Equilibrium digrams for the melting and crystallization of igneous rocks have many similarities to saturation diagrams for ice-water-salt mixtures. The temperatures are higher, but molten silicate liquids can be saturated with minerals. This chapter introduces binary (two-component) equilibrium diagrams for simple igneous systems. Concepts that are developed include:
- liquidus curves
- eutectic points
- congruent melting
- incongruent melting
- peritectic points