The Lorraine Grèzes Litées Deposits

M. Deshaies, S. Ghanini, D. Harmand and A. Weisrock

Permafrost and Periglacial Processes, 1995, vol. 6, issue 2, 119-123

Abstract: Des dépǒts stratifiés de grèzes litées sont décrits dans des sites voisins de Tilly‐sur‐Meuse et Domrémy‐la‐Pucelle. Les matériaux proviennent du substratum local. Il y a un déficit de fines dans ces formations et le ruissellement est considéré comme le processus de dépǒt le plus probable. Grèzes (stratified deposits) are described from localities near Tilly‐sur‐Meuse and Domrémy‐la‐Pucelle. The sediments are derived from local bedrock. There is a lack of fines in the deposits, and slopewash is regarded as the most likely process of deposition.

Date: 1995
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Persistent link: https://EconPapers.repec.org/RePEc:wly:perpro:v:6:y:1995:i:2:p:119-123

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