TY - GEN
T1 - Full-waveform inversion with reflected waves for 2D VTI media
AU - Pattnaik, Sonali
AU - Tsvankin, Ilya
AU - Wang, Hui
AU - Alkhalifah, Tariq Ali
N1 - KAUST Repository Item: Exported on 2020-10-01
Acknowledgements: This work was supported by the Consortium Project on Seismic Inverse Methods for Complex Structures at CWP. Tariq Alkhalifah thanks KAUST for its support.
PY - 2016/9
Y1 - 2016/9
N2 - Full-waveform inversion in anisotropic media using reflected waves suffers from the strong non-linearity of the objective function and trade-offs between model parameters. Estimating long-wavelength model components by fixing parameter perturbations, referred to as reflection-waveform inversion (RWI), can mitigate nonlinearity-related inversion issues. Here, we extend RWI to acoustic VTI (transversely isotropic with a vertical symmetry axis) media. To minimize trade-offs between the model parameters, we employ a new hierarchical two-stage approach that operates with the P-wave normal-moveout velocity and anisotropy coefficents ζ and η. First, is estimated using a fixed perturbation in ζ, and then we invert for η by fixing the updated perturbation in . The proposed 2D algorithm is tested on a horizontally layered VTI model.
AB - Full-waveform inversion in anisotropic media using reflected waves suffers from the strong non-linearity of the objective function and trade-offs between model parameters. Estimating long-wavelength model components by fixing parameter perturbations, referred to as reflection-waveform inversion (RWI), can mitigate nonlinearity-related inversion issues. Here, we extend RWI to acoustic VTI (transversely isotropic with a vertical symmetry axis) media. To minimize trade-offs between the model parameters, we employ a new hierarchical two-stage approach that operates with the P-wave normal-moveout velocity and anisotropy coefficents ζ and η. First, is estimated using a fixed perturbation in ζ, and then we invert for η by fixing the updated perturbation in . The proposed 2D algorithm is tested on a horizontally layered VTI model.
UR - http://hdl.handle.net/10754/625272
UR - http://library.seg.org/doi/10.1190/segam2016-13967833.1
UR - http://www.scopus.com/inward/record.url?scp=85019079989&partnerID=8YFLogxK
U2 - 10.1190/segam2016-13967833.1
DO - 10.1190/segam2016-13967833.1
M3 - Conference contribution
SP - 413
EP - 418
BT - SEG Technical Program Expanded Abstracts 2016
PB - Society of Exploration Geophysicists
ER -