首页> 外文期刊>Geophysics: Journal of the Society of Exploration Geophysicists >Multidirectional-vector-based elastic reverse time migration and angle-domain common-image gathers with approximate wavefield decomposition of P- and S-waves
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Multidirectional-vector-based elastic reverse time migration and angle-domain common-image gathers with approximate wavefield decomposition of P- and S-waves

机译:基于多向载体的弹性反向时间迁移和角度域的共同图像聚集具有P-和S波的近似波场分解

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Elastic reverse time migration (E-RTM) has limitations when the migration velocities contain strong contrasts. First, the traditional scheme of P/S-wave mode separation is based on Helmholtz's equations, which ignore the conversion between P-and S-waves at the current separation time. Thus, it contains an implicit assumption of the constant shear modulus and requires smoothing the heterogeneous model to approximately satisfy a locally constant condition. Second, the vector-based imaging condition needs to use the reflection-image normal, and it also cannot give the correct polarity of the PP image in all possible conditions. Third, the angle-domain common-image gathers (ADCIGs) calculated using the Poynting vectors (PVs) do not consider the wave interferences that happen at each reflector. Therefore, smooth models are often used for E-RTM. We relax this condition by proposing an improved data flow that involves three new contributions. The first contribution is an improved system of P/S-wave mode separation that considers the converted wave generated at the current time, and thus it does not require the constant-shear-modulus assumption. The second contribution is the new elastic imaging conditions based on multidirectional vectors; they can give the correct image polarity in all possible conditions without knowledge of the reflection-image normal. The third contribution is two methods to calculate multidirectional propagation vectors (PRVs) for RTM images and ADCIGs: One is the elastic multidirectional PV, and the other uses the sign of wavenumber-over-frequency (k/omega) ratio obtained from an amplitude-preserved approximate-propagation-angle-based wavefield decomposition to convert the particle velocities into multidirectional PRVs. The robustness of the improved data flow is determined by several 2D numerical examples. Extension of the schemes into 3D and amplitude-preserved imaging conditions is also possible.
机译:弹性相反时间迁移(E-RTM)在迁移速度包含强对比度时具有局限性。首先,P / S波模式分离的传统方案基于Helmholtz的等式,该方程式忽略了当前分离时间的P-and波之间的转换。因此,它包含恒定剪切模量的隐式假设,并且需要平滑异构模型以大致满足局部恒定条件。其次,基于向量的成像条件需要使用反射图像法线,并且它也不能在所有可能的条件下给出PP图像的正确极性。第三,使用POYNTING矢量(PVS)计算的角度域共同图像聚集(ADCIG)不考虑在每个反射器处发生的波干扰。因此,平滑模型通常用于E-RTM。我们通过提出涉及三个新贡献的改进数据流来放宽这种情况。第一贡献是一种改进的P / S波模式分离系统,其考虑在当前时间产生的转换波,因此它不需要恒定剪切模量假设。第二种贡献是基于多向载体的新的弹性成像条件;它们可以在所有可能的条件下给出正确的图像极性,而不知道反射图像正常。第三种贡献是计算RTM图像的多向传播向量(PRV)的两种方法,并且ADCIGS:一个是弹性多向PV,另一个使用从幅度 - 保存的基于近似传播角的波场分解,以将粒子速度转换为多向PRV。改进数据流的稳健性由几个2D数值示例确定。还可以将方案扩展到3D和幅度保存的成像条件中。

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