Deformaciones plio-cuaternarias en el región de Rabat

1. Akil, M.
2. Galindo Zaldívar, Jesús
3. Tahayt, A.
4. Jabaloy Sánchez, Antonio
5. Chabli, Ahmed
6. Ruano Roca, Patricia
7. Chalouan, Ahmed

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Abstract

The 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 basin

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