Structural Geology Flashcards

1
Q

Definition of Structural Geology

A

The observation of deformed rocks, and the explanation for how [the process(es)] and why [cause(s)] they ended up in their present state

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is the important of structural geology?

A

Crucial for the exploration, mapping and exploitation of a wide range of Earth materials/resources

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Materials/Resources that structural geology helps exploits

A

Building stones, ores, groundwater, oil and gas

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What are the two types of geologic structure which can be described and measured?

A

Planar and Linear

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Examples of Planar structures

A

Bedding plane, Cleavage plane, Fault Plane etc.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Examples of Linear structures

A

Fold Hinge Line, Stretching lineation, Worm tube etc

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

How does increasing the metamorphic grade effect foliations?

A

Change, with increasing coarsisity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What is the order of foliation with increasing metamorphic grade?

A

Slaty cleavage, Schistosity, Gneissic foliation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

How does compositional variation effect bedding plane?

A

Changes bedding plan visibility

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What are lineations?

A

A set of lines produced by deformation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

What four types of lineations?

A

Crenulation, Stretching, Mineral, Intersection

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is stretching lineation?

A

the long axes of stretched grains e.g. quartz

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

What is mineral lineation?

A

long axes of aligned metamorphic minerals which grew in a set orientation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

How are folds created?

A

Compressive forces in earth’s crust

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Name anatomy of a fold

A

Limbs, hing zone/fold axis, hinge points, axial trace, profile plane, inflection points, antiform/synform, anticline/syncline, symmetric/asymmetric, plunge, upright/inclined/recumbent

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

What are the three main features needed to define geometry of planar structure?

A

Strike, Dip angle, Dip direction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

Definition of Strike

A

orientation of horizontal line

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

Definition of Dip angle

A

angle of inclination, which is perpendicular to strike

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

An example of strike, dip angle & direction as seen in fieldwork

A

090/45 S

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

What is intersection lineation?

A

lines formed by the intersection of two planes e.g. bedding/cleavage

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
21
Q

What are bedding-cleavage intersections like at a single deformation event?

A

parallel to fold axis

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
22
Q

What are the two main features required to define geometry of linear structure?

A

plunge and plunge direction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
23
Q

What is the difference between plunge and plunge direction?

A

Plunge is angle of inclination relative to the horizontal while plunge direction is the compass direction

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
24
Q

What are stereonets used for?

A

Understanding slope stability

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
25
Q

What can poles be used to study?

A

plate/tectonic processes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
26
Q

What are the two structures plotted on a stereonet?

A

plane and line

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
27
Q

TRUE or FALSE: Pitch is the angle between strike and lineation

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
28
Q

What is used to further analyse the relationship between planar surfaces?

A

Pole to the plane

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
29
Q

What is ‘Pole to the plane’?

A

the projection of a line drawn normal (perpendicular) to the surface of a plane

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
30
Q

What are terms used to describe folds observed in the field?

A

Fold hinge, Axial - planar cleavage, intersections of cleavage planes on folded bedding plane

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
31
Q

What are terms used to describe folds determined using a stereonet?

A

Fold axial plane, fold axis, fold profile plane

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
32
Q

What can be determined of intersecting planes using a stereonet?

A

The plunge/plunge direction of intersection and angle between planar beds

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
33
Q

What allows you to measure fold axis without the seeing it?

A

bedding and cleavage planes, as they are parallel to the fold axis

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
34
Q

What can you do if you don’t have cleavage measurements when determining fold axis?

A

just using bedding data on a stereonet

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
35
Q

What can you determine through plotting of bedding data alone?

A

Strike, dip and dip direction of profile plane.
Plunge and plunge direction of fold hinge.
Cylindrical nature of the fold.
Inter-limb angle of the fold.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
36
Q

What are uses of poles and planes?

A

observation of mineral alignment and determination of cause

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
37
Q

What are potential causes of mineral alignment determined through poles and planes?

A

tectonic activity after magma cools evidenced by quartz infill in biotie.

fabric broadly already parallel to rim of a pluton and some parallel to a fault.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
37
Q

What does stereonets help with?

A

processing large quantities of data e.g. reconstructing kinematics of mountain forming

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
38
Q

Why are sterenoets used to model folds?

