Rock Deformation Flashcards

1
Q

Where do rocks get deformed?

A

Where tectonic forces exert pressure (stress) on rocks -> Mostly at or near plate boundaries

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2
Q

what is stress?

A

force applied per unit area

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3
Q

what does stress cause?

A

strain

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4
Q

what does uniform stress (=confining pressure) do to rocks

A

squeezes rock (no shape change)

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5
Q

what does differential stress (=directed pressure; unequal application of stress) do to rocks?

A

distorts rock

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6
Q

what is yield stress?

A

amount of stress needed to deform the rock (to make it “yield”)

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7
Q

what does yield stress depend on?

A

rock strength

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8
Q

what is strain?

A

change in shape of body by deformation

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9
Q

what are the two types of strain?

A

(1) Brittle deformation - breaks/fractures (faults, joints)
(2) Ductile deformation - bends/flows (folds)
Type depends on composition, P, T, strain rate.

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10
Q

when are rocks stronger?

A

at higher pressure (greater depths)

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11
Q

when are rocks weaker?

A

at higher temperatures

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12
Q

deformation at shallower depths…

A

brittle

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13
Q

deformation at greater depth…

A

more ductile

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14
Q

what are the three types of differential stress?

A

tensional stress -> EXTENSION
compressional stress -> COMPRESSION
shear stress -> Lateral shift

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15
Q

what are some example of geological structure formed by deformation?

A
Brittle deformation
- Joints
- Faults
Ductile deformation
- Folds
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16
Q

what are joints?

A

fractures with no movement

17
Q

what do joints result from?

A

may result from cooling -> contraction (e.g. basalt columns)
OR
pressure unloading -> sheeting

18
Q

what are faults?

A

fractures along which displacement has occurred (one side moves relative to the other)

19
Q

what does a sudden, rapid slip on fault plane lead to?

A

earthquakes

slip of cm to 10s of m in one event

20
Q

what are the types of faults?

A

Strike-slip faults
-Movement is horizontal (to left or right)
-Parallel to the strike of the fault
Dip-slip faults
-Movement up or down
-Parallel to the dip of the fault surface
-e.g. Normal faults and Reverse (thrust) faults

21
Q

San Andreas is a transform plate boundary, strike-slip fault. is it left or right lateral?

A

right lateral

22
Q

how is the type of dip-slip fault defined?

A

the relative motion (slip) of:
hanging wall vs. footwall
(i.e. does the hanging wall move up or down)

23
Q

what happens at a normal fault?

A

Hanging wall (upper block) moves DOWN the dip of the fault surface

  • Caused by extensional stress
  • Leads to crustal thinning
24
Q

what happens at a reverse (thrust) fault?

A

Hanging wall (upper block) moves UP the dip of the fault surface

  • Caused by compressional stress
  • Leads to crustal thickening, shortening
25
Q

what is a thrust fault?

A

reverse fault with dip angle ≤ 45°

26
Q

what are folds?

A

Warping of rock layers at all scales (micro to mega)

  • Shortening – contraction
  • Form over long time periods as rocks yield to compressional stress – ductile behaviour
  • Mountain belts – regional folding of rocks, and many folds can be refolded, overturned etc
27
Q

what is an example of ductile extensional deformation?

A

boudins