We consider the problem of constructing a wave extrapolation operator in a variable and possibly anisotropic medium. Our construction involves Fourier transforms in space combined with the help of a lowrank approximation of the space-wavenumber wave-propagator matrix. A lowrank approximation implies selecting a small set of representative spatial locations and a small set of representative wavenumbers. We present a mathematical derivation of this method, a description of the lowrank approximation algorithm and numerical examples that confirm the validity of the proposed approach. Wave extrapolation using lowrank approximation can be ap-plied to seismic imaging by reverse-time migration in 3D heterogeneous isotropic or anisotropic media
The primary factor that prevents full waveform inversion from universal success is the band-limited ...
Depth extrapolation equation used for seismic migration is often solved by finite-difference techniq...
Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation ...
Seismic imaging in geologically complex areas, such as sub-salt or attenuating areas, has been one o...
Elastic wave extrapolation in the time domain is significant for an elastic wave equation-based proc...
textNowadays, subsalt oil and gas exploration is drawing more and more attention from the hydrocarbo...
ABSTRACT Wavefield extrapolation in pseudo-acoustic orthorhombic anisotropic media suffers from wave...
The objective of this paper is to provide a general view on methods of wave field extrapolation as u...
We propose a computationally efficient technique for extrapolating seismic waves in an arbitrary iso...
An explicit algorithm for the extrapolation of one-way wavefields is proposed which combines recent ...
An efficient full 3D wavefield extrapolation technique is presented. The method can be used for any ...
Generally, the seismic industry has been interested more in correct p&e (traveltimes) than in co...
The bandwidth of wave field extrapolation operators in the dou-ble wavenumber domain is directly rel...
Riemannian spaces are described by non-orthogonal curvilinear coordinates. We generalize one-way wav...
The original publication can be found at www.springerlink.com Copyright © 2006 Birkhauser Verlag, Ba...
The primary factor that prevents full waveform inversion from universal success is the band-limited ...
Depth extrapolation equation used for seismic migration is often solved by finite-difference techniq...
Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation ...
Seismic imaging in geologically complex areas, such as sub-salt or attenuating areas, has been one o...
Elastic wave extrapolation in the time domain is significant for an elastic wave equation-based proc...
textNowadays, subsalt oil and gas exploration is drawing more and more attention from the hydrocarbo...
ABSTRACT Wavefield extrapolation in pseudo-acoustic orthorhombic anisotropic media suffers from wave...
The objective of this paper is to provide a general view on methods of wave field extrapolation as u...
We propose a computationally efficient technique for extrapolating seismic waves in an arbitrary iso...
An explicit algorithm for the extrapolation of one-way wavefields is proposed which combines recent ...
An efficient full 3D wavefield extrapolation technique is presented. The method can be used for any ...
Generally, the seismic industry has been interested more in correct p&e (traveltimes) than in co...
The bandwidth of wave field extrapolation operators in the dou-ble wavenumber domain is directly rel...
Riemannian spaces are described by non-orthogonal curvilinear coordinates. We generalize one-way wav...
The original publication can be found at www.springerlink.com Copyright © 2006 Birkhauser Verlag, Ba...
The primary factor that prevents full waveform inversion from universal success is the band-limited ...
Depth extrapolation equation used for seismic migration is often solved by finite-difference techniq...
Extrapolating wavefields and imaging at each depth during three-dimensional recursive wave-equation ...