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Presence d'un etage periglaciaire a sols structures actifs au sommet des montagnes quartzitiques du Donegal (Irlande). L'exemple du Muckish.

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Sellier, D and Wilson, P (1994) Presence d'un etage periglaciaire a sols structures actifs au sommet des montagnes quartzitiques du Donegal (Irlande). L'exemple du Muckish. Environnements Periglaciaires, 1 . pp. 71-86. [Journal article]

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Item Type:Journal article
Faculties and Schools:Faculty of Life and Health Sciences
Faculty of Life and Health Sciences > School of Environmental Sciences
Research Institutes and Groups:Environmental Sciences Research Institute
Environmental Sciences Research Institute > Quaternary Environmental Change
ID Code:11979
Deposited By:Dr Peter Wilson
Deposited On:17 Feb 2010 09:31
Last Modified:28 Mar 2012 16:22

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