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- W2735042815 abstract "Abstract The study of the often polygenic Tertiary sands of southern Ardennes allows the local evolution of the drainage pattern during the Paleogene and the Neogene to be traced. The history of these sands starts with a strong Eocene weathering and the formation of a deep ferruginized quartzose saprolite. Some fossilized outcrops remain unchanged: the outcrop of Regniowez is interpreted as a thick colluvium on which a ferruginous pedogenesis took place during the Eocene, resulting in an allothigenous cuirasse protecting the sands from erosion. Others undergo a complex evolution: the outcrop of Doische represents the rehandling of the same kind of Eocene sands, first in a marine Oligocene environment, then by continental Miocene streams. In that case, nevertheless, the heavy minerals assemblage shows the link with the almost in situ sands such as those of Regniowez, and therefore the local origin of the material. The lack of allogenic heavy minerals (characteristic of the Meuse lorraine) in the fluvial sands of the Ardennes plateau prior to the Trainee mosane (attributed to the Middle Miocene) confirms the Miocene capture of the Meuse lorraine, flowing westward so far, between the Paleozoic basement and the Sormonne valley, as assumed by Pissart in the early sixties. On the other hand, as the topographic glacis between the Ardennes and the Paris Basin was still active during the Stampian, the drainage pattern of the Meuse lorraine before the capture is post-Oligocene." @default.
- W2735042815 created "2017-07-21" @default.
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- W2735042815 date "2000-01-01" @default.
- W2735042815 modified "2023-10-18" @default.
- W2735042815 title "Signification des sables tertiaires de l'Ardenne méridionale : du nouveau sur la capturede la Meuse lorraineSignificance of the Tertiary sands of southern Ardennes: new data on the capture of the Meuse lorraine." @default.
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- W2735042815 doi "https://doi.org/10.1016/s0985-3111(00)00106-6" @default.
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