Week 5- DYNAMIC PLANET: Structural Geology and Vertical Crustal Movements Flashcards

1
Q

what is structural geology?

A

the study of the deformation in the lithosphere generated by stresses

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2
Q

why are rocks stressed?

A
  1. Load pressure (lithostatic stress/confining stress)

-results from the weight of overlying rock
-stress acts uniformly in EVERY direction
-analogous to the hydrostatic pressure beneath a head of water

  1. Deviatoric stress (differential/triaxial)

-stresses do not act uniformly on the rock
-caused y lateral transmission of horizontal tectonic forces through the solid Earth’s crust (contraction or extension)
-in 3D world will ALWAYS be 3 principal, perpendicular stresses acting on an object
-the maximum principal stress
-the intermediate principal stress
-the minimum principal stress
=TRIAXIAL STATE OF STRESS

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3
Q

What categories do faults fall into? How are they classified?

A
  1. Normal
  2. reverse/ “thrust”
  3. strike-slip

According to the orientation of principal stresses in the triaxial state (Anderson’s classification of tectonic stress)
-aka based on the direction of slip

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3
Q

What are faults?

A

Fault are fracture surfaces, along which displacement has taken place.

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4
Q

What are dip slip faults?

A

where movement has occurred along a dipping surface, and the two blocks have moved with a vertical component relative to the surface of the earth

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5
Q

What are the characteristics of normal faults?

A

-hanging wall is downthrown
-Steep (~60 degrees from horizontal)
-when б1 is vertical, б2 and б3 are horizontal (extension)
-fault surface dips parallell to б3
-Thins the crust

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6
Q

What are characteristics of thrust/reverse fault?

A

-Hangingwall is upthrown
-Low angle (~30o from horizontal_
-when б3 is vertical, б2 and б1 are horizontal (compression)
-fault surface dips parallel to б1
-Thickens crust
-thrusts occurring in contractional zones often occur with folds= “fold thrust belts”

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7
Q

What are characteristic of strike-slip faults?

A

Movement has occurred along a largely vertical surface, and the two blocks have moved with a horizontal component relative to the surface of the earth
-No hangingwall-footwall
-Vertical fault
-when б2 is vertical, б1 and б3 are horizontal (shearing)
-No net change in crustal thickness

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8
Q

What are folds? What are they caused by? How are they classified?

A

The majority of folding is caused by buckling: compression resulting in plastic deformation and shortening.
-Compression zones include continental-continental
collisions (orogens).

Classified:
1. according to the orientation of axial plane (=the plane that exactly bisects the interlimb angle)
2.the tightness of the fold (= the interlimb angle)
The classification works at all scales

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