Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2197-2020
https://doi.org/10.5194/se-11-2197-2020
Research article
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23 Nov 2020
Research article | Highlight paper |  | 23 Nov 2020

Tectonic exhumation of the Central Alps recorded by detrital zircon in the Molasse Basin, Switzerland

Owen A. Anfinson, Daniel F. Stockli, Joseph C. Miller, Andreas Möller, and Fritz Schlunegger

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Owen Anfinson on behalf of the Authors (13 Aug 2020)  Author's response 
ED: Referee Nomination & Report Request started (01 Sep 2020) by Kei Ogata
RR by Laura Stutenbecker (16 Sep 2020)
RR by Jan Wijbrans (22 Sep 2020)
ED: Publish subject to technical corrections (29 Sep 2020) by Kei Ogata
ED: Publish subject to technical corrections (02 Oct 2020) by Elias Samankassou (Executive editor)
AR by Owen Anfinson on behalf of the Authors (08 Oct 2020)  Author's response   Manuscript 
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Short summary
We present new U–Pb age data to provide insights into the source of sediment for the Molasse Sedimentary Basin in Switzerland. The paper aims to help shed light on the processes that built the Central Alpine Mountains between ~35 and ~15 Ma. A primary conclusion drawn from the results is that at ~21 Ma there was a significant change in the sediment sources for the basin. We feel this change indicates major tectonic changes within the Central Alps.