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

<div>Plot of homogenization temperature (Th) versus salinity for fluid inclusions in different host minerals and stages, showing characteristics of fluid evolution in the Fuzishan Cu-Mo deposit. Note that the dotted ellipses representing fluid inclusion inferred for greater than 550°C in the prograde skarn stage.</div>

Geofluids

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Figure 11

Figure 11: 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 11 | 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 