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Seismic p-wave modelling in an inhomogeneous transversely isotropic medium with a tilted symmetry axis

机译:具有对称轴倾斜的非均质横向各向同性介质中的地震p波建模

摘要

An improved method for P-wave modeling in inhomogeneous transversely isotropic media with tilted symmetry axis (TTI media), suitable for anisotropic reverse-time migration, is based on an acoustic TI approximation. The resulting wave equations (2.20) & (2.21) are derived directly from first principles, Hooke's law and the equations of motion, and therefore make no assumptions on spatial variation of medium parameters. Like in the acoustic VTI case, the wave equations are written as a set of two second-order partial differential equations. However, unlike in the acoustic VTI case, the acoustic TTI wave equations contain mixed second-order derivatives. The discretization scheme uses centered finite-difference operators for first- and second-order derivative operators to approximate the mixed and non-mixed second-order derivatives in the wave equation. The discretization scheme is stabilized by slightly weighing down the mixed derivatives, with almost negligible effect on the wave field kinematics.
机译:基于声学TI近似,一种适用于各向异性反向时间偏移的,具有倾斜对称轴的非均匀横向各向同性介质(TTI介质)中的P波建模的改进方法。最终的波动方程(2.20)和(2.21)直接从第一原理,胡克定律和运动方程式导出,因此不对介质参数的空间变化做出任何假设。像在声学VTI情况下一样,波动方程被写为一组两个二阶偏微分方程。但是,与声学VTI情况不同,声学TTI波动方程包含混合的二阶导数。离散化方案对一阶和二阶导数算子使用居中有限差分算子,以近似波动方程中的混合和非混合二阶导数。离散化方案通过稍微权衡混合的导数来稳定,对波场运动学的影响几乎可以忽略不计。

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