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 13

Average concentration of L1-type fluid inclusions (FI) contained in primary quartz from the Beauvoir B1 granite determined by LA-ICPMS versus average whole-rock concentration of the B1 granite compiled from Cuney et al. [12] and Raimbault et al. [13].