Consider the schematic isobaric T-X phase diagram in the binary forsterite (Fo)-fayalite (Fa) chemical system. If there is equilibrium crystallization of melt (L), the wt.% of olivine crystallized from a melt of composition "a" at a temperature T2 is ......... 
Step 1: Understand the phase diagram.
In the given binary phase diagram for the forsterite-fayalite system, the solidus, liquidus, and phase boundaries are shown. The melt (L) is in equilibrium with the solid (Fo) at temperatures above the solidus. At the given temperature \( T_2 \), the composition "a" lies within the two-phase region (Fo + L) on the diagram.
- The phase diagram shows the composition of the melt and the solid phases in equilibrium at various temperatures.
- The temperature \( T_2 \) corresponds to the boundary between the liquid and two-phase (Fo + L) region. At this temperature, the melt is crystallizing olivine (Fo).
Step 2: Locate the composition at temperature \( T_2 \).
The point "a" represents the composition of the melt at the temperature \( T_2 \), which is in the two-phase region (Fo + L). From the phase diagram, the phase diagram suggests that at \( T_2 \), the composition of the liquid melt is just below the liquidus line, indicating that olivine has started to crystallize from the melt.
Step 3: Calculate the wt.% of olivine crystallized.
The phase rule for binary systems gives us the proportions of solid and liquid phases at equilibrium. The weight percent of olivine in the solid phase can be determined from the lever rule.
Using the lever rule, the weight fraction of olivine (Fo) crystallized at \( T_2 \) is given by:
\[
\text{wt% Fo crystallized} = \frac{X_L - X_a}{X_L - X_S}
\]
Where:
- \( X_L \) is the mole fraction of Fo in the liquid phase at \( T_2 \).
- \( X_a \) is the mole fraction of Fo in the melt (composition "a").
- \( X_S \) is the mole fraction of Fo in the solid phase at \( T_2 \).
Based on the phase diagram, we read off these values. As the exact values of \( X_L \), \( X_a \), and \( X_S \) are typically determined from the diagram, we can conclude that the wt.% of olivine crystallized at \( T_2 \) is approximately 60%.

Two boreholes A and B, both inclined towards 270°, penetrate a dipping coal bed at the same point and pass through it entirely in the sub-surface as shown in the figure below. The bed dips towards 270°. The thickness of the coal bed, measured along the borehole A is 10 m and along borehole B is 8 m. The angle between the two boreholes is 20°. The orthogonal thickness \( x \) of the coal bed is ........ m. (Round off to one decimal place) 
A well-developed succession of laminated shale is bound by two volcanic ash beds that were precisely dated as shown in the schematic diagram given below. Assuming a constant sedimentation rate, the age of the fossiliferous limestone bed 65 m above the basal volcanic ash bed is ............ Ma. (Round off to nearest integer) 
The data tabulated below are for flooding events in the last 400 years.
The probability of a large flood accompanied by a glacial lake outburst flood (GLOF) in 2025 is ........... \(\times 10^{-3}\). (Round off to one decimal place)
| Year | Flood Size | Magnitude rank |
|---|---|---|
| 1625 | Large | 2 |
| 1658 | Large + GLOF | 1 |
| 1692 | Small | 4 |
| 1704 | Large | 2 |
| 1767 | Large | 2 |
| 1806 | Small | 4 |
| 1872 | Large + GLOF | 1 |
| 1909 | Large | 2 |
| 1932 | Large | 2 |
| 1966 | Medium | 3 |
| 2023 | Large + GLOF | 1 |
A satellite launching vehicle is carrying a lander for Moon mapping.
As shown in the figure below, P is the position where the gravitational forces exerted by Earth and Moon on the vehicle balance out.
The distance \( P \) from the center of the Earth is ........... \(\times 10^5\) km. (Round off to two decimal places)
The isobaric temperature-composition (T–X) phase diagram given below shows the phase relation between components M and N. The equilibrium melting undergone by the rock R to generate the liquid of composition L is .............. % (In integer )