Download original image
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.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.