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

Abstract The High Atlas intracontinental belt is an inverted rift formed along the Northwest
African Craton, between the Central Atlantic Ocean and the Africa-Eurasia plates' …

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 …

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

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 …

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 field study of salt ridges and minibasins of the Moroccan High Atlas near Rich
that shows the along-and across-strike variability of such structures. Salt walls evolved from …

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 …

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 …

Continental passive margins and their hinterlands in the Atlantic realm have been the locus
of many Low Temperature Thermochronology (LTT) and time‐Temperature (t‐T) modelling …