Holocene relative sea-level changes in western Brittany (France) between 7600 and 4000 cal. BP: Reconstitution from basal-peat deposits

With respect to others European oceanic facades, the Holocene relative sea-level (RSL) changes along the French Atlantic coasts have received relatively little attention. Even if it received some attention for geophysical modelling (Van de Plassche, 1991; Lambeck, 1997; Leorri et al., 2012), only tw...

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Détails bibliographiques

Auteurs principaux:	Goslin, Jérôme, Vliet-Lanoë, Brigitte Van, Stéphan, Pierre, Delacourt, Christophe, Fernane, Assia, Gandouin, Emmanuel, Hénaff, Alain, Penaud, Aurélie, Suanez, Serge
Format:	Artigo
Langue:	Inglês
Publié:	Groupe français de géomorphologie 2013
Sujets:	Holocène Bretagne niveau marin relatif tourbes de base isotopes stables du carbone Holocene Brittany RSL basal peats stable C isotopes
Accès en ligne:	https://doi.org/10.4000/geomorphologie.10386 https://hdl.handle.net/20.500.13089/giqq https://journals.openedition.org/geomorphologie/10386
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