Least-squares path-summation diffraction imaging using sparsity constraints

被引:0
|
作者
Merzlikin D. [1 ]
Fomel S. [1 ]
Sen M.K. [2 ]
机构
[1] University of Texas at Austin, Bureau of Economic Geology, Jackson School of Geosciences, University Station, Box X, Austin, 78713-8924, TX
[2] University of Texas at Austin, Institute for Geophysics, John A. and Katherine G. Jackson School of Geosciences, J. J. Pickle Research Campus, 10100 Burnet Road (R2200), Austin, 78758-4445, TX
来源
Geophysics | 2019年 / 84卷 / 03期
关键词
diffraction; faults; inversion; migration;
D O I
10.1190/geo2018-0609.1
中图分类号
TQ [化学工业];
学科分类号
0817 ;
摘要
Diffraction imaging aims to emphasize small-scale subsurface heterogeneities, such as faults, pinch-outs, fracture swarms, channels, etc. and can help seismic reservoir characterization. The key step in diffraction imaging workflows is based on the separation procedure suppressing higher energy reflections and emphasizing diffractions, after which diffractions can be imaged independently. Separation results often contain crosstalk between reflections and diffractions and are prone to noise. We have developed an inversion scheme to reduce the crosstalk and denoise diffractions. The scheme decomposes an input full wavefield into three components: reflections, diffractions, and noise. We construct the inverted forward modeling operator as the chain of three operators: Kirchhoff modeling, plane-wave destruction, and path-summation integral filter. Reflections and diffractions have the same modeling operator. Separation of the components is done by shaping regularization. We impose sparsity constraints to extract diffractions, enforce smoothing along dominant local event slopes to restore reflections, and suppress the crosstalk between the components by local signal-and-noise orthogonalization. Synthetic- and field-data examples confirm the effectiveness of the proposed method. © The Authors.
引用
收藏
页码:S187 / S200
页数:13
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