We present a new approach to the problem of detecting point diffractors from active source surface seismic data. We formulate an optimization problem in the configuration space of possible collections of scatterers and construct a birth-and-death spatial dynamic, which converges to the optimal solution. By design, this dynamic does not have resolution limits typical of migration based techniques, which allows for subwavelength sensing.Massachusetts Institute of Technology. Earth Resources Laborator
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...
Energy-angle distributions in the local image matrix, which is a function of local incident and rece...
Consider a process of events on a line L, where, for the most part, the events occur randomly in bot...
One of the problems encountered in a variety of near-surface investigations is detecting and mapping...
Detecting small-size objects is a primary challenge at archaeological sites due to the high degree o...
We introduce a new target-oriented localisation technique which does not require picking of events i...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
It is both an experimental and theoretical fact that imaging of scatterers using bandlimited signals...
International audienceWe describe a time-resolved monitoring technique for heterogeneous media. Our ...
International audienceDiffracted waves carry high-resolution information that can help interpreting ...
We investigated the construction of diffraction kernels (DKs) for surface waves using two-point conv...
International audienceNumerical experiments of seismic wave propagation in a laterally homogeneous l...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...
Energy-angle distributions in the local image matrix, which is a function of local incident and rece...
Consider a process of events on a line L, where, for the most part, the events occur randomly in bot...
One of the problems encountered in a variety of near-surface investigations is detecting and mapping...
Detecting small-size objects is a primary challenge at archaeological sites due to the high degree o...
We introduce a new target-oriented localisation technique which does not require picking of events i...
One of the main objectives of seismic interpretation is the identification and positioning of struct...
It is both an experimental and theoretical fact that imaging of scatterers using bandlimited signals...
International audienceWe describe a time-resolved monitoring technique for heterogeneous media. Our ...
International audienceDiffracted waves carry high-resolution information that can help interpreting ...
We investigated the construction of diffraction kernels (DKs) for surface waves using two-point conv...
International audienceNumerical experiments of seismic wave propagation in a laterally homogeneous l...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Diffracted waves are seismic waves that backscatter from localized discontinuities in the earth. The...
Discontinuities and small structures induce diffractions on seismic or ground-penetrating radar (GPR...
Energy-angle distributions in the local image matrix, which is a function of local incident and rece...
Consider a process of events on a line L, where, for the most part, the events occur randomly in bot...