In the isochemical phase diagram shown below, the curved arrow represents the P-T path. The variance at peak metamorphism is _. 
| Group-I | Group-II | ||
| P | Core-mantle | 1 | Radiating fibrous aggregate of K-feldspar with or without quartz |
| Q | Decussate | 2 | Large strained mineral grains surrounded by fine-grained, recrystallized grains |
| R | Spherulite | 3 | Inclusion trails in a porphyroblast curves into the matrix foliation by developing concave outward pattern |
| S | Millipede | 4 | Randomly oriented mineral grains dominated by crystal faces, such as in sheet silicates |
| Group-I | Group-II | ||
| P | Diopside | 1 | Cubic |
| Q | Galena | 2 | Octahedral |
| R | Calcite | 3 | Prismatic |
| S | Fluorite | 4 | Rhombohedral |