Articles | Volume 36, issue 5
https://doi.org/10.5194/ejm-36-879-2024
https://doi.org/10.5194/ejm-36-879-2024
Research article
 | 
24 Sep 2024
Research article |  | 24 Sep 2024

Multifaceted orogenic fluid dynamics unraveled by hydrothermal epidote

Veronica Peverelli, Alfons Berger, Martin Wille, Thomas Pettke, Benita Putlitz, Andreas Mulch, Edwin Gnos, and Marco Herwegh

Viewed

Total article views: 445 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
285 25 135 445 15 3 5
  • HTML: 285
  • PDF: 25
  • XML: 135
  • Total: 445
  • Supplement: 15
  • BibTeX: 3
  • EndNote: 5
Views and downloads (calculated since 24 Sep 2024)
Cumulative views and downloads (calculated since 24 Sep 2024)

Viewed (geographical distribution)

Total article views: 436 (including HTML, PDF, and XML) Thereof 436 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 20 Nov 2024
Download
Short summary
We used U–Pb dating and Pb–Sr–O–H isotopes of hydrothermal epidote to characterize fluid circulation in the Aar Massif (central Swiss Alps). Our data support the hypothesis that Permian fluids exploited syn-rift extensional faults. In the Miocene during the Alpine orogeny, fluid sources were meteoric, sedimentary, and/or metamorphic water. Likely, Miocene shear zones were exploited for fluid circulation, with implications for the Sr isotope budget of the granitoids.