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hypothesized to exist at the base of the lithosphere beneath the French Massif Central and the Pyrenees. Thermometric analyses of mineral assemblages (e.g., olivine-bearing basalts) will be used to estimate
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atmospheric models WRF-Chem and/or CHIMERE, developing new descriptions of primary ice formation from sources such as aviation, wildfire emissions, and mineral dust. High-resolution simulations of selected case
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well as new minerals to build a detailed picture of the evolution of the Earth's atmosphere from Archean to present. The post-doctoral researcher will also have access to the noble gas analytical platform
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composed of specialists in the geology and mineralogy of ophiolites and engineers who are experts in ion chromatography and mineral synthesis. This multidisciplinary team is particularly concerned with