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Time-domain incomplete Gauss-Newton full-waveform inversion of Gulf of Mexico data

机译:时域不完全高斯 - 牛顿全波形反演墨西哥湾数据

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We apply the incomplete Gauss-Newton full-waveform inversion (TDIGN-FWI) to Gulf of Mexico (GOM) data in the space-time domain. In our application, iterative least-squares reverse-time migration (LSRTM) is used to estimate the model update at each non-linear iteration, and the number of LSRTM iterations is progressively increased after each non-linear iteration. With this method, model updating along deep reflection wavepaths are automatically enhanced, which in turn improves imaging below the reach of diving-waves. The forward and adjoint operators are implemented in the space-time domain to simultaneously invert the data over a range of frequencies. A multiscale approach is used where higher frequencies are down-weighted significantly at early iterations, and gradually included in the inversion. Synthetic data results demonstrate the effectiveness of reconstructing both the high- and low-wavenumber features in the model without relying on diving waves in the inversion. Results with Gulf of Mexico field data show a significantly improved migration image in both the shallow and deep sections.
机译:我们应用不完全高斯 - 牛顿全波形反演(TDIGN-FWI)墨西哥(GOM)在空时域数据的海湾。在我们的应用,迭代最小二乘逆时偏移(LSRTM)用于在每一个非线性迭代估计模型更新和LSRTM迭代次数各非线性迭代之后逐渐增加。通过这种方法,沿深反射波形的模型更新自动增强,这反过来改善了潜水波下方的成像。正向和伴随运营商都在空间 - 时间域中实现以同时反转在一个频率范围的数据。使用多尺度方法,其中较高的频率被显著在早期迭代向下加权,逐渐包括在反转。合成的数据结果表明两者重建模型中的高和低波数设有的有效性,而不在反演依靠潜水波。结果与墨西哥湾字段的数据显示在浅和深部两者显著改进的迁移图像。

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