Geochemical Signature of Magmatic-Hydrothermal Fluids Exsolved from the Beauvoir Rare-Metal Granite (Massif Central, France): Insights from LA-ICPMS Analysis of Primary Fluid Inclusions

<div>Vapour-brine distribution coefficients determined by LA-ICPMS analysis of coexisting V2- and L2-type fluid inclusions from the Beauvoir granite and the La Bosse stockwork. Columns represent the average value calculated for each fluid inclusion population, whereas error bars indicate the standard deviation (1<i>σ</i>) associated with these averages.</div>

Geofluids

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Figure 14

Figure 14: Geochemical Signature of Magmatic-Hydrothermal Fluids Exsolved from the Beauvoir Rare-Metal Granite (Massif Central, France): Insights from LA-ICPMS Analysis of Primary Fluid Inclusions 

Figure 14 | Geochemical Signature of Magmatic-Hydrothermal Fluids Exsolved from the Beauvoir Rare-Metal Granite (Massif Central, France): Insights from LA-ICPMS Analysis of Primary Fluid Inclusions 