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>Raman spectrum of a cassiterite crystal contained in a primary L1-type fluid inclusion within a magmatic quartz crystal of the Beauvoir granite (sample B1-379c, FI n°6a). The Raman shift values indicated on the spectrum correspond to the Raman peaks of cassiterite. The other peaks are those of the host-quartz.</div>

Geofluids

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Figure 8

Figure 8: 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 8 | 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 