Tafraout Group
| Tafraout Group | |
|---|---|
| Stratigraphic range: Toarcian-Aalenian Polymorphum-Bradfordensis | |
Profile at Jebel Akenzoud (Dadès Gorges) where the Tagoudite, Tafraout and Azilal Fms can be seen. (B) Close-up view of the left side ooidal shoal with lateral accretions (white arrows). (C) Stratigraphic correlation. (D) Close up of the right side shoulder. (E) Close up on the erosion surface. | |
| Type | Geological Group |
| Sub-units |
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| Underlies |
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| Overlies |
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| Thickness | 3,000 m (9,800 ft) |
| Lithology | |
| Primary |
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| Location | |
| Location | Assif Tafraout |
| Coordinates | 31°29′N 5°35′W / 31.49°N 5.58°W |
| Approximate paleocoordinates | 26°36′N 3°24′W / 26.6°N 3.4°W |
| Region | High Atlas and Middle Atlas |
| Country | Morocco |
| Type section | |
| Named for | Douar Tafraout near Jbel/Assif Tafraout |
| Named by | Abdellah Milhi |
| Location | Right side valley of Assif Tafraout. The village of Tafraout lies about 1 km to the north |
| Year defined | 1992 |
| Region | Taghia, Southern Béni Mellal-Khénifra |
| Thickness at type section | ~2,200 m (7,200 ft) |
Tafraout Group (Morocco) | |
The Tafraout Group (Full name: Douar Tafraout Group, to not confuse it with Tafraout in other region, also known as "Zawyat Ahançal Group") is a geological group of Toarcian-Aalenian (Lower Jurassic-Middle Jurassic) age in the Azilal, Béni-Mellal, Imilchil, Zaouiat Ahansal, Ouarzazate, Tinerhir, Tinejdad and Errachidia areas of the High Atlas of Morocco. The Group represents the remnants of a local massive Siliciclastic-Carbonate platform ("Tafraout Platform"), best assigned to succession W-E of fluvial to tidal flat to inner platform to open marine settings, recording a dramatic decrease of the carbonate productivity under increasing terrigenous sedimentation, as well the Toarcian Oceanic Anoxic Event. Fossils include large reef biotas with richness in "lithiotidae" bivalves and coral mounts ("Patch reef", Tafraout Formation), but also by remains of vertebrates such as the sauropod Tazoudasaurus and the basal ceratosaur Berberosaurus, along with several undescribed genera. While there have been attributions of its lowermost layers to the Latest Pliensbachian, the current oldest properly measured are part of the Earliest Toarcian regression ("MRST10").
This group is composed of the following units W-E: the Azilal Formation (continental to subtidal, including its synonyms the "Wazzant Formation", "Continental Series of Toundoute" as well the "Aguerd-nˈTazoult Formation"); the Tafraout I-IV Formations (deposited in a subtidal to inner platform environment, includes the "Amezraï Fm"). They are connected with the offshore Tagoudite Formation, Ait Athmane Formation and the deeper shelf deposits of the Agoudim Formation.