Research Article

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 2

Interpretative cross-section of the Beauvoir granite from the GPF1 drill hole showing the vertical magmatic internal zoning composed by the three successive facies B1, B2, and B3 (modified from [12]). The location of the samples studied in this work is also reported.