Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-241-2020
https://doi.org/10.5194/se-11-241-2020
Research article
 | 
26 Feb 2020
Research article |  | 26 Feb 2020

Determining the Plio-Quaternary uplift of the southern French Massif Central; a new insight for intraplate orogen dynamics

Oswald Malcles, Philippe Vernant, Jean Chéry, Pierre Camps, Gaël Cazes, Jean-François Ritz, and David Fink

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Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Oswald Malcles on behalf of the Authors (13 Nov 2019)  Author's response 
ED: Referee Nomination & Report Request started (25 Nov 2019) by Federico Rossetti
RR by Anonymous Referee #2 (07 Dec 2019)
ED: Publish subject to minor revisions (review by editor) (08 Dec 2019) by Federico Rossetti
AR by Oswald Malcles on behalf of the Authors (14 Dec 2019)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (10 Jan 2020) by Federico Rossetti
AR by Oswald Malcles on behalf of the Authors (16 Jan 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (21 Jan 2020) by Federico Rossetti
ED: Publish subject to technical corrections (21 Jan 2020) by Federico Rossetti (Executive editor)
AR by Oswald Malcles on behalf of the Authors (28 Jan 2020)  Author's response   Manuscript 
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Short summary
We aim to better understand the challenging areas that are the intraplate regions using one example: the southern French Massif Central and its numerous hundreds of meters deep valleys. We apply a multidisciplinary approach there using geomorphology, geochronology, and numerical modeling. Our dating results show that the canyon incisions are part of the Plio-Quaternary evolution with incision rate of ~ 80 m Ma−1. We propose then that this incision is possible due to an active regional uplift.