16-Structural Geology Flashcards

1
Q

Stress and strain in rocks

A

Stress= force applied over unit area
Strain = how force manifests itself in the rock

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2
Q

Result of compression, extensional, and shear on rocks

A

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

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3
Q

3 types of deformation(elastic, plastic, brittle)

A

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

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4
Q

What does brittle or ductile deformation depend on

A

-type of stress
-amount of stress
-temperature
- strength of material (lithology)
-length of time rock is subjected to stress (strain rate)
-confining pressure (depth)

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5
Q

What depths do rocks experience brittle vs ductile behaviour

A

Rocks become more ductile with depth
Transition zone (6-15km) depending on lithology, fluid present
Few rocks exhibit brittle behaviour below 30km

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6
Q

Folding

A

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

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7
Q

Faulting

A

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

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8
Q

Types of faults and forces that cause them

A

Normal- tensional forces
Reverse-compression forces
Strike slip- shearing forces
**thrust faults are low angle reverse faults(<30 degrees)

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9
Q

Engineering hazard- fault zones

A

Represent major zones of weakness
Provide pathway for increased fluid flow (eg groundwater)

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10
Q

Rock joints

A

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

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