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Please use this identifier to cite or link to this item:
http://hdl.handle.net/10362/4690
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| Title: | Les formations fluviatiles quaternaires de la plaine de Doukkala (Méséta Occidentale Marocaine). Sédimentologie et nouvelles données chronostratigraphiques |
| Authors: | Ouadia, M. Aberkan, M. |
| Keywords: | Quaternary Meseta sedimentology chronostratigraph |
| Issue Date: | 28-Dec-2010 |
| Abstract: | The Quaternary fluvial formations of the Doukkala plain are, until now, slightly studied. Our study has allowed to precise
that the fluvial terraces of the oued "the Ourn Rbia oued", are clearly distinguished from the secondary oueds terraces by the
dynamic deposit of the alluvial materials. Moreover, the mammal fossils recolted from some of these terraces allow to review the
ages attributed by Gigout (1951). |
| URI: | http://hdl.handle.net/10362/4690 |
| Appears in Collections: | FCT: DCT - Ciências da Terra
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