| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4694717 | Tectonophysics | 2007 | 12 Pages |
Abstract
From an area delimited by spatial distribution of aftershocks, the linear dimension of the fault was estimated. The fault area determined in this study correlates well with those of previous studies which occurred in the Western Rift Valley of Africa including the Tanganyika and Upemba Rift.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Tuluka Mavonga,