Classical acoustic wave-field representations consist of volume and boundary integrals, of which the integrands contain specific combinations of Green's functions, source distributions, and wave fields. Using a unified matrix-vector wave equation for different wave phenomena, these representations can be reformulated in terms of Green's matrices, source vectors, and wave-field vectors. The matrix-vector formalism also allows the formulation of representations in which propagator matrices replace the Green's matrices. These propagator matrices, in turn, can be expressed in terms of Marchenko-type focusing functions. An advantage of the representations with propagator matrices and focusing functions is that the boundary integrals in these rep...
The term seismic interferometry refers to the principle of generating new seismic responses by cross...
scripts; lower-case Latin subscripts except t run from 1 to 3. In ex-GEOPHYSICS, VOL. 72, NO. 5 SEP...
A Green's function in an acoustic medium can be retrieved from reflection data by solving a multidim...
Marchenko-type integrals typically relate so-called focusing functions and Green's functions via the...
Acoustic, electromagnetic, elastodynamic, poroelastic, and electroseismic waves are all governed by ...
In wave theory, the homogeneous Green’s function consists of the impulse response to a point source,...
Standard Marchenko redatuming and imaging schemes neglect evanescent waves and are based on the assu...
Green's theorem plays a fundamental role in a diverse range of wavefield imaging applications, such ...
The propagator matrix “propagates” a full wave field from one depth level to another, accounting for...
In wave theory, a Green’s function is defined as the response of a medium to an impulsive point sour...
The matrix-vector wave equation is a compact first-order differential equation. It was originally us...
The Marchenko integral, key to inverse scattering problems across many disciplines, is a long-standi...
A general one-way representation of seismic data can be obtained by substituting a Green’s one-way w...
The Gel'fand-Levitan equation, the Gopinath-Sondhi equation, and the Marchenko equation are develope...
Marchenko methods are based on integral representations which express Green’s functions for virtual ...
The term seismic interferometry refers to the principle of generating new seismic responses by cross...
scripts; lower-case Latin subscripts except t run from 1 to 3. In ex-GEOPHYSICS, VOL. 72, NO. 5 SEP...
A Green's function in an acoustic medium can be retrieved from reflection data by solving a multidim...
Marchenko-type integrals typically relate so-called focusing functions and Green's functions via the...
Acoustic, electromagnetic, elastodynamic, poroelastic, and electroseismic waves are all governed by ...
In wave theory, the homogeneous Green’s function consists of the impulse response to a point source,...
Standard Marchenko redatuming and imaging schemes neglect evanescent waves and are based on the assu...
Green's theorem plays a fundamental role in a diverse range of wavefield imaging applications, such ...
The propagator matrix “propagates” a full wave field from one depth level to another, accounting for...
In wave theory, a Green’s function is defined as the response of a medium to an impulsive point sour...
The matrix-vector wave equation is a compact first-order differential equation. It was originally us...
The Marchenko integral, key to inverse scattering problems across many disciplines, is a long-standi...
A general one-way representation of seismic data can be obtained by substituting a Green’s one-way w...
The Gel'fand-Levitan equation, the Gopinath-Sondhi equation, and the Marchenko equation are develope...
Marchenko methods are based on integral representations which express Green’s functions for virtual ...
The term seismic interferometry refers to the principle of generating new seismic responses by cross...
scripts; lower-case Latin subscripts except t run from 1 to 3. In ex-GEOPHYSICS, VOL. 72, NO. 5 SEP...
A Green's function in an acoustic medium can be retrieved from reflection data by solving a multidim...