2022
DOI: 10.1007/s10712-022-09725-0
|View full text |Cite
|
Sign up to set email alerts
|

Pre-Stack Seismic Inversion With L1-2-Norm Regularization Via A Proximal DC Algorithm And Adaptive Strategy

Abstract: Seismic inversion in geophysics is an effective way to obtain underground rock properties from seismic survey data on the Earth's surface. Especially, we can obtain much more information to characterize subsurface geological structure and lithology via pre-stack seismic inversion due to offset information added to the inversion than by post-stack seismic inversion. However, pre-stack seismic inversion is usually a nonlinear and complicated process. In this article, we adopt a 12 L  -norm as a constraint on pr… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
0
0

Year Published

2023
2023
2024
2024

Publication Types

Select...
3

Relationship

0
3

Authors

Journals

citations
Cited by 3 publications
(1 citation statement)
references
References 38 publications
0
0
0
Order By: Relevance
“…This type of approach constrains the solution by using sparse norms or long-tailed distributions, imposing it to exhibit blocky features. Typical sparse regularization for impedance inversion includes total-variation regularization [11][12][13][14], L0 norm [15], L1 norm [16,17], L1-2 norm [18,19], Lp (0 < p < 1) norm [20], and Cauchy distribution [21,22]. Although sparse regularization preserves important edge information, it is inadequate for describing the prior information of rock impedance.…”
Section: Introductionmentioning
confidence: 99%
“…This type of approach constrains the solution by using sparse norms or long-tailed distributions, imposing it to exhibit blocky features. Typical sparse regularization for impedance inversion includes total-variation regularization [11][12][13][14], L0 norm [15], L1 norm [16,17], L1-2 norm [18,19], Lp (0 < p < 1) norm [20], and Cauchy distribution [21,22]. Although sparse regularization preserves important edge information, it is inadequate for describing the prior information of rock impedance.…”
Section: Introductionmentioning
confidence: 99%