RT Conference Proceedings
T1 Structure, cinématique et chronologie des déformations dans la dorsale du Haouz (Rif, Maroc)
T1 Structure kinematic and chronology of deformations in the Haouz Dorsal (Rif, Morocco)
A1 Hlila, Rachid
A1 Sanz de Galdeano, Carlos
AB The complex thrust-slice structure of the Haouz Mountains was formed during the Neogene in several phases, in which we recognize: a- Paroxysmal tectonic events, occurred in the Early Miocene, responsible of the formation of the thrust slices verging towards the W and SW as well as backthrusts verging towards the E and NE. These backthrusts appeared after the blockage of the thrust slices by the Fiysch nappes situated in a more external position, and are interpreted as antiformai stack phenomena. b- Post - paroxysmal tectonic events with lesser importance, alternating as distensive and compressive phases, occurred during the Middle and Late Miocene
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13923
UL http://hdl.handle.net/10272/13923
LA fra
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026