Fluid Evolution of Fuzishan Skarn Cu-Mo Deposit from the Edong District in the Middle-Lower Yangtze River Metallogenic Belt of China: Evidence from Petrography, Mineral Assemblages, and Fluid Inclusions

Figure 10

Histograms of final homogenization temperatures (Th) and salinities for all inclusion types in different host minerals and stages. Prograde skarn stage (a), (b). Retrograde skarn stage (c), (d). Quartz-Sulfide stage (e), (f). Carbonate stage (g), (h). Grt: garnet; Di: diopside; Ep: epidote; Qtz: quartz; Adr II: late anhydrite; Cal: calcite.

(a)

(b)

(c)

(d)

(e)

(f)

(g)

(h)