Step 1: Understand the Calculation of \( X_{Mg} \).
To calculate the overall mole fraction of magnesium (\( X_{Mg} \)) in the eclogite, we use the mole fractions of magnesium in garnet and omphacite, and their respective mineral abundances. The total mole fraction \( X_{Mg} \) of the eclogite is given by:
\[
X_{Mg} = \frac{X_{Mg,garnet} \times W_{garnet} + X_{Mg,omphacite} \times W_{omphacite}}{W_{garnet} + W_{omphacite}}
\]
Where:
- \( X_{Mg,garnet} = 0.50 \),
- \( X_{Mg,omphacite} = 0.75 \),
- \( W_{garnet} = 60 \) (percentage of garnet),
- \( W_{omphacite} = 40 \) (percentage of omphacite).
Step 2: Apply the Formula.
Substitute the values into the formula:
\[
X_{Mg} = \frac{(0.50 \times 60) + (0.75 \times 40)}{60 + 40} = \frac{30 + 30}{100} = \frac{60}{100} = 0.60
\]
Thus, the \( X_{Mg} \) of eclogite is 0.60.
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? 