Articles | Volume 11, issue 4
https://doi.org/10.5194/se-11-1617-2020
https://doi.org/10.5194/se-11-1617-2020
Research article
 | 
31 Aug 2020
Research article |  | 31 Aug 2020

Regional-scale paleofluid system across the Tuscan Nappe–Umbria–Marche Apennine Ridge (northern Apennines) as revealed by mesostructural and isotopic analyses of stylolite–vein networks

Nicolas E. Beaudoin, Aurélie Labeur, Olivier Lacombe, Daniel Koehn, Andrea Billi, Guilhem Hoareau, Adrian Boyce, Cédric M. John, Marta Marchegiano, Nick M. Roberts, Ian L. Millar, Fanny Claverie, Christophe Pecheyran, and Jean-Paul Callot

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nicolas Beaudoin on behalf of the Authors (23 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (06 Jul 2020) by Randolph Williams
AR by Nicolas Beaudoin on behalf of the Authors (13 Jul 2020)
ED: Publish as is (22 Jul 2020) by Randolph Williams
ED: Publish as is (23 Jul 2020) by CharLotte Krawczyk (Executive editor)
AR by Nicolas Beaudoin on behalf of the Authors (23 Jul 2020)
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Short summary
This paper reports a multiproxy approach to reconstruct the depth, timing, and extent of the past fluid flow during the formation of a fold-and-thrust belt in the Northern Apennines, Italy. The unique combination of paleopiezometry and absolute dating returns the absolute timing of the sequence of deformation. Combined with burial models, this leads to predict the expected temperatures for fluid, highlighting a limited hydrothermal fluid flow we relate to the large-scale subsurface geometry.