Mafic rocks like basalt can undergo metamorphism under various conditions, resulting in different mineral assemblages. The question asks which assemblages can typically form in a metamorphosed basaltic composition.
Considering the typical metamorphic environments and the resultant mineral assemblages from a basaltic parent rock, the correct assemblages are:
| Group I | Group II |
| P. Stylolite | 1. Liquefaction |
| Q. Pseudonodule | 2. Diagenesis |
| R. Current crescent | 3. Organo-sedimentary binding |
| S. Stromatolite | 4. Scouring |