Image-guided wavefield tomography for VTI media

V. Li, A. Guitton, I. Tsvankin, T. Alkhalifah
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Abstract

Processing algorithms for transversely isotropic (TI) media are widely used in depth imaging and typically bring substantial improvements in reflector focusing and positioning. Here, we develop acoustic image-domain tomography (IDT) for reconstructing VTI (TI with a vertical symmetry axis) models from P-wave reflection data. The modeling operator yields an integral wave-equation solution, which is based on a separable dispersion relation and contains only P-waves. The zero-dip NMO velocity (Vnmo) and anellipticity parameter η are updated by focusing energy in space-lag images obtained by least-squares reverse time migration (LSRTM). Application of LSRTM helps suppress apertureand illumination-induced artifacts in space-lag gathers and improve the robustness of η-estimation. The trade-off between Vnmo and η is mitigated by a three-stage inversion algorithm that gradually relaxes the constraints on the spatial variation of η. Assuming that the depth profile of the Thomsen parameter δ is known at two or more borehole locations, we employ image-guided interpolation to constrain the depth scale of the parameter fields and the migrated image. Image-guided smoothing is also applied to the IDT gradients to facilitate convergence towards geologically plausible models. The algorithm is tested on synthetic reflection and borehole data from the structurally complicated elastic VTI Marmousi-II model. Although the initial velocity field is purely isotropic and substantially distorted, all three relevant parameters (Vnmo, η, and δ) are estimated with sufficient accuracy. The algorithm is also applied to a line from a 3D ocean-bottom-node data set acquired in the Gulf of Mexico.
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VTI介质的成像引导波场层析成像
横向各向同性(TI)介质的处理算法被广泛应用于深度成像,并且通常在反射器聚焦和定位方面带来实质性的改进。在这里,我们开发了声学图像域层析成像(IDT),用于从p波反射数据重建VTI(具有垂直对称轴的TI)模型。建模算子得到基于可分离色散关系且只包含纵波的积分波方程解。利用最小二乘逆时偏移(LSRTM)技术对空间滞后图像进行能量聚焦,更新零倾角NMO速度(Vnmo)和非椭圆参数η。LSRTM的应用有助于抑制空间滞后集中孔径和光照引起的伪像,提高η估计的鲁棒性。通过一种逐步放宽η空间变化约束的三步反演算法,减轻了Vnmo和η之间的权衡。假设已知两个或多个钻孔位置的Thomsen参数δ深度剖面,我们采用图像引导插值来约束参数场和偏移图像的深度尺度。图像引导平滑也应用于IDT梯度,以促进收敛到地质上合理的模型。利用结构复杂的弹性VTI Marmousi-II模型的综合反射和井眼数据对该算法进行了验证。虽然初始速度场是纯各向同性的,并且基本上是扭曲的,但所有三个相关参数(Vnmo, η和δ)都有足够的精度估计。该算法还应用于从墨西哥湾获得的三维海底节点数据集中的一条线。
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