A cryptotephra from the Upper Pleistocene volcanism of the Bas-Vivarais in the sedimentary infilling of the Chauvet-Pont d’Arc cave (Ardèche, France)

A cryptotephra from the Upper Pleistocene volcanism of the Bas-Vivarais in the sedimentary infilling of the Chauvet-Pont d’Arc cave (Ardèche, France)

A cryptotephra belonging to the Upper Pleistocene volcanism of the Bas-Vivarais was identified for the first time in the sedimentary infilling of the entrance area of the Chauvet-Pont d’Arc cave. This slightly reworked tephra fall is characterized by its heavy minerals assemblage, among which magnes...

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Bibliographic Details
Main Authors: Pastre, Jean-François, Debard, Évelyne, Ferrier, Catherine, Fialin, Michel, Gély, Bernard, Kervazo, Bertrand, Maksud, Frédéric, Mokadem, Fatima, Nomade, Sébastien, Rividi, Nicolas, Saulnier-Copard, Ségolène
Format: Article
Language:English
Published: Académie des sciences 2021-05-01
Series:Comptes Rendus. Géoscience
Subjects:
Chauvet-Pont d’Arc cave
Cryptotephra
Phreatomagmatism
Bas-Vivarais volcanism
Upper Pleistocene
Online Access:https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.52/

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https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.52/

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