Lecture 13 // Crustal Deformation - Folds Flashcards

1
Q

Strike

A

A line made by the intersection of the inclined surface with the horizontal Earth’s surface.

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2
Q

Dip

A

The direction of incline (from the Earth’s surface downwards) plus the dip angle (angle between the inclined bed and the Earth’s surface).

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3
Q

Geologic map symbols

A

(including strike and dip) Are used on geologic maps to indicate the orientation beneath the Earth’s surface of layers (strata), planar features (such as faults), and folds.

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4
Q

Folds

A

Form from ductile deformation, typically at great depth under compressional stress.

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5
Q

Hinge

A

The tightest part of the fold.

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6
Q

Axial plane

A

An imaginary plane that runs through the hinge of the fold.

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7
Q

Axis

A

The imaginary line on the Earth’s surface made by the axial plane.

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8
Q

Limbs

A

The sides (‘arms’) of a fold.

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9
Q

symmetrical anticlines and symmetrical synclines

A
  • Upturned parts of folded rock.

- Downturned parts of folded rock.

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10
Q

monoclines

A

A slight bend in parallel layers of rock.

Monoclines commonly form due to reactivation of old buried faults.

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11
Q

asymmetrical anticlines and synclines

A

Axial plane is not vertical, thus dip angles differ (limbs are not symmetrical) as do the width of beds on the surface.

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12
Q

overturned anticlines and synclines

A

Axial plane is even more off vertical and limbs now point in the same direction (one limb is completely overturned).

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13
Q

recumbent folds

A

These are folds so compressed that anticlines and synclines become stacked upon each other.

The axial plane and limbs are
horizontal or near horizontal.

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14
Q

plunging anticlines and synclines

A

When plunging anticlines & synclines are uplifted and eroded, a V pattern is revealed on the Earth’s surface.

Rule of V for uplifted & eroded plunging folds:

  • Vs point in the same direction as tilt for plunging anticlines.
  • Vs point in the opposite direction as tilt for plunging synclines.
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15
Q

domes and basins

A

Rock is deformed upwards (domes) or downwards (basins) in all directions. Uplifted and eroded domes and basins show circular patterns.
Domes: The oldest rock is at the centre of an eroded dome.
Basins: The youngest rock is at the centre of an eroded basin.

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