L8: Structural Geology Basics Flashcards
Brittle vs Ductile
Defines if rocks will break or bend under deformation
Usually, temperatures allowing for bending happen at 10-15 km depending on the rheology of the rock.
Rheology
Strength of rock
3 types of deformational forces and their faults
Compressional - Pushed together; collision zones; reverse faults
Tensional - Pulled apart; normal faulting; occurs at rifts and mid-ocean ridges
Shearing - Sliding past each other; strike-slip faults; conservative boundaries
Dextral vs sinistral strike-slip faults
Dextral - right displacment
Sinistral - left displacment
Throw and Heave in normal and reverse faulting
Throw is the vertical displacement
Heave is the horizontal displacement
Horst and Graben
When normal antithetic faults have their dips facing the block between them slips and forms a basin called a Graben
When normal antithetic faults have their dips facing away from each other this forms a topographically high block between them called a horst
Reverse faults
- When there is a compressional fault, occurs in collision zones and subduction zones
- Causes thickening of crust
- Hanging-wall is pushed up (against gravity).
- Less than 30 degrees are thrusts
- Rollover anticlines are formed.
Normal faults
- When there is a tensional fault; occurs in rifts and mid-ocean ridges
- Causes thinning of the crust
- Hanging-wall slides down (aided by gravity)
- Younger faults develop in the hanging-wall.
- Steep angles of 60 degrees are common.
- When multiple faults occur domino faults occur as the blocks rotate and listric faults are curved and concave upwards
Fold axis
Line of maximum curvature in a fold
Fold limbs
Rocks either side of the axis
Axial plane
Fold axis of multiple layers joined
Antiform
Upwards fold
Synform
Downwards fold
Recumbent fold
Sideways fold
Symmetric fold
Same both sides