Step 1: Understanding the mineral sequence.
The order of increasing degree of sharing of (SiO₄)⁴⁻ tetrahedra refers to how the silicate tetrahedra are linked in minerals. In this context, minerals like Olivine have isolated tetrahedra, while minerals like Quartz have fully linked tetrahedra.
Step 2: Analyzing the options.
(A) Olivine → Tremolite → Enstatite → Quartz: This is incorrect, as the sequence of increasing tetrahedral sharing is not followed correctly.
(B) Olivine → Enstatite → Tremolite → Quartz: Correct — This sequence correctly reflects the increasing degree of tetrahedral sharing, from isolated in Olivine to fully linked in Quartz.
(C) Quartz → Tremolite → Enstatite → Olivine: Incorrect, as Quartz should be at the end.
(D) Olivine → Quartz → Enstatite → Tremolite: Incorrect, as Quartz should be at the end in terms of tetrahedral sharing.
Step 3: Conclusion.
The correct answer is (B) Olivine → Enstatite → Tremolite → Quartz.
| Group I | Group II |
| P. Sillimanite | 1. First order |
| Q. Quartz | 2. Second order |
| R. Muscovite | 3. Greater than third order |
| S. Calcite | 4. Third order variegated |
| Group I | Group II |
| P. Bababudan Group | 1. Eastern Dharwar |
| Q. Banded Gneissic Complex-I | 2. Western Dharwar |
| R. Bonai Granite | 3. Aravalli |
| S. Kolar Group | 4. Singhbhum |