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Bulletin de la Societe Geologique de France; January 2003; v. 174; no. 1; p. 83-92; DOI: 10.2113/174.1.83
© 2003 Societe Geologique de France
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L’extension continentale au Néo-Protérozoïque supérieur-Cambrien inférieur dans l’Anti-Atlas (Maroc)

Abderrahmane Soulaimani1, Mohamed Bouabdelli2 and Alain Piqué2

1 Laboratoire de Géologie structurale, Faculté des Sciences Semlalia, Marrakech (Maroc).
2 Institut universitaire européen de la mer, Université de Bretagne occidentale, Brest.

Abstract

Dans l’Anti-Atlas (sud du Maroc), la couverture du Néo-protérozoïque supérieur, discordante sur les structures panafricaines, s’organise en « séries » volcaniques et détritiques (Groupe du Saghro et de Ouarzazate), recouvertes par les dépôts carbonatés cambriens. De nouvelles observations réalisées dans cette couverture montrent qu’elle résulte d’un épisode extensif dont témoignent, outre les structures extensives, des mises en place de magmas et des manifestations hydrothermales. Cet épisode, qui se maintiendra jusqu’au Cambrien inférieur, est interprété en termes d’extension continentale post-panafricaine.

Key Words: Anti-Atlas (Maroc) • Extension continentale • Néo-Protérozoïque • Cambrien




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This Article
Right arrow Abstract
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Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Web of Science (11)
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