Research Article
Geochemical Modeling of Water-Rock Interaction in the Granulite Rocks of Lower Crust in the Serre Massif (Southern Calabria, Italy)
Figure 5
Moles of destroyed solid reactants 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, and (c) pCO2 of 10-2.8 bar.
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