Folds Flashcards

1
Q

Fold with beds that young away from the core

A

Anticline

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2
Q

Surface fold where there is no strain

A

Neutral-surface fold

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3
Q

Large scale antiform formed from smaller scale antiform and synform

A

Anticlinorium

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4
Q

Fold with the hinge zone at the top

A

Antiform

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5
Q

Fold that doesn’t have their axial surfaces approximately perpendicular (± 10 degrees) to the enveloping surface

A

Asymmetric fold

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6
Q

Box-shaped fold detached from the underlying and overlying layers

A

Box fold

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7
Q

Large-scale fold with straight limbs and sharp hinges

A

Chevron fold

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8
Q

Structures with hinge lines that laterally change curvature (< 50 degrees)

A

Doubly plunging fold

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9
Q

Fold produced near fault surfaces that appear to be pulled into a fault during movement

A

Drag fold

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10
Q

Fold that forms when a normal fault breaks and displaces between rocks but die upward into the sedimentary cover

A

Drape fold

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11
Q

Gradually opening fold is replaced by a neighboring, gradually tightening fold of opposite form

A

En echelon fold

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12
Q

Thrust sheet wherein dip flattens as it passes over a ramp

A

Fault-bend fold

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13
Q

Accommodation structures above the frontal top of a thrust

A

Fault propagation fold

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14
Q

Fold that forms from slip between layers

A

Flexural slip fold

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15
Q

Fold with 120 - 180 degrees interlimb angle

A

Gentle fold

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16
Q

Fold that plunges nearly to entirely horizontal (0 - 10 degrees)

A

Horizontal fold

17
Q

Fold with 60 - 120 degrees interlimb angle

A

Open fold

18
Q

Asymmetric fold in which one limb has been tilted beyond the vertical

A

Overturned fold

19
Q

Fold with dip isogons perpendicular to the bedding throughout the fold

A

Parallel fold

20
Q

Smaller fold related to a large structure

A

Parasitic fold

21
Q

Irregular and isolated fold structures that typically occurs as a tightly folded vein or thin later of strongly contrasting lithology

A

Ptygmatic fold

22
Q

A steeply plunging, inclined fold

A

Reclined fold

23
Q

Fold with a horizontal (0 to 10 degrees) axial surface and horizontal hinge line

A

Recumbent fold

24
Q

Fold plunging at 10 - 30 degrees

A

Shallow Fold

25
Q

Fold with a hinge line showing extreme curvature, to the extent that the hinge line curvature approaches parallelism ( change in plunge up to 180 degrees)

A

Sheath fold

26
Q

Fold with dip isogons parallel to each other

A

Similar fold

27
Q

Fold steeply (60 to 80 degrees) punging

A

Steep fold

28
Q

Fold that has their axial surfaces approximately perpendicular (± 10 degrees) to the enveloping surface

A

Symmetric fold

29
Q

Fold with beds that young toward the core

A

Syncline

30
Q

Large-scale synform formed from smaller-scale antiform and synform

A

Synclinorium

31
Q

Fold with an inclined (10 - 70 degrees) axial surface

A

Inclined fold

32
Q

Fold plunging at 30 - 60 degrees

A

Intermediate fold

33
Q

Fold with 0 - 10 degrees limb angle or beds on both limbs are nearly parallel whether upright, overturned or recumbent

A

Isoclinal fold

34
Q

Small fold (less than a meter) characterized by straight limbs and sharp hinges

A

Kink fold

35
Q

Fold structure with only one tilted limb, with one limb being horizontal

A

Monocline

36
Q

Fold with hinge zone at the bottom

A

Synform

37
Q

Fold with 10 - 60 degrees interlimb angle

A

Tight fold

38
Q

Fold with an axial surface nearly to entirely dipping upright (70-90 degrees)

A

Upright fold

39
Q

Fold vertically (80-90 degrees) plunging

A

Vertical fold