Step 1: Understanding blueschist facies metamorphism:
Blueschist facies represents high-pressure, low-temperature metamorphism, typically occurring in subduction zones where oceanic crust is rapidly buried to great depths without significant heating.
Step 2: Evaluating each option:
(A) Hornblende: Common amphibole in amphibolite facies (medium-grade metamorphism). Not diagnostic of blueschist facies
(B) Anthophyllite: An orthorhombic amphibole. Not characteristic of high-pressure conditions
(C) Glaucophane: Sodium-rich blue amphibole. The presence of glaucophane is diagnostic of blueschist facies
(D) Actinolite: Calcium-magnesium amphibole. Not diagnostic of blueschist facies
Answer: (C) glaucophane
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? 