Mineral X (volume %) Y (volume %) Quartz 15 25 Plagioclase 20 60 Alkali feldspar 65 15
The table below presents the modal volume percentages of essential minerals for rocks X and Y, which are used for their classification:
| Mineral | X (volume %) | Y (volume %) |
|---|---|---|
| Quartz | 15 | 25 |
| Plagioclase | 20 | 60 |
| Alkali feldspar | 65 | 15 |
The International Union of Geological Sciences (IUGS) classifies coarse-grained granitoid rocks using the QAPF diagram. This classification hinges on the relative proportions of Quartz (Q), Alkali feldspar (A), and Plagioclase (P).
The classification criteria involve:
Specific boundaries relevant here are:
Evaluate the mineral composition of Rock X against the IUGS criteria:
Evaluate the mineral composition of Rock Y against the IUGS criteria:
Based on the analysis using IUGS criteria:
| Group-I | Group-II |
| P. Boninite | 1. Continental anorogenic |
| Q. Lamproite | 2. Island-arc |
| R. Phonolite | 3. Continental collision |
| S. Leucogranite | 4. Intraplate oceanic |
Match the following igneous textures in Group-I with their definitions in Group-II.
Group-I | Group-II | ||
| P | Vitrophyre | 1 | Alkali feldspar rimmed by plagioclase |
| Q | Rapakivi | 2 | Aggregate of radially arrayed, needle-like crystals of plagioclase with or without clinopyroxene |
| R | Ocelli | 3 | Sub-parallel skeletal, platy olivine and/or pyroxene |
| S | Spinifex | 4 | Large phenocrysts within a glassy matrix |