Term 1 - Fold mechanisms + Analysis of fold geometries Flashcards

1
Q

3 basic configurations by which external forces can act on layers (such as bedding) to cause folding

A

Not mutually exclusive – can get “mixed” boundary conditions, or boundary conditions that change during progressive strain
Active vs passive mechanisms

Layer-parallel compression: Force applied parallel to bedding
Bending: Force applied across bedding
Shearing: Force applied oblique to bedding
- Called “passive folding” if the strength of the layer does not influence fold development

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2
Q

Layer-parallel compression and competence

A

Force applied to each side of bedding resulting in either
o Homogeneous shortening
o Folding

  • “Competence” is a qualitative description of rock strength
  • In this case, “competence” is equivalent to viscosity [μ, a measure of the dependence of stress on strain rate: ‘ease of flow’]
  • Competence of the layer relative to that of the matrix is a key factor

Low competence = shortening
High competence = folding

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3
Q

Role of layer thickness during buckling

A
  • Folds in thick layers have greater wavelengths (λ) than folds in thin layers
  • Where the competent layers are far apart, the layers will fold independently of each other
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4
Q

Shear (flow) folding:

A
  • Commonly observed in shear zones
  • Form by progressive simple shear of initial irregularity
  • Shear folds cannot be used to estimate shortening
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5
Q

Strain within buckle folds:

A
  • Ideal buckle folding produces folds with constant layer thickness
  • Tangential longitudinal strain: outer arc extension; inner arc compression separated by a neutral surface
  • Bent eraser analogy
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6
Q

Flexural slip folding in multilayers:

A
  • Ideal flexural slip folding produces folds with constant layer thickness
  • Slip is maximum on the fold limbs; zero at the hinge
  • Phone book analogy
  • Favoured by thin beds separated by weak layers (e.g. shale)
  • Slickenlines preserved on bedding planes in fold limbs
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7
Q

Flexural flow folding

A
  • Ideal flexural flow folding produces folds with constant layer thickness
  • Occurs during deformation at high temperatures, or when incompetent layer is “sandwiched” between competent beds
  • Layer-parallel simple shear decreases towards the hinges (last slide
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8
Q

Contours on stereonets

A
  • Data can be contoured to highlight preferred orientations

* Contours are typically labelled as % of data per 1% area of the stereonet

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