Structure, cinématique et chronologie des déformations dans la dorsale du Haouz (Rif, Maroc).

• Autores: Rachid Hlila, Carlos Sanz de Galdeano Equiza
• Localización: Geogaceta, ISSN 0213-683X, Nº. 17, 1994, págs. 95-97
• Idioma: francés
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• 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