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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    Thank You