Final answer:
Low temperature, low confining pressure, low strain rate, and absence of water can all promote ductile deformation in rocks.
Step-by-step explanation:
Low temperature, low confining pressure, low strain rate, and absence of water can all promote ductile deformation in rocks.
- Low temperature: At low temperatures, the rocks are less likely to undergo brittle fracture and are more likely to deform plastically.
- Low confining pressure: Low confining pressure allows the rocks to deform more easily without fracturing.
- Low strain rate: A low strain rate means that the rocks are being deformed slowly, allowing them to deform plastically rather than fracturing.
- Absence of water: The presence of water can weaken the rocks and make them more likely to fracture, so the absence of water can promote ductile deformation.