Prosiectau fesul blwyddyn
Crynodeb
The purpose of this study is to better understand the system of Quaternary loess-palaeosol sequences (LPS) of the Matmata region in southern Tunisia. Results from a combination of predominantly classical methods (grain size and mineral analysis, CaCO3-content estimation, environmental magnetism) indicate strong soil formation phases during which the conditions of sedimentation changed drastically. The heavy mineral analysis underlines northwest, west and southwest provenances of the loessic material. Furthermore, we discuss the process of soil formation in LPS and explain why these soils are very sandy in comparison to the loess units. During phases of soil formation, the northwestern sediment transport path was blocked while sandy material was blown dominantly from the southwestern Grand Erg. Therefore, we present a conceptual model including a provenance analysis of the loessic material that support and improve earlier results of Coudé-Gaussen and collaborators.
Cyfieithiad o deitl y cyfraniad | Sandy soils in silty loess: The loess system of Matmata (Tunisia) |
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Iaith wreiddiol | Ffrangeg |
Tudalennau (o-i) | 175-186 |
Nifer y tudalennau | 12 |
Cyfnodolyn | Quaternaire |
Cyfrol | 31 |
Rhif cyhoeddi | 3 |
Dynodwyr Gwrthrych Digidol (DOIs) | |
Statws | Cyhoeddwyd - 01 Medi 2020 |
Ôl bys
Gweld gwybodaeth am bynciau ymchwil 'Des sols sableux dans du loess limoneux: Le système loessique de Matmata (Tunisie)'. Gyda’i gilydd, maen nhw’n ffurfio ôl bys unigryw.Prosiectau
- 1 Wedi Gorffen
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CREDit: CREDit - Chronological REference Datasets and Sites (CREDit) towards improved accuracy and precision in luminescence-based chronologies
Duller, G. (Prif Ymchwilydd), Kreutzer, S. (Prif Ymchwilydd), Roberts, H. (Prif Ymchwilydd) & Sirocko, F. (Cyd-ymchwilydd)
Horizon 2020 -European Commission
01 Ion 2020 → 30 Ebr 2022
Prosiect: Ymchwil a ariannwyd yn allanol