Deformaciones recientes en el frente de la Cordillera Rifeña (Prerif, Marruecos)

1. Chalouan, Ahmed
2. Galindo Zaldívar, Jesús
3. Bargach, K.
4. Jabaloy Sánchez, Antonio
5. Ahmamou, M.
6. Benmakhlouf, M.
7. Sanz de Galdeano Equiza, Carlos
8. Akil, M.

Exporter

Exporter

×

MLA

modern-language-association

APA

apa

Chicago

chicago-fullnote-bibliography

Harvard

harvard-cite-them-right

Vancouver

vancouver-author-date

---

RIS BibTex

Exporter

×

Le document ne peut pas être exporté car il appartient à un autre portail.

Texte intégral

lock_openArias Montano externo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

D'autres publications dans: Geogaceta

Résumé

The Prerif ridges form pari of the foreland of the Rif Mountains. They are formed by superposed slices, with folds and faults, originated during the late Miocene WSWwards displacement of the Prerif units. At present, they thrust over the Plio-Quaternary formations of the Sa/'s and Charb basins. The analysis of the deformations in the Prerif ridges and the Plio-Quaternary lacustrine formations of the Sai'ss basin, as well as the thrust structures, indicates a recent tectonics with a N-S to NW-SE compression, subparallel to the trend of the present Iberian-Africa convergence

La source de données: Dialnet