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首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Common-reflection-point migration velocity analysis of 2D P-wave data from TTI media
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Common-reflection-point migration velocity analysis of 2D P-wave data from TTI media

机译:来自TTI介质的二维P波数据的共反射点迁移速度分析

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摘要

We have developed a common-reflection-point (CRP)- based kinematic migration velocity analysis for 2D P-wave reflection data to estimate the four transversely isotropic (TI) parameters V_(Po), δ, and ε, and the tilt angle φ of the symmetry axis in a TI medium. In each iteration, the tomographic parameter was updated alternately with prestack anisotropic ray-based migration. Iterations initially used layer stripping to reduce the number of degrees of freedom; after convergence was reached, a couple of more iterations over all parameters and all CRPs ensured global interlayer coupling and parameter interaction. The TI symmetry axis orientation was constrained to be locally perpendicular to the reflectors. The V_(Po) dominated the inversion, and so it was weighted less than δ and ε in the parameter updates. Estimates of δ and ε were influenced if the error in φ was >5°; estimates of V_(Po) were also influenced if the error in φ was >10°. Examples included data for a simple model with a homogeneous TI layer whose dips allowed recovery of all anisotropy parameters from noise-free data, and a more realistic model (the BP tilted transversely isotropic (TTI) model) for which only V_(Po), δ, and ? were recoverable. The adequacy of the traveltimes predicted by the inverted anisotropic models was tested by comparing migrated images and common image gathers, with those produced using the known velocity models.
机译:我们已经针对2D P波反射数据开发了基于共反射点(CRP)的运动学迁移速度分析,以估算四个横向各向同性(TI)参数V_(Po),δ和ε,以及倾斜角φ TI介质中对称轴的角度。在每次迭代中,层析成像参数都会与叠前基于各向异性射线的偏移交替更新。迭代最初使用层剥离来减少自由度的数量。达到收敛后,在所有参数和所有CRP上进行了多次迭代,确保了全局层间耦合和参数交互。 TI对称轴方向被约束为局部垂直于反射器。 V_(Po)主导了反演,因此在参数更新中其权重小于δ和ε。如果φ的误差> 5°,则会影响δ和ε的估计值;如果φ的误差> 10°,也会影响V_(Po)的估计值。例子包括一个简单模型的数据,该模型具有均匀的TI层,其倾角允许从无噪声的数据中恢复所有各向异性参数,以及更实际的模型(BP倾斜横向各向同性(TTI)模型),其中仅V_(Po), δ和?是可以恢复的。通过将迁移的图像和常见的图像集与使用已知速度模型生成的图像进行比较,测试了由反向各向异性模型预测的行程时间是否足够。

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