Résumé
On the southern margin of the Western Mediterranean sea, the Moroccan Rif Cordillera is a thin-skinned fold and thrust belt resulting from the NW-SE convergence between the African and Eurasian lithospheric plates. At the present-day, the kinematics of the W and S borders of the Rif are characterized by active thrusting consistent with the compressional setting. However, in the NE Rif, the present-day deformation is characterized by normal/transtensional faults oblique to the convergence and coeval with regional uplift movement. How did extensional/transtensional faults set up in a compressive regional stress field? And then how to explain uplift in this extensional pattern? In order to better constrain the present-day deformation in the NE Rif, we present results of morphotectonics and quaternary geochronology analysis performed along N-S (the Trougout, Rouadi and Boujibar conjugated faults) and NE-SW faults (the Nekor faults) surrounding the Al-Hoceima Bay hit by two destructives earthquakes in 1994 (Mw approximately 6) and 2004 (Mw approximately 6.4). High-resolution Digital Elevation Models (DEM) of depleted alluvial/marine markers and faults scarps coupled to (super 14) C and TCN (terrestrial Cosmogenic Nuclides) dating of key sites allow determining (i) vertical and horizontal slip rates of approximately 2 mm/yr and approximately 1.5 mm/yr, respectively along the Trougout transtensional fault, (ii) horizontal slip rate of approximately 1.5 mm/yr along the Nekor sinistral fault and (iii) < 1 mm/yr along the Rouadi and Boujibar normal faults. Cosmogenic (super 10) Be/ (super 3) He dating of perched fluvial and marine surfaces yields an average uplift of approximately 0.2mm/yr consistent with previous U/Th dating. These new morphotectonics constraints are consistent with the occurrence of an asymmetric 15-km wide pull-apart basin structure controlled by two major sinistral faults: the Nekor fault to the south and the Trans-Alboran Shear Zone to the north (?). The eastern side of the bay is likely controlled by the main Trougout fault, while on the western side the deformation is distributed along several minor faults (Rouadi, Boujibar). Whereas the asymmetry of the basin could imply a crustal detachment at the basement level connected to the major Trougout fault at the surface, the South-Westward motion of the basin coupled to the regional uplift suggest a mantle process (delamination and/or slab roll back?).