- Hydrocarbon traps are broadly classified into structural traps (caused by tectonic deformation) and stratigraphic traps (caused by depositional or erosional processes, i.e., facies changes).
- Salt dome is a structural trap caused by diapirism of salt, not by facies change.
- Unconformity traps occur where erosion or non-deposition truncates reservoir units, followed by sealing. This is a stratigraphic effect.
- Pinch out traps form when a porous reservoir facies thins out and pinches against non-permeable facies. This is due to facies variation.
- Sand lens traps occur where isolated sand bodies are encased in shale due to depositional changes.
Hence, traps due to sedimentary facies changes are (B), (C), and (D).