23.vck_geometric classification of folds
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8/10/2019 23.VCK_Geometric Classification of Folds
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Fold-Folds may be defined as wavy structure formed when originally flat and
planar surfaces such as bedding, foliation or other originally planar surface in rocksare bent or curved as a result of deformation.
Folds range in size from mm to km.
Are a manifestation of ductile deformation.i.e., form at depth where T, P are high and fracturing does not occur
Fault related folds as well,
Differential compaction, intrusion etc
Can form in varieties of deformational environments ofEarthss crust from near surface brittle condition tolower crust ductile conditions
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Limb
Limb
Hinge points
Anatomy of Fold
Axial trace
Inflectionpoint
Fold Axis
Interlimb
angle
Amplitude
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Based on the orientation of various anatomical features of
the fold, geometrically it can be classified into the following
1)Based on the sense of curvature
2) Based on the plunge of Fold Axis
3) Based on the orientation of axial plane
4) Based on direction of younging relative to sense of fold
closure:
5) Based on symmetry of folds
6) Based on the nature of Axial plane and Hinge line.
7) Based on interlimb angle
8) Based on the shape of the hinge
9) Based on number of hinge
10) Based on the geometrical relations among neighbouring
structures:
11) Morphological Classification
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3) Based on the orientation of axial plane
Upright fold
Recumbent fold
Inclined fold
Reclined fold
Overturned fold
Fleuty (1964) further made the following
classification based on the amount of dip of
axial plane-
Upright fold: dip 800-900
Steeply inclined fold: dip 600-800
Moderately inclined fold: dip 300-600
Gently inclined fold: dip 100-300
Recumbent fold: dip 00-100
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Based on the dip of the Axial Plane vs Plunge of the Fold Axis (Fleuty 1964)
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4) Based on direction of younging relative to sense of fold closure:
Syncline
Anticline
AntiformalSyncline
SynformalAnticline
Anticlinoriuum andSynclinorium
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5) Based on symmetry of folds
Symmetric fold axial plane is the plane ofsymmetry .Symmetric folds are sometime describe as
M-Type folds (Ramsay 1967)
Asymmetric fold axial plane is not theplane of symmetry
Example- S and Z-Type folds (Ramsay 1967)
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6) Based on the nature of Axial plane and Hinge line.
Plane cylindrical- axial planeand hinge line both straight
(Type 0)
Plane non cylindrical- axial plane
straight but hinge line curved (Type I)
Non plane non cylindrical- axial
plane and hinge line both are
curved (Type II)
Non plane cylindrical- axial plane
curved but hinge line straight (Type III)
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7) Based on interlimb angle
Gentle fold- between 180 and 120
Open fold- between 120 and 70
Close fold- between 70 and 30
Tight fold- between 30 and > 0
Isoclinal fold-00
Elastica- Negative interlimb angle
Interlimb angles are measured on profile plane of folds
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Round-hinged fold
broad hinge zonecompared to limb
Chevron fold straight limbs and sharp
hinge
Arrow-head fold sharp hinge anddistinctly curved limbs
Cuspate fold A train of folds with sharphinges on one set of closure and withrounded hinges on the oppositedirectedclosure
8) Based on the shape of the hinge
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9) Based on number of hinge
Single-hinged fold- with singlehinge between two pointsof inflection
Conjugate fold A double hingedfold with sharp hinges
Box fold A double hinged foldwith more or less rounded hinges,
flat top and steeply dipping limbs
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10) Based on the geometrical relations among neighbouring structures:
Periodic folds -A train of folds with more or less
the same geometry between alternate points ofinflection.
Non-periodic folds - Not periodic in nature.
Polyclinal folds A group of folds with non-parallel axial planes but with sub-parallelhinge lines
Disharmonic folds A group of folds in
which the folds of one layer differ in size orstyle from folds of an overlying or underlyinglayer.
Decollement A train of folds in a layerwhich becomes detached from the adjacent
layer.
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Morphological Classification of Ramsay-1967:
Dip Isogon:line of equal dip
Based on
Thickness
a. Orthogonal thickness (t)-measuredbetween tangents on limb
b. Thickness parallel to the axial trace ofthe fold (T)
t= T
cos
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Ramsay classification scheme for folds
Class
Comparison of
Curvature of
inner arc &
outer arc
Dip isogon geometry
(towards inner arc)
1 Cinner> Couter Dip isogons converge
1A Strongly Convergent
1BConvergent
(Parallel folds)
1C Slightly Convergent
2 Cinner= CouterDip isogons are parallel:
(similar folds)
3 Cinner< Couter Dip isogons diverge
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