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- W1972518825 abstract "Resume La peneplanation des chaines de montagnes est generalement consideree comme resultant de l'action de l'erosion a long terme, qui lisse le relief et diminue leur altitude jusqu'a tendre vers le niveau marin. Nous proposons un nouveau modele, dans lequel la sedimentation de piedmont traduit une montee du niveau de base de la chaine, entrainant son aplanissement en altitude. Ce modele est illustre a travers l'evolution morphologique du versant sud des Pyrenees durant le Cenozoique. Pour citer cet article : J. Babault, J. Van Den Driessche, C. R. Geoscience 337 (2005)." @default.
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- W1972518825 date "2005-12-01" @default.
- W1972518825 modified "2023-10-17" @default.
- W1972518825 title "L'érosion des chaînes de montagnes : influence de la sédimentation de piedmont" @default.
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- W1972518825 doi "https://doi.org/10.1016/j.crte.2005.09.010" @default.
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