International audienceThe quality of focusing panels (Common Image Gathers) plays a fundamental role in the construction of the macro-model via image domain techniques. Recent works demonstrated that iterative least-squares migration is recommended for obtaining reliable focusing panels: this ensures relevant tomographic macro-velocity updates. In practice, iterative least-squares migration needs to be accelerated through suitable pre-conditioners such as pseudo-inverses of the forward modelling operator. The pseudo-inverses are currently limited to the constant density acoustic case. In this paper, we first discuss the impact of density variations on focusing panels, and then propose an approach to quantitatively reconstruct two acoustic p...
Full waveform inversion (FWI) is a nonlinear PDE constrained optimization problem, which seeks to es...
We introduce an approach to velocity and reflectivity estimation based on optimizing the coherence o...
Seismic imaging is one of the most effective methods for estimating the Earth’s physical parameters ...
International audienceFor quantitative seismic imaging, iterative least-squares reverse time migrati...
Migration velocity analysis with the constant-density acoustic wave equation can be accomplished by ...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
International audienceElastic least-squares reverse time migration is a state-of-the-art linear imag...
Density and bulk modulus variations in an acoustic earth are separately recoverable from standard re...
We present a stochastic full-waveform inversion that uses genetic algorithms (GA FWI) to estimate ac...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
This paper introduces an iterative scheme for acoustic model inversion where the notion of proximity...
International audienceSUMMARY Iterative least-squares reverse time migration (LSRTM) is the state-of...
International audienceAmong different migration algorithms, least-squares reverse-time migration is ...
This paper proposes a reflectivity constraint for velocity estimation to optimally solve the inverse...
We present a stochastic full-waveform inversion that makes use of a genetic algorithm to estimate ac...
Full waveform inversion (FWI) is a nonlinear PDE constrained optimization problem, which seeks to es...
We introduce an approach to velocity and reflectivity estimation based on optimizing the coherence o...
Seismic imaging is one of the most effective methods for estimating the Earth’s physical parameters ...
International audienceFor quantitative seismic imaging, iterative least-squares reverse time migrati...
Migration velocity analysis with the constant-density acoustic wave equation can be accomplished by ...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
International audienceElastic least-squares reverse time migration is a state-of-the-art linear imag...
Density and bulk modulus variations in an acoustic earth are separately recoverable from standard re...
We present a stochastic full-waveform inversion that uses genetic algorithms (GA FWI) to estimate ac...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
This paper introduces an iterative scheme for acoustic model inversion where the notion of proximity...
International audienceSUMMARY Iterative least-squares reverse time migration (LSRTM) is the state-of...
International audienceAmong different migration algorithms, least-squares reverse-time migration is ...
This paper proposes a reflectivity constraint for velocity estimation to optimally solve the inverse...
We present a stochastic full-waveform inversion that makes use of a genetic algorithm to estimate ac...
Full waveform inversion (FWI) is a nonlinear PDE constrained optimization problem, which seeks to es...
We introduce an approach to velocity and reflectivity estimation based on optimizing the coherence o...
Seismic imaging is one of the most effective methods for estimating the Earth’s physical parameters ...