Reverse-time migration from rugged topography using irregular, unstructured mesh

被引:16
|
作者
Liu, Qiancheng [1 ,2 ]
Zhang, Jianfeng [1 ]
Gao, Hongwei [1 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, POB 9825, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
关键词
Unstructured mesh; Near surface; Reverse-time migration; CENTROIDAL VORONOI TESSELLATIONS; PERFECTLY MATCHED LAYERS; SV-WAVE PROPAGATION; HETEROGENEOUS MEDIA; IMAGING CONDITION; DEPTH MIGRATION; GRID METHOD; LAND DATA; EXTRAPOLATION; GENERATION;
D O I
10.1111/1365-2478.12415
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We developed a reverse-time migration scheme that can image regions with rugged topography without requiring any approximations by adopting an irregular, unstructured-grid modelling scheme. This grid, which can accurately describe surface topography and interfaces between high-velocity-contrast regions, is generated by Delaunay triangulation combined with the centroidal Voronoi tessellation method. The grid sizes vary according to the migration velocities, resulting in significant reduction of the number of discretized nodes compared with the number of nodes in the conventional regular-grid scheme, particularly in the case wherein high near-surface velocities exist. Moreover, the time sampling rate can be reduced substantially. The grid method, together with the irregular perfectly matched layer absorbing boundary condition, enables the proposed scheme to image regions of interest using curved artificial boundaries with fewer discretized nodes. We tested the proposed scheme using the 2D SEG Foothill synthetic dataset.
引用
收藏
页码:453 / 466
页数:14
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