Fig. 19


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Compositions of fluid inclusions from the Puy-les-Vignes deposit determined by microthermometry and Raman spectroscopy. (A–C) Homogenization temperature for the Lc-w and Lw-c hosted in quartz and wolframite as function of the CO2 melting temperature (Tm CO2), the clathrate melting temperature (Tm clat), and salinity. (D) Homogenization temperature for the Lw hosted in quartz as function of salinity. (E) Volatile composition of the gas phase of Lc-w and Lw-c plotted in the CO2–CH4–N2 ternary diagram. (F) Bulk composition of Lc-w and Lw-c plotted in the H2O/10–∑volatile–NaCl ternary diagram.

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