We present a new numerical method to solve the heterogeneous anelastic seismic wave equa-tions with arbitrary high order of accuracy in space and time on unstructured triangular and tetrahedral meshes in two and three space dimensions, respectively. Using the velocity-stress formulation provides a linear hyperbolic system of equations with source terms that is com-pleted by additional equations for the anelastic functions including the strain history of the ma-terial. These additional equations result from the rheological model of the generalized Maxwell body and permit the incorporation of realistic attenuation properties of viscoelastic material ac-counting for the behaviour of elastic solids and viscous ßuids. The proposed method relies ...
Summarization: Two finite-difference schemes for solving the elastic wave equation in heterogeneous ...
International audienceA numerical method for longitudinal wave propagation in nonlinear elastic soli...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
We present a new numerical method to solve the heterogeneous anelastic, seismic wave equa-tions with...
We present a new numerical method to solve the heterogeneous elastic anisotropic wave equa-tion with...
Summarization: When treating the forward full waveform case, a fast and accurate algorithm for model...
We present a scheme to solve three-dimensional viscoelastic anisotropic wave propagation on structur...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
We present a high-order discontinuous Galerkin method for the simulation of P-SV seismic wave propag...
The paper aims at presenting a numerical technique used in simulating the propagation of waves in in...
We apply the method of Support Operators (SOM) to solve the three dimensional, viscoelastic equation...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Behavior of acoustic waves in a rapidly-varying heterogeneous medium may be investigated analyticall...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
We present a study of elastic wave propagation in heterogeneous media. The Discontinuous Galerkin Me...
Summarization: Two finite-difference schemes for solving the elastic wave equation in heterogeneous ...
International audienceA numerical method for longitudinal wave propagation in nonlinear elastic soli...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...
We present a new numerical method to solve the heterogeneous anelastic, seismic wave equa-tions with...
We present a new numerical method to solve the heterogeneous elastic anisotropic wave equa-tion with...
Summarization: When treating the forward full waveform case, a fast and accurate algorithm for model...
We present a scheme to solve three-dimensional viscoelastic anisotropic wave propagation on structur...
Real Earth media are not perfectly elastic. Instead, they attenuate propagating mechanical waves. Th...
We present a high-order discontinuous Galerkin method for the simulation of P-SV seismic wave propag...
The paper aims at presenting a numerical technique used in simulating the propagation of waves in in...
We apply the method of Support Operators (SOM) to solve the three dimensional, viscoelastic equation...
Abstract We address the basic theoretical and algorithmic aspects of memory-efficient implementation...
Behavior of acoustic waves in a rapidly-varying heterogeneous medium may be investigated analyticall...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
We present a study of elastic wave propagation in heterogeneous media. The Discontinuous Galerkin Me...
Summarization: Two finite-difference schemes for solving the elastic wave equation in heterogeneous ...
International audienceA numerical method for longitudinal wave propagation in nonlinear elastic soli...
The representation of viscoelastic media in the time domain becomes more challenging with greater ba...