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An iterative, fast-sweeping-based eikonal solver for 3D tilted anisotropic media

机译:基于迭代,快速扫描的3D倾斜各向异性介质的本征求解器

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摘要

Computation of first-arrival traveltimes for quasi-P waves in the presence of anisotropy is important for high-end near-surface modeling, microseismic-source localization, and fractured-reservoir characterization - and it requires solving an anisotropic eikonal equation. Anisotropy deviating from elliptical anisotropy introduces higher order nonlinearity into the eikonal equation, which makes solving the eikonal equation a challenge. We addressed this challenge by iteratively solving a sequence of simpler tilted elliptically anisotropic eikonal equations. At each iteration, the source function was updated to capture the effects of the higher order nonlinear terms. We used Aitken's extrapolation to speed up convergence rate of the iterative algorithm. The result is an algorithm for computing first-arrival traveltimes in tilted anisotropic media. We evaluated the applicability and usefulness of our method on tilted transversely isotropic media and tilted orthorhombic media. Our numerical tests determined that the proposed method matches the first arrivals obtained by wavefield extrapolation, even for strongly anisotropic and highly complex subsurface structures. Thus, for the cases where two-point ray tracing fails, our method can be a potential substitute for computing traveltimes. The approach presented here can be easily extended to compute first-arrival traveltimes for anisotropic media with lower symmetries, such as monoclinic or even the triclinic media.
机译:各向异性存在下准P波的初到传播时间的计算对于高端近地表建模,微震源定位和裂缝性储层表征很重要-它需要求解各向异性的方程式。偏离椭圆各向异性的各向异性将高阶非线性引入了本征方程,这使得求解本征方程成为挑战。我们通过迭代求解一系列更简单的倾斜的椭圆各向异性方程,解决了这一挑战。在每次迭代中,源函数都会更新以捕获高阶非线性项的影响。我们使用艾特肯外推法来加快迭代算法的收敛速度。结果是一种用于计算倾斜各向异性介质中第一到达时间的算法。我们评估了我们的方法在倾斜的横向各向同性介质和倾斜的斜方介质上的适用性和实用性。我们的数值测试确定,即使对于强各向异性和高度复杂的地下结构,所提出的方法也与通过波场外推法获得的初次到达相匹配。因此,对于两点射线追踪失败的情况,我们的方法可以替代计算旅行时间。此处介绍的方法可以轻松地扩展为计算对称性较低的各向异性介质(如单斜晶系甚至三斜晶系介质)的初次到达时间。

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