16-Structural Geology Flashcards
Stress and strain in rocks
Stress= force applied over unit area
Strain = how force manifests itself in the rock
Result of compression, extensional, and shear on rocks
Compression = crustal rocks pushed together, leads to horizontal shortening/vertical lengthening
Extensional = crustal rocks pulled apart, leads to horizontal lengthening/vertical shortening
Shear = rocks pushed in opposite directions, leads to rocks breaking into sub-parallel blocks
3 types of deformation(elastic, plastic, brittle)
Elastic = temporary changes, recovers when stress is removed, stores energy
Plastic = permanent change, in rocks results in folding
Brittle = loss of cohesion due to stress, in rocks results in faults or fractures
What does brittle or ductile deformation depend on
-type of stress
-amount of stress
-temperature
- strength of material (lithology)
-length of time rock is subjected to stress (strain rate)
-confining pressure (depth)
What depths do rocks experience brittle vs ductile behaviour
Rocks become more ductile with depth
Transition zone (6-15km) depending on lithology, fluid present
Few rocks exhibit brittle behaviour below 30km
Folding
Deformation event resulting from horizontal compression of rock layers by internal forces of the earth along plate boundaries
-plastic-ductile deformation
-no breaking, rocks remain intact
-occurs over millions of years
Faulting
Process by which rocks break and move along a fracture
-brittle deformation
-fracturing, rock layers too rigid to bend/fold
-Occurs in seconds
-associated with earthquakes
Types of faults and forces that cause them
Normal- tensional forces
Reverse-compression forces
Strike slip- shearing forces
**thrust faults are low angle reverse faults(<30 degrees)
Engineering hazard- fault zones
Represent major zones of weakness
Provide pathway for increased fluid flow (eg groundwater)
Rock joints
Involve fracture along which there has been no observable movement of one side relative to the other
3 types
1. Tectonic joints: tectonic stresses induce tensile failure
2. Unloading joints: uplift and erosion removes the overlaying rock thereby reducing the compressive load and allowing rock to expand laterally
3. Cooling joints: cooling of hot magma/lava introducing stresses that induce tensile failure of the rock