Synthetic seismograms enable to model the theoretical seismic response of the Earth interior due to different structural features and changes in the physical properties of crust and mantle. This approximation provides a best understanding of the real seismic data recorded in field experiments. In this paper, we are showing the development and application of a new scheme based on a multi-order explicit finite-difference algorithm for acoustic waves in a 2D heterogeneous media. The results of the modeling are compared with the seismic data acquired within the SIMA project providing new insight about the internal structure of the subsurface allowing improving the velocity model obtained in previous works.Peer Reviewe
International audienceWe present a two-dimensional distributional-finite-difference algorithm for mo...
<p>The presence of topography poses a challenge for seismic modeling with finite-difference codes. T...
International audienceTo analyze seismic wave propagation in geological structures, it is possible t...
Forward modeling plays a key role in both the creation of predictive models and the study of the sur...
Summarization: When treating the forward full waveform case, a fast and accurate algorithm for model...
The finite-difference method is applied to compute the seismic response of 2-D in-homogeneous struct...
Recent interest in finite-difference modeling of the wave equation has raised questions regarding th...
Recent interest in finite-difference modeling of the wave equation has raised questions regarding th...
The finite-difference method is among the most popular methods for modelling seismic wave propagatio...
A systematic comparison is carried out between some standard finite difference schemes, regarding th...
We propose a new numerical approach for the solution of the 2D acoustic wave equation to model the p...
Wave propagation phenomena are important in many DOE applications such as nuclear explosion monitori...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
Finding the effect of a structure with known parameters such as geometry, velocity and density under...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
International audienceWe present a two-dimensional distributional-finite-difference algorithm for mo...
<p>The presence of topography poses a challenge for seismic modeling with finite-difference codes. T...
International audienceTo analyze seismic wave propagation in geological structures, it is possible t...
Forward modeling plays a key role in both the creation of predictive models and the study of the sur...
Summarization: When treating the forward full waveform case, a fast and accurate algorithm for model...
The finite-difference method is applied to compute the seismic response of 2-D in-homogeneous struct...
Recent interest in finite-difference modeling of the wave equation has raised questions regarding th...
Recent interest in finite-difference modeling of the wave equation has raised questions regarding th...
The finite-difference method is among the most popular methods for modelling seismic wave propagatio...
A systematic comparison is carried out between some standard finite difference schemes, regarding th...
We propose a new numerical approach for the solution of the 2D acoustic wave equation to model the p...
Wave propagation phenomena are important in many DOE applications such as nuclear explosion monitori...
Abstract We transform the seismic wave equations in 2D inhomogeneous aniso-tropic media into a syste...
Finding the effect of a structure with known parameters such as geometry, velocity and density under...
Seismograms (i.e., recordings of seismic waves that propagate through the earth) can be used to unco...
International audienceWe present a two-dimensional distributional-finite-difference algorithm for mo...
<p>The presence of topography poses a challenge for seismic modeling with finite-difference codes. T...
International audienceTo analyze seismic wave propagation in geological structures, it is possible t...