| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5785490 | Journal of African Earth Sciences | 2017 | 30 Pages |
Abstract
The thermal variations may be as a result of variations in the geothermal gradient accompanying continental rifting from one district to the other. The variations in the chemistry between the Lower Benue and the Upper Benue paragenic minerals may be as a result of the distinct lithological differences across the Benue Trough.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Ibukun Emmanuel Ogundipe,