Pre-stack seismic full waveform inversion (FWI) is based on wave equation forward modeling technology to describe the propagation characteristics of seismic wave,using non-constrained iterative local optimization method to get high resolution inversion result.Compared with other inversion methods,FWI uses pre-stack common shot gather to perform inversion,in which the seismic data are free of the process of stack and preserve the features of waveform parameters variation with offset.The inversion result is no longer simple interface and traveltime information but depth-domain data volume which reflects formation velocity and structural characteristics,and this is helpful to the analysis and understanding of the geological body.In this paper,the technical advantages are analyzed in the aspect of pre-stack full waveform inversion methods,and the key technology to do a good job of pre-stack full waveform inversion is also analyzed through synthetic data.Furthermore,the technical advantages of pre-stack full waveform inversion are illustrated through inversion results in migration processing and its application in reservoir description of fluvial facies,and the existing difficulties and the future development direction of pre-stack seismic full waveform inversion are also analyzed,which will provide reference for further development and application of pre-stack seismic full waveform inversion.
[1] Lailly P.The seismic inverse problem as a sequence of before stack migrations[C]//Society for Industrial and Applied Mathematics,Philadelphia,PA,1983.
[2] Tarantola A.Inversion of seismic data in acoustic approximation[J].Geophysics,1984,49(8):1259-1266.
[3] Tarantola A.Inverse problem theory:Methods for data fitting and model parameter estimation[M].Elsevier,1987.
[4] Pratt R G,Shin C,Hicks G J.Gauss-Newton and full Newton methods in frequency-space seismic waveform inversion[J].Geophysical Journal of International,1998,13(3):341-362.
[5] Li X S,Demmel J W.SuperLU_DIST:A scalable distributed-memory sparse direct solver for unsymmetric linear systems[J].ACM Transactions on Mathematical Software (TOMS),2003,29(2):110-140.
[6] Sirgue L,Pratt R G.Efficient waveform inversion and imaging:A strategy for selecting temporal frequencies[J].Geophysics,2004,69(1):231-248.
[7] Pratt R G.Seismic waveform inversion in the frequency domain,Part 1:Theory and verification in a physical scale model[J].Geophysics,1999,64(3):888-901.
[8] Pratt R G,Shipp R M.Seismic waveform inversion in the frequency domain,Part 2:Fault delineation in sediments using crosshole data[J].Geophysics,1999,64(3):902-914.
[9] Sheen D H,Tuncay K,Baag C E,et al.Time domain Gauss-Newton seismic waveform inversion in elastic media[J].Geophysical Journal of International,2006,167(3):1373-1384.
[10] Shin C,Cha Y H.Waveform inversion in the Laplace-Fourier domain[J].Geophysical Journal International[J].2009,177(3):1067-1079.
[11] Virieux J,Operto S E P.An overview of full-waveform inversion in exploration geophysics[J].Geophysics,2009,74(6):C1-C26.
[12] 卞爱飞,于文辉,周华伟.频率域全波形反演方法研究进展[J].地球物理学进展,2010,25(3):982-993.
[13] 杨午阳,王西文,雍学善,等.地震全波形反演方法研究综述[J].地球物理学进展,2013,28(2):766-776.