The representation of viscoelastic media in the time domain becomes more challenging with greater bandwidth of the propagating waves and number of travelled wavelengths. With the continuously increasing computational power, more extreme parameter regimes become ac-cessible, which requires the reassessment and improvement of the standard ‘memory variable’ methods to implement attenuation in time-domain seismic wave-propagation methods. In this paper, we propose a method to minimize the error in the wavefield for a fixed complexity of the anelastic medium. This method consists of defining an appropriate misfit criterion based on a first-order analysis of how errors in the discretized medium propagate into errors in the wavefield and a simulat...
We derive an expression for the error introduced by the second-order accurate temporal finitediffere...
We apply the method of Support Operators (SOM) to solve the three dimensional, viscoelastic equation...
Forward modelling of seismic waves is an essential tool in the determination of the underlying struc...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
International audienceThis article concerns the numerical modeling of time-domain mechanical waves i...
In recent years, it has been recognized that the seismic wave equation solved with a finite-differen...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
International audienceIn this paper, we study 3-D multiparameter full waveform inversion (FWI) in vi...
We derive an expression for the error introduced by the second-order accurate temporal finitediffere...
We apply the method of Support Operators (SOM) to solve the three dimensional, viscoelastic equation...
Forward modelling of seismic waves is an essential tool in the determination of the underlying struc...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
International audienceThis article concerns the numerical modeling of time-domain mechanical waves i...
In recent years, it has been recognized that the seismic wave equation solved with a finite-differen...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
International audienceIn this paper, we study 3-D multiparameter full waveform inversion (FWI) in vi...
We derive an expression for the error introduced by the second-order accurate temporal finitediffere...
We apply the method of Support Operators (SOM) to solve the three dimensional, viscoelastic equation...
Forward modelling of seismic waves is an essential tool in the determination of the underlying struc...