GEOLOGICAL STRUCTURE OF THE HAOUZ MOUNTAI NS (INTERNAL RIF, MOROCCO) - INTERPRETATION AND CHRONOLOGICAL ASPECTS

Authors
HLILA R DEGALDEANO CS
Citation
R. Hlila et Cs. Degaldeano, GEOLOGICAL STRUCTURE OF THE HAOUZ MOUNTAI NS (INTERNAL RIF, MOROCCO) - INTERPRETATION AND CHRONOLOGICAL ASPECTS, Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre, 318(9), 1994, pp. 1261-1266
Citations number
12
Categorie Soggetti
Multidisciplinary Sciences
Journal title
Comptes rendus de l'Academie des sciences. Serie 2, Mecanique, physique, chimie, sciences de l'univers, sciences de la terre → ACNP
ISSN journal
07644450
Volume
318
Issue
9
Year of publication
1994
Part
2
Pages
1261 - 1266
Database
ISI
SICI code
0764-4450(1994)318:9<1261:GSOTHM>2.0.ZU;2-7
Abstract
The thrust and backthrust of the Haouz Mountains result from the westw ard migration of the Internal Betic-Rif Zones, being practically stopp ed at the end of the Burdigalian by the Flysch nappes situated in a mo re external position. We interpret the backthrusts as being encapuchon nement (antiformal stack) phenomena.