| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4729760 | Journal of African Earth Sciences | 2007 | 5 Pages |
Abstract
The southern end of the line with high seismic velocities comprises basement rocks located in the footwall block of the Kunyere Border Fault of the Okavango Rift. The step-wise downthrown hanging wall block consists of the low to intermediate velocity basin deposits in the northern part of the profile.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
K. Laletsang, M.P. Modisi, E.M. Shemang, L. Moffat, O.R. Moagi,