The formula to calculate the ϕ (phi) value of a sediment grain is:
\[ ϕ = -\log_2 \left( \frac{D}{1} \right) \]
Where:
Given that the diameter D = 0.125 mm, we substitute this value into the formula:
\[ ϕ = -\log_2 (0.125) \]
Since \( \log_2 (0.125) = -3 \), we get:
\[ ϕ = 3 \]
Thus, the correct value of ϕ is: 3.
| 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 |