2020
DOI: 10.1093/gji/ggaa009
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Eigenvector models for solving the seismic inverse problem for the Helmholtz equation

Abstract: We study the seismic inverse problem for the recovery of subsurface properties in acoustic media. In order to reduce the ill-posedness of the problem, the heterogeneous wave speed parameter is represented using a limited number of coefficients associated with a basis of eigenvectors of a diffusion equation, following the regularization by discretization approach. We compare several choices for the diffusion coefficient in the partial differential equations, which are extracted from the field of image processin… Show more

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Cited by 13 publications
(10 citation statements)
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References 87 publications
(126 reference statements)
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“…Here both the shapes and contrast in amplitude are accurately obtained. We notice some oscillatory noise in the reconstructed models, which could certainly be reduced by incorporating a regularization criterion in the minimization ( [19]).…”
Section: Reconstruction Using Fwimentioning
confidence: 99%
See 1 more Smart Citation
“…Here both the shapes and contrast in amplitude are accurately obtained. We notice some oscillatory noise in the reconstructed models, which could certainly be reduced by incorporating a regularization criterion in the minimization ( [19]).…”
Section: Reconstruction Using Fwimentioning
confidence: 99%
“…For simplicity, we do not encode a regularization term in Equation 6.3 and refer the readers to, e.g., [19,27] and the reference therein.…”
Section: Reconstruction Using Full Waveform Inversionmentioning
confidence: 99%
“…where the choice of misfit function, depending on the data-sets and inverted parameters, is the subject of numerous studies, e.g., [58,28,9,63,35,21,26,23]. Per simplicity, we rely on the l 2 -distance of the difference, such that…”
Section: Reconstruction With Iterative Minimization Fwimentioning
confidence: 99%
“…Recently, it was extended to electromagnetic inverse scattering problems at fixed frequency [9] and also to time-dependent inverse scattering problems when the illuminating source is unknown [10]. In [11], AS decompositions were used for solving 2-D and 3-D seismic inverse problems for the Helmholtz equation. First theoretical estimates for AS decompositions together with an approach for adapting the dimension of the search space were derived in [5].…”
Section: Introductionmentioning
confidence: 99%