Waveform inversion for acoustic VTI media in frequency domain

Handle URI:
http://hdl.handle.net/10754/625267
Title:
Waveform inversion for acoustic VTI media in frequency domain
Authors:
Wu, Zedong; Alkhalifah, Tariq Ali ( 0000-0002-9363-9799 )
Abstract:
Reflected waveform inversion (RWI) provides a method to reduce the nonlinearity of the standard full waveform inversion (FWI) by inverting for the background model using a single scattered wavefield from an inverted perturbation. However, current RWI methods are mostly based on isotropic media assumption. We extend the idea of the combining inversion for the background model and perturbations to address transversely isotropic with a vertical axis of symmetry (VTI) media taking into consideration of the optimal parameter sensitivity information. As a result, we apply Born modeling corresponding to perturbations in only for the variable e to derive the relative reflected waveform inversion formulation. To reduce the number of parameters, we assume the background part of η = ε and work with a single variable to describe the anisotropic part of the wave propagation. Thus, the optimization variables are the horizontal velocity v, η = ε and the e perturbation. Application to the anisotropic version of Marmousi model with a single frequency of 2.5 Hz shows that this method can converge to the accurate result starting from a linearly increasing isotropic initial velocity. Application to a real dataset demonstrates the versatility of the approach.
KAUST Department:
King Abdullah University of Science and Technology, , Saudi Arabia
Citation:
Wu Z, Alkhalifah T (2016) Waveform inversion for acoustic VTI media in frequency domain. SEG Technical Program Expanded Abstracts 2016. Available: http://dx.doi.org/10.1190/segam2016-13867221.1.
Publisher:
Society of Exploration Geophysicists
Journal:
SEG Technical Program Expanded Abstracts 2016
Conference/Event name:
SEG International Exposition and 86th Annual Meeting, SEG 2016
Issue Date:
6-Sep-2016
DOI:
10.1190/segam2016-13867221.1
Type:
Conference Paper
Sponsors:
We thank Bruce VerWest, Esteban D´ıaz and P.J.Wellington for their insights in the CGG data and Operto St´ephane for some useful discussions. The seismic data shown in this abstract is proprietary to and provided courtesy of CGG. The well-log information is provided by Geoscience Australia. We especially thank TonyWeatherall and Lynda Thomas for reviewing our abstract. We thank KAUST for its support and the SWAG group for collaborative environment.
Additional Links:
http://library.seg.org/doi/10.1190/segam2016-13867221.1
Appears in Collections:
Conference Papers

Full metadata record

DC FieldValue Language
dc.contributor.authorWu, Zedongen
dc.contributor.authorAlkhalifah, Tariq Alien
dc.date.accessioned2017-07-26T06:19:11Z-
dc.date.available2017-07-26T06:19:11Z-
dc.date.issued2016-09-06en
dc.identifier.citationWu Z, Alkhalifah T (2016) Waveform inversion for acoustic VTI media in frequency domain. SEG Technical Program Expanded Abstracts 2016. Available: http://dx.doi.org/10.1190/segam2016-13867221.1.en
dc.identifier.doi10.1190/segam2016-13867221.1en
dc.identifier.urihttp://hdl.handle.net/10754/625267-
dc.description.abstractReflected waveform inversion (RWI) provides a method to reduce the nonlinearity of the standard full waveform inversion (FWI) by inverting for the background model using a single scattered wavefield from an inverted perturbation. However, current RWI methods are mostly based on isotropic media assumption. We extend the idea of the combining inversion for the background model and perturbations to address transversely isotropic with a vertical axis of symmetry (VTI) media taking into consideration of the optimal parameter sensitivity information. As a result, we apply Born modeling corresponding to perturbations in only for the variable e to derive the relative reflected waveform inversion formulation. To reduce the number of parameters, we assume the background part of η = ε and work with a single variable to describe the anisotropic part of the wave propagation. Thus, the optimization variables are the horizontal velocity v, η = ε and the e perturbation. Application to the anisotropic version of Marmousi model with a single frequency of 2.5 Hz shows that this method can converge to the accurate result starting from a linearly increasing isotropic initial velocity. Application to a real dataset demonstrates the versatility of the approach.en
dc.description.sponsorshipWe thank Bruce VerWest, Esteban D´ıaz and P.J.Wellington for their insights in the CGG data and Operto St´ephane for some useful discussions. The seismic data shown in this abstract is proprietary to and provided courtesy of CGG. The well-log information is provided by Geoscience Australia. We especially thank TonyWeatherall and Lynda Thomas for reviewing our abstract. We thank KAUST for its support and the SWAG group for collaborative environment.en
dc.publisherSociety of Exploration Geophysicistsen
dc.relation.urlhttp://library.seg.org/doi/10.1190/segam2016-13867221.1en
dc.rightsArchived with thanks to SEG Technical Program Expanded Abstracts 2016en
dc.titleWaveform inversion for acoustic VTI media in frequency domainen
dc.typeConference Paperen
dc.contributor.departmentKing Abdullah University of Science and Technology, , Saudi Arabiaen
dc.identifier.journalSEG Technical Program Expanded Abstracts 2016en
dc.conference.date2011-10-16 to 2011-10-21en
dc.conference.nameSEG International Exposition and 86th Annual Meeting, SEG 2016en
dc.conference.locationDallas, TX, USAen
dc.eprint.versionPublisher's Version/PDFen
kaust.authorWu, Zedongen
kaust.authorAlkhalifah, Tariq Alien
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