The question asks about the optical properties of the apatite mineral's {0001} section. Apatite is commonly observed under a petrographic microscope, and its optical properties can help in its identification.
In conclusion, the correct properties of the apatite {0001} section are Centered uniaxial interference figure because it reflects the characteristic optical behavior of uniaxial minerals like apatite when aligned correctly. The other property, Isotropic under crossed nicols, is incorrect but was mistakenly included in the context of the available choices. The centered uniaxial interference figure is a definitive characteristic.
| 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 |