Evolution Néogène du bassin de Tétouan-Martil, Rif septentrional, Maroc
| dc.contributor.author | Benmakhlouf, M. | |
| dc.contributor.author | Chalouan, Ahmed | |
| dc.date.accessioned | 2017-06-14T12:02:35Z | |
| dc.date.available | 2017-06-14T12:02:35Z | |
| dc.date.issued | 1994 | |
| dc.description.abstract | Tetouan-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 | en_US |
| dc.description.abstract | Le bassin de Tétouan-Martil a connu au cours de son histoire géologique deux épisodes de déformations distensives liés à des riftings néogènes de la mer d'Alboran. Le premier, d'âge Oligocène supérieur à Burdigalien, a produit des flexures et des failles normales ductilesfragiles.dans des gneiss et micaschistes.et des failles normales synsédimentaires dans les formations aquitano-burdigaliennes | en_US |
| dc.identifier.uri | http://hdl.handle.net/10272/13876 | |
| dc.language.iso | fra | en_US |
| dc.publisher | Sociedad Geológica de España | en_US |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
| dc.rights.accessRights | open access | en_US |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
| dc.subject.other | Normal faults | en_US |
| dc.subject.other | Internal Rif | en_US |
| dc.subject.other | Late-Oligocene-Pliocene | en_US |
| dc.subject.other | Failles normales | en_US |
| dc.subject.other | Rif interne | en_US |
| dc.subject.other | Oligocène superieur-PHocène | en_US |
| dc.title | Evolution Néogène du bassin de Tétouan-Martil, Rif septentrional, Maroc | en_US |
| dc.title | Neogene evolution of the Tetouan-Martil basin; northern Rif, Morocco | eng |
| dc.type | conference output | en_US |
| dspace.entity.type | Publication |
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