Fold classification Flashcards

(38 cards)

1
Q

Four common folds classification

A
  1. Sense of curvature
  2. Symmetry and vergence
  3. Dip of axial surface and plunge of hinge line
  4. Interlimb angle
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2
Q

limbs dip down and away from the hinge zone

convex Upward

A

Antiform

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3
Q

hínge Zone is at the botom (outlining a valley):

convex downward.

A

Synform

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4
Q

large (megascopic, regional-scale) of antifom and synforms

A

Anticlinorium and synclinorium

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5
Q

The rocks in the core of the fold are the ______

A

youngest

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6
Q

rock layers get
younger away from
the core BUT has the
shape of a synform.

A

Synformal anticline

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7
Q

rock layers get
younger towards the
core BUT has the
shape of an antiform.

A

Antiformal anticline

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8
Q

the enveloping surface and axial Surface are perpendicular to each other.

A

Symmetric folds

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9
Q

the enveloping
surface and axial
surface are NOT
perpendicular to
each other.

A

Asymmetric folds

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10
Q

Large folds commonly have
smaller-scale folds in their
limbs and crest. They are
USUally referred to as higher
order (2nd, 3rd order etc.)

A

parasitic folds.

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11
Q

They form during flexure of
layered rock where slip
OCCUrs between rock layers

A

flexural slip

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12
Q

The difference
between S- and Z-folds
lies in their sense of
rotation or _______

A

vergence

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13
Q

Vergence of parasitic
folds is _____

A

towards the
hinge line

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14
Q

Clockwise

A

Z-folds

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15
Q

Anticlockwise

A

S-folds

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16
Q

fold structures with only one tilted limb; the beds on either side of the tilted limb are horizontal.

A

Monoclinal fold/ monoclines

17
Q

fold structures wherein the layers dip uniformly in a single direction having the same general inclination.

A

Homoclinal fold/ homoclines

18
Q

folds can be describes by:

A
  1. Dip of axial surface
  2. Plunge of hinge line
19
Q

Dip of axial surface: Upright

20
Q

Dip of axial surface: Inclined

21
Q

Dip of axial surface: Recumbent

22
Q

angle enclosed by its
two limbs.

A

Interlimb angle

23
Q

Fold geometry can be classified by means of

24
Q

5 Folding Mechanisms

A

Active folding or buckling
passive folding
bending
flexural folding
kinking and chevron folding

25
Based on dip isogons, folds coan be classified into the three main types.
Class 1: Dip isogons converge toward the inner arc, which is tighter than the outer arc. Class 2: Similar folds, also called shear folds. Class 3: Dio isogons diverge toward the inner arc, which is more open than the outer arc.
26
Class 1
1A 1B 1C
27
Class 2
thinned limbs and thickened hinges.
28
Class 3
even thinner limbs and thickened hinges.
29
How do folds form?
Considerations: 1. The way stress act ona layered rock. 2. How layer(s) react to stress. 3. we will know if rocks fold Actively or passively.
30
Fold mechanisms that can initiate when a layer is shortened parallel to the layering.
Active folding or Buckling
31
_______ is typical for rocks where passive flow occurs, i.e. where the layering exerts no mechanical influence on the folding.
Passive folding
32
Passive folds are frequently found in
shear zone
33
this occurs when forces act **across layers** at a high angle (unlike buckling where the main force acts parallel to a layer.)
Bending
34
________ maintains bed thickness.
Flexural folding
35
In cases where strain is more evenly distributed in thelimbs in the form of shear strain, flexural slip turns into the closely related mechanism called
flexural shear or flexural flow.
36
Kink folds & Chevron folds
straight limbs and sharp hinges. formed by displacements between individual laminae. sharp & angular folds.
37
well-rounded hinges.
Concentric folds
38
box-shaped; wide flat top and steep flanks. formed when a layer is detached from the underlying and overlying layers.
Box folds