Abstract
An algorithm is presented to solve the elastic-wave equation by replacing the partial differentials with finite differences. It enables wave propagation to be simulated in three dimensions through generally anisotropic and heterogeneous models. The use of finite difference approximations to the partial derivatives results in a frequency-dependent error in the group and phase velocities of waves. For anisotropic media, the use of staggered grids implies that some of the elements of the stress and strain tensors must be interpolated to calculate the Hook sum. This interpolation induces an additional error in the wave properties. The overall error depends on the precision of the derivative and interpolation operators, the anisotropic symmetry system, its orientation and the degree of anisotropy. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1203-1216 |
| Number of pages | 14 |
| Journal | Geophysics |
| Volume | 60 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1995 |
ASJC Scopus subject areas
- Geochemistry and Petrology
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