Many common processing steps are degraded by static shifts in the data. The effects of static shifts are analogous to noise or missing samples in the data, and therefore can be treated using constraints on sparsity or simplicity. In this paper we show that random static shifts decrease sparsity in the Fourier and Radon transforms, as well as increase the rank of seismic data. We also show that the concepts of sparsity promotion and rank re-duction can be used to solve for static shifts as well as to carry out conventional processes in the presence of statics. The first algorithm presented is a modification to the reinsertion step of Projection Onto Convex Sets (POCS) and Tensor Completion (TCOM) that allows for the compensation of residual ...
Correcting seismic data for the effects of the earth’s near-surface remains a significant problem in...
All the conventional methods for residual statics analysis require normal moveout (NMO) correction a...
According to the principle of compressed sensing (CS), under-sampled seismic data can be interpolate...
The Radon transform (RT) has many desirable properties which make it particularly useful for multip...
The development of new tools for high-resolution seismic imaging has been for many years one of the ...
Seismic signals are generally spread across many data samples of the recorded data. Applying a mathe...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
In seismic data analysis, recorded data often are transformed to various domains to discriminate ag...
The Radon transform (RT) suffers from the typical problems of loss of resolution and aliasing that a...
The purpose of a seismic survey is to produce an image of the subsurface providing an overview of th...
The statics problem, whether short wavelength, long wavelength, residual, or trim, has always been o...
This work determines whether the amount of frequency components present in the data can be reduced, ...
Despite recent developments in improved acquisition, seismic data often remains undersampled along s...
In exploration geophysics the linear Radon transform projects seismic data from time-offset (t-x) d...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
Correcting seismic data for the effects of the earth’s near-surface remains a significant problem in...
All the conventional methods for residual statics analysis require normal moveout (NMO) correction a...
According to the principle of compressed sensing (CS), under-sampled seismic data can be interpolate...
The Radon transform (RT) has many desirable properties which make it particularly useful for multip...
The development of new tools for high-resolution seismic imaging has been for many years one of the ...
Seismic signals are generally spread across many data samples of the recorded data. Applying a mathe...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
In seismic data analysis, recorded data often are transformed to various domains to discriminate ag...
The Radon transform (RT) suffers from the typical problems of loss of resolution and aliasing that a...
The purpose of a seismic survey is to produce an image of the subsurface providing an overview of th...
The statics problem, whether short wavelength, long wavelength, residual, or trim, has always been o...
This work determines whether the amount of frequency components present in the data can be reduced, ...
Despite recent developments in improved acquisition, seismic data often remains undersampled along s...
In exploration geophysics the linear Radon transform projects seismic data from time-offset (t-x) d...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
Correcting seismic data for the effects of the earth’s near-surface remains a significant problem in...
All the conventional methods for residual statics analysis require normal moveout (NMO) correction a...
According to the principle of compressed sensing (CS), under-sampled seismic data can be interpolate...