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首页> 外文期刊>Journal of Seismic Exploration >METHODOLOGY OF WAVEFORM INVERSION FOR ACOUSTIC ORTHORHOMBIC MEDIA
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METHODOLOGY OF WAVEFORM INVERSION FOR ACOUSTIC ORTHORHOMBIC MEDIA

机译:声正交介质的波形反演方法

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Three-dimensional seismic waveform inversion (WI) for anisotropic media is highly challenging due to its computational cost and trade-offs between multiple model parameters. Here, we develop a methodology of 3D WI for orthorhombic media in the acoustic approximation using two mixed-domain modeling algorithms, one of which is based on low-rank decomposition and the other on the generalized pseudospectral method. Numerical testing shows that both techniques produce kinematically accurate compressional wavefields with an acceptable computational cost. To take advantage of the superior stability and accuracy of the low-rank-decomposition-based method, it is employed to simulate both the forward and adjoint wavefields. The gradient of the data-difference objective function, however, is more convenient to obtain from the wave equations derived with the pseudospectral method. The inversion is conducted with a limited-memory version of the quasi-Newton optimization algorithm. Under the assumption that the symmetry-plane orientation is known, we invert wide-azimuth data for all six parameters of acoustic orthorhombic media. The performance of the developed wavefield-extrapolation and gradient-computation algorithms is evaluated for a medium with Gaussian anomalies in each parameter. Then we apply the method to a modified SEG/EAGE overthrust model to demonstrate the feasibility of waveform inversion and illustrate parameter trade-offs for structurally complicated orthorhombic media.
机译:各向异性介质的三维地震波形反演(WI)具有很高的挑战性,因为它的计算成本高,并且需要在多个模型参数之间进行权衡。在这里,我们使用两种混合域建模算法开发了一种正交各向异性介质的正交各向异性介质的3D WI方法,其中一种基于低秩分解,另一种基于广义伪谱方法。数值测试表明,这两种技术都可以产生运动学​​上精确的压缩波场,并且具有可接受的计算成本。为了利用基于低秩分解的方法的出色稳定性和准确性,该方法可用于模拟前向波场和伴随波场。然而,数据差异目标函数的梯度更容易从使用伪光谱方法导出的波动方程中获得。反演是使用拟牛顿优化算法的有限内存版本进行的。在已知对称平面取向的假设下,我们对正交正交介质的所有六个参数求出宽方位角数据。对于每个参数均具有高斯异常的介质,将评估已开发的波场外推和梯度计算算法的性能。然后,我们将该方法应用于改进的SEG / EAGE上冲模型,以证明波形反演的可行性,并说明结构复杂的斜方介质的参数折衷。

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