Deformation
Deformation of Rock: Stress-Strain Recap
Stress – forces applied to a rock by Earth movements or the mass of overlying rock
Strain – a change in the shape or volume of a body as a result of applied stress
Factors that Affect a Rocks Behaviour
• Temperature – higher temperature makes the rock more plastic
• Time – slow = fold, fast = fracture
• Pressure – confining pressure – depth into crust
• Strength – composition determines whether it is competent or incompetent
Faults
Principal Stress Orientations Heave
Throw
Maximum Stress Pmax σ1
Intermediate Stress Pmin σ2
Minimum Stress Pint σ3
Normal Fault (Tensional Stress)
Pmax
Footwall Hanging Wall
Pmin → Pmin Thrust Fault (Compressional Stress)
Pmin
Pint Pmax
Pmax
Reverse Fault (Compressional Stress)
Pmax →
Pmin
Pint Pmin
Pmax → Pmax Strike Slip Fault (Shear Stress)
Pmax Pmin
Pint
Pmin
SWAN – Synclines are Wider on the downthrown side
and Anticlines are Narrower
Pmin
Pmax
Pint
Deformation of Rock: Stress-Strain Recap
Stress – forces applied to a rock by Earth movements or the mass of overlying rock
Strain – a change in the shape or volume of a body as a result of applied stress
Factors that Affect a Rocks Behaviour
• Temperature – higher temperature makes the rock more plastic
• Time – slow = fold, fast = fracture
• Pressure – confining pressure – depth into crust
• Strength – composition determines whether it is competent or incompetent
Faults
Principal Stress Orientations Heave
Throw
Maximum Stress Pmax σ1
Intermediate Stress Pmin σ2
Minimum Stress Pint σ3
Normal Fault (Tensional Stress)
Pmax
Footwall Hanging Wall
Pmin → Pmin Thrust Fault (Compressional Stress)
Pmin
Pint Pmax
Pmax
Reverse Fault (Compressional Stress)
Pmax →
Pmin
Pint Pmin
Pmax → Pmax Strike Slip Fault (Shear Stress)
Pmax Pmin
Pint
Pmin
SWAN – Synclines are Wider on the downthrown side
and Anticlines are Narrower
Pmin
Pmax
Pint