Step 1: Identify the crystal class.
The point group 4/m 3 2/m belongs to the isometric (cubic) system, specifically the octahedral class (also called the full cubic symmetry).
Step 2: List symmetry elements.
The octahedral (4/m 3 2/m) class contains:
- Axes of rotation:
- 3 fourfold axes (along cube axes),
- 4 threefold axes (along cube body diagonals),
- 6 twofold axes (along cube face diagonals).
Total = 13 rotational axes.
- Mirror planes:
- 9 mirror planes (3 axial, 6 diagonal).
- Center of symmetry:
- 1 inversion center.
- Rotoinversion/symmetry combinations:
- These generate the full set such that the total count = 24 distinct symmetry elements.
Step 3: Confirm standard reference.
In crystallography tables, the point group 4/m 3 2/m (Oh) is known to have the maximum possible symmetry elements: 24.
Final Answer:
\[
\boxed{24}
\]
The following table provides the mineral chemistry of a garnet. All oxides are in weight percentage and cations in atoms per formula unit. Total oxygen is taken as 12 based on the ideal garnet formula. Consider Fe as Fetotal and Fe\(^{3+}\) = 0. The Xpyrope of this garnet is _.
The following table provides the mineral chemistry of a garnet. All oxides are in weight percentage and cations in atoms per formula unit. Total oxygen is taken as 12 based on the ideal garnet formula. Consider Fe as Fetotal and Fe\(^{3+}\) = 0. The Xpyrope of this garnet is _.

Choose the correct combination of minerals (listed in Group A) with the corresponding locations of their deposits (listed in Group B).

While doing Bayesian inference, consider estimating the posterior distribution of the model parameter (m), given data (d). Assume that Prior and Likelihood are proportional to Gaussian functions given by \[ {Prior} \propto \exp(-0.5(m - 1)^2) \] \[ {Likelihood} \propto \exp(-0.5(m - 3)^2) \] 
The mean of the posterior distribution is (Answer in integer)
Consider a medium of uniform resistivity with a pair of source and sink electrodes separated by a distance \( L \), as shown in the figure. The fraction of the input current \( (I) \) that flows horizontally \( (I_x) \) across the median plane between depths \( z_1 = \frac{L}{2} \) and \( z_2 = \frac{L\sqrt{3}}{2} \), is given by \( \frac{I_x}{I} = \frac{L}{\pi} \int_{z_1}^{z_2} \frac{dz}{(L^2/4 + z^2)} \). The value of \( \frac{I_x}{I} \) is equal to 
Suppose a mountain at location A is in isostatic equilibrium with a column at location B, which is at sea-level, as shown in the figure. The height of the mountain is 4 km and the thickness of the crust at B is 1 km. Given that the densities of crust and mantle are 2700 kg/m\(^3\) and 3300 kg/m\(^3\), respectively, the thickness of the mountain root (r1) is km. (Answer in integer)