Step 1: Pressure–temperature slope.
The Clapeyron relation for an equilibrium is
\[
\frac{dP}{dT}=\frac{\Delta S_r}{\Delta V_r}.
\]
For a good geothermometer we want $T$ to be well constrained with minimal sensitivity to $P$.
Step 2: Conditions that reduce $P$-sensitivity and increase $T$-sensitivity.
- A small $\Delta V_r$ makes the equilibrium nearly insensitive to pressure (baric effect minimized).
- A large $\Delta S_r$ (hence often large $\Delta H_r$) makes the equilibrium strongly temperature dependent (steep $\frac{dP}{dT}$; isopleths are near-vertical, so uncertainty in $P$ produces little uncertainty in $T$).
Step 3: Eliminate alternatives.
(B) gives $P$-sensitive, $T$-insensitive behavior (good for barometers, not thermometers).
(C) and (D) give signs, not magnitudes; sign alone doesn't ensure thermometer suitability.
Final Answer:
\[
\boxed{\text{(A) small }\Delta V_r\ \text{but large }\Delta S_r}
\]
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?