Step 1: Understanding crystallization in layered intrusions.
In layered intrusions, plagioclase crystallizes from a basic magma as a function of temperature and pressure. Early crystallization forms anorthite-rich (calcium-rich) plagioclase at the base, while late-stage crystallization leads to albite-rich (sodium-rich) plagioclase at the top.
Step 2: Analyzing the options.
(A) Cumulus texture at the base: This is correct as cumulus texture refers to the texture formed by the settling of crystals.
(B) Anorthite-rich early plagioclase at the base: This is the correct answer as anorthite-rich plagioclase is the first to crystallize from a basic magma.
(C) Albite-rich late plagioclase at the top: This is correct.
(D) Quench texture at the base: This is incorrect because quench textures form rapidly from a cooling lava, not in the crystallization of plagioclase in a layered intrusion.
Step 3: Conclusion.
The correct answer is (A), (B) and (C).
| Group I | Group II |
| P. Stylolite | 1. Liquefaction |
| Q. Pseudonodule | 2. Diagenesis |
| R. Current crescent | 3. Organo-sedimentary binding |
| S. Stromatolite | 4. Scouring |