Articles | Volume 8, issue 3
https://doi.org/10.5194/gchron-8-387-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-8-387-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Dating circulations of hydrothermal fluids in the crystalline basements of unconformity-related metal deposits using in situ Rb ∕ Sr geochronology: proof of concept
Quentin Boulogne
CORRESPONDING AUTHOR
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
LabCom CREGU, GeoRessources, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France
Gaétan Milesi
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
LabCom CREGU, GeoRessources, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France
Chantal Peiffert
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
Emmy Fischer
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
LabCom CREGU, GeoRessources, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France
Christophe Ballouard
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
Mehdi Serdoun
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
Orano Canada, Saskatoon, Canada
Thomas Obin
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
LabCom CREGU, GeoRessources, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France
Andreï Lecomte
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
Pierre Martz
Orano Canada, Saskatoon, Canada
Andrew Kaczowka
Cameco Corporation, Saskatoon, Canada
Julien Mercadier
Université de Lorraine, CNRS, GeoRessources, F-54000 Nancy, France
LabCom CREGU, GeoRessources, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France
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Marie Gerardin, Gaétan Milesi, Julien Mercadier, Michel Cathelineau, and Danièle Bartier
Geosci. Instrum. Method. Data Syst., 13, 309–323, https://doi.org/10.5194/gi-13-309-2024, https://doi.org/10.5194/gi-13-309-2024, 2024
Short summary
Short summary
Clay minerals are helpful markers of low-temperature geological processes. The combination of their characterization with geochronology is a powerful tool to constrain physical and chemical processes, improving our understanding of the evolution of the Earth system. This paper aims to present the platform along with the associated methods developed at the GeoRessources laboratory (University of Lorraine) to separate and characterize clay minerals and date illites using the K–Ar method.
Delphine Charpentier, Gaétan Milesi, Pierre Labaume, Ahmed Abd Elmola, Martine Buatier, Pierre Lanari, and Manuel Muñoz
Solid Earth, 15, 1065–1086, https://doi.org/10.5194/se-15-1065-2024, https://doi.org/10.5194/se-15-1065-2024, 2024
Short summary
Short summary
Understanding the fluid circulation in fault zones is essential to characterize the thermochemical evolution of hydrothermal systems in mountain ranges. The study focused on a paleo-system of the Pyrenees. Phyllosilicates permit us to constrain the evolution of temperature and redox of fluids at the scale of the fault system. A scenario is proposed and involves the circulation of a single highly reducing hydrothermal fluid (~300 °C) that evolves due to redox reactions.
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Short summary
This study investigates Rb–Sr system behavior in hydrothermally altered muscovite using in-situ LA-ICP-MS/MS (Laser Ablation-Inductively Coupled Plasma-Tandem Mass Spectrometry) analyses from the Athabasca Basin. Unaltered muscovite records Paleoproterozoic crystallization ages, whereas muscovite altered to illite and sudoite yields a consistent age of ~1640 Ma, corresponding to alteration halos related to unconformity-type uranium deposits. These results highlight the potential of Rb–Sr dating to constrain hydrothermal processes and fluid–rock interactions.
This study investigates Rb–Sr system behavior in hydrothermally altered muscovite using in-situ...