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Seismic ambient noise reconstruction based on the multi-taper spectral method: Application to the seismic full waveform inversion

机译:基于多锥谱方法的地震环境噪声重构:在地震全波形反演中的应用

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The seismic ambient noises contain real seismic waves that transmit through the subsurface media. Using seismic interferometry, the disorganized ambient noises recorded on surface can be reconstructed into the virtual source records that are similar to the conventional active source seismic data. However, the conventional reconstruction methods introduce additional noises into the final result, which adds the difficulty of the applications. In this paper, we propose an optimal length multi-taper spectral method based seismic interferometry to reconstruct the virtual source records, and point out that a suitable taper length is important for noise suppression. After that, we propose the source independent full waveform inversion method for the reconstructed virtual source data, which avoids virtual wavelet estimation. The final results demonstrate that the multi-taper spectral method with optimal taper length can reconstruct high quality virtual source data for the full waveform inversion.
机译:地震环境噪声包含通过地下介质传输的真实地震波。使用地震干涉测量法,可以将记录在地面上的杂乱无章的环境噪声重建为类似于常规主动震源地震数据的虚拟震源记录。然而,常规的重建方法将额外的噪声引入到最终结果中,这增加了应用的难度。在本文中,我们提出了一种基于最佳长度多锥谱方法的地震干涉法来重建虚拟源记录,并指出合适的锥度对于抑制噪声非常重要。在此之后,我们提出了用于重构的虚拟源数据的独立于源的全波形反演方法,该方法避免了虚拟小波估计。最终结果表明,具有最佳锥度的多锥谱方法可以为整个波形反演重建高质量的虚拟源数据。

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