Jump to content
Wikipedia The Free Encyclopedia

Mauritanide Belt

From Wikipedia, the free encyclopedia
Ancient orogen parallel to the west coast of Africa from Morocco to Guinea-Bissau
Paleogeographic reconstruction of the supercontinent Pangaea, including the Central Pangean Mountains of which the Mauritanide Belt formed a part.

The Mauritanide Belt is an ancient orogen running parallel to the west coast of Africa from Morocco to Guinea-Bissau. The orogeny that formed the Mauritanide Belt was active between 320 and 270 million years ago in the Carboniferous and Permian. During this time period the eastern nappes of the belt thrust over rocks of Devonian age in the Taoudeni Basin. During the Triassic the Mauritanide Belt was split from the Appalachian Mountains (with which it was previously a single orogen) as the Atlantic Ocean opened.[1]

References

[edit ]
Major African geological formations
Plates
Cratons and shields
Shear zones
Orogens
Rifts
Sedimentary basins
Mountain ranges
Inselbergs (aka koppie)


Stub icon

This article about a specific stratigraphic formation in Africa is a stub. You can help Wikipedia by expanding it.

AltStyle によって変換されたページ (->オリジナル) /