Adding a third chemical component to a magma leads to some qualitatively different features upon crystallization. These features are revealed by examining ternary (three-component) equilibrium diagrams for simple igneous systems. Concepts that are developed in this chapter include:
- saturation of ternary liquids
- ternary lever rule
- ternary liquidus surfaces
- ternary cotectic curves
- ternary reaction curves
- ternary eutectic points