Abstract
We provide new constraints for the fluid flow system at the origin of two F-Ba deposits located at the unconformity between the south of the Paris Basin and the northern edge of the French Massif Central. We used microthermometry and bulk crush-leach analyses to determine isotope ratios of mineralizing fluids (δ18O, δD, δ37Cl), together with cation and anion composition of fluid inclusions hosted by fluorite. Chlorinity and Cl/Br molar ratios (212–521) indicate the involvement of a brine, whose origin likely corresponds to Triassic evaporated seawater compatible with supratidal dolomitic facies preserved nearby. Microthermometry reveals high Ca/Na ratios, suggesting that the brine composition evolved from hydrothermal alteration of the Variscan basement and partial dissolution and replacement of the host sedimentary rocks. δ37Cl values are lower than the expected value of evaporated seawater, suggesting Cl isotope fractionation by ion filtration in clay-rich horizons. Fluorite crystallized at minimum temperatures of 70 to 110 °C, 10–40 °C warmer than the host Triassic sedimentary rocks. Ascending brines were expelled during the Early Cretaceous and experienced a drop in pressure and temperature, together with possible mixing with the SO4-rich pore water of the sedimentary rocks, causing precipitation of silica, followed by fluorite and barite, forming a stratabound deposit similar to those found in many areas in Western Europe.
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Acknowledgements
The authors acknowledge S. Fernando for providing crush-leach solutions of fluorite and R. Millot, S. Andrieu and T. Conte from BRGM (Bureau des Recherches Géologiques et Minières) for technical advice on ICP-MS analyses. This work was supported by the Paris Ile-de-France Region – DIM “Matériaux anciens et patrimoniaux.” We would like to thank Mathias Burisch and an anonymous reviewer for the constructive comments on our manuscript, as well as associate editor David Banks and editor Georges Beaudoin.
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All authors contributed to the study conception and design. Antonin Richard, Diana Chourio-Camacho, and Gaël Monvoisin were involved in the crush-leach analysis. Pierre Agrinier and Gérard Bardoux supervised the quantification of stable chlorine isotopes. Thomas Rigaudier supervised the measurements of fluid inclusions oxygen and hydrogen stable isotope composition. Antonin Richard, Alexandre Tarantola, Jocelyn Barbarand, and Benjamin Brigaud were involved in data interpretation and the improvement of the paper. The first draft of the manuscript was written by Louise Lenoir and Thomas Blaise, and all authors read, commented on previous versions of the manuscript, and approved the final version.
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Lenoir, L., Blaise, T., Chourio-Camacho, D. et al. The origin of fluorite-barite mineralization at the interface between the Paris Basin and its Variscan basement: insights from fluid inclusion chemistry and isotopic (O, H, Cl) composition. Miner Deposita 59, 397–417 (2024). https://doi.org/10.1007/s00126-023-01219-2
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DOI: https://doi.org/10.1007/s00126-023-01219-2