Phanerozoic evolution of Africa
✍ Scribed by Octavian Catuneanu; René Guiraud; Pat Eriksson; Bob Thomas; Russell Shone; Roger Key
- Book ID
- 104019893
- Publisher
- Elsevier Science
- Year
- 2005
- Tongue
- English
- Weight
- 67 KB
- Volume
- 43
- Category
- Article
- ISSN
- 1464-343X
No coin nor oath required. For personal study only.
📜 SIMILAR VOLUMES
The Pan-African event assembled the supercontinent of Gondwana during the Late Proterozoic, and is manifest within the African plate by an anastomosing pattern of tectonic sutures and mobile belts. The development of African basins during the Phanerozoic can be thought of as relating to the polyphas
The Phanerozoic geological evolution of the Equatorial Atlantic domain has been controlled since the end of Early Cretaceous by the Romanche and Saint Paul transform faults. These faults did not follow the PanAfrican shear zones, but were surimposed on Palaeozoic basins. From Neocomian to Barremian,