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Workflow for near-surface velocity automatic estimation: Source-domain full-traveltime inversion followed by waveform inversion

机译:近地表速度自动估计的工作流程:源域全行程时间反演,然后进行波形反演

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摘要

This paper presents a workflow for near-surface velocity automatic estimation using the early arrivals of seismic data. This workflow comprises two methods, source-domain full traveltime inversion (FTI) and early-arrival waveform inversion. Source-domain FTI is capable of automatically generating a background velocity that can kinematically match the reconstructed plane-wave sources of early arrivals with true plane-wave sources. This method does not require picking first arrivals for inversion, which is one of the most challenging aspects of ray-based first-arrival tomographic inversion. Moreover, compared with conventional Born-based methods, source-domain FTI can distinguish between slower or faster initial model errors via providing the correct sign of the model gradient. In addition, this method does not need estimation of the source wavelet, which is a requirement for receiver-domain wave-equation velocity inversion. The model derived from source-domain FTI is then used as input to early-arrival waveform inversion to obtain the short-wavelength velocity components. We have tested the workflow on synthetic and field seismic data sets. The results show source-domain FTI can generate reasonable background velocities for early-arrival waveform inversion even when subsurface velocity reversals are present and the workflow can produce a high-resolution near-surface velocity model.
机译:本文介绍了使用地震数据的早期到达进行近地表速度自动估算的工作流程。该工作流程包括两种方法,源域全行程时间反演(FTI)和提前到达波形反演。源域FTI能够自动生成背景速度,该背景速度可以将早期到达的重构平面波源与真实的平面波源进行运动学匹配。该方法不需要选取初次到达进行反演,这是基于射线的首次到达层析成像反演中最具挑战性的方面之一。此外,与传统的基于Born的方法相比,源域FTI可以通过提供模型梯度的正确符号来区分较慢或较快的初始模型错误。另外,该方法不需要估计源子波,这是接收器域波方程速度反演的要求。然后将从源域FTI导出的模型用作早期到达波形反演的输入,以获得短波长速度分量。我们已经在合成和现场地震数据集上测试了工作流程。结果表明,即使存在地下速度反转,源域FTI仍可为早期到达的波形反演生成合理的背景速度,并且工作流可以生成高分辨率的近地表速度模型。

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