Step 1: Recall contact metamorphism process. Contact metamorphism occurs when rocks are heated by intrusion of magma, usually at relatively shallow crustal levels. High temperature is the dominant factor.
Step 2: Effect of increasing temperature. With increasing temperature: - Grain boundaries become unstable, grains break down into smaller crystals. - As grains become finer, their surface area per unit volume increases.
Step 3: Interpret the ratio. \[ \text{Ratio} = \frac{\text{Volume}}{\text{Surface Area}} \] - For smaller grains, surface area increases faster than volume. - Therefore, the ratio \(\dfrac{V}{A}\) decreases.
Step 4: Eliminate wrong options. - (A) Increases → incorrect. - (C) Reaction kinetics become slower → wrong, they become faster at higher temperature. - (D) Hydrous minerals become more stable → wrong, they tend to dehydrate and break down.
Final Answer: \[ \boxed{\text{the ratio of volume to surface area of mineral grains decreases.}} \]
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?
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?
A color model is shown in the figure with color codes: Yellow (Y), Magenta (M), Cyan (Cy), Red (R), Blue (Bl), Green (G), and Black (K). Which one of the following options displays the color codes that are consistent with the color model?