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Sur l'origine des sables limoneux des Monts de Matmata (Sud tunisien)

Abstract : A very precise study of the heavy minerals of silty sands of Matmata Mounts (South Tunisia), and that of present and pleistocene winds show that those eolian sediments came from deflation on the Grands Chotts (great playas) rather than from migration of Grand Erg Oriental sands.
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Contributor : Jean-Louis BALLAIS Connect in order to contact the contributor
Submitted on : Wednesday, June 21, 2017 - 4:20:34 PM
Last modification on : Tuesday, October 19, 2021 - 11:35:03 PM
Long-term archiving on: : Saturday, December 16, 2017 - 1:05:56 AM


Sur l'origine des sables limon...
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  • HAL Id : hal-01544440, version 1



Jean-Louis Ballais, Viviane Balland. Sur l'origine des sables limoneux des Monts de Matmata (Sud tunisien). Travaux du CREGEPE, Centre de recherche en géographie physique de l'environnement (CREGEPE), 1983, 3, p. 7-17. ⟨hal-01544440⟩



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