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3D orthorhombic elastic full waveform inversion in the reflection domain from hydrophone data

机译:3D从水听器数据中反射域中的3D正交弹性全波形反转

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We formulate the theory of 3D orthorhombic full-waveform inversion using adjoint state techniques for recovery of shear and p-wave elastic stiffness coefficients from acquired pressure data. In formulating the adjoint of forward Born scattering, we use a novel transformation of wavefields that allows us to use the same high performance elastic propagation kernel for the adjoint that we use for forward elastic modeling. We further derive inversion equations suitable for recovery of p-wave and shear velocities in fixed inhomogeneous density media with fixed inhomogeneous anisotropic coefficients, through the use of a chain rule formulation. We demonstrate that for a simple model with a strong Class 2 AVO signature involving phase reversal, a sequence of short-offset p-wave elastic stiffness recovery (equivalently velocity or impedance) folllowed by long offset shear elastic stiffness recovery produces a significant uplift in data fitting when compared to simple acoustic inversion for p-wave velocity. We also demonstrate effective recovery in 2D using similar techniques, for a more complex model with thin sands exhibiting strong AVO behavior.
机译:我们使用伴随状态技术制定3D正交全波形反演的理论,用于从获取的压力数据中恢复剪切和P波弹性刚度系数。在制定前期出生散射的伴随时,我们使用的是波场的新型转换,使我们能够使用相同的高性能弹性传播核来伴随我们用于前进弹性建模。我们通过使用链规则配方,我们进一步推出适于恢复固定的非均匀密度介质中的固定非均匀密度介质中的P波和剪切速度的反演方程,其具有固定的不均匀各向异性系数。我们证明,对于具有涉及相位逆转的强大2 AVO签名的简单模型,由长偏移剪切弹性刚度恢复具有短的短偏移P波弹性刚度恢复(等效速度或阻抗),产生了显着的数据隆起与P波速度的简单声反转相比,拟合。我们还使用类似的技术展示了2D的有效恢复,对于具有强大AVO行为的薄砂的更复杂模型。

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