Multi-image, reverse-time and Kirchhoff migrations with compact Green′s functions

IF 3 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Geophysics Pub Date : 2023-10-05 DOI:10.1190/geo2023-0106.1
Carlos Cunha, Gerson Ritter, Alexandre Sardinha, Bruno Pereira Dias, Claudio Guerra, Fernanda Thedy, Nelson Hargreaves, Rodrigo Coacci
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Abstract

We define a common framework for reverse-time migration (RTM) and Kirchhoff migration based on compact representations of Green’s functions. These compact Green’s functions (CGF) are 3D volumes containing traveltimes and amplitudes for the N most representative events in the upcoming/downgoing decomposed 4D wavefields originating from a point source. Within this framework, we implement an RTM algorithm using a multivalued excitation time/amplitude imaging condition. This new approach produces four complementary imaging volumes (different combinations of source and receiver decomposed wavefields) and angle/azimuth gathers with computational effort less than 15% greater than that of plain (one image, no gathers) RTM algorithms. The advantages of separating the image volume into four complementary volumes are well-established in the literature (low frequency noise separation and turning-wave imaging); however, its use has been limited by the computational cost. Despite using two source propagations to decompose the source wavefield, we reduce the computations to less than 20% of a single source propagation by performing finite-difference propagation with half the frequency limit used in the receiver wavefield propagation. The combination of CGF and an excitation time/amplitude imaging condition allows receiver wavefield decomposition with only one wavefield propagation. Our RTM algorithm constructs angle/azimuth gathers using a post-migration computation of the source and receiver wavefield’s propagation directions. To compute the propagation directions after migration, we use a new concept: the cumulative wavefield volumes, which are 3D, imaging-condition-guided compressions, of the 4D source and receiver wavefields. We also use CGF to implement a Kirchhoff migration algorithm that produces four complementary image volumes with RTM-like quality. Further, we present synthetic and field data examples to clarify the new concepts and illustrate the results obtained using both methods.
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紧致格林函数的多图像、逆时和Kirchhoff迁移
基于格林函数的紧凑表示,我们定义了逆时迁移(RTM)和Kirchhoff迁移的通用框架。这些紧凑的格林函数(CGF)是三维体,包含了来自一个点源的即将/将要分解的四维波场中N个最具代表性事件的传播时间和振幅。在此框架内,我们使用多值激励时间/振幅成像条件实现RTM算法。这种新方法产生了四个互补成像体(源和接收器分解波场的不同组合)和角度/方位角集,计算量比普通RTM算法(一幅图像,没有集)多出不到15%。将图像体积分成四个互补体积的优点在文献中得到了证实(低频噪声分离和转波成像);然而,它的使用受到计算成本的限制。尽管使用两个源传播来分解源波场,但通过使用接收器波场传播中使用的一半频率限制进行有限差分传播,我们将计算量减少到单个源传播的20%以下。CGF和激励时间/振幅成像条件的结合允许仅通过一次波场传播进行接收波场分解。我们的RTM算法通过对源波场和接收波场的传播方向进行偏移后计算来构建角度/方位角集。为了计算偏移后的传播方向,我们使用了一个新的概念:累积波场体积,即四维源波场和接收波场的三维成像条件压缩。我们还使用CGF实现了Kirchhoff迁移算法,该算法产生了四个具有类似rtm质量的互补图像体。此外,我们还提供了综合和现场数据实例来阐明新概念并说明使用这两种方法获得的结果。
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来源期刊
Geophysics
Geophysics 地学-地球化学与地球物理
CiteScore
6.90
自引率
18.20%
发文量
354
审稿时长
3 months
期刊介绍: Geophysics, published by the Society of Exploration Geophysicists since 1936, is an archival journal encompassing all aspects of research, exploration, and education in applied geophysics. Geophysics articles, generally more than 275 per year in six issues, cover the entire spectrum of geophysical methods, including seismology, potential fields, electromagnetics, and borehole measurements. Geophysics, a bimonthly, provides theoretical and mathematical tools needed to reproduce depicted work, encouraging further development and research. Geophysics papers, drawn from industry and academia, undergo a rigorous peer-review process to validate the described methods and conclusions and ensure the highest editorial and production quality. Geophysics editors strongly encourage the use of real data, including actual case histories, to highlight current technology and tutorials to stimulate ideas. Some issues feature a section of solicited papers on a particular subject of current interest. Recent special sections focused on seismic anisotropy, subsalt exploration and development, and microseismic monitoring. The PDF format of each Geophysics paper is the official version of record.
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