Least-squares reverse time migration with velocity errors

Jizhong Yang, Y. Li, A. Cheng, Yuzhu Liu, Liangguo Dong
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引用次数: 1

Abstract

An accurate migration velocity model is required for reverse time migration (RTM) to correctly predict the kinematics of wave propagation in the subsurface. Leastsquares reverse time migration (LSRTM), which aims to match the amplitudes of the modeled data with the observed data in an iterative inverse procedure, is more sensitive to the accuracy of the migration velocity model. If the migration velocity model contains errors, the final migration images will be defocused and incoherent. As a partial solution, we utilize an LSRTM scheme based on the extended imaging condition, which is called as leastsquares extended RTM (LSERTM). It is well accepted that LSERTM can fit the observed data regardless of the accuracy of the migration velocity model. We further explore this property and find that after stacking the extended migration images along the subsurface offset axis within properly selected ranges, we can obtain an image with better coherency and focusing than the conventional LSRTM. We demonstrate the efficacy of our method with numerical examples on a Salt-like model and the Marmousi model.
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带速度误差的最小二乘逆时偏移
逆时偏移(RTM)需要精确的偏移速度模型,才能正确预测波在地下的传播运动学。最小二乘逆时偏移(LSRTM)对偏移速度模型的精度更为敏感,其目的是通过迭代逆过程将建模数据的振幅与观测数据进行匹配。如果迁移速度模型存在误差,最终的迁移图像会出现散焦和不连贯。作为部分解决方案,我们采用了一种基于扩展成像条件的LSRTM方案,称为最小二乘扩展RTM (LSERTM)。无论偏移速度模型的精度如何,LSERTM都能很好地拟合观测数据,这一点已被广泛接受。我们进一步探索了这一特性,发现在适当选择的范围内,沿着地下偏移轴叠加扩展偏移图像,可以获得比传统LSRTM具有更好的相干性和聚焦性的图像。通过类盐模型和Marmousi模型的数值算例验证了该方法的有效性。
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