International audienceNew datings of calcareous sandstone lenses and olistolites exposed in the middle part of the siliciclastic Mouchenkour Formation indicate a Late Asbien/Early Brigantian age (Cfm7/Cfm8 Moroccan biozone). The calcareous microfossil assemblages are characterized by the problematic algae Ungdarella, Fasciella and Koninckopora and foraminifers Archaediscus (concavus stage), Pseudoendothyra and Eostafella. An Asbien/Brigantian palaeogeography based on the depositional environments is reconstructed from northwest to southeast, from the Tizra to the Mouchenkour areas. The units, although in tectonic contacts, nearly preserve their initial location and relations
This sedimentological and palaeontological analysis of the Aptian–Albian sedimentary succession of t...
Analysis of Mississippian coral assemblages from the Khenifra region of Central Morocco together wit...
International audienceThe Essaouira-Agadir Basin (EAB) of Morocco contains the most extensive exposu...
Revision of foraminifers, algae and problematic algae of well-known late Viséan formations in the Je...
Des lentilles gréso-carbonatées et des olistolithes calcaires permettent d\u27attribuer un âge Asbie...
Foraminifera have been used to revise the biostratigraphy of all known Mississippian outcrops in Mor...
Lower Carboniferous from High Atlas of Marrakech (Morocco) : facies, microfossils and fossil traces....
The northern flank of the Tindouf Syncline in southern Morocco exhibits a continuous, well exposed C...
A new early Visean coral assemblage has been recorded from turbidite facies in the southern part of ...
New micropaleontological and palynological datations in the Visean from the Northwestern margin of t...
Foraminifera, Algae and Pseudo-Algae from the Visean of Oulmes area (Morocco). In the Oulmes area (...
The Anti-Atlas area in southern Morocco preserves one of the most complete latest Ediacaran to Cambr...
International audienceAptian to early Albian times are marked by various geodynamic and paleoenviron...
The Djebel Ouarkziz Formation, located in the northern part of the Tindouf Basin, in western Algeria...
This sedimentological and palaeontological analysis of the Aptian–Albian sedimentary succession of t...
Analysis of Mississippian coral assemblages from the Khenifra region of Central Morocco together wit...
International audienceThe Essaouira-Agadir Basin (EAB) of Morocco contains the most extensive exposu...
Revision of foraminifers, algae and problematic algae of well-known late Viséan formations in the Je...
Des lentilles gréso-carbonatées et des olistolithes calcaires permettent d\u27attribuer un âge Asbie...
Foraminifera have been used to revise the biostratigraphy of all known Mississippian outcrops in Mor...
Lower Carboniferous from High Atlas of Marrakech (Morocco) : facies, microfossils and fossil traces....
The northern flank of the Tindouf Syncline in southern Morocco exhibits a continuous, well exposed C...
A new early Visean coral assemblage has been recorded from turbidite facies in the southern part of ...
New micropaleontological and palynological datations in the Visean from the Northwestern margin of t...
Foraminifera, Algae and Pseudo-Algae from the Visean of Oulmes area (Morocco). In the Oulmes area (...
The Anti-Atlas area in southern Morocco preserves one of the most complete latest Ediacaran to Cambr...
International audienceAptian to early Albian times are marked by various geodynamic and paleoenviron...
The Djebel Ouarkziz Formation, located in the northern part of the Tindouf Basin, in western Algeria...
This sedimentological and palaeontological analysis of the Aptian–Albian sedimentary succession of t...
Analysis of Mississippian coral assemblages from the Khenifra region of Central Morocco together wit...
International audienceThe Essaouira-Agadir Basin (EAB) of Morocco contains the most extensive exposu...