首页> 外文会议>nternational Workshop on Seismic Anisotropy; 20061022-27; Beijing(CN) >P-wave Nonhyperbolic Moveout Velocity Analysis in Transversely Isotropic Medium
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P-wave Nonhyperbolic Moveout Velocity Analysis in Transversely Isotropic Medium

机译:横观各向同性介质中的P波非双曲时差速度分析

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With the development of seismic exploration, the exploration targets have already turned from structural reservoirs to subtle reservoirs step by step. NMO velocity and Amplitude Versus Offset (AVO) analysis of subtle reservoirs represent anisotropy generally, so it becomes more and more important to study the propagation law of seismic-wave in anisotropic medium. Velocity analysis is one of key steps in seismic data processing , its precision has direct impact on the effects of the following steps, such as NMO correction, statistic correction, imaging and migration. So how to improve the accuracy of velocity analysis in anisotropic media becomes the key problem for geophysicists pursuing on either method study or data processing.
机译:随着地震勘探的发展,勘探目标已经逐步从结构性储层转向精细储层。精细油藏的NMO速度和幅值对偏移(AVO)分析通常代表各向异性,因此研究地震波在各向异性介质中的传播规律变得越来越重要。速度分析是地震数据处理中的关键步骤之一,其精度直接影响到以下步骤的效果,例如NMO校正,统计校正,成像和偏移。因此,如何提高各向异性介质中速度分析的精度成为地球物理学家进行方法研究或数据处理的关键问题。

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