Least-squares diffraction imaging using shaping regularization by anisotropic smoothing

Author:

Merzlikin Dmitrii1ORCID,Fomel Sergey2ORCID,Wu Xinming3ORCID

Affiliation:

1. Formerly Bureau of Economic Geology, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, USA; presently WesternGeco, Schlumberger, 3750 Briarpark Drive, Houston, Texas 77042, USA.(corresponding author).

2. Bureau of Economic Geology, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, USA..

3. Formerly Bureau of Economic Geology, John A. and Katherine G. Jackson School of Geosciences, The University of Texas at Austin, University Station, Box X, Austin, Texas 78713-8924, USA; presently School of Earth and Space Sciences, University of Science and Technology of China, Hefei, China..

Abstract

We have used least-squares migration to emphasize edge diffractions. The inverted forward-modeling operator is the chain of three operators: Kirchhoff modeling, azimuthal plane-wave destruction, and the path-summation integral filter. Azimuthal plane-wave destruction removes reflected energy without damaging edge-diffraction signatures. The path-summation integral guides the inversion toward probable diffraction locations. We combine sparsity constraints and anisotropic smoothing in the form of shaping regularization to highlight edge diffractions. Anisotropic smoothing enforces continuity along edges. Sparsity constraints emphasize diffractions perpendicular to edges and have a denoising effect. Synthetic and field data examples illustrate the effectiveness of the proposed approach in denoising and highlighting edge diffractions, such as channel edges and faults.

Funder

TCCS

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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