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Evaluation of traveltime tomography in estimating near-surface velocity inversion

机译:近表面速度反转估算旅行时间断层扫描的评估

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摘要

Near-surface velocity structures are generally inverted by ray-based traveltime tomography in which the objective function is usually constructed using raypath traveltime residuals. However, inversion accuracy in these situations remains low due to the asymptotic assumption. On the contrary, phase and instantaneous traveltime tomographies invert frequency-dependent traveltime rather than the asymptotic raypath version that is contained in the first-arrival waveform for near-surface velocities. They also take the finite-frequency effect of the seismic wave propagation into account by using wavepaths instead of raypaths as sensitivity kernels. In this context, we firstly compare synthetic results between raypath traveltime, phase traveltime and instantaneous traveltime in this study before comparing their corresponding sensitivity kernels. We then analyse three sets of inversion results to prove that it is still an acceptable way to construct the objective function using raypath traveltime for tomography within the seismic exploration frequency band. In this way, time-domain wave-equation forward simulation can be avoided and therefore the computational cost can be dramatically reduced. We also demonstrate that a sensitivity kernel that takes the finite-frequency effect into account is more important for inversion accuracy than traveltime used in tomography.
机译:近表面速度结构通常通过基于射线的行进时间断层摄影反转,其中客观函数通常使用雷路行程残差构造。然而,由于渐近的假设,这些情况下的反转精度保持低。相反,阶段和瞬时旅行时间断层刻录物反转频率相关的旅行时间,而不是渐近的射线射线版本,该版本包含在近表面速度的第一到来波形中。它们还通过使用波纹观作为敏感性核来考虑地震波传播的有限频率效应。在这种情况下,在比较它们相应的灵敏度内核之前,我们首先将雷达旅行时间,相位旅行时间和瞬时旅行时间之间的合成结果进行比较。然后,我们分析了三组反转结果,以证明使用RayPath Travelify在地震勘探频带内断层扫描构建目标函数仍然是一种可接受的方法。以这种方式,可以避免时域波方向正向模拟,因此可以显着减少计算成本。我们还证明,考虑有限频率效应的灵敏度内核对于倒置精度比在断层扫描中使用的旅行时间更重要。

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