Earth Structure Flashcards
Ductile deformation
A solid-state flow that results in a change in size and shape of rocks without fracturing. Occurs in high temperature and pressure environment.
Folds
Flat-lying sedimentary and volcanic rocks bent into a series of wavelike undulations. Result of compressional stresses.
- anticlines: unfolding
- syncline: downfolded
Dome
Circular or slightly elongated, up-warped displacement of rocks, oldest rocks in core
Basin
Circular or slightly elongated, down-warped displacement of rocks, youngest rocks in core
Faults
Fractures (breaks) in rocks along which appreciable displacement had taken place
Dip-slip faults
Faults in which movement is primarily vertical. Movement along inclination (dip) of fault plane.
Normal faults
Hanging wall block moves down relative to the foot wall block caused by tension all forces
Reverse faults and thrust faults
Dip-slip faults in which the hanging wall block moves up relative to the foot wall block caused by compressional stresses.
- reverse faults >45 degrees
- thrust faults
Strike-slip faults
Faults in which the dominant displacement is horizontal and parallel to the trend or strike of the fault surface.
Transform faults
Large strike-slip faults that cut through lithosphere-often associated with plate boundaries
Joints
Fractures along which no appreciable displacement has occurred. Most are result of brittle failure of rock units located in outermost crust.
Deformation
Changes in shape and volume of a rock body.