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dc.contributor.authorLi, Jing
dc.contributor.authorDutta, Gaurav
dc.contributor.authorSchuster, Gerard T.
dc.date.accessioned2017-03-06T11:13:36Z
dc.date.available2017-03-06T11:13:36Z
dc.date.issued2017-02-08
dc.identifier.citationLi J, Dutta G, Schuster G (2017) Wave-equation Qs Inversion of Skeletonized Surface Waves. Geophysical Journal International. Available: http://dx.doi.org/10.1093/gji/ggx051.
dc.identifier.issn0956-540X
dc.identifier.issn1365-246X
dc.identifier.doi10.1093/gji/ggx051
dc.identifier.urihttp://hdl.handle.net/10754/622971
dc.description.abstractWe present a skeletonized inversion method that inverts surface-wave data for the Qs quality factor. Similar to the inversion of dispersion curves for the S-wave velocity model, the complicated surface-wave arrivals are skeletonized as simpler data, namely the amplitude spectra of the windowed Rayleigh-wave arrivals. The optimal Qs model is the one that minimizes the difference in the peak frequencies of the predicted and observed Rayleigh wave arrivals using a gradient-based wave-equation optimization method. Solutions to the viscoelastic wave-equation are used to compute the predicted Rayleigh-wave arrivals and the misfit gradient at every iteration. This procedure, denoted as wave-equation Qs inversion (WQs), does not require the assumption of a layered model and tends to have fast and robust convergence compared to full waveform inversion (FWI). Numerical examples with synthetic and field data demonstrate that the WQs method can accurately invert for a smoothed approximation to the subsurface Qs distribution as long as the Vs model is known with sufficient accuracy.
dc.description.sponsorshipThe research reported in this publication was supported by the King Abdullah University of Science and Technology (KAUST) in Thuwal, Saudi Arabia. We are grateful to the sponsors of the Center for Subsurface Imaging and Modeling (CSIM) consortium for their financial support. For computer time, this research used the resources of the IT Research Computing Group and the Supercomputing Laboratory at KAUST. We thank them for providing the computational resources required for carrying out this work.
dc.publisherOxford University Press (OUP)
dc.relation.urlhttps://academic.oup.com/gji/article/2978033/Wave-equation
dc.rightsThis article has been accepted for publication in Wave-equation Qs Inversion of Skeletonized Surface Waves ©: The Author 2017. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.
dc.subjectSurface waves
dc.subjectattenuation
dc.subjectSkeletonized Qs inversion
dc.titleWave-equation Qs Inversion of Skeletonized Surface Waves
dc.typeArticle
dc.contributor.departmentCenter for Subsurface Imaging and Fluid Modeling
dc.contributor.departmentEarth Science and Engineering Program
dc.contributor.departmentPhysical Science and Engineering (PSE) Division
dc.identifier.journalGeophysical Journal International
dc.eprint.versionPost-print
kaust.personLi, Jing
kaust.personDutta, Gaurav
kaust.personSchuster, Gerard T.
refterms.dateFOA2018-06-13T16:53:54Z
dc.date.published-online2017-02-08
dc.date.published-print2017-05


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