Many methods exist for interpolation of seismic data in one and two spatial dimensions, but few can interpolate properly in three or four spatial dimensions. Marine multi-streamer data typically are sampled relatively well in the midpoint and absolute offset coordinates but not in the azimuth because the crossline shot coordinate is significantly under sampled. We approach the problem of interpolation of marine-streamer data in four spatial dimensions by splitting the problem into a 1D interpolation along the densely sampled streamers and a 3D Fourier reconstruction for the remaining spatial coordinates. In Fourier reconstruction, the Fourier coefficients that synthesize the nonuniformly sampled seismic data are estimated in a least-squares...
Seismic data are often irregularly and inadequately sampled spatially due to economic and logistic c...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
In 3D seismic data acquisition, sufficiently dense spatial sampling is most often not possible, beca...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
Many seismic processing techniques, for example migration, have strict requirements on the regular s...
Interpolation of seismic data has received renewed attention over he last few years with the widespr...
Fourier reconstruction is basically a linear inverse problem that attempts to recover the Fourier sp...
been developed for marine streamer surveys. Marine data are usual-GEOPHYSICS, VOL. 74, NO. 6 NOVEMBE...
We present the theory and numerical results for interferomet-rically interpolating 3D marine surface...
One of the main challenges of 3-D reflection seismology is providing the spatial sampling required t...
Seismic exploration in complex geological settings and shallow geological targets has led to a deman...
Least-squares Fourier reconstruction is basically a discrete linear inverse problem that attempts to...
Constrained by practical and economical considerations, one often uses seismic data with missing tra...
Seismic data acquisition is frequently carried out at irregular sampling intervals along spatial coo...
Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation ...
Seismic data are often irregularly and inadequately sampled spatially due to economic and logistic c...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
In 3D seismic data acquisition, sufficiently dense spatial sampling is most often not possible, beca...
In seismic exploration an image of the subsurface is generated from seismic data through various dat...
Many seismic processing techniques, for example migration, have strict requirements on the regular s...
Interpolation of seismic data has received renewed attention over he last few years with the widespr...
Fourier reconstruction is basically a linear inverse problem that attempts to recover the Fourier sp...
been developed for marine streamer surveys. Marine data are usual-GEOPHYSICS, VOL. 74, NO. 6 NOVEMBE...
We present the theory and numerical results for interferomet-rically interpolating 3D marine surface...
One of the main challenges of 3-D reflection seismology is providing the spatial sampling required t...
Seismic exploration in complex geological settings and shallow geological targets has led to a deman...
Least-squares Fourier reconstruction is basically a discrete linear inverse problem that attempts to...
Constrained by practical and economical considerations, one often uses seismic data with missing tra...
Seismic data acquisition is frequently carried out at irregular sampling intervals along spatial coo...
Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation ...
Seismic data are often irregularly and inadequately sampled spatially due to economic and logistic c...
We present a robust iterative sparseness-constrained interpolation algorithm using 2/3D curvelet fra...
In 3D seismic data acquisition, sufficiently dense spatial sampling is most often not possible, beca...