RT Journal Article
T1 Deformaciones plio-cuaternarias en la region de Rabat
T1 Plio-Quaternary deformations in the Rabat region
A1 Akil, Mustafa
A1 Galindo Zaldívar, Jesús
A1 Tahayt, A.
A1 Jabaloy, A.
A1 Chabli, A.
A1 Ruano, Patricia
A1 Chalouan, Ahmed
AB 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
PB Sociedad Geológica de España
YR 2000
FD 2000
LK http://hdl.handle.net/10272/9765
UL http://hdl.handle.net/10272/9765
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026