Structure, cinématique et chronologie des déformations dans la dorsale du Haouz (Rif, Maroc).
- Hlila, Rachid
- Sanz de Galdeano Equiza, Carlos
ISSN: 0213-683X
Año de publicación: 1994
Número: 17
Páginas: 95-97
Tipo: Artículo
Otras publicaciones en: Geogaceta
Resumen
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