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首页> 外文期刊>Journal of geophysics and engineering >Joint velocity updating for anisotropic PP and PS prestack time migration based on hyperbolic correction of nonhyperbolic moveout
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Joint velocity updating for anisotropic PP and PS prestack time migration based on hyperbolic correction of nonhyperbolic moveout

机译:基于非滑动性偏移的双曲校正的各向异性PP和PS PL复位时间迁移的联合速度

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摘要

The analysis of anisotropic velocity has been well researched to support multicomponent seismic migration of anisotropic media. Because of anisotropy and asymmetric ray paths, PS-wave reflection moveout is more nonhyperbolic than PP-wave reflection moveout, which makes conventional root-mean-square velocity analysis no longer applicable. Hence, additional work is needed to reform the existing seismic data processing software or to develop new velocity analysis modules. For this reason, we propose a method of joint anisotropic velocity updating for PP and PS prestack time migration based on the hyperbolic correction of nonhyperbolic moveout. Our velocity analysis method can be performed using conventional velocity analysis. According to the PP-wave moveout equation in VTI media, we derive an accurate double-square-root moveout equation for PS-waves, which is then used to generate PP and PS common-imaging-point gathers. The travel time and offset of each sample are maintained when moving the amplitude from the shot record to the common-imaging-point gather. Both moveout attributes of PP-and PS-waves are validated to be insensitive to the velocity models by synthetic data analysis. We iteratively establish the anisotropic velocity models through velocity analyses using the small-offset and large-offset gathers, respectively. Then, based on the updated anisotropic velocity models, the anisotropic reflection time of PP and PS common-imaging-point gathers is corrected to the equivalent hyperbolic time. Eventually, we apply normal moveout and stacking to the hyperbolic-corrected common-imaging-point gathers to derive migration results. In our method, the generation of both PP and PS common-imaging-point gathers is independent of the velocity models. Application to synthetic and field seismic data demonstrates that the proposed method represents a feasible, new scheme for anisotropic velocity model building during the multicomponent prestack time migration process.
机译:研究了各向异性速度的分析,以支持各向异性培养基的多组分地震迁移。由于各向异性和不对称的光线路径,PS波反射偏离比PP波反射升降更加非滑动,这使得传统的根均方向速度分析不再适用。因此,需要额外的工作来改革现有的地震数据处理软件或开发新的速度分析模块。因此,我们提出了一种基于非恒压移除的双曲线校正的PP和PS PRESTACK时间迁移的联合各向异性速度更新方法。我们的速度分析方法可以使用传统的速度分析来执行。根据VTI介质中的PP波移位方程,我们推导了PS-Waves的精确双方根转口方程,然后用于生成PP和PS共同影像点集。当从拍摄记录移动到公共影像点收集时,保持每个样品的行进时间和偏移。通过合成数据分析验证PP-和PS-波的两个MoveOut属性对速度模型不敏感。我们可以通过使用小偏移和大偏移收集的速度分析来迭代地建立各向异性速度模型。然后,基于更新的各向异性速度模型,PP和PS共同影像点集的各向异性反射时间校正为等效的双曲线时间。最终,我们将正常的偏移和堆叠堆叠到双曲线校正的共同影像点,以派生迁移结果。在我们的方法中,PP和PS共同影像点集的产生与速度模型无关。在合成和场地震数据中的应用表明,所提出的方法代表了多组分预先复位时间迁移过程中的各向异性速度模型建设的可行性新方案。

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