The Jurassic evolution of the central Middle Atlas is governed by various factors (climate and eustatism). The use of the concepts of sequential stratigraphy in the regions of Tagnamas and Boulemane allowed to interpret the geometry and the vertical sequence of sedimentary sets. Twelve sequences are identified and delimited by sedimentary discontinuities. The lithostratigraphic division adopted in this study is synchronous with the coastal aggradation charter of Haq & al. (1987 & 1988) and Rioult & al. (1991). The correlations on a regional scale, between different Jurassic lithostratigraphic units is possible, whose the major factors controlling the evolution of intraplate basins are climate and eustatism
Located at the extreme tip of the western Mediterranean, the Betic-Rif orogenic system is built thro...
Les marnes de la partie supérieure de la Formation du Tigri du Crétacé supérieur des Hauts Plateaux ...
The main topic of this work concerns the micropaleontological and sedimentological study of the emer...
The Jurassic evolution of the central Middle Atlas is governed by various factors (climate and eusta...
At the level of the north hillside of the western High Atlas, only the training of limestones and do...
During the Toarcian, shelves undergo block-faulting with mechanisms of tilting. It results the break...
The Atlas system of Morocco during the Jurassic -Structural Evolution and Geodynamic setting During ...
The sedimentological and biostratigraphic study of Upper Cretaceous in the region of Imin'Tanout all...
The South-Rifain ridges are located at 30 Km in the North of Meknes City, they constitute the extrem...
The J. Boudinar is located at the junction between several of the main structural trends of Tunisia ...
Structural study of the recent deformations of the Eç-çour area, located on the southern slope of th...
International audienceL'analyse de la carte aéromagnétique du Moyen Atlas a permis de caractériser l...
Des associations significatives de charophytes et d\u27ostracodes ont été récoltées dans l\u27unité ...
Located at the extreme tip of the western Mediterranean, the Betic-Rif orogenic system is built thro...
Les marnes de la partie supérieure de la Formation du Tigri du Crétacé supérieur des Hauts Plateaux ...
The main topic of this work concerns the micropaleontological and sedimentological study of the emer...
The Jurassic evolution of the central Middle Atlas is governed by various factors (climate and eusta...
At the level of the north hillside of the western High Atlas, only the training of limestones and do...
During the Toarcian, shelves undergo block-faulting with mechanisms of tilting. It results the break...
The Atlas system of Morocco during the Jurassic -Structural Evolution and Geodynamic setting During ...
The sedimentological and biostratigraphic study of Upper Cretaceous in the region of Imin'Tanout all...
The South-Rifain ridges are located at 30 Km in the North of Meknes City, they constitute the extrem...
The J. Boudinar is located at the junction between several of the main structural trends of Tunisia ...
Structural study of the recent deformations of the Eç-çour area, located on the southern slope of th...
International audienceL'analyse de la carte aéromagnétique du Moyen Atlas a permis de caractériser l...
Des associations significatives de charophytes et d\u27ostracodes ont été récoltées dans l\u27unité ...
Located at the extreme tip of the western Mediterranean, the Betic-Rif orogenic system is built thro...
Les marnes de la partie supérieure de la Formation du Tigri du Crétacé supérieur des Hauts Plateaux ...
The main topic of this work concerns the micropaleontological and sedimentological study of the emer...