RT Journal Article
T1 Fallas de salto en dirección en el Haouz meridional (Complejo de la Dorsal, Rif interno, N de Tetuán, Marruecos). Comparación con las Béticas (España)
T1 Strike-slip faults in the south Haouz (Calcareous Dorsal, Internal Rif, N of Tetouan, Maroc). Comparison with theBetics (Spain)
A1 El Adraoui, A.
A1 Aït Brahim, L.
A1 Sanz de Galdeano, Carlos
AB Different sets of strike-slip faults of the Haouz Mountains (from Tetouan to the strait of Gibraltar) deformthe tectonic slices of the Calcareous Dorsal there present. In this paper we study those faults at thesouthern part of the Haouz. Three fault formation stages can be distinguished and correspond to theprogressive s1 rotation during the Neogene from a near E-W position to approximately N-S, in a progressiveanticlockwise rotation. The faults and other related structures are compared with similar ones existing inthe Betic Cordillera, in equivalent areas of the arc of Gibraltar
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8488
UL http://hdl.handle.net/10272/8488
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026