Four common folds classification
limbs dip down and away from the hinge zone
convex Upward
Antiform
hínge Zone is at the botom (outlining a valley):
convex downward.
Synform
large (megascopic, regional-scale) of antifom and synforms
Anticlinorium and synclinorium
The rocks in the core of the fold are the ______
youngest
rock layers get
younger away from
the core BUT has the
shape of a synform.
Synformal anticline
rock layers get
younger towards the
core BUT has the
shape of an antiform.
Antiformal anticline
the enveloping surface and axial Surface are perpendicular to each other.
Symmetric folds
the enveloping
surface and axial
surface are NOT
perpendicular to
each other.
Asymmetric folds
Large folds commonly have
smaller-scale folds in their
limbs and crest. They are
USUally referred to as higher
order (2nd, 3rd order etc.)
parasitic folds.
They form during flexure of
layered rock where slip
OCCUrs between rock layers
flexural slip
The difference
between S- and Z-folds
lies in their sense of
rotation or _______
vergence
Vergence of parasitic
folds is _____
towards the
hinge line
Clockwise
Z-folds
Anticlockwise
S-folds
fold structures with only one tilted limb; the beds on either side of the tilted limb are horizontal.
Monoclinal fold/ monoclines
fold structures wherein the layers dip uniformly in a single direction having the same general inclination.
Homoclinal fold/ homoclines
folds can be describes by:
Dip of axial surface: Upright
70°-90°
Dip of axial surface: Inclined
10°-70°
Dip of axial surface: Recumbent
0°-10°
angle enclosed by its
two limbs.
Interlimb angle
Fold geometry can be classified by means of
dip isogons.
5 Folding Mechanisms
Active folding or buckling
passive folding
bending
flexural folding
kinking and chevron folding