The question is related to the geological contact between the Talchir Formation and the underlying Precambrian basement. Understanding this requires knowledge of geological unconformities and stratigraphy. The options present various types of unconformities, each representing different geological processes:
For the Talchir Formation, which is the lowest formation of the Gondwana sequence resting over the older Precambrian rocks, the contact is characterized as an unconformity. This general term indicates a significant time gap between the deposition of the Precambrian basement and the overlying Talchir rocks, without specifying the nature (parallel, angular, etc.) of the strata involved.
Conclusion: The correct answer is an unconformity because the Talchir Formation lies unconformably over the Precambrian basement due to the significant time and depositional gap, but it does not specify the detailed nature of the unconformity, whether angular or parallel.
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) 
Match the stratigraphic units in Group I with their corresponding basins in Group II.
| Group I | Group II |
|---|---|
| P. Kajrahat Limestone | 1. Cuddapah |
| Q. Shahabad Limestone | 2. Pranhita-Godavari |
| R. Chanda Limestone | 3. Vindhyan |
| S. Narji Limestone | 4. Bhima |
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) 
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 )