International audienceIn this article we present a new method for seismic image restoration. When observed, a seismic image is the result of an initial deposit system that has been transformed by a set of successive geological deformations (flexures, fault slip, etc) that occurred over a large period of time. The goal of seismic restoration consists in inverting the deformations to provide a resulting image that depicts the geological deposit system as it was in a previous state. Providing a tool that quickly generates restored images helps the geophysicists to recognize geological features that may be too strongly altered in the observed image. The proposed approach is based on a minimization process that expresses geological deformations ...
In geosciences, we often need to combine two or images of the same area: in data fusion, we must com...
AbstractA nonlinear singularity-preserving solution to seismic image recovery with sparseness and co...
a) b) c) Figure 1. A seismic image (a) is first unfaulted (b) and then flattened (c) using fault thr...
In this article we present a new method for seismic image restoration. When observed, a seismic imag...
AbstractIn this article we present a new method for seismic image restoration. When observed, a seis...
We present a new method for seismic image restoration. When observed, a seismic image is the result ...
Nous présentons une nouvelle méthode pour la restauration d'images sismiques. Quand on l'observe, un...
A non-linear singularity-preserving solution to the least-squares seismic imaging problem with spars...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
A critical problem in inversion of geophysical data is developing a stable inverse problem solution ...
In this paper, we recover the amplitude of a seismic image by approximating the normal (demigration-...
This thesis will address the large computational costs of solving least-squares migration and full-w...
In this paper, we recover the amplitude of a seismic image by approximating the normal (demigrationm...
Accurate mapping of subsurface structure through seismic techniques is essential in oil and gas expl...
The classical least-squares migration (LSM) translates seismic imaging into a data-fitting optimizat...
In geosciences, we often need to combine two or images of the same area: in data fusion, we must com...
AbstractA nonlinear singularity-preserving solution to seismic image recovery with sparseness and co...
a) b) c) Figure 1. A seismic image (a) is first unfaulted (b) and then flattened (c) using fault thr...
In this article we present a new method for seismic image restoration. When observed, a seismic imag...
AbstractIn this article we present a new method for seismic image restoration. When observed, a seis...
We present a new method for seismic image restoration. When observed, a seismic image is the result ...
Nous présentons une nouvelle méthode pour la restauration d'images sismiques. Quand on l'observe, un...
A non-linear singularity-preserving solution to the least-squares seismic imaging problem with spars...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
A critical problem in inversion of geophysical data is developing a stable inverse problem solution ...
In this paper, we recover the amplitude of a seismic image by approximating the normal (demigration-...
This thesis will address the large computational costs of solving least-squares migration and full-w...
In this paper, we recover the amplitude of a seismic image by approximating the normal (demigrationm...
Accurate mapping of subsurface structure through seismic techniques is essential in oil and gas expl...
The classical least-squares migration (LSM) translates seismic imaging into a data-fitting optimizat...
In geosciences, we often need to combine two or images of the same area: in data fusion, we must com...
AbstractA nonlinear singularity-preserving solution to seismic image recovery with sparseness and co...
a) b) c) Figure 1. A seismic image (a) is first unfaulted (b) and then flattened (c) using fault thr...