@conference{10272/13923,
year = {1994},
url = {http://hdl.handle.net/10272/13923},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Structure, cinématique et chronologie des déformations dans la dorsale du Haouz (Rif, Maroc)},
title = {Structure kinematic and chronology of deformations in the Haouz Dorsal (Rif, Morocco)},
author = {Hlila, Rachid and Sanz de Galdeano, Carlos},
}