Registration-guided least-squares waveform inversion

Full waveform inversion with frequency sweeping cannot start from zero frequency because of the lack of low-frequency data, requiring a good starting model. We study a di fferent iterative scheme where the notion of proximity of two traces is not the usual least-squares distance, but instead involve...

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Main Authors: Baek, Hyoungsu, Calandra, Henri, Demanet, Laurent
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Language:en_US
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2014
Subjects:
Online Access:http://hdl.handle.net/1721.1/90511
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author Baek, Hyoungsu
Calandra, Henri
Demanet, Laurent
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Baek, Hyoungsu
Calandra, Henri
Demanet, Laurent
author_sort Baek, Hyoungsu
collection MIT
description Full waveform inversion with frequency sweeping cannot start from zero frequency because of the lack of low-frequency data, requiring a good starting model. We study a di fferent iterative scheme where the notion of proximity of two traces is not the usual least-squares distance, but instead involves registration as in image processing. In order to create transported data, we introduce a nonconvex optimization problem and solve it in a multiscale fashion from low to high frequencies. This process requires defining low-frequency augmented signals in order to seed the frequency sweep at zero frequency. Successful registrations of noisy data, and application of the new method to model velocity estimation are demonstrated. In a crosshole seismic inversion example (transmission setting), we show that the new method decreases the model velocity error while conventional least-squares inversion converges to a spurious model.
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spelling mit-1721.1/905112019-04-11T09:46:10Z Registration-guided least-squares waveform inversion Baek, Hyoungsu Calandra, Henri Demanet, Laurent Massachusetts Institute of Technology. Earth Resources Laboratory FWI Inversion Full waveform inversion with frequency sweeping cannot start from zero frequency because of the lack of low-frequency data, requiring a good starting model. We study a di fferent iterative scheme where the notion of proximity of two traces is not the usual least-squares distance, but instead involves registration as in image processing. In order to create transported data, we introduce a nonconvex optimization problem and solve it in a multiscale fashion from low to high frequencies. This process requires defining low-frequency augmented signals in order to seed the frequency sweep at zero frequency. Successful registrations of noisy data, and application of the new method to model velocity estimation are demonstrated. In a crosshole seismic inversion example (transmission setting), we show that the new method decreases the model velocity error while conventional least-squares inversion converges to a spurious model. 2014-10-02T13:00:58Z 2014-10-02T13:00:58Z 2013-01-15 Technical Report http://hdl.handle.net/1721.1/90511 en_US Earth Resources Laboratory Industry Consortia Annual Report;2013-29 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle FWI
Inversion
Baek, Hyoungsu
Calandra, Henri
Demanet, Laurent
Registration-guided least-squares waveform inversion
title Registration-guided least-squares waveform inversion
title_full Registration-guided least-squares waveform inversion
title_fullStr Registration-guided least-squares waveform inversion
title_full_unstemmed Registration-guided least-squares waveform inversion
title_short Registration-guided least-squares waveform inversion
title_sort registration guided least squares waveform inversion
topic FWI
Inversion
url http://hdl.handle.net/1721.1/90511
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AT calandrahenri registrationguidedleastsquareswaveforminversion
AT demanetlaurent registrationguidedleastsquareswaveforminversion