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True Amplitude Angle Gathers from Reverse Time Migration by Wavefield Decomposition at Excitation Amplitude Time

Author

Listed:
  • Zhe Yan

    (Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China)

  • Yonglong Yang

    (Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China
    Current affiliation: CCCC Second Highway Consultants, Co., Ltd., Wuhan 430052, China.)

  • Shaoyong Liu

    (Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, China)

Abstract

Reservoir parameter estimation is one of the goals of amplitude-versus-angle (AVA) inversion and angle-domain common image gathers are the basis of AVA inversion. Therefore, the accuracy of kinematic and kinetic information on angle gathers is very important for reservoir characterization. Reverse time migration is one of the most physically accurate migration method. Generating angle gathers from reverse time migration with the Poynting vector method is very efficient. However, due to inaccurate angle measurement and uneven illumination, angle gathers calculated by the Poynting vector method are often not suitable for AVA inversion. In this paper, we propose an efficient method of angle gathers with accurate angular information and amplitude from reverse time migration. We firstly decompose source and receiver wavefield to their up-going and down-going parts by using analytic wavefield. We calculate propagation directions for source down-going wavefield and receiver up-going wavefield by the Poynting vector method and form the angle gathers with these angle information and decomposed wavefield. To reduce memory storage and improve computational efficiency, we decompose wavefield at excitation amplitude time by using a local spatial Fourier transform. We also use a spatial smoothed Poynting vector to improve the stability of angle measurement. We apply an illumination compensation image condition to recover the true amplitude. Numerical examples on Marmousi model and the SEAM two-dimensional (2D) model demonstrate the advantages of our proposed method. The angle gathers based on our method are cleaner with more focus on events energy and better continuity, suffering from less low-frequency noise in the shallow parts and with a distinct cutoff at large angle where reflection terminates. At last, we demonstrate the effectiveness of proposed method on a 2D marine field data example.

Suggested Citation

  • Zhe Yan & Yonglong Yang & Shaoyong Liu, 2020. "True Amplitude Angle Gathers from Reverse Time Migration by Wavefield Decomposition at Excitation Amplitude Time," Energies, MDPI, vol. 13(23), pages 1-16, November.
  • Handle: RePEc:gam:jeners:v:13:y:2020:i:23:p:6204-:d:451073
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    References listed on IDEAS

    as
    1. Zhen Yang & Jun Lu, 2020. "Second-Order Approximation of the Seismic Reflection Coefficient in Thin Interbeds," Energies, MDPI, vol. 13(6), pages 1-19, March.
    2. Lei Shi & Yuhang Sun & Yang Liu & David Cova & Junzhou Liu, 2020. "High-Order AVO Inversion for Effective Pore-Fluid Bulk Modulus Based on Series Reversion and Bayesian Theory," Energies, MDPI, vol. 13(6), pages 1-18, March.
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