Akil, MustafaGalindo Zaldívar, JesúsTahayt, A.Jabaloy, A.Chabli, A.Ruano, PatriciaChalouan, Ahmed2015-01-282015-01-282000http://hdl.handle.net/10272/9765The Rabat region, located in the northern border of the Moroccan Meseta, is generally considered as a present-day stable region. However, the fluvial and marine sedimentary rocks, with Pliocene and Quaternary ages, are deformed by joints, generally tensional, and by normal and strike-slip faults. The brittle structures indicate N-S compressional deformations, probably related to the present-day regional stresses in the crust, and extensional deformations related to the proximity to the Gharb basinspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Moroccan MesetaRabatRecent tectonicsBrittle deformationsjournal articleopen access