Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-199-2020
https://doi.org/10.5194/se-11-199-2020
Research article
 | 
21 Feb 2020
Research article |  | 21 Feb 2020

Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)

Christian A. Bergemann, Edwin Gnos, Alfons Berger, Emilie Janots, and Martin J. Whitehouse

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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 Christian Bergemann on behalf of the Authors (15 Jul 2019)  Manuscript 
ED: Referee Nomination & Report Request started (23 Jul 2019) by Bernhard Grasemann
RR by Meinert Rahn (16 Aug 2019)
ED: Reconsider after major revisions (20 Aug 2019) by Bernhard Grasemann
AR by Christian Bergemann on behalf of the Authors (28 Oct 2019)  Manuscript 
ED: Referee Nomination & Report Request started (30 Oct 2019) by Bernhard Grasemann
RR by Fraukje Brouwer (19 Dec 2019)
ED: Publish subject to minor revisions (review by editor) (27 Dec 2019) by Bernhard Grasemann
AR by Christian Bergemann on behalf of the Authors (10 Jan 2020)  Author's response   Manuscript 
ED: Publish as is (20 Jan 2020) by Bernhard Grasemann
ED: Publish as is (20 Jan 2020) by Federico Rossetti (Executive editor)
AR by Christian Bergemann on behalf of the Authors (27 Jan 2020)
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Short summary
Metamorphic domes are areas in a mountain chain that were unburied and where deeper parts of the crust rose to the surface. The Lepontine Dome in the Swiss and Italian Alps is such a place, and it is additionally bordered on two sides by shear zones where crustal blocks moved past each other. To determine when these tectonic movements happened, we measured the ages of monazite crystals that form in fluid-filled pockets inside the rocks during these movements of exhumation and deformation.