Global seismic tomography with sparsity constraints: Comparison with smoothing and damping regularization

被引:42
作者
Charlety, Jean [1 ]
Voronin, Sergey [1 ]
Nolet, Guust [1 ]
Loris, Ignace [2 ]
Simons, Frederik J. [3 ]
Sigloch, Karin [4 ]
Daubechies, Ingrid C. [5 ]
机构
[1] Univ Nice Sophia Antipolis, CNRS, UMR 6526, Observ Cote Azur,Geoazur, Valbonne, France
[2] Univ Libre Bruxelles, Dept Math, Brussels, Belgium
[3] Princeton Univ, Dept Geosci, Princeton, NJ 08544 USA
[4] Univ Munich, Dept Earth & Environm Sci, Munich, Germany
[5] Duke Univ, Dept Math, Durham, NC 27706 USA
基金
美国国家科学基金会;
关键词
inversion; finite-frequency tomography; l1 regularized least squares; compressed sensing; LINEAR INVERSE PROBLEMS; THRESHOLDING ALGORITHM; WAVE TOMOGRAPHY; LIFTING SCHEME; TRAVEL-TIME; EQUATIONS; MANTLE; VELOCITIES; SYSTEMS; BASES;
D O I
10.1002/jgrb.50326
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present a realistic application of an inversion scheme for global seismic tomography that uses as prior information the sparsity of a solution, defined as having few nonzero coefficients under the action of a linear transformation. In this paper, the sparsifying transform is a wavelet transform. We use an accelerated iterative soft-thresholding algorithm for a regularization strategy, which produces sparse models in the wavelet domain. The approach and scheme we present may be of use for preserving sharp edges in a tomographic reconstruction and minimizing the number of features in the solution warranted by the data. The method is tested on a data set of time delays for finite-frequency tomography using the USArray network, the first application in global seismic tomography to real data. The approach presented should also be suitable for other imaging problems. From a comparison with a more traditional inversion using damping and smoothing constraints, we show that (1)we generally retrieve similar features, (2)fewer nonzero coefficients under a properly chosen representation (such as wavelets) are needed to explain the data at the same level of root-mean-square misfit, (3)the model is sparse or compressible in the wavelet domain, and (4)we do not need to construct a heterogeneous mesh to capture the available resolution.
引用
收藏
页码:4887 / 4899
页数:13
相关论文
共 51 条
[1]   DEEP-STRUCTURE OF AN ARC-CONTINENT COLLISION - EARTHQUAKE RELOCATION AND INVERSION FOR UPPER MANTLE P AND S-WAVE VELOCITIES BENEATH PAPUA-NEW-GUINEA [J].
ABERS, GA ;
ROECKER, SW .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1991, 96 (B4) :6379-6401
[2]  
[Anonymous], COMPRESSIVE SENSING
[3]  
[Anonymous], 2008, DIFFERENCE
[4]  
[Anonymous], 1997, Wavelets and Filter Banks
[5]  
[Anonymous], WAVELET TOUR SIGNAL
[6]  
[Anonymous], 2001, Ripples in Mathematics
[7]   Estimating nuisance parameters in inverse problems [J].
Aravkin, Aleksandr Y. ;
van Leeuwen, Tristan .
INVERSE PROBLEMS, 2012, 28 (11)
[8]   A Fast Iterative Shrinkage-Thresholding Algorithm for Linear Inverse Problems [J].
Beck, Amir ;
Teboulle, Marc .
SIAM JOURNAL ON IMAGING SCIENCES, 2009, 2 (01) :183-202
[9]   From Sparse Solutions of Systems of Equations to Sparse Modeling of Signals and Images [J].
Bruckstein, Alfred M. ;
Donoho, David L. ;
Elad, Michael .
SIAM REVIEW, 2009, 51 (01) :34-81
[10]   An introduction to compressive sampling: A sensing/sampling paradigm that goes against the common knowledge in data acquisition [J].
Candes, Emmanuel J. ;
Wakin, Michael B. .
IEEE Signal Processing Magazine, 2008, 25 (02) :21-30