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Anisotropic forward modeling, boundary CPML
4.0
Two dimensional anisotropic elastic waves, and three dimensional visco elastic seismic wave propagation simulation, the numerical simulation method and CPML (these authors perfect matched layer) of the finite difference time domain (FDTD), the absorption effect of the boundary is the single absorption boundary in the best. MPI compiler.
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Two dimensional anisotropic elastic wave seismic w
4.0
Two-dimensional anisotropic elastic wave seismic wave propagation simulation, using the numerical simulation method and the PML (perfect matched layer) and mixed Collino boundary finite difference time domain (FDTD), absorbed too is superior to the single absorbing boundary.
宋宋 2 0
1
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