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Volcans de la chaîne des Puys (Massif central,France) : point sur la chronologie Vasset–Kilian–Pariou–Chopine
Authors:Didier Miallier  Laurent Michon  Jacques Évin  Thierry Pilleyre  Serge Sanzelle  Gérard Vernet
Institution:1. Laboratoire de physique corpusculaire, université Blaise-Pascal, CNRS–IN2P3, UMR 6533, 63177 Aubière cedex, France;2. Laboratoire des sciences de la Terre, université de la Réunion, 15, rue René-Cassin, 97715 Saint-Denis cedex 9, France;3. Centre de datation par le radiocarbone, université Claude-Bernard, Lyon-1, bât. 217, 43, bd du 11-Novembre-1918, 69622 Villeurbanne cedex, France;4. Inrap et UMR 6042 du CNRS, 19, rue Élisée-Reclus, 63000 Clermont-Ferrand, France
Abstract:On the basis of radiocarbon ages obtained on wood burned by base surges and tephrochronological observations, it has been possible to assess that the Puy Chopine, aged ca 9700 yr is older by a few centuries than both the Vasset and Kilian volcanoes. The last two have nearly the same age, ca 9300–9400 yr. Layers of trachytic tephra, most probably originated from Kilian or Vasset, can be observed overlapping those from the Pariou. This last volcano had been previously thought to be the younger of the area on the basis of the observation of trachytic tephra beneath its own tephra. However, new observations allow us to assume that those trachytes originated from the acid phase of the Pariou itself. Therefore, it can be assessed that the four volcanoes erupted according to the following sequence: Chopine/Pariou/?Vasset?/Kilian; the chronological situation of Vasset lies on poor arguments and it should be confirmed. To cite this article: D. Miallier et al., C. R. Geoscience 336 (2004).
Keywords:volcans  chaîne des Puys  téphrochronologie  datation radiocarbone  volcanoes  Chaîne des Puys  tephrochronology  radiocarbon dating
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