A

They are less susceptible to human error

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
39
Q

Define pi-plot/girdle

A

Plotting bedding from the fold as poles

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
40
Q

What are poles for cylindrical expressed as?

A

constant orientation of the hinge line which defines a single great circle

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
41
Q

Define cylindrical fold

A

Fold profile constructed without ambiguity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
42
Q

Define ambiguity of fold profile

A

lack of error when plotting line of best fit on stereoplot

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
43
Q

when is a fold classified as non-cylindrical?

A

If a best fit line great circle cannot be drawn

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
43
Q

What can be inferred from the interlimb angle?

A

the degree of shortening a fold has experienced

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
44
Q

What can be used to determine the inter limb angle?

A

Maths or a stereonet

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
45
Q

TRUE or FALSE: There are techincal names for degree range of inter limb angle

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
46
Q

give examples of techincal terms for inter limb angles

A

great: 180 -120
open: 120 - 70
close: 70 - 30
tight: 30 - 0
isoclinal: 0
elastica: negative values

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
47
Q

What are inflections points?

A

Where the angle of bed inclination changes

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
48
Q

How do you measure the inter-limb angle?

A

Examine the shape of the fold along the fold profile

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
49
Q

Method for inter-limb angle measuring?

A

Poles method

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
50
Q

TRUE or FALSE: there are techincal classifications for plunging ranges

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
51
Q

What causes failure of a rock face?

A

the orientation of the cracks

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
52
Q

What does folding involve?

A

low composition contrast between successive layers and/or shear or folding at high temps

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
53
Q

What does fold/shear at high temps allow?

A

Plasticity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
54
Q

Define fold bluntness

A

describes the shape of the fold hinge

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
55
Q

What is fold classification based on?

A

orientation of hinge line and axial surface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
56
Q

What is needed to describe fold orientation?

A

inclination and plunging of fold

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
57
Q

What is used to describe fold geometry?

A

symmetry, interlimb angle, orinetation of axial surface and hinge line, consistency, aspect ratio and bluntness

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
58
Q

Examples of terms for fold tightness

A

Gentle, open, close, tight, isoclinal, fan, involute

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
59
Q

What folds are obtuse?

A

Fan and involute

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
60
Q

Examples of fold aspect ratio terms

A

Wide, broad, equant, tall, elongate

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
61
Q

examples of fold bluntness terms

A

Chevron, sharp, angular, subangular, subrounded, circular fold, blunt

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
62
Q

Examples of fold classification terms

A

Vertical, upright plunging, upright horizontal, inclined plunging, inclined horizontal, reclined, recumbent

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
63
Q

What are Dip Isogons?

A

these compare fold styles of the two surfaces of the layer

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
64
Q

What is the origin of Dip Isogons?

A

Ramsey’s classification (1967)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
65
Q

TRUE or FALSE: Materials of different competency don’t behave differently when folded

A

FALSE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
66
Q

How do you find the class via dip isogons?

A

Draw lines between tanferental points

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
67
Q

What are the classes of folds?

A

Class 1A
Class 1B Parallel
Class 1C
Class 1C Similar
Class 3

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
68
Q

TRUE or FALSE: There is a relationship between stress, rheology and fold mechanisms

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
69
Q

What are the types of folding?

A

Active folding; buckling, bending.
Passive folding

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
70
Q

Define Passive folding

A

Folded layers have no little or no rheological influnence as there is no competence between folding laters and host rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
71
Q

Define competence

A

Viscosity contrast between successive layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
72
Q

Define Active buckling folding

A

Competence between folding layers and host rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
73
Q

Define bending folding

A

Forces applied across the layer at a high angle, may or may not be competence contrast

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
74
Q

In passive folding where does deformation take place?

A

Grain scale in a mechanically isotropic rock

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
75
Q

What do layers serve as in passive folding?

A

Geometrical strain marker only

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
76
Q

Where is passive folding found?

A

Mylonite zones, paraticitically in monomineralic

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
77
Q

Example of passive folding

A

Moine rocks in the highlands

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
78
Q

Where does active bending folding occur?

A

Between boudins
Above thrust ramps
