Analyzing the fault geometry:
Given information:
- Northerly dipping fault (F-F)
- Beds P, Q, R are displaced
- Thickness of beds is constant across the fault
- Map view shows bed patterns on both sides
Observations from the map:
- The fault dips northward, making the north block the hanging wall and the south block the footwall
- Beds P, Q, R appear on both blocks
- The beds strike obliquely to the fault trace
Determining vertical displacement:
Examining the stratigraphic sequence across the fault:
- The hanging wall (north block) exposes stratigraphically older or higher structural levels
- This indicates the hanging wall has moved upward relative to the footwall
- Vertical component: Reverse fault
Determining lateral displacement:
Analyzing the horizontal offset of beds:
- Tracing any bed (e.g., bed Q) across the fault from south to north
- Standing on the south block and looking north across the fault, the corresponding bed on the north block is displaced to the left (west)
- This indicates left-lateral (sinistral) displacement
- Horizontal component: Sinistral fault
Conclusion:
The fault exhibits oblique-slip motion with two components:
- Reverse fault component (dip-slip): hanging wall moved up
- Sinistral fault component (strike-slip): left-lateral offset
Answer: (B) Reverse fault and (D) Sinistral fault