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Modélisation magnétique de la suture ophiolitique de Bou Azzer–El Graara (Anti-Atlas central,Maroc). Implications sur la reconstitution géodynamique panafricaine
Authors:Abderrahmane Soulaimani  Mohammed Jaffal  Lhou Maacha  Azzouz Kchikach  Abdessamad Najine  Abdellatif Saidi
Institution:1. Faculté des sciences Semlalia, université Cadi-Ayyad, BP 2390, Marrakech, Maroc;2. Faculté des sciences et techniques, université Cadi-Ayyad, BP 549, Marrakech, Maroc;3. Reminex, Managem, Groupe ONA, 52, av. Hassan-II, Casablanca, Maroc;4. Faculté des sciences et techniques, université Cadi-Ayyad, Béni-Méllal, Maroc
Abstract:Aeromagnetic data of the Anti-Atlas Mountains show an important magnetic anomaly along the ‘Major Anti-Atlas Fault’, produced by different mafic and ultramafic rocks of a Neoproterozoic ophiolite complex. The magnetic modelling of Bou Azzer–El Graara ophiolitic suture shows a deep-seated anomaly through the upper continental crust corresponding to a north-dipping subduction. The polarity of the Pan-African subduction in the Anti-Atlas is therefore compatible with the contemporaneous Pan-African orogenic belts, where polarity of subduction dipped away from the West African Craton during the amalgamation of Western Gondwana. To cite this article: A. Soulaimani et al., C. R. Geoscience 338 (2006).
Keywords:Modélisation  Magnétisme  Ophiolites  Panafricain  Anti-Atlas  Maroc  Modelling  Magnetism  Ophiolites  Pan-African  Anti-Atlas  Morocco
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