A schematic deformation (D)-metamorphism (M)-time map of a metamorphic belt is shown below. The belt recorded two phases of deformation, D₁-D₂ and attendant schistosity, S₁-S₂ and metamorphism, M₁-M₂. The metamorphic minerals stable during these events are shown by solid lines. On the basis of this information, which of the following statement(s) is/are correct? 
Step 1: Analysis of the D-M-time diagram:
Reading the diagram:
Step 2: Evaluating each statement:
(A) - M₁ is a long-duration, broad event associated with deformation (D₁/S₁ and D₂/S₂) - characteristic of regional metamorphism. M₂ is a shorter, localized thermal event without associated deformation, producing andalusite - characteristic of contact metamorphism from igneous intrusion.
(B) - S₁ is the first schistosity formed during D₁. Crenulation cleavage forms when a pre-existing foliation is refolded, creating a new cleavage. Since S₁ is the first fabric, it would be a slaty cleavage or schistosity, not a crenulation cleavage. S₂ might be a crenulation cleavage formed by deforming S₁.
(C) - The diagram shows garnet is stable during the D₁/S₁ peak. "Syntectonic" means growing during deformation. Since garnet's stability coincides with D₁, it grew syntectonically with D₁.
(D) - Andalusite appears only during M₂, which occurs after D₂/S₂ has ended (note M₂ is to the right of the D₂/S₂ peak). Andalusite grew during M₂ contact metamorphism, post-dating D₂, not during its waning phase.
Answer: (A) and (C) are correct
The schematic diagram given below shows textual relationship among garnet, muscovite, biotite and kyanite in a metapelite. Biotite defines S1 foliation and muscovite defines S2 and S3 foliations. S1, S2, and S3 fabrics were developed during distinct deformation events D1, D2, and D3, respectively. Which one of the following represents the pre-D3 mineral assemblage? 
The shaded region (P) in the given ACF diagram represents the compositional range of mafic rocks that have undergone granulite facies metamorphism. Which of the following equilibrium mineral assemblages is/are identified in these mafic rocks? 