4.4 Peritectic Point

Le-SiO2 vs. T Diagram

Figure 4.04. KAl(Si2O6)-SiO2 (Le-Silica) equilibrium phase diagram with the peritectic point labeled. The peritectic point due to the incongruent melting of sanidine is labeled. It gives the composition (42.2% SiO2) of a liquid that is saturated with both Lct and Sa at 1150°C. Click on the diagram to see the enlarged, interactive version of Figure 4.03 with the peritectic label.

When a mineral that melts incongruently is present in a binary (two-component) system, the liquidus curves for that mineral (e.g. sanidine) and its melting product mineral (e.g. leucite) meet at a peritectic point. The peritectic point for sanidine and leucite is labled here on Figure 04. A peritectic point marks the temperature of the incongruent melting reaction and the composition of the liquid involved in that reaction.

When a Lct-Silica liquid with less than 42.2% SiO2 is cooled, it will start crystallizing leucite when it's temperature reaches the Lct liquidus curve. As the temperature falls further, more Lct will crystallize and the liquid composition will become richer in SiO2 following the liquidus curve. When the temperature reaches the peritectic temperature (1150°C), the leucite present will react with the remaining liquid in the proportions 48% Lct to 52% Liquid to form sanidine crystals. For most bulk compositions, either the Lct will be used up or the Liquid will be used up in this reaction, leaving the other reactant remaining. Answer the following questions to show that you understand which reactant will remain.

For equilibrium cooling of a Lct-SiO2 magma with a bulk composition of 30% SiO2, which of the two peritectic reactant phases (Lct or Liquid) will remain at 1050°C?