The concentration of Sm in the basaltic magma can be calculated using the partition coefficient formula:
\[ K_d = \frac{C_{\text{clinopyroxene}}}{C_{\text{magma}}} \]
Where:
Rearranging the equation to solve for Cmagma:
\[ C_{\text{magma}} = \frac{C_{\text{clinopyroxene}}}{K_d} \]
Substitute the given values into the equation:
\[ C_{\text{magma}} = \frac{24 \, \text{ppm}}{1.2} = 20 \, \text{ppm} \]
The concentration of Sm in the basaltic magma is: 20 ppm.
| Group I | Group II |
| P. Stylolite | 1. Liquefaction |
| Q. Pseudonodule | 2. Diagenesis |
| R. Current crescent | 3. Organo-sedimentary binding |
| S. Stromatolite | 4. Scouring |