@article{10272/9765,
year = {2000},
url = {http://hdl.handle.net/10272/9765},
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},
publisher = {Sociedad Geológica de España},
title = {Deformaciones plio-cuaternarias en la region de Rabat},
title = {Plio-Quaternary deformations in the Rabat region},
author = {Akil, Mustafa and Galindo Zaldívar, Jesús and Tahayt, A. and Jabaloy, A. and Chabli, A. and Ruano, Patricia and Chalouan, Ahmed},
}