We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet frames and Fourier-like transforms that exploits continuity along reflectors in seismic data. By choosing generic transforms, we circumvent the necessity to make parametric assumptions (e.g. through linear/parabolic Radon or demigration) regarding the shape of events in seismic data. Simulation and real data examples for data with moderately sized gaps demonstrate that our algorithm provides interpolated traces that accurately reproduce the wavelet shape as well as the AVO behavior. Our method also shows good results for de-aliasing judged by the behavior of the (f-k)-spectrum before and after regularization.Science, Faculty ofEarth and Ocean Sc...
In this paper we propose a stable high-resolution deconvolution algorithm that combines a priori inf...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Insufficient data often require regularized solutions to inverse problems in geophysics. In other wo...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
We propose an efficient iterative data interpolation method using continuity along reflectors in sei...
We propose an efficient iterative data interpolation method using continuity along reflectors in sei...
A robust data interpolation method using curvelets frames is presented. The advantage of this method...
We propose a method for seismic data interpolation based on 1) the reformulation of the problem as a...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
AbstractA nonlinear singularity-preserving solution to seismic image recovery with sparseness and co...
We propose an efficient iterative curvelet-regularized deconvolution algorithm that exploits continu...
Continuity along reflectors in seismic images is used via Curvelet representation to stabilize the c...
Wavefield reconstruction is a crucial step in the seismic processing flow. For instance, unsuccessfu...
We propose an efficient iterative curvelet-regularized deconvolution algorithm that exploits continu...
In many cases, seismic measurements are coarsely sampled in at least one dimension. This leads to al...
In this paper we propose a stable high-resolution deconvolution algorithm that combines a priori inf...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Insufficient data often require regularized solutions to inverse problems in geophysics. In other wo...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
We propose an efficient iterative data interpolation method using continuity along reflectors in sei...
We propose an efficient iterative data interpolation method using continuity along reflectors in sei...
A robust data interpolation method using curvelets frames is presented. The advantage of this method...
We propose a method for seismic data interpolation based on 1) the reformulation of the problem as a...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
AbstractA nonlinear singularity-preserving solution to seismic image recovery with sparseness and co...
We propose an efficient iterative curvelet-regularized deconvolution algorithm that exploits continu...
Continuity along reflectors in seismic images is used via Curvelet representation to stabilize the c...
Wavefield reconstruction is a crucial step in the seismic processing flow. For instance, unsuccessfu...
We propose an efficient iterative curvelet-regularized deconvolution algorithm that exploits continu...
In many cases, seismic measurements are coarsely sampled in at least one dimension. This leads to al...
In this paper we propose a stable high-resolution deconvolution algorithm that combines a priori inf...
Assuming that transmission responses are known between the surface and a particular depth level in t...
Insufficient data often require regularized solutions to inverse problems in geophysics. In other wo...