




Baptiste Le Bellego, Celia Dalou, Béatrice Luais, Pierre Condamine, Vincent Motto-Ros, Laurent Tissandier Geochimica et Cosmochimica Acta 422: 397-411 Voir en ligne : https://doi.org/10.1016/j.gca.2025.11.038 The segregation of metallic cores from silicate mantles during early planetary differentiation is a key process shaping the chemical evolution of terrestrial bodies. A critical factor controlling metal-silicate equilibration during this stage
J. Gamblin, E. Füri, B. Luais, L. Zimmermann Geochemical Perspectives Letters v39 Voir en ligne : https://doi.org/10.7185/geochemlet.2607 To gain new insights into nitrogen (N) isotopic variations in the early Solar System, N and noble gas (Ne, Ar) isotopes were measured in metal fragments and olivine separates from thirteen pallasites and five IIIAB iron meteorites. While δ15N
Juliette Pin, Lydéric France, Gilles Chazot, Etienne Deloule, Mohamed Ahmed Daoud, Bernard Le Gall Geology (2026) 54 (4): 348–353. Voir en ligne : https://doi.org/10.1130/G53776.1 Magmatism plays a central role in rift dynamics, yet the structure and evolution of magma plumbing systems during continental break-up remain poorly constrained. The Afar Rift offers a rare opportunity to study
Qasid Ahmad, Damien Cividini & Béatrice Luais Journal of Analytical Atomic Spectrometry, 41(3), 935–941 Voir en ligne : https://doi.org/10.1039/D5JA00471C Germanium (Ge) isotope measurements (δ74/70Ge relative to NIST3120a) have attracted increasing attention in geochemistry and cosmochemistry; however, analyses of silicate material with low Ge contents remain difficult due to complex sample preparation and purification procedures. Here, we
Toussaint A., France L. Lithos, Volumes 522–523, February 2026, 108395 Voir en ligne : https://doi.org/10.1016/j.lithos.2025.108395 Quantifying the parameters that govern magma differentiation is key to understanding the evolution of igneous systems. We present an approach combining thermodynamic modeling of magma differentiation using Rhyolite-MELTS with chemical composition, temperature, pressure, and oxygen fugacity (X-T-P-fO2)-dependent partition coefficients (D) for
nos thèmes de recherche
Cosmochimie et Planétologie
Cycles, Atmosphère, Climats
Magmas
et Fluides
Profonds
Tectonique, Érosion et Évolution du Relief
Nos instruments nationaux
LG-SIMS-Nancy
Sondes Ioniques
SARM
Service d’Analyse des Roches
et des Minéraux
nos plateformes instrumentales
Spectrométrie Gaz Rares
Isotopes Radiogéniques & Stables - Spectrométrie de Masse
Spectrométrie Isotopes Stables
Cosmochimie et Magmatologie Experimentales
Microscopie et microsonde électronique
Nos partenaires de formation
Nos RESEAUX & partenaires financiers
Les FEDER CRISTMAG et STEHLo sont cofinancés par l’Union européenne dans le cadre du Programme opérationnel FEDER-FSE Lorraine et Massif des Vosges 2014-2020.



