An Experimental Study of the Formation of Talc through CaMg(CO<sub>3</sub>)<sub>2</sub>–SiO<sub>2</sub>–H<sub>2</sub>O Interaction at 100–200°C and Vapor-Saturation Pressures

<div>X-ray patterns of the solid relicts in FSCCs containing dolomite and water after heating at 150°C for ~40 days (lower blue line) and at 200°C for ~20 days (middle orange line) and ~80 days (upper black line).</div>

Geofluids

fig5

Figure 5

Figure 5: An Experimental Study of the Formation of Talc through CaMg(CO<sub>3</sub>)<sub>2</sub>–SiO<sub>2</sub>–H<sub>2</sub>O Interaction at 100–200°C and Vapor-Saturation Pressures 

Geofluids

An Experimental Study of the Formation of Talc through CaMg(CO3)2–SiO2–H2O Interaction at 100–200°C and Vapor-Saturation Pressures

Figure 5

An Experimental Study of the Formation of Talc through CaMg(CO₃)₂–SiO₂–H₂O Interaction at 100–200°C and Vapor-Saturation Pressures