| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6428173 | Earth and Planetary Science Letters | 2015 | 13 Pages |
Abstract
- Seismic model of southern Africa utilizes tomographic inversion of body wave data.
- The Kaapvaal and Zimbabwe fast keels reach depths of â¼350 and â¼250km, respectively.
- Limpopo belt represents a negative velocity perturbations down to a depth of â¼250km.
- Finite-frequency sensitivity kernels allow resolving relatively small-scale anomalies.
- Various resolution tests allow evaluation of the extent of smearing effects.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
M. Youssof, H. Thybo, I.M. Artemieva, A. Levander,