转换波反射全波形反演的实际实现

N. Masmoudi, A. Ratcliffe, M. Wang, Y. Xie, T. Wang
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引用次数: 0

摘要

转换波(P-to- s)海底地震(OBS)数据的深度成像需要一个纵波和横波速度的深度模型。建立横波速度模型非常具有挑战性:传统的技术包括PP和PS图像配准,或PP和PS联合层析成像。由于典型OBS调查的稀疏接收器采集,在模型的浅层部分缺乏可靠的PS图像,这些方法往往受到阻碍,并且处理复杂的横向速度变化的分辨率有限。我们介绍了一种新的全波形反演技术,利用OBS测量中记录的径向分量的转换波反射数据来更新s波速度。该方法的关键方面包括使用声学born建模,鲁棒目标函数来处理运动学和动力学差异,以及层剥离策略来简化反演问题的非线性。该方法在不同的合成材料上进行了验证,并在现场数据示例中进行了验证,从而提高了PS成像的s波速度和反射面连续性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A practical implementation of converted-wave reflection full-waveform inversion
Depth imaging of converted-wave (P-to-S) ocean-bottom seismic (OBS) data requires a depth model for both the P- and S-wave velocities. Building the S-wave velocity model is very challenging: conventional techniques include PP and PS image registration, or joint PP and PS tomography. These approaches are often impeded by the lack of a reliable PS image in the shallow part of the model due to the sparse-receiver acquisition of typical OBS surveys, and have limited resolution to deal with complex lateral velocity variations. We introduce a new full-waveform inversion technique to update the S-wave velocity using converted-wave reflection data recorded in the radial component of OBS surveys. Key aspects of the method include the use of acoustic Born-modeling, a robust objective function to handle kinematic and dynamic differences, and a layer-stripping strategy to simplify the non-linearity of the inversion problem. The proposed approach is validated on different synthetics, and demonstrated on a field data example, giving an improved S-wave velocity and better reflector continuity for PS imaging.
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