Evolution Néogène du bassin de Tétouan-Martil, Rif septentrional, Maroc.
1994; Issue: 17 Linguagem: Francês
ISSN
2173-6545
AutoresM. Benmakhlouf, Ahmed Chaloüan,
Tópico(s)Archaeological and Geological Studies
ResumoEnglishTetouan-MartHpost-nappes basin is opened by two rifting stages: the first in late Oligocene-Burdigalian times, is accompanied by ductile normal faults in Aquitanian-Burdigalian rocks; the second of post Burdigaiian and pre-PHocene age, has produced two low angle norma/ fault systems, trending NE-SW and NW-SE, leading to the collapse of this basin francaisLe bassin de Tetouan-Martil a connu au cours de son histoire geologique deux episodes de deformations distensives lies a des riftings neogenes de la mer d'Alboran. Le premier, d'âge Oligocene superieur a Burdigalien, a produit des flexures et des failles normales ductilesfragiles.dans des gneiss et micaschistes.et des failles normales synsedimentaires dans les formations aquitano-burdigaliennes
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