Lecture 9: Deformation Flashcards
Define Deformation and where it occurs
any changes in the original form of a rock body subjected to stress; most deformation of earth’s crust occurs along or near margins of lithospheric plates
What is strain?
The observed result of stress (revealed by structures produced by deformation)
What is stress? (2 types)
- Uniform Stress: applied to material equally in all directions
- Differential stress: applied unequally
What is differential stress? (3 types)
Compressional stress: squeezing, causes rock bodies to shorten and thicken vertically
Tensional: stretching, lengthen and thin vertically
Shear: slicing, causes rock bodies to change shape laterally
What are the 3 types of plate boundaries?
Convergent plate boundary: lithospheric plates move toward one another (compressive stress)
Divergent plate boundary: plates move away from one another (tensional stress)
Transform plate boundary: move past one another (shear stress)
What are the 2 ways in which rocks deform?
Brittle Deformation: rocks behave like a brittle solid and break (producing fractures)
Ductile: rocks can “flow” internally and behave in a more plastic manner (tending to bend and fold rather than breaking)
What happens when rocks have been deformed?
They can be tilted or bent
Fractures are often inclined
What is strike and dip? (Go over how to calculate it in the textbook)
We can recognize a dipping plane
The intersection of the dipping plane with a horizontal plane defines a line of strike
What is a joint?
A brittle deformation feature: fractures along which no significant displacement has occurred; “tension” cracks by relatively gentle warping of the crust (ex dolostone)
Can also develop as cooling features (shrinkage cracks) in lava flows and other igneous rock bodies (ex basalt)
What is a fault?
A brittle deformation feature: • Fractures along which significant displacement has occurred
What are the 2 main types of faults?
Dip slip faults and strike slip faults
What are dip slip faults?
“block” of rock above the dipping fault plane is called the “hanging wall” “block” of rock below the dipping fault plane is called the footwall
What are the main types of dip slip faults?
normal fault: produced when hanging wall moves down relative to footwall
reverse fault: produced when the hanging wall moves up relative to the footwall
Where are normal faults common?
at divergent plate margins where tensional stress predominates, normal faults commonly develop
bounded by normal faults are downthrown blocks called grabens
upthrown blocks called horsts
Where are reverse faults common?
at convergent plate margins where compressional stress predominates, reverse faults commonly develop