Folds Mechanics Theory and Practice
May be very complex
More common information
More common information
Folding Theories
Single-Layer Buckling
Basics of Folding Mechanics
“Buckles” in the Laboratory
But Pushing on Rock Layers Makes Folds
Strain Patterns
Bending Stress State
Pure Elastic Solution
Photo-Elastic Models
Rock Model Studies
Stress Pattern in Numerical Model of Flexure
Same Pattern in Numerical Models of Buckle Folds
Testing the Flexural Model
Another Model Design: Details
Examples of Specimen Data
Effects of Multiple Layers
Observed Fabrics
Multiple Beams Develop
Translations of Layers
Not Uniformly!
ex Strains Vary Along Layers
Multi-Layer Numerical Simulations
Some conclusions
5.90M
Category: geographygeography

Folds mechanics theory and practice

1. Folds Mechanics Theory and Practice

MSc REM Reservoir Structure ½ Module
Folds
Mechanics Theory and Practice
Sergei Parnachov
Gary Couples

2. May be very complex

MSc REM Reservoir Structure ½ Module
May be very complex
Complex fold map (top) and
explanation for Milton area, North
Carolina (Hatcher, 1996)
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3. More common information

MSc REM Reservoir Structure ½ Module
More common information
Моноклиналь в отеч.
терминологии
Twiss & Moores, 1992
Флексура в отеч.
терминологии
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4. More common information

MSc REM Reservoir Structure ½ Module
More common information
Different order folds on the molting glacier
Hatcher, 1996
Pumpelly’s rule: small-scale structure
generally mimic larger-scale structures
formed the same time
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5. Folding Theories

MSc REM Reservoir Structure ½ Module
Folding Theories
Buckling (продольный изгиб)
“week” matrix layer
“strong” layer
“week” matrix layer
Bending (поперечный изгиб)





Compactional drapes
Laccoliths
Fault-blocks
Salt domes
etc
d 2 t 3
1
2
were:
λd - dominant wavelength of the
“strong” layer,
t – thickness of “strong” layer,
μ1 – viscosity of the “strong” layer,
μ2 – viscosity of the supporting
matrix of “week” layers
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6. Single-Layer Buckling

MSc REM Reservoir Structure ½ Module
Single-Layer Buckling
Layer is surrounded by a “medium”
No deflections
s < scrit
s = scrit
Sudden deflection
scrit = f (thickness, ratio of stiffnesses)
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7. Basics of Folding Mechanics

MSc REM Reservoir Structure ½ Module
Basics of Folding Mechanics
Ortogonal Flexure
Passive-Shear
Folding
Flexural-Shear Folding
Volume-loss Folding: compressional
solution bends formation!! – кливаж
осевой поверхности
Twiss & Moores, 1992
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8. “Buckles” in the Laboratory

MSc REM Reservoir Structure ½ Module
“Buckles” in the Laboratory
Blue and green curves show that strain gages
are recording deflections from the beginning
of the experiment
These experiments
reveal that EVERY
plate tested begins to
deflect from the instant
that load is applied.
Yes, there is an
accelerated deflection
that occurs near peak
load.
But these results do
not support the notion
of buckling.
Experimental work by Mike Fahy, 1974-76
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9. But Pushing on Rock Layers Makes Folds

MSc REM Reservoir Structure ½ Module
But Pushing on Rock Layers Makes Folds
These rock-layer models
were deformed at confining
pressure as a consequence
of layer-parallel shortening.
The different fold shapes
are related to differences in
lithology and confining
pressure.
Layers originally 20 cm long (after Handin et al, 1972)
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10. Strain Patterns

MSc REM Reservoir Structure ½ Module
Strain Patterns
Simple conceptual models
derived from observations
of simple “free” beams, and
extrapolation to realistic
flexures
Unfortunately, these ideas
aren’t supported by
observations
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11. Bending Stress State

