To determine which textural feature results from exsolution, we first need to understand the term exsolution. Exsolution is a process where an initially homogeneous solid solution separates into two different crystalline minerals without the addition or removal of material. This typically occurs in minerals as they cool and results in exsolved textures.
Now let's examine the options:
Thus, the correct answer is Perthitic, as it specifically results from the exsolution process.
In summary, perthitic texture is a result of the exsolution process where plagioclase and potassium feldspar separate at lower temperatures, leading to the characteristic intergrowth.
| 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 |