International audienceMigration velocity analysis is a method devoted to the evaluation of both reflectivity and background velocity models, associated with the high and low wavenumber components of the model, respectively. Inversion velocity analysis is one of its improved versions, leading to more stable background velocity updates. Still, the impact of the user parameters should be understood for an optimal update of the background velocity. We show that a sign reversal of the background velocity gradient could occur when the selected surface offset range or the space lag range is too small. We derive the theoretical limits and check their consistency through simulations in a simple model with a single interface. These guidelines determi...
Waveform (output least squares) inversion of seismic reflection data can reconstruct remarkably deta...
International audienceFull Waveform Inversion (FWI) is a data-fitting method that allows retrieving ...
Abstract-In this paper, ray theoretical amplitudes and travel times are calculated in slightly pertu...
International audienceMigration velocity analysis is a method devoted to the evaluation of both refl...
Abstract: Inversion velocity analysis is a variant of wave equation migration velocity analysis, bas...
International audienceThe determination of background velocity by Full Waveform Inversion (FWI) is k...
International audienceMigration velocity analysis aims at determining the background velocity model....
In conventional migration velocity analysis methods, a velocity model is estimated that results in f...
b)a) Figure 1. Slowness models computed with (a) conventional full waveform inversion and (b) full w...
International audienceMigration velocity analysis is a family of methods aiming at automatically rec...
Migration velocity analysis with the wave equation can be accomplished by focusing of extended migra...
Migration velocity analysis with the wave equation can be accomplished by focusing of extended migra...
Image-domain seismic inversion with subsurface offset extension may converge to kinematically accura...
International audienceIn the context of velocity model building, we examine if the velocity models o...
Active seismic experiments are widely used to characterize the structure of the subsurface. Migratio...
Waveform (output least squares) inversion of seismic reflection data can reconstruct remarkably deta...
International audienceFull Waveform Inversion (FWI) is a data-fitting method that allows retrieving ...
Abstract-In this paper, ray theoretical amplitudes and travel times are calculated in slightly pertu...
International audienceMigration velocity analysis is a method devoted to the evaluation of both refl...
Abstract: Inversion velocity analysis is a variant of wave equation migration velocity analysis, bas...
International audienceThe determination of background velocity by Full Waveform Inversion (FWI) is k...
International audienceMigration velocity analysis aims at determining the background velocity model....
In conventional migration velocity analysis methods, a velocity model is estimated that results in f...
b)a) Figure 1. Slowness models computed with (a) conventional full waveform inversion and (b) full w...
International audienceMigration velocity analysis is a family of methods aiming at automatically rec...
Migration velocity analysis with the wave equation can be accomplished by focusing of extended migra...
Migration velocity analysis with the wave equation can be accomplished by focusing of extended migra...
Image-domain seismic inversion with subsurface offset extension may converge to kinematically accura...
International audienceIn the context of velocity model building, we examine if the velocity models o...
Active seismic experiments are widely used to characterize the structure of the subsurface. Migratio...
Waveform (output least squares) inversion of seismic reflection data can reconstruct remarkably deta...
International audienceFull Waveform Inversion (FWI) is a data-fitting method that allows retrieving ...
Abstract-In this paper, ray theoretical amplitudes and travel times are calculated in slightly pertu...