Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-237-2021
https://doi.org/10.5194/se-12-237-2021
Research article
 | 
28 Jan 2021
Research article |  | 28 Jan 2021

Extensional reactivation of the Penninic frontal thrust 3 Myr ago as evidenced by U–Pb dating on calcite in fault zone cataclasite

Antonin Bilau, Yann Rolland, Stéphane Schwartz, Nicolas Godeau, Abel Guihou, Pierre Deschamps, Benjamin Brigaud, Aurélie Noret, Thierry Dumont, and Cécile Gautheron

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Antonin Bilau on behalf of the Authors (30 Nov 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (03 Dec 2020) by Giancarlo Molli
AR by Antonin Bilau on behalf of the Authors (08 Dec 2020)  Author's response   Manuscript 
ED: Publish as is (11 Dec 2020) by Giancarlo Molli
ED: Publish as is (11 Dec 2020) by Federico Rossetti (Executive editor)
AR by Antonin Bilau on behalf of the Authors (11 Dec 2020)
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Short summary
As a result of the collision between the European and Apulian plates, the Alps have experienced several evolutionary stages. The Penninic frontal thrust (PFT) (major thrust) was associated with compression, and now seismic studies show ongoing extensional activity. Calcite mineralization associated with shortening and extensional structures was sampled. The last deformation stages are dated by U–Pb on calcite at ~ 3.5 and ~ 2.5 Ma. Isotope analysis evidences deep crustal fluid mobilization.