Term 1 - Fold mechanisms + Analysis of fold geometries Flashcards
3 basic configurations by which external forces can act on layers (such as bedding) to cause folding
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
Layer-parallel compression and competence
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
Role of layer thickness during buckling
- 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
Shear (flow) folding:
- Commonly observed in shear zones
- Form by progressive simple shear of initial irregularity
- Shear folds cannot be used to estimate shortening
Strain within buckle folds:
- 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
Flexural slip folding in multilayers:
- 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
Flexural flow folding
- 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
Contours on stereonets
- Data can be contoured to highlight preferred orientations
* Contours are typically labelled as % of data per 1% area of the stereonet