Le matériel de deux édifices dunaires postérieurs au dernier Pluvial (Nord du Mali et Sud-Ouest du Maroc)(Post late-pluvial aeolian dunes in Mali and Morocco)

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1982

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MESR

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Copyright PERSEE 2003-2023. Works reproduced on the PERSEE website are protected by the general rules of the Code of Intellectual Property. For strictly private, scientific or teaching purposes excluding all commercial use, reproduction and communication to the public of this document is permitted on condition that its origin and copyright are clearly mentionned.




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Geneviève Coudé-Gaussen et al., « Le matériel de deux édifices dunaires postérieurs au dernier Pluvial (Nord du Mali et Sud-Ouest du Maroc)(Post late-pluvial aeolian dunes in Mali and Morocco) », Bulletin de l'Association de Géographes Français, ID : 10.3406/bagf.1982.5304


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Aeolian sands were analyzed from km to km along the In Kous- samene erg (Mali) and the Cap Sim (Morocco). They show that. 1 ° With an increase in transport distance from a common source area, the ratio of quartz to shelly limes tone, or quartz to gypsum and clay increases. 2° A part of silt is formed by mechanical reduction of sand-sized marine organisms, clay and gypsum particles during aeolian transport. 3° The setting in motion of dust is very active near the source area of the aeolian sands.

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