
From the given phase diagram, we observe that point P lies at a composition between A and B. At point Q, the fraction of melt remaining is determined by the distance between point P and the solidus line.
The fraction of melt remaining at point Q for a magma with initial composition at point P is given as 0.5, according to the phase diagram.
The fraction of melt remaining at point Q is: 0.5.
| Group I | Group II |
| P. Stylolite | 1. Liquefaction |
| Q. Pseudonodule | 2. Diagenesis |
| R. Current crescent | 3. Organo-sedimentary binding |
| S. Stromatolite | 4. Scouring |