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Theses

Le système alluvial de la moyenne terrasse de la Moselle en Lorraine méridionale : approche morphosédimentaire et pétrographique

Abstract : The middle terrace system of the Moselle River in southern Lorraine constitutes a strong alluvial accumulation over the Vosges western piedmont. This work constitutes a morphostratigraphical revision of these deposits. The study of this middle terrace reveals the existence of three alluvial formations. These are probably the sedimentary expression of three detritals evacuations remobilized from the slopes of the Moselle's mountainnous basin. These formations are probably the morphosedimentary expression of three major glacial fluctuations during the saalien glaciations in the Vosges highland.
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Submitted on : Tuesday, April 24, 2018 - 4:05:02 PM
Last modification on : Monday, May 3, 2021 - 3:22:55 PM

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  • HAL Id : tel-01776690, version 1

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Ali Taous. Le système alluvial de la moyenne terrasse de la Moselle en Lorraine méridionale : approche morphosédimentaire et pétrographique. Géographie. Université Nancy 2, 1994. Français. ⟨NNT : 1994NAN21007⟩. ⟨tel-01776690⟩

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