The propagator matrix “propagates” a full wave field from one depth level to another, accounting for all propagation angles and evanescent waves. The Marchenko focusing function forms the nucleus of data-driven Marchenko redatuming and imaging schemes, accounting for internal multiples. These seemingly different concepts appear to be closely related to each other. With this insight, the strong aspects of the propagator matrix (such as the handling of evanescent waves) can be transferred to the focusing function. Vice-versa, the propagator matrix inherits from the focusing function that it can be retrieved from the reflection response, which reduces its sensitivity to the subsurface model.Applied Geophysics and Petrophysic
The Marchenko integral, key to inverse scattering problems across many disciplines, is a long-standi...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
Standard Marchenko redatuming and imaging schemes neglect evanescent waves and are based on the assu...
Marchenko redatuming can retrieve the impulse response to a subsurface virtual source from the singl...
Focusing functions are defined as wavefields that focus at a specified location in a heterogeneous s...
Marchenko methods compute a focusing function for a receiver at the acquisition surface and a virtua...
Marchenko-type integrals typically relate so-called focusing functions and Green's functions via the...
Classical acoustic wave-field representations consist of volume and boundary integrals, of which the...
A focussing function is a specially constructed field that focusses on to a purely downgoing pulse a...
Recently, an iterative scheme was introduced to retrieve up- and downgoing Green’s functions at an a...
With the acoustic single-sided Marchenko method it is possible to retrieve the Green’s function of a...
The presence of evanescent modes and their impact on the Marchenko method has been until very recent...
Marchenko imaging is a novel imaging technique that is capable to retrieve images from single-sided ...
Recently, an iterative scheme was introduced to retrieve up- and downgoing Green’s functions at an a...
The Marchenko integral, key to inverse scattering problems across many disciplines, is a long-standi...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...
Standard Marchenko redatuming and imaging schemes neglect evanescent waves and are based on the assu...
Marchenko redatuming can retrieve the impulse response to a subsurface virtual source from the singl...
Focusing functions are defined as wavefields that focus at a specified location in a heterogeneous s...
Marchenko methods compute a focusing function for a receiver at the acquisition surface and a virtua...
Marchenko-type integrals typically relate so-called focusing functions and Green's functions via the...
Classical acoustic wave-field representations consist of volume and boundary integrals, of which the...
A focussing function is a specially constructed field that focusses on to a purely downgoing pulse a...
Recently, an iterative scheme was introduced to retrieve up- and downgoing Green’s functions at an a...
With the acoustic single-sided Marchenko method it is possible to retrieve the Green’s function of a...
The presence of evanescent modes and their impact on the Marchenko method has been until very recent...
Marchenko imaging is a novel imaging technique that is capable to retrieve images from single-sided ...
Recently, an iterative scheme was introduced to retrieve up- and downgoing Green’s functions at an a...
The Marchenko integral, key to inverse scattering problems across many disciplines, is a long-standi...
With the Marchenko method it is possible to retrieve Green's functions between virtual sources in th...
Traditionally, the Marchenko equation forms a basis for 1D inverse scattering problems. A 3D extensi...