S. Lallam et al., EVIDENCE OF TETHYSIAN MARGIN DYNAMIC FROM HETTANGIAN TO AALENIAN AGE IN THE DORSALE CALCAIRE (TETOUAN, RIF, MOROCCO), Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 324(11), 1997, pp. 923-930
The external Dorsal cherry limestones and breccias of Sinemurian-Plien
sbachian age, that crop out near Tetouan, correspond to various facies
, deposited by low, middle and high density turbidity currents and gra
vity flows along carbonate slopes. They are closely related to early T
ethyian rifting movements, which began in the Hettangian age and conti
nued until the Toarcian-Aalenian.