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A staggered-grid high-order finite-difference modeling for elastic wave field in arbitrary tilt anisotropic media

机译:任意倾斜各向异性介质中弹性波场的交错网格高阶有限差分建模

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The paper presents a staggered-grid any even-order accurate finite-difference scheme for two-dimensional (2D),three-component (3C), first-order stress-velocity elastic wave equation and its stability condition in the arbitrary tilt anisotropic media; and derives a perfectly matched absorbing layer (PML) boundary condition and its staggered-grid any even-order accurate difference scheme in the 2D arbitrary tilt anisotropic media. The results of numerical modeling indicate that the modeling precision is high, the calculation efficiency is satisfactory and the absorbing boundary condition is better. The wave-front shapes of elastic waves are complex in the anisotropic media, and the velocity of qP wave is not always faster than that of qS wave. The wave-front triplication of qS wave and its events in both reflected domain and propagated domain, which are not commonly hyperbola, is a common phenomenon. When the symmetry axis is tilted in the TI media, the phenomenon of S-wave splitting is clearly observed in the snaps of three components and synthetic seismograms, and the events of all kinds of waves are asymmetric.
机译:提出了二维(2D),三分量(3C),一阶应力-速度弹性波方程的交错网格任意偶数精确有限差分方案及其在任意倾斜各向异性介质中的稳定性条件;并推导了在2D任意倾斜各向异性介质中的完美匹配的吸收层(PML)边界条件及其交错网格的任何偶数阶精确差分方案。数值模拟结果表明,建模精度高,计算效率令人满意,吸收边界条件较好。弹性波的波前形状在各向异性介质中很复杂,qP波的速度并不总是快于qS波的速度。 qS波的波前三重及其在反射域和传播域中的事件(通常不是双曲线)是一种常见现象。当对称轴在TI介质中倾斜时,在三个分量和合成地震图的捕捉中清楚地观察到S波分裂的现象,并且各种波的事件都是不对称的。

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