To determine which structures form in a marine environment, we need to understand the characteristics of the options given:
These structures are typically found in fluvial and deltaic environments. However, they can also form in marine environments in certain settings, particularly where sediments accumulate laterally along tidal channels or estuarine settings.
Hummocky cross stratification is a type of sedimentary structure commonly associated with storm-dominated marine environments. It forms in shallow marine settings, such as on continental shelves, where oscillatory currents created by storms rework the bottom sediments.
This structure typically forms in tidal environments, which are part of marine settings. Herringbone cross stratification results from alternating tidal currents that change direction, creating cross-bedding that appears to criss-cross.
Barchanoids or barchan dunes are generally associated with aeolian (wind-driven) processes and occur in desert environments. Therefore, they do not typically form in marine environments.
Based on the explanations above, the correct structures that form in marine environments are:
Therefore, the correct answer involves identifying these structures as appropriate for marine settings, as they are influenced by water currents and sedimentation patterns unique to marine and tidal settings.
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 )