
The AFM diagram is used to understand the stability of minerals in different zones of metamorphic rocks, particularly pelitic rocks. In the given AFM diagram, we have to identify the compositions characterized by the equilibrium assemblage of muscovite, garnet, biotite, and quartz.
Understanding the Diagram:
Based on the diagram:
Conclusion:
Thus, the options characterized by the equilibrium assemblage of muscovite + garnet + biotite + quartz are P and R.
| Group I | Group II |
| P. Stylolite | 1. Liquefaction |
| Q. Pseudonodule | 2. Diagenesis |
| R. Current crescent | 3. Organo-sedimentary binding |
| S. Stromatolite | 4. Scouring |