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
Q

Normal fault

A

Formed by tension, hanging wall moves down relative to footwall

26
Q

Reverse fault

A

Formed by compression, hanging wall moves up relative to footwall

27
Q

Strike-slip fault

A

Slip is parallel to strike.
Right lateral (formed by motion to right) and left lateral (formed by motion to left)

28
Q

Structural traps

A

Formed by folding and faulting of rocks.

29
Q

Stratigraphic traps

A

Formed by the sequence of deposition that placed an impermeable cap rock above a porous reservoir layer.

30
Q

Thrust fault

A

Special case of a reverse fault, dip less than 45°.