Lecture 9: Deformation Flashcards

1
Q

Define Deformation and where it occurs

A

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

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2
Q

What is strain?

A

The observed result of stress (revealed by structures produced by deformation)

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3
Q

What is stress? (2 types)

A
  1. Uniform Stress: applied to material equally in all directions
  2. Differential stress: applied unequally
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4
Q

What is differential stress? (3 types)

A

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

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5
Q

What are the 3 types of plate boundaries?

A

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)

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6
Q

What are the 2 ways in which rocks deform?

A

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)

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7
Q

What happens when rocks have been deformed?

A

They can be tilted or bent

Fractures are often inclined

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8
Q

What is strike and dip? (Go over how to calculate it in the textbook)

A

We can recognize a dipping plane

The intersection of the dipping plane with a horizontal plane defines a line of strike

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9
Q

What is a joint?

A

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)

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10
Q

What is a fault?

A

A brittle deformation feature: • Fractures along which significant displacement has occurred

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11
Q

What are the 2 main types of faults?

A

Dip slip faults and strike slip faults

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12
Q

What are dip slip faults?

A

“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

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13
Q

What are the main types of dip slip faults?

A

normal fault: produced when hanging wall moves down relative to footwall
reverse fault: produced when the hanging wall moves up relative to the footwall

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14
Q

Where are normal faults common?

A

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

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15
Q

Where are reverse faults common?

A

at convergent plate margins where compressional stress predominates, reverse faults commonly develop

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16
Q

What is a strike slip fault?

A

The fault is vertical (so there is no hanging wall or foot wall) the blocks move laterally relative to one another
Strike slip faults are right lateral or left lateral depending on the relative movement of the blocks
Example: right lateral strike slip fault…. Looking at the rock from one rock.. it looks as if its moving right regardless

17
Q

What are folds?

A

A Ductile Deformation Feature: tend to warp, fold or crinkle; consider dip and strike patterns of strata exposed at the surface, we then can deduce their structure under the surface

18
Q

Describe the anatomy of a fold

A

simple symmetrical fold features:

  • an axial plane that divides the fold into mirror-image “limbs”
  • a fold axis that defines the direction of the crest of the fold. In a symmetrical fold, the axis is horizontal
19
Q

A symmetrical fold whose fold axis is tilted is said to….

A

“plunge”. As in “dip”, the plunge of a fold has a plunge angle (relative to the horizontal) and direction (compass direction)

20
Q

What are the main types of folds?

A

if relative ages of strata are known*, we can identify synclines and anticlines

21
Q

What is a syncline?

A

(a trough-like structure) strata dip TOWARD centre of fold with OLDEST strata in center

22
Q

What is an anticline?

A

(a arch-like structure) strata dip AWAY from centre of fold with YOUNGEST strata in centre

23
Q

What is a plunging fold?

A

When exposed in a horizontal erosion surface, arrowhead shaped patterns emerge
in syncline arrowhead pattern points AWAY from the direction of the plunge
in anticline arrowhead pattern points TOWARD the direction of the plunge

24
Q

What is a basin?

A

basins are bowl shaped with youngest strata in centre

25
Q

What is a dome?

A

domes are hump shaped with oldest strata in centre