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Amplitude spectrum compensation and phase spectrum correction of seismic data based on the generalized S transform
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  • 作者:Huai-Lai Zhou (1) (2) (3)
    Jun Wang (4)
    Ming-Chun Wang (5)
    Ming-Cheng Shen (3)
    Xin-Kun Zhang (3)
    Ping Liang (6)

    1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation
    ; CDUT ; Chengdu ; 610059 ; China
    2. Key Lab of Earth Exploration & Information Techniques of Ministry of Education
    ; CDUT ; Chengdu ; 610059 ; China
    3. College of Geophysics
    ; Chengdu University of Technology ; Chengdu ; 610059 ; China
    4. Institute of Sedimentary Geology
    ; Chengdu University of Technology ; Chengdu ; 610059 ; China
    5. Exploration and Development Institute of Bohai Oil Field of CNOOC Co.
    ; Ltd Tianjin Branch ; Tianjing ; 300452 ; China
    6. College of Energy Resource
    ; Chengdu University of Technology ; Chengdu ; 610059 ; China
  • 关键词:generalized S transform ; amplitude spectra ; phase spectra ; seismic resolution ; phase correction
  • 刊名:Applied Geophysics
  • 出版年:2014
  • 出版时间:December 2014
  • 年:2014
  • 卷:11
  • 期:4
  • 页码:468-478
  • 全文大小:951 KB
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  • 刊物主题:Geophysics/Geodesy; Geotechnical Engineering & Applied Earth Sciences;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1993-0658
文摘
We propose a method for the compensation and phase correction of the amplitude spectrum based on the generalized S transform. The compensation of the amplitude spectrum within a reliable frequency range of the seismic record is performed in the S domain to restore the amplitude spectrum of reflection. We use spectral simulation methods to fit the time-dependent amplitude spectrum and compensate for the amplitude attenuation owing to absorption. We use phase scanning to select the time-, space-, and frequencydependent phases correction based on the parsimony criterion and eliminate the residual phase effect of the wavelet in the S domain. The method does not directly calculate the Q value; thus, it can be applied to the case of variable Q. The comparison of the theory model and field data verify that the proposed method can recover the amplitude spectrum of the strata reflectivity, while eliminating the effect of the residual phase of the wavelet. Thus, the wavelet approaches the zero-phase wavelet and, the seismic resolution is improved.

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