Structural Geology Flashcards

1
Q

Structural Geology

A

Study of how rocks deform in response to stresses in the Earth

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2
Q

Types of Earth Stressors?

A

1.) Compression : contraction/shortening of rock or fossil (pushed together); common at convergent boundaries
2.)Normal Stresses: Act at right angles to a surface (Common at all 3 tectonic settings)
-small area=high stress
-large area= low stress
3.) Tension: elongation/stretching (pulled apart); common at divergent boundaries
4.) Shear

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3
Q

Tectonic Setting of Compression

A

Convergent Boundary

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4
Q

Tectonic Setting of Tension

A

Divergent Boundary

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5
Q

Tectonic Setting of Shear Stress

A

Transform, Divergent, Convergent

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6
Q

Brittle Deformation

A

Fracture of rock due to stress

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7
Q

Ductile Deformation

A

Bend and Flow of rock due to stress (w/out brittle fracture)
*Pliable not Brittle

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8
Q

Brittle-Ductile Transition
-> depth of deformation?
->Factors that determine how a rock Deforms?

A

-Rocks deform ductiley ~300-400 °C
-10-15km depth (ie; pressure)
-ductile-brittle transition is dependent on rock type
*Below brittle-ductile transition ; faults = shear zones due to no fracture in the rock
Factors:
1.)Temp/Pressure
2.) Deformation Rate:
-slow deformation=ductile
-fast deformation=brittle
3.) Rock Type

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9
Q

Brittle Faults Settings

A

1.) Normal
2.) Reverse
3.) Strike-Slip

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10
Q

Normal Faults

A

Hanging wall is down relative to footwall
occur @ Divergent Boundaries:
-continental expansion settings (ex: Nevada Basin and Range)
-Mid-Ocean Ridges

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11
Q

Reverse Faults

A

Hanging wall up, footwall down
@Convergent Boundaries
-subduction plate=footwall
-overriding plate=hanging wall
Low angle reverse faults=thrust faults

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12
Q

Strike-Slip

A

Vertical fault, lateral displacement
ex; San Andreas, Alpine Fault

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13
Q

Restraining Bend

A

Bend within strike-slip fault which causes compression across the straining bend
ex: Santa barbs and Mt. Denali

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14
Q

Ductile Fault Settings

A

Shear zones

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15
Q

Faulting

A

slip between two rocks along brittle fracture

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16
Q

Tilting

A

Rotations of rock layers due to stress

17
Q

Folding

A

Bending of rock layers due to stress

18
Q

Joint Formation

A

Brittle fractures with no displacement (naturally formed cracks in rock)

19
Q

Types of Folding (2)

A

1.) Anticline
2.) Syncline

20
Q

Anticline

A

Concave down

Type of folding

21
Q

Syncline

A

Concave up

22
Q

Deformation in Santa Barbara

A

Resistant band along the San Andreas Fault causes compression and uplifting wave-cut terraces and the Santa Ynez Mts.
-Folding under Santa Barbs