Akrabou Formation | |
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Stratigraphic range: latest Cenomanian to ?middle Turonian ~ | |
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Type | Geological formation |
Sub-units | Agoult, Goulmima, others |
Overlies | Kem Kem Group |
Lithology | |
Primary | Limestone |
Location | |
Coordinates | 30°30′N 4°48′W / 30.5°N 4.8°W |
Approximate paleocoordinates | 17°48′N 4°48′W / 17.8°N 4.8°W |
Region | Er Rachidia |
Country | ![]() ![]() |
Extent | central and eastern Morocco north and south of the Pre-African Trough |
Type section | |
Named by | El Mostafa Ettachfini, Bernard Andreu |
Year defined | 2004 |
The Akrabou Formation is a Late Cretaceous (latest Cenomanian to early/mid Turonian)-aged geological formation and Konservat-Lagerstätte in Morocco.[1] It overlies the slightly older freshwater deposits of the Kem Kem Group, which it was once thought to be a part of. It was deposited over following the Kem Kem ecosystem's submergence by the Tethys Ocean during a marine transgression from the Cenomanian-Turonian boundary event, as part of a wider deposition of carbonate platforms across the region from the event.[2][3][4]