Akrabou Formation | |
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Stratigraphic range: latest Cenomanian to ?middle Turonian ~ | |
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 | Morocco, Algeria |
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 apart 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]