A new decoupling and elastic propagator for efficient elastic reverse time migration

被引:0
|
作者
Du Q. [1 ,2 ,3 ]
Zhao Q. [1 ,2 ,3 ]
Li Q. [1 ,2 ,3 ]
Fu L. [1 ,2 ,3 ]
Sun Q. [4 ]
机构
[1] China University of Petroleum (East China), Key Laboratory of Deep Oil and Gas, Changjiang West Road 66th, Qingdao
[2] Qingdao National Laboratory for Marine Science and Technology, Laboratory for Marine Mineral Resources, Qingdao
[3] Cnpc China University of Petroleum (East China), Key Laboratory of Geophysical Prospecting, Changjiang West Road 66th, Qingdao
[4] China University of Petroleum (East China), College of Computer Science and Technology, Changjiang West Road 66th, Qingdao
来源
Geophysics | 2020年 / 85卷 / 05期
基金
中国国家自然科学基金;
关键词
depth migration; elastic; reverse time migration;
D O I
10.1190/geo2019-0830.1
中图分类号
学科分类号
摘要
Methods to decompose the elastic wavefield into compressional wave (P-wave) and shear wave (S-wave) components in heterogeneous media without wavefield distortions or energy leakage are the key issues in elastic imaging and inversion. We have introduced a decoupled P- and S-wave propagator to form an efficient elastic reverse time migration (RTM) framework, without assuming homogeneous Lamé parameters. Also, no wave-mode conversions occur using the proposed propagator in the presence of strong heterogeneities, which avoids the potential imaging artifacts caused by wave-mode conversions in the receiver-side backward extrapolation. In the proposed elastic RTM framework, the source-side forward wavefield is simulated with a P-wave propagator. The receiver-side wavefield is back extrapolated with the proposed propagator, using the recorded multicomponent seismic data as input. Compared to the conventional elastic RTM, the proposed framework reduces the computational complexity while preserving the imaging accuracy. We have determined its accuracy and efficiency using two synthetic examples. © 2020 Society of Exploration Geophysicists.
引用
收藏
页码:A31 / A36
页数:5
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