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首页> 外文期刊>IEEE Geoscience and Remote Sensing Letters >Stable and High-Efficiency Attenuation Compensation in Reverse-Time Migration Using Wavefield Decomposition Algorithm
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Stable and High-Efficiency Attenuation Compensation in Reverse-Time Migration Using Wavefield Decomposition Algorithm

机译:使用波场分解算法的逆时偏移中的稳定高效衰减补偿

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摘要

Q-compensated reverse time migration (Q-RTM) can compensate seismic attenuation caused by the anelastic behavior of subsurface media. Although, the traditional Q-RTM has high computational efficiency, it is instable because the high frequency or wavenumber ambient noise is exponentially boosted during forward and backward seismic wavefield propagation. The existing stable Q-RTM method costs twice as much computing time and memory compared to the traditional Q-RTM. In this letter, we propose a new Q-RTM method to address the above issues simultaneously. First, a new viscoacoustic wave equation is derived based on a wavefield decomposition method to obtain the velocity-dispersion-only and viscoacoustic wavefields efficiently. Then, a theoretical framework of stable and high-efficiency Q-RTM method is proposed based on the velocity-dispersion-only and viscoacoustic wavefields. The synthetic example shows that the new stable Q-RTM results match well with the reference images (without attenuation images). Moreover, the field data images also demonstrate the stability and high-efficiency of our proposed Q-RTM method.
机译:Q补偿的逆时偏移(Q-RTM)可以补偿由于地下介质的非弹性行为引起的地震衰减。尽管传统的Q-RTM具有很高的计算效率,但它是不稳定的,因为在向前和向后地震波场传播过程中,高频或波数环境噪声呈指数增加。与传统的Q-RTM相比,现有的稳定Q-RTM方法的计算时间和内存消耗是其两倍。在这封信中,我们提出了一种新的Q-RTM方法来同时解决上述问题。首先,基于波场分解方法推导了新的粘声波方程,从而有效地获得了仅速度分散型和粘声波场。然后,基于纯速度色散和粘声波场,提出了稳定高效的Q-RTM方法的理论框架。综合示例表明,新的稳定Q-RTM结果与参考图像(无衰减图像)匹配得很好。此外,现场数据图像还证明了我们提出的Q-RTM方法的稳定性和高效率。

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