2022
DOI: 10.1038/s41598-022-26488-1
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Seismic inversion with L2,0-norm joint-sparse constraint on multi-trace impedance model

Abstract: Impedance inversion of post-stack seismic data is a key technology in reservoir prediction and characterization. Compared to the common used single-trace impedance inversion, multi-trace impedance simultaneous inversion has many advantages. For example, it can take lateral regularization constraint to improve the lateral stability and resolution. We propose to use the L2,0-norm of multi-trace impedance model as a regularization constraint in multi-trace impedance inversion in this paper. L2,0-norm is a joint-s… Show more

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Cited by 4 publications
(2 citation statements)
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“…The (p, 0)-norm of a matrix is obtained from the definition in (1) with r = 0. This norm counts the number of rows in its matrix argument that contain nonzero entries, and hence enforces row-sparsity [22], [58]. Thus, in our case, the constraint of the joint sparsity assumption implies that the matrix [Vec ℓ (G), Vec ℓ ( B)] is a row-sparse matrix, i.e.…”
Section: Cmlementioning
confidence: 99%
“…The (p, 0)-norm of a matrix is obtained from the definition in (1) with r = 0. This norm counts the number of rows in its matrix argument that contain nonzero entries, and hence enforces row-sparsity [22], [58]. Thus, in our case, the constraint of the joint sparsity assumption implies that the matrix [Vec ℓ (G), Vec ℓ ( B)] is a row-sparse matrix, i.e.…”
Section: Cmlementioning
confidence: 99%
“…This goal is normally achieved by finding the solutions to an ill-posed and highly nonlinear geophysical inverse problem accounting for nonunique solutions, due to noise in the recorded geophysical data and assumed models during data processing 1,[6][7][8] . When fullstack seismic reflection data is inverted, the subsurface acoustic impedance (𝐈 𝐩 ) can be used as the facies-dependent elastic property to model the relationship between facies and observed seismic data (𝐝 𝐨𝐛𝐬 ) domains 7,9 . The prediction of facies from fullstack seismic data can be summarized as follows: synthetic seismic data is calculated from a facies pattern using the colocated 𝐈 𝐏 distribution; the solutions to the inverse problem are the facies patterns that minimize the misfit between synthetic seismic data and 𝐝 𝐨𝐛𝐬 6, [10][11][12] .…”
Section: Introductionmentioning
confidence: 99%