Research Article

Geology, Mineralogy, Fluid Inclusion, and H–O–S–Pb Isotope Constraints on Ore Genesis of the Keyue Sb–Pb–Zn–Ag Deposit in Southern Tibet

Figure 10

Representative laser Raman spectra of FIs in the Keyue Sb–Pb–Zn–Ag deposit. (a) CO2 spectra of vapor phase in the W-type FIs of assemblage 2 Mn–Fe carbonate; (b) H2O spectra of liquid phase in the CO2-bearing W-type FIs of assemblage 2 Mn–Fe carbonate; (c) CO2 spectra of vapor phase in the CO2-bearing W-type FIs of assemblage 3 quartz; (d) H2O spectra of liquid phase in the CO2-bearing W-type FIs of assemblage 3 quartz; (e) CO2 spectra of vapor phase in the G-type FIs of assemblage 3 quartz; (f) CO2 spectra of vapor phase in the C-type FIs of assemblage 3 quartz; (g) CO2 spectra of vapor phase in the C-type FIs of assemblage 3 quartz; (h) H2O spectra of liquid phase in the C-type FIs of assemblage 3 quartz; (i) CO2 spectra of vapor phase in the CO2-bearing W-type FIs of assemblage 4 quartz; (j) H2O spectra of liquid phase in the CO2-bearing W-type FIs of assemblage 4 quartz.
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