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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