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首页> 外文期刊>Annals Of Geophysics >Rayleigh wave dispersion equation with real terms in a layered transversely isotropic half space
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Rayleigh wave dispersion equation with real terms in a layered transversely isotropic half space

机译:分层横观各向同性半空间中具有实项的瑞利波频散方程

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We consider transversely isotropic media with vertical axis of symmetry (VTI).? Solutions of P-SV equation of motion in a homogeneous VTI medium contain depth decay factors r 1 and r 2 , which sometimes become complex depending on VTI parameters.? In this case, r 1 and r 2 are complex conjugates.? Using this property, we obtain dispersion equation of Rayleigh waves with real terms for a layered VTI half space through Thomson-Haskell method with reduced delta matrix.? Phase and group velocities as well as surface ellipticity of Rayleigh waves are computed in real domain for a few oceanic and continental VTI structures of the earth.? Present computation in real domain is similar to that in a layered isotropic half space using the same method.? Thus it is presumed that such computation in a layered VTI half space will allow efficient evaluation of a VTI structure of the earth.
机译:我们考虑具有垂直对称轴(VTI)的横向各向同性介质。在均匀VTI介质中的P-SV运动方程的解包含深度衰减因子r 1和r 2,它们有时会根据VTI参数而变得复杂。在这种情况下,r 1和r 2是复共轭。利用该特性,我们通过具有减少的增量矩阵的Thomson-Haskell方法获得了分层VTI半空间的瑞利波的实部色散方程。对于地球上的一些海洋和大陆VTI结构,瑞利波的相位和群速度以及表面椭圆率是在实际域中计算的。当前的实域计算与使用相同方法的分层各向同性半空间中的计算相似。因此,假定在分层的VTI半空间中进行这种计算将可以有效评估地球的VTI结构。

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