In the given schematic diagram, cross beds are exposed on a vertical rock face. The feature XY (bold line) represents a/an:

Step 1: What is a reactivation surface?
Within a set of cross beds produced by migrating dunes, episodes of brief flow-strength changes or minor scour create a gently erosional surface that truncates older foresets and is then overlain by a new set of foresets with a slightly different dip—this is a reactivation surface.
Step 2: Read the diagram features.
The bold XY line:
These are hallmark traits of a reactivation surface.
Step 3: Eliminate incorrect options.
- (B) Foreset: a foreset is a bed inclined in the flow direction, not a truncation surface; XY clearly truncates foresets.
- (C) Scoured channel base: would display a major concave-up erosional surface separating distinct lithofacies; XY is a thin internal surface within cross-beds.
- (D) Angular unconformity: separates older tilted strata from younger overlying beds at a large angular discordance; XY is much smaller-scale within a single dune set.
Final Answer:
\[ \boxed{\text{Reactivation surface}} \]
The schematic diagram represents thin section of a carbonate rock. The type of cement formed by large calcite crystals is known as:

Match the following structures in Group I with the corresponding environment of deposition in Group II: 
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)