International audienceLeast-squares reverse time migration (RTM) has become the method of choice for quantitative seismic imaging. The main drawback of such a scheme is that it requires many migration/modeling cycles. The convergence of least-squares RTM can be accelerated by using a suitable preconditioner. In the context of an extended domain in variable-density acoustic media, the pseudoinverse Born operator is the recommended preconditioner, providing quantitative results within a single iteration. This method consists of two steps: application of the pseudoinverse Born operator and inversion of two parameters using an efficient weighted least-squares approach based on the Radon transform. As expected, crosstalk artifacts are generated ...
International audienceA seismic processing workflow based on iterative migration/inversion and targe...
Accurate mapping of subsurface structure through seismic techniques is essential in oil and gas expl...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
International audienceAmong different migration algorithms, least-squares reverse-time migration is ...
International audienceFor quantitative seismic imaging, iterative least-squares reverse time migrati...
International audienceElastic least-squares reverse time migration is a state-of-the-art linear imag...
Time-domain elastic least-squares reverse time migration (LSRTM) is formulated as a linearized elast...
Reverse time migration (RTM), for imaging complex Earth models, is a reversal procedure of the forwa...
Seismic imaging is one of the most effective methods for estimating the Earth’s physical parameters ...
The classical least-squares migration (LSM) translates seismic imaging into a data-fitting optimizat...
A seismic processing workflow based on iterative ray + Born migration/inversion and target-oriented ...
Least-squares reverse-time migration (RTM) works with an inverse operation, rather than an adjoint o...
Seismic imaging in geologically complicated areas is playing an extremely important role for hydroca...
International audienceThe quality of focusing panels (Common Image Gathers) plays a fundamental role...
International audienceA seismic processing workflow based on iterative migration/inversion and targe...
Accurate mapping of subsurface structure through seismic techniques is essential in oil and gas expl...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...
International audienceLeast-squares reverse time migration (RTM) has become the method of choice for...
International audienceAmong different migration algorithms, least-squares reverse-time migration is ...
International audienceFor quantitative seismic imaging, iterative least-squares reverse time migrati...
International audienceElastic least-squares reverse time migration is a state-of-the-art linear imag...
Time-domain elastic least-squares reverse time migration (LSRTM) is formulated as a linearized elast...
Reverse time migration (RTM), for imaging complex Earth models, is a reversal procedure of the forwa...
Seismic imaging is one of the most effective methods for estimating the Earth’s physical parameters ...
The classical least-squares migration (LSM) translates seismic imaging into a data-fitting optimizat...
A seismic processing workflow based on iterative ray + Born migration/inversion and target-oriented ...
Least-squares reverse-time migration (RTM) works with an inverse operation, rather than an adjoint o...
Seismic imaging in geologically complicated areas is playing an extremely important role for hydroca...
International audienceThe quality of focusing panels (Common Image Gathers) plays a fundamental role...
International audienceA seismic processing workflow based on iterative migration/inversion and targe...
Accurate mapping of subsurface structure through seismic techniques is essential in oil and gas expl...
In this work, the inverse problem of exploration geophysics is solved through two techniques based o...