Acoustic-elastic coupled least-squares reverse time migration in marine environment with rugged seabed interface

被引:5
作者
Qu, Yingming [1 ,2 ]
Qurmet, Worral [2 ]
Zhou, Chang [2 ]
Huang, Chongpeng [2 ]
Li, Zhenchun [2 ]
机构
[1] Natl Engn Lab Offshore Oil Explorat, Beijing, Peoples R China
[2] China Univ Petr, Sch Geosci, Qingdao 266580, Peoples R China
基金
中国国家自然科学基金;
关键词
Elastic; reverse-time; depth migration; marine; WAVE-PROPAGATION; SOLID INTERFACE; REFLECTIVITY; INVERSION;
D O I
10.1080/08123985.2021.1904778
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
The severe rugged seabed interfaces bring great difficulties to seismic imaging in the marine environment. To accurately image submarine structures under the rugged seabed interface, an acoustic-elastic coupled curvilinear-coordinated least-squares reverse time migration (AE-CLSRTM) is proposed. This method is based on the coupled equation method, which uses the acoustic wave equations in seawater and the elastic wave equations in the underlying elastic medium. The pressure in the acoustic wave equations and the stresses in the elastic wave equations are transmitted steadily and continuously by using acoustic-elastic control equations at the seabed interface. To overcome the influence of the rugged seabed interface, the acoustic-elastic model is meshed into non-uniform curvilinear grids, and the corresponding mapping technique is used to transform the model with the rugged seabed interface to a horizontal one in the curvilinear coordinate system through the coordinate transformation. Based on the acoustic-elastic coupled equations in the curvilinear coordinate system, the acoustic-elastic coupled LSRTM algorithm in the rugged seafloor structure is realised. The numerical examples on a simple model and an actual area model show that the proposed LSRTM method can obtain the accurate imaging results of submarine structures in both P- and S-velocity components.
引用
收藏
页码:169 / 185
页数:17
相关论文
共 50 条
  • [31] Adaptive variable-grid least-squares reverse-time migration
    Huang, Jianping
    Chen, Liang
    Wang, Ziying
    Song, Cheng
    Han, Jiale
    FRONTIERS IN EARTH SCIENCE, 2023, 10
  • [32] Vertical transversely isotropic elastic least-squares reverse time migration based on elastic wavefield vector decomposition
    Chen, Ke
    Liu, Lu
    Zhang, Lele
    Zhao, Yang
    GEOPHYSICS, 2023, 88 (01) : S27 - S45
  • [33] Model parameterizations in the time-domain multi-parameter acoustic least-squares reverse time migration
    Zhang, Wei
    Gao, Jinghuai
    ACTA GEOPHYSICA, 2021, 69 (02) : 441 - 458
  • [34] Joint least-squares reverse time migration of primary and prismatic waves
    Yang, Jizhong
    Liu, Yuzhu
    Li, Yunyue Elita
    Cheng, Arthur
    Dong, Liangguo
    Du, Yue
    GEOPHYSICS, 2019, 84 (01) : S29 - S40
  • [35] Mesh-free least-squares reverse-time migration
    Deng, Xiaofan
    Wu, Han
    Sun, Chengyu
    Gao, Rui
    JOURNAL OF GEOPHYSICS AND ENGINEERING, 2023, 20 (02) : 185 - 195
  • [36] Least-squares reverse-time migration with extended imaging condition
    Liu Yu-Jin
    Li Zhen-Chun
    CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION, 2015, 58 (10): : 3771 - 3782
  • [37] Forward modelling formulas for least-squares reverse-time migration
    Yao, Gang
    da Silva, Nuno, V
    Wu, Di
    EXPLORATION GEOPHYSICS, 2018, 49 (04) : 506 - 518
  • [38] Anisotropic elastic least-squares reverse time migration with density variations in vertical transverse isotropic media
    Zhong, Yu
    Gu, Hanming
    Liu, Yangting
    Luo, Xia
    Mao, Qinghui
    Xu, Kai
    ACTA GEOPHYSICA, 2024, 72 (01) : 67 - 83
  • [39] LEAST-SQUARES REVERSE-TIME MIGRATION TOWARD "TRUE" REFLECTIVITY
    Zhang, Hao
    Liu, Qiancheng
    Hao, Jun
    JOURNAL OF SEISMIC EXPLORATION, 2017, 26 (02): : 183 - 198
  • [40] Least-squares based rectangular-grid cross and rhombus stencils for acoustic wave propagation and reverse time migration
    Cai, Xiaohui
    Chen, Guoxing
    Fan, Xiaoping
    Chen, Yangkang
    JOURNAL OF COMPUTATIONAL PHYSICS, 2019, 392 : 335 - 353