Abstract The end Pliensbachian–Toarcian is characterized by several carbon-cycle
perturbations and faunal turnovers (eg, ammonites and foraminifera), which are most likely …

Based on the interpretation of geological maps, seismic reflection and well data
complemented with a bibliographic compilation and field work in the Rif, we investigate the …

Triassic Keuper evaporites have long been recognized as the main detachment level for
thrusting in the Pyrenean fold–thrust belts. The deformed Late Cretaceous–Eocene foreland …

Abstract The Central High Atlas is distinguished by map-scale, sigmoid, and narrow
magmatic-cored ridges, which separate wide and open synclines. The origin of these …

Subsidence analysis study for several Triassic carbonate platforms from the eastern
Northern Calcareous Alps shows that salt expulsion allowed for the growth of thick isolated …

Standard sequence stratigraphy interpretations are commonly built upon the premise of
fairly constant sediment supply, leaving vast uncertainties about sequence architecture and …

The red detrital formations of the Central and Eastern High Atlas of Morocco continue to
spark a large scientific debate around their age varying from the middle Jurassic to the …

We present a series of 2D thermo-mechanical numerical experiments of thick-skinned
crustal extension including a pre-rift salt horizon and subsequent thin-, thick-skinned, or …

Surface and subsurface data together with balanced cross-sections are used to emphasize
the structural style and regional-scale deformation of the Southern Atlas Front in Tunisia and …

We report the structural geometry and facies architecture of a small diapir-related carbonate-
dominated basin from the Jurassic rift of the Moroccan High Atlas. The Azag minibasin is a …