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A new parameter set for anisotropic multiparameter full-waveform inversion and application to a North Sea data set

机译:各向异性多参数全波形反演的新参数集并应用于北海数据集

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Parameterization lies at the center of anisotropic full-waveform inversion (FWI) with multiparameter updates. This is because FWI aims to update the long and short wavelengths of the perturbations. Thus, it is important that the parameterization accommodates this. Recently, there has been an intensive effort to determine the optimal parameterization, centering the fundamental discussion mainly on the analysis of radiation patterns for each one of these parameterizations, and aiming to determine which is best suited for multiparameter inversion. We have developed a new parameterization in the scope of FWI, based on the concept of kinematically equivalent media, as originally proposed in other areas of seismic data analysis. Our analysis is also based on radiation patterns, as well as the relation between the perturbation of this set of parameters and perturbation in traveltime. The radiation pattern reveals that this parameterization combines some of the characteristics of parameterizations with one velocity and two Thomsen's parameters and parameterizations using two velocities and one Thomsen's parameter. The study of perturbation of traveltime with perturbation of model parameters shows that the new parameterization is less ambiguous when relating these quantities in comparison with other more commonly used parameterizations. We have concluded that our new parameterization is well-suited for inverting diving waves, which are of paramount importance to carry out practical FWI successfully. We have demonstrated that the new parameterization produces good inversion results with synthetic and real data examples. In the latter case of the real data example from the Central North Sea, the inverted models show good agreement with the geologic structures, leading to an improvement of the seismic image and flatness of the common image gathers.
机译:参数化位于具有多参数更新功能的各向异性全波形反演(FWI)的中心。这是因为FWI旨在更新微扰的长波和短波。因此,重要的是参数化要适应这一点。近来,人们一直在努力确定最佳的参数化,将基本讨论主要集中在对这些参数化中每一个的辐射方向图的分析上,并旨在确定最适合多参数反演的方法。正如在地震数据分析的其他领域中最初提出的那样,我们根据运动学等效介质的概念,在FWI范围内开发了一种新的参数化方法。我们的分析还基于辐射方向图,以及这组参数的摄动与旅行时间摄动之间的关系。辐射图表明,该参数化结合了具有一个速度和两个Thomsen参数的参数化的某些特征,以及使用两个速度和一个Thomsen参数的参数化。对行程时间摄动与模型参数摄动的研究表明,与其他更常用的参数化相比,将这些量关联起来时,新参数化的模棱两可性较少。我们得出的结论是,我们的新参数设置非常适合反转潜水波,这对于成功进行实际FWI至关重要。我们已经证明了新的参数化具有综合和真实数据示例的良好反演结果。在中北部海域真实数据示例的后一种情况下,反演模型与地质结构显示出良好的一致性,从而改善了地震图像并提高了公共图像集的平坦度。

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