Geochemical Modeling of Water-Rock Interaction in the Granulite Rocks of Lower Crust in the Serre Massif (Southern Calabria, Italy)

Figure 6

Moles of solid product phases against alkalinity, showing the results of reaction path modeling for the dissolution of granulite (a) pCO₂ of 10^-2.0 bar, (b) pCO₂ of 10^-2.4 bar, (c) pCO₂ of 10^-2.8 bar.

(a)

(b)

(c)