We derive a fast acoustic inversion method for a piecewise homogeneous horizontally layered medium. The method obtains medium parameters from the reflection response. The method can be implemented to obtain the parameters on either side of a reflector at an arbitrary depth. Three processing steps lead to the inversion result. First, we solve a modified Marchenko type equation to obtain a focusing wavefield. We then apply wavefield continuation across a reflecting boundary to the focusing wavefield and retrieve the reflection coefficient of a reflector as a function of horizontal slowness. Finally, we use the reflection coefficient to obtain the velocities and the ratio of the densities above and below the reflector. Because the two-way trav...
This paper analyzes the nonlinear correspondence between the re-flectivity profile (model) and the p...
Density and bulk modulus variations in an acoustic earth are separately recoverable from standard re...
Radar data collected on two sides of a horizontally dissipative layered medium are required to inver...
We derive a fast acoustic inversion method for a piecewise homogeneous horizontally layered medium. ...
Acoustic inversion in one-dimension gives impedance as a function of travel time.Inverting the refle...
We present a data driven method of full waveform inversion in one dimension. This means that the inv...
The increasing demand for oil and gas in the world today drives the need for new and improved method...
Two wavefields can be retrieved from the measured reflection response at the surface. One is the Gre...
Surface waves are often used to estimate a near-surface shear-velocity profile. The inverse problem ...
A fast algorithm for recovering profiles of density and Lame parameters as functions of depth for th...
I have developed a Direct Waveform Inversion (DWI) scheme to simultaneously address several existing...
International audienceFull-waveform inversion is re-emerging as a powerful data-fitting procedure fo...
A modified implementation of Marchenko redatuming leads to a filter that removes internal multiples ...
We present an imaging method that creates a map of reflection coefficients in correct one-way time w...
Migration, velocity and amplitude analysis are the employed processing steps to find the desired sub...
This paper analyzes the nonlinear correspondence between the re-flectivity profile (model) and the p...
Density and bulk modulus variations in an acoustic earth are separately recoverable from standard re...
Radar data collected on two sides of a horizontally dissipative layered medium are required to inver...
We derive a fast acoustic inversion method for a piecewise homogeneous horizontally layered medium. ...
Acoustic inversion in one-dimension gives impedance as a function of travel time.Inverting the refle...
We present a data driven method of full waveform inversion in one dimension. This means that the inv...
The increasing demand for oil and gas in the world today drives the need for new and improved method...
Two wavefields can be retrieved from the measured reflection response at the surface. One is the Gre...
Surface waves are often used to estimate a near-surface shear-velocity profile. The inverse problem ...
A fast algorithm for recovering profiles of density and Lame parameters as functions of depth for th...
I have developed a Direct Waveform Inversion (DWI) scheme to simultaneously address several existing...
International audienceFull-waveform inversion is re-emerging as a powerful data-fitting procedure fo...
A modified implementation of Marchenko redatuming leads to a filter that removes internal multiples ...
We present an imaging method that creates a map of reflection coefficients in correct one-way time w...
Migration, velocity and amplitude analysis are the employed processing steps to find the desired sub...
This paper analyzes the nonlinear correspondence between the re-flectivity profile (model) and the p...
Density and bulk modulus variations in an acoustic earth are separately recoverable from standard re...
Radar data collected on two sides of a horizontally dissipative layered medium are required to inver...