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- W2000628127 abstract "Les carbonates magnésiens autochtones et le gypse présents dans les sédiments holocènes lacustres du marais de Sarliève (Puy-de-Dôme, France) dénotent une composition alcaline, magnésienne et sulfatée des eaux qu'expliquent les flux dissous issus du substratum oligocène du bassin versant, ainsi qu'un confinement morphologique sous déficit hydrique, ce dont témoignent les flores algaires micro- et macrophytes. Un déconfinement intervient au cours de la période historique lié à l'évolution naturelle et anthropique du lac. Pour citer cet article : J.-G. Bréhéret et al., C. R. Geoscience 335 (2003). The autochthonous magnesian carbonates and the gypsum depicted in the Holocene deposits from the ‘Marais de Sarliève’ (Limagne, France) result from an alkaline, magnesian and sulphated composition of waters. This is also recorded by the composition of algal micro- and macrophytes. This may be explained by the dissolved fluxes from the Oligocene catchment and from a restriction. During the historical period, the lake evolved towards a lesser restriction. To cite this article: J.-G. Bréhéret et al., C. R. Geoscience 335 (2003)." @default.
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- W2000628127 date "2003-05-01" @default.
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- W2000628127 title "Indices de confinement dans les dépôts lacustres holocènes de Sarliève (Limagne, France)" @default.
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