TY - GEN
T1 - Migration velocity analysis using prestack wavefields
AU - Alkhalifah, T.
AU - Wu, Z.
PY - 2015
Y1 - 2015
N2 - Using both the image and data domains to perform velocity inversion can help us resolve the long and short wavelength components of the velocity model, usually in that order. This translates to integrating migration velocity analysis (MVA) into full waveform inversion (FWI). The MVA part of the inversion often requires computing extended images, which is pricy using conventional methods. As a result, we use prestack wavefield (the double-square-root (DSR)) extrapolation, which includes the extended information (subsurface offsets) naturally, to make the process far more efficient and stable. The combination of the forward and adjoint prestack wavefields provides us with update options that can be easily conditioned to improve convergence. We, specifically, use a modified differential semblance operator to divide the extended image to the residual part for classic differential semblance operator (DSO) updates and the image modeling part, which provides reflections for higher resolution information. In our implementation, we invert for the velocity and the image simultaneously through a dual objective function. Application to the Marmousi model demonstrates the features of the approach.
AB - Using both the image and data domains to perform velocity inversion can help us resolve the long and short wavelength components of the velocity model, usually in that order. This translates to integrating migration velocity analysis (MVA) into full waveform inversion (FWI). The MVA part of the inversion often requires computing extended images, which is pricy using conventional methods. As a result, we use prestack wavefield (the double-square-root (DSR)) extrapolation, which includes the extended information (subsurface offsets) naturally, to make the process far more efficient and stable. The combination of the forward and adjoint prestack wavefields provides us with update options that can be easily conditioned to improve convergence. We, specifically, use a modified differential semblance operator to divide the extended image to the residual part for classic differential semblance operator (DSO) updates and the image modeling part, which provides reflections for higher resolution information. In our implementation, we invert for the velocity and the image simultaneously through a dual objective function. Application to the Marmousi model demonstrates the features of the approach.
UR - http://www.scopus.com/inward/record.url?scp=85037548811&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.201412571
DO - 10.3997/2214-4609.201412571
M3 - Conference contribution
AN - SCOPUS:85037548811
T3 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
SP - 1490
EP - 1494
BT - 77th EAGE Conference and Exhibition 2015
PB - European Association of Geoscientists and Engineers, EAGE
T2 - 77th EAGE Conference and Exhibition 2015: Earth Science for Energy and Environment
Y2 - 1 June 2015 through 4 June 2015
ER -