Chapter 9 Flashcards

Deformation of Rocks

1
Q

Structural geology

A

Study of the deformation pf rocks (shape, volume, position, orientation)

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2
Q

Stress

A

Force per unit area. Compressional (convergent plate boundaries, shortening, folding), tensional (divergent plate boundaries, extension, faulting) or shear (transform plate boundaries)

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3
Q

Strain

A

Change in shape of a rock when stress is applied.

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4
Q

Elastic behavior

A

Material returns to its original shape when stress is removed. Occurs up to a maximum value of strain, called the elastic limit. (rocks = 0.001)

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5
Q

Plastic behavior

A

Material does not return to its original shape when stress is removed, behaves as a very viscous liquid.

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6
Q

Primary structures

A

Happen during rock formation (strata, cross bedding, ripple marks, mud-cracks, graded beds)

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7
Q

Secondary structures

A

Happen after rock is formed (folds, faults, fractures)

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8
Q

Differential stress

A

When the force is not the same in each direction

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9
Q

Brittle deformation

A

Elastic deformation followed by limited plastic deformation. Lower temperatures/pressures (near surface) and high strain rates (fast deformation). Crystalline igneous rocks more susceptible, forms joints and faults.

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10
Q

Ductile Deformation

A

Plastic strain at constant stress. Higher temperatures/pressures (deeper/close to magma) and low strain rates (slow deformation). Weaker and layered (sedimentary & metamorphic) rocks, forms folds.

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11
Q

Strike direction

A

Intersection of a horizontal plane with an inclined plane.

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12
Q

Dip angle

A

Maximum angle of an inclined plane.

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13
Q

Anticline fold

A

Concave downwards (arch)

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14
Q

Syncline fold

A

Concave upwards (saucer)

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15
Q

Axial plane

A

Axis of symmetry with limb on each side

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16
Q

Axis

A

Intersection of axial plane and a particular rock layer.

17
Q

Plunge

A

Difference in angle between horizontal and axis

18
Q

Folds

A

Geologic structure that is formed by layers or beds of rock being bent. Visible by outcrops or seismic reflection.

19
Q

Upright folds

A

Symmetric, vertical axial plane, limbs dip at same angle in opposite directions

20
Q

Inclined folds

A

Asymmetric, axial plane not vertical, limbs dip at different angles in opposite directions

21
Q

Overturned folds

A

Asymmetric, axial plane not vertical, limbs dip at different angles in same direction

22
Q

Joints

A

Fractures along which no displacement has occurred, occurs in igneous and sedimentary rocks

23
Q

Faults

A

Fractures along which displacement has occurred. Classified by strike, dip, slip.

24
Q

Dip-slip faults

A

Slip is parallel to dip. Hanging wall located above, footwall located below.

25
Normal fault
Formed by tension, hanging wall moves down relative to footwall
26
Reverse fault
Formed by compression, hanging wall moves up relative to footwall
27
Strike-slip fault
Slip is parallel to strike. Right lateral (formed by motion to right) and left lateral (formed by motion to left)
28
Structural traps
Formed by folding and faulting of rocks.
29
Stratigraphic traps
Formed by the sequence of deposition that placed an impermeable cap rock above a porous reservoir layer.
30
Thrust fault
Special case of a reverse fault, dip less than 45°.