MSc REM Reservoir Structure ½ Module
Bending Stress State
Derived from multiple sources: elasticity, photo-elastic models,
physical models, outcrops, numerical simulations
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12. Pure Elastic Solution

MSc REM Reservoir Structure ½ Module
Map this
solution onto
finite flexure
Pure Elastic Solution
(after Hafner, 1951; Couples, 1977)
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13. Photo-Elastic Models

MSc REM Reservoir Structure ½ Module
Photo-Elastic Models
Gelatine balls: located in the
glass with a piston on the
top. Black bands visible in
polarized light, indicate σ1
axe trajectories
This image illustrates the
method – but it is not a fold!
Using a gelatin material, and
subjecting it to a
deformation (an elastic one,
even with high strains), we
determine stress directions
and magnitudes.
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14. Rock Model Studies

MSc REM Reservoir Structure ½ Module
Rock Model Studies
Crest of anticline in buckled single-layer of Leuders
Limestone
Note pattern of induced fractures (after Mel Friedman, ca. 1971)
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15. Stress Pattern in Numerical Model of Flexure

MSc REM Reservoir Structure ½ Module
Stress Pattern in Numerical Model of Flexure
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16. Same Pattern in Numerical Models of Buckle Folds

MSc REM Reservoir Structure ½ Module
Same Pattern in Numerical Models
of Buckle Folds
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17. Testing the Flexural Model

MSc REM Reservoir Structure ½ Module
Testing the Flexural Model
Experimental models
Numerical simulations
Field observations
Derive general prediction for fracture/ damage
distributions in flexural deformations (folding)
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18. Another Model Design: Details

MSc REM Reservoir Structure ½ Module
Another Model Design: Details
Machined steel blocks: perfect
circular arcs, lubricated
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19. Examples of Specimen Data

MSc REM Reservoir Structure ½ Module
Examples of
Specimen Data
Side jacket of lead, with scribed
grid that records displacement
during experiment
Model after epoxy impregnation
and cutting on rock saw
Inside of opposite lead side
jacket, showing that it was welded
to sample during deformation
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20. Effects of Multiple Layers

MSc REM Reservoir Structure ½ Module
Effects of Multiple Layers
As bedding-plane slip
activates, pre-existing fabric
elements are abandoned, and
new ones form
The new fabrics overprint
the old, and they indicate
bending within new multilayer packages defined by the
active slip surfaces
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21. Observed Fabrics

MSc REM Reservoir Structure ½ Module
Observed Fabrics
L=limestone,
D=dolostone,
P=lead
Flexural slip modifies the locations
and amounts of induced damage
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22. Multiple Beams Develop

MSc REM Reservoir Structure ½ Module
Multiple Beams Develop
Sheets of
lead
Stack of paper cards, lubricated
with graphite dust
Slip develops only on some
interfaces – as needed
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23. Translations of Layers

MSc REM Reservoir Structure ½ Module
Translations of Layers
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24. Not Uniformly!

MSc REM Reservoir Structure ½ Module
Not Uniformly!
Derived from distorted grids
The rock layers move away
from, and towards, the fold –
all by themselves!
Lateral movement is part of
the energy re-distribution
operating in flexures
(Don’t assume pin-lines for
balancing)
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25. ex Strains Vary Along Layers

MSc REM Reservoir Structure ½ Module
ex Strains Vary Along Layers
In these models, ex = evol
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26. Multi-Layer Numerical Simulations

MSc REM Reservoir Structure ½ Module
Multi-Layer Numerical Simulations
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27. Some conclusions

MSc REM Reservoir Structure ½ Module
Some conclusions
The more experimental works – the less
understandable the process (at least on this stage):
ALL MODELS ARE WRONG
Adding flexure sliding along buckled folds reduces
brittle deformation drastically
By opposite – fixing flexure (say by adding a dikes)
will lead to the increasing of fracturing
Volume-loss folds have a compressional solution
bands crossing the beds which may cause fluid
migration obstacle
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