Add to ORKGInternational audienceA 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.L'étude très précise du cortège des minéraux lourds des sables limoneux des Monts de Matmata, ainsi que celle des vents actuels et pléistocènes, indique que ces dépôts d'origine éolienne proviennent plus sûrement de la déflation sur les Grands Chotts tunisiens que de la migration des sables du Grand Erg Oriental
International audienceCompiling of bibliographic data has been completed with unpublished data and p...
Le travail mené dans cette thèse se présente sous la forme d'études expérimentales des processus d'é...
The Tagdaoust excavation in Mauritania yielded a large number of imported ceramic artifacts. Origina...
International audienceA very precise study of the heavy minerals of silty sands of Matmata Mounts (S...
National audienceIt is generally assumed that the so-called "peridesertic loess" Matmata aeolian san...
In South Tunisia, the Dahar chain trapped in its depressions an abundant eolian material which was m...
The best-known examples of desert loess are in the northern Sahara Margins the Matmata plateau (sout...
The genetic relationship of these lower sand-silty terraces with the in situ loesses of plateau and ...
Aeolian sands were analyzed from km to km along the In Kous- samene erg (Mali) and the Cap Sim (Moro...
The wadis flowing down from the Matmata mounts have deposited two main pleistocene terraces in the D...
En Tunisie orientale, le système conjugué de Gotaia et Eliane dans la région de Mahdia est formé par...
International audienceCompiling of bibliographic data has been completed with unpublished data and p...
Twelve cores sampled in the siculo-tunisian area are studied with regard to sedimentology, grain-siz...
Sands of the Tunisian shelf consist of a mixture in different proportions of bioclasts, generally pr...
Significant variations in the amount of carbonate and gypsum and also in the thickness of preserved ...
International audienceCompiling of bibliographic data has been completed with unpublished data and p...
Le travail mené dans cette thèse se présente sous la forme d'études expérimentales des processus d'é...
The Tagdaoust excavation in Mauritania yielded a large number of imported ceramic artifacts. Origina...
International audienceA very precise study of the heavy minerals of silty sands of Matmata Mounts (S...
National audienceIt is generally assumed that the so-called "peridesertic loess" Matmata aeolian san...
In South Tunisia, the Dahar chain trapped in its depressions an abundant eolian material which was m...
The best-known examples of desert loess are in the northern Sahara Margins the Matmata plateau (sout...
The genetic relationship of these lower sand-silty terraces with the in situ loesses of plateau and ...
Aeolian sands were analyzed from km to km along the In Kous- samene erg (Mali) and the Cap Sim (Moro...
The wadis flowing down from the Matmata mounts have deposited two main pleistocene terraces in the D...
En Tunisie orientale, le système conjugué de Gotaia et Eliane dans la région de Mahdia est formé par...
International audienceCompiling of bibliographic data has been completed with unpublished data and p...
Twelve cores sampled in the siculo-tunisian area are studied with regard to sedimentology, grain-siz...
Sands of the Tunisian shelf consist of a mixture in different proportions of bioclasts, generally pr...
Significant variations in the amount of carbonate and gypsum and also in the thickness of preserved ...
International audienceCompiling of bibliographic data has been completed with unpublished data and p...
Le travail mené dans cette thèse se présente sous la forme d'études expérimentales des processus d'é...
The Tagdaoust excavation in Mauritania yielded a large number of imported ceramic artifacts. Origina...