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Processing surface-reflected shear-wave signatures from an azimuthally-anisotropic geological formation

机译:处理来自各向异性各向异性地质构造的表面反射剪切波信号

摘要

A method for measuring and using anisotropy in a coal bed sequence. The method includes the steps of: stripping layers where polarization changes are indicated by applying a static shift to components aligned with the slow shear wave polarization direction and applying one half of the static shift to components neither aligned with the slow shear wave polarization direction nor aligned with the fast shear wave polarization direction; obtaining for a coal bed a measure of the amplitude of the envelope of the fast polarization trace; rotating, by about 45 degrees away from a principal direction, the data set for that coal bed; obtaining a measure of the amplitude of the envelope of at least one of the mixed/mismatched polarization traces of that coal bed; and obtaining the ratio of the amplitude of the envelope of the fast polarization trace to the amplitude of the envelope of one mixed/mismatched polarization trace in that coal bed.
机译:一种在煤层序中测量和使用各向异性的方法。该方法包括以下步骤:剥离层,其中通过对与慢剪切波偏振方向对准的分量施加静态位移来指示极化变化,并对与慢剪切波偏振方向对准或对准的分量施加静态位移的一半。具有快剪切波的极化方向;为煤层获得快速极化迹线包络振幅的量度;将该煤层的数据集与主方向旋转大约45度。获得该煤层中至少一条混合/不匹配的极化迹线包络线幅度的量度;求出快速极化迹线的包络线幅度与该煤层中一条混合/不匹配极化迹线的包络线幅度的比值。

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