Figure 3From: On the potential for CO2mineral storage in continental flood basalts – PHREEQC batch- and 1D diffusion–reaction simulationsMass fractions of minerals following basalt alteration at 60, 80, and 100 C over 10000 years: a, d, g) primary basalt minerals and glass; b,e, h) secondary phases except the carbonates; and c, f, j) carbonates.Back to article page