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- W2022679949 abstract "A deeply weathered diamicton, more than 1,40 m thick and with numerous slickensides has been uncovered at the lower part of the «Formation de Lannemezan» (alluvial cone of Belair). The micro-faults exhibit striations, thin millimetric grooves and crag and tails suggesting that the whole diamicton has been laminated and submitted to internal periodic shearing. This structures developped prior to the accumulation of more than 40 m of alluvial deposits that formed the bulk of the Belair cone. The sequence is of lower Pleistocene age. We interpret the diamicton as a deformation till. It may have developped beneath a piedmont glacier from the Ossau watershed. From a chronological point of view, the diamicton is correlated with the «Belair Glaciation» recently discovered at only 1 100 m from the outcrop described in this paper." @default.
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- W2022679949 date "1992-01-01" @default.
- W2022679949 modified "2023-09-24" @default.
- W2022679949 title "Un till de déformation du Pléistocene inférieur à la basé de la Formation du Lannemezan (Piémont des Pyrénées Atlantiques, France)" @default.
- W2022679949 doi "https://doi.org/10.3406/quate.1992.1973" @default.
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