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(synchrotron-based), fluid inclusion analysis (FIA), Raman spectroscopy, ICP-MS, and isotope geochemistry. The results of this work, combined with those of parallel studies carried out within the GEOTHERBAMINE
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(CY Cergy Paris Université, AGM) and Marie Kratz (ESSEC, IDO dept. & CREAR), to contribute to the development and analysis of models within this broad framework. Located in the Paris area, the AGM
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