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 11

Typical LA-ICPMS spectrum of a primary magmatic L1-type fluid inclusion hosted in a globular quartz crystal from the Beauvoir granite (sample B1-379a; FI n°A6b). The analysed fluid inclusion (picture in inset) is 17 μm in size and was ablated using a laser spot diameter of 32 μm (dashed white circle).