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 accessible, 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 simulate...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
International audienceIn this paper, we study 3-D multiparameter full waveform inversion (FWI) in vi...
In recent years, it has been recognized that the seismic wave equation solved with a finite-differen...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
International audienceThis article concerns the numerical modeling of time-domain mechanical waves i...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
A recursive algorithm to incorporate attenuation into a time-domain finite-difference calculation i...
Earth introduces strong attenuation and dispersion to propagating waves. The time-fractional wave eq...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
International audienceIn this paper, we study 3-D multiparameter full waveform inversion (FWI) in vi...
In recent years, it has been recognized that the seismic wave equation solved with a finite-differen...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
International audienceThis article concerns the numerical modeling of time-domain mechanical waves i...
Accurate seismic exploration demands sophisticated seismic techniques that can be applied to any com...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
Real Earth media are anelastic, which affects both the kinematics and dynamics of propagating waves:...
A recursive algorithm to incorporate attenuation into a time-domain finite-difference calculation i...
Earth introduces strong attenuation and dispersion to propagating waves. The time-fractional wave eq...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Real Earth media is anelastic, which affects both kinematics and dynamics of propagating waves. Wave...
Real sedimentary media can usually be characterized as transverse isotropy. To reveal wave propagati...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
International audienceIn this paper, we study 3-D multiparameter full waveform inversion (FWI) in vi...
In recent years, it has been recognized that the seismic wave equation solved with a finite-differen...