Step 1: Relate Retardation, Thickness, and Birefringence
The retardation ($\Gamma$) is defined by the difference in path length between the two rays (O-ray and E-ray) traveling through the mineral, and is calculated as:
$$\Gamma = t \cdot |n_o - n_e|$$
Where:
$\Gamma$ = Retardation (path difference)
$t$ = Thickness of the mineral (thin section)
$n_o$ = Refractive index of the O-ray (Ordinary ray)
$n_e$ = Refractive index of the E-ray (Extraordinary ray)
Step 2: Standardize Units
Convert the given thickness ($t$) from millimeters ($\text{mm}$) and the retardation ($\Gamma$) from nanometers ($\text{nm}$) to the same unit, meters ($\text{m}$), for consistency:
Thickness: $t = 0.03 \text{ mm} = 0.03 \times 10^{-3} \text{ m}$
Retardation: $\Gamma = 5160 \text{ nm} = 5160 \times 10^{-9} \text{ m}$
Step 3: Calculate Birefringence
Rearrange the retardation formula to solve for birefringence ($|n_o - n_e|$):
$$|n_o - n_e| = \frac{\Gamma}{t}$$
Substitute the standardized values:
$$|n_o - n_e| = \frac{5160 \times 10^{-9} \text{ m}}{0.03 \times 10^{-3} \text{ m}}$$
$$|n_o - n_e| = \frac{5160}{0.03} \times 10^{-6} = 172000 \times 10^{-6}$$
$$|n_o - n_e| = 0.172$$
Step 4: Determine $n_o$
The problem states the mineral is uniaxial negative. For a uniaxial negative mineral, the $\text{O-ray}$ has a greater refractive index than the $\text{E-ray}$ ($n_o > n_e$).
Therefore, the birefringence is calculated as:
$$n_o - n_e = 0.172$$
We are given the refractive index of the E-ray: $n_e = 1.486$.
Solve for $n_o$:
$$n_o = n_e + 0.172$$
$$n_o = 1.486 + 0.172$$
$$n_o = 1.658$$
The value of the refractive index of the O-ray is 1.658.
A magma having density of 2900 kg m\(^-3\) just reaches the surface through a two-layered crust as shown in the figure below. Assuming isostatic equilibrium, its depth of melting is .......... km. (Round off to one decimal place) 
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)