Igneous rocks are broadly classified based on their chemical composition, particularly their alkali (Na₂O + K₂O) content. The Tholeiitic and Calc-alkaline series represent two major compositional fields commonly encountered in igneous petrology.
True alkaline rocks possess a significantly higher concentration of alkali metals (Na₂O and K₂O). Both the Tholeiitic and Calc-alkaline series are grouped under the broader category of subalkaline rocks, differentiating them from the distinctly alkaline rock suites.
Based on their geochemical characteristics, both Tholeiitic and Calc-alkaline rock series are defined as subalkaline in nature.
| 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 |