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SE | Articles | Volume 11, issue 4
Solid Earth, 11, 1617–1641, 2020
https://doi.org/10.5194/se-11-1617-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue: Faults, fractures, and fluid flow in the shallow crust

Solid Earth, 11, 1617–1641, 2020
https://doi.org/10.5194/se-11-1617-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

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 et al.

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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 Svenja Lange on behalf of the Authors (22 Jul 2020)  Author's response
ED: Publish as is (22 Jul 2020) by Randolph Williams
ED: Publish as is (23 Jul 2020) by CharLotte Krawczyk(Executive Editor)
Publications Copernicus
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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.
This paper reports a multiproxy approach to reconstruct the depth, timing, and extent of the...
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