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model
|  solution format | |
The table below lists the defined models. To see/download a detailed description, please
click an appropriate link to a PDF or ZIP file.
Wave Propagation Model Set
a 3D wavefield due to a DC point source is to be generated in all configurations
| WP1_HSP1a | homogeneous space | elastic | near receivers
| WP1_HSP1b | homogeneous space | elastic | distant receivers
| WP1_HSP2a | homogeneous space | viscoelastic | near receivers
| WP1_HSP2b | homogeneous space | viscoelastic | distant receivers
| WP1_HHS1 | homogeneous halfspace | elastic |
| WP1_HHS2 | homogeneous halfspace | viscoelastic |
| WP2_LOH1 | layer over homogeneous halfspace | elastic |
| WP2_LOH3 | layer over homogeneous halfspace | viscoelastic |
| WP2_AHSP1a | homogeneous space | anisotropic, elastic | near receivers
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E2VP-2 - EuroSeistest Verification and Validation Project, Phase 2
( The project is organized by CEA - Commissariat a l'énergie atomique et aux énergies alternatives, France )
a 3D wavefield due to a point source (DC or single-force) is to be generated in all configurations
| E2VP_Can0 | | unbounded homogeneous isotropic elastic medium with large VP/VS ratio
| E2VP_Can1 |  | homogeneous isotropic elastic halfspace with large VP/VS ratio
| E2VP_Can2 |  | 3 homogenous layers over halfspace, isotropic elastic medium large VP/VS in the surface layer
| E2VP_Can3 |  | 3 gradient layers over halfspace, isotropic elastic medium large VP/VS in the surface layer
| E2VP_Can4 |  | simplified model of the Mygdonian basin, homogeneous layers inside the basin
| E2VP_Can5 |  | simplified model of the Mygdonian basin, gradient layers inside the basin
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