To solve the problem of finding the variance (degree of freedom) of a mineral assemblage containing kyanite, sillimanite, and quartz, we will use the phase rule formula in thermodynamics of geology. The phase rule is expressed as:
F = C - P + 2
Where:
In this context, the components typically refer to the chemical components necessary to describe the minerals. For kyanite, sillimanite, and quartz, the principal components are usually aluminum (Al) and silicon dioxide (SiO₂), which implies:
Substituting into the phase rule formula:
F = 2 - 3 + 2
= 1
The degree of freedom F is 1.
| Group I | Group II |
| P. Sillimanite | 1. First order |
| Q. Quartz | 2. Second order |
| R. Muscovite | 3. Greater than third order |
| S. Calcite | 4. Third order variegated |
| Group I | Group II |
| P. Bababudan Group | 1. Eastern Dharwar |
| Q. Banded Gneissic Complex-I | 2. Western Dharwar |
| R. Bonai Granite | 3. Aravalli |
| S. Kolar Group | 4. Singhbhum |