observations modeling and migration
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摘要 近年来,由于井下地震震源和特殊的数据采集设备的研制及不断改进,井间地震观测系统,及其随后的井间速度模型的地震旅行时反演(又称地震层析方法)正在发展成为一项用于储层研究、油藏描述和解决某些油藏工程问题的实用技术。文章给出了用于井间地震数据模拟和偏移的有限单元波动方程数值解模型,提出了适用于该算法的吸收边界条件,并导出了可靠的数值解结果。 In recent with the advancement of seismic source and special acquisition equipment manufacturing and their on-going improvement, crosshole seismic observation system and seismic travel time inversion for crosshole velocitymodeling (also tomography) is developing imto a practical technique for reservoir research, description and resolvesome problems concerning reseroir engineering. A finite element wave-equation numerical model are given, absorp-tion boundary condition for the method are put forward and rwliable numerical result is derived.
作者 杜世通
出处 《油气地球物理》 2004年第4期78-82,共5页 Petroleum Geophysics
关键词 数据模拟技术 井间地震技术 有限单元法 偏移技术 地震震源 储层 分辨率 地层 crosshole seismic observation, absorption boundary condition, finite element method, numerical model-ing, migration reposition
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参考文献5

  • 1Howell L H,,Trefethen L N.Ⅲ-posedness of absorbing boundary conditions for migration[].Geophysics.1988
  • 2Benz G M,Smith R B.Kinematic source modeling of normal faulting earthquakes using the finite element method[].Geophysics J RoySoc.1987
  • 3Hu L,McMechan G A and Harris J M.Acoustic prestack migration of crosshole data[].Geophysics.1988
  • 4Clatton R,Engquist B.Absorbing boundary conditions for acoustic and elastic wave equations[].Bulletin of the Seismological Society of America.
  • 5Chang W F and McMechan G A.Reverse-time migration of offset vertical seismic profiling data using the excitation-time imaging condition[].Geophysics.1986

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