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- W2034223013 abstract "The old alluvial terraced deposits of the river Sarthe below Le Mans are made of glaucomtic sands, pebbles of silex and Paleozoic sandstones and of some pebbles of granite. They are climatical penglacial deposits. Their weathering has given a deep soil with a red colour. From the younger level to the older, the rate per cent of the 2/1 clay minerals of the sands and of the granites decreases while the rate per cent of kaolinite grows. The Mossbauer spectrometry shows that the rates of the iron hydroxides appeared in the glauconites and the biotites increase too." @default.
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- W2034223013 date "1986-01-01" @default.
- W2034223013 modified "2023-10-17" @default.
- W2034223013 title "Les formations alluviales anciennes de la Sarthe en aval du Mans et leur degré d'altération" @default.
- W2034223013 doi "https://doi.org/10.3406/quate.1986.1820" @default.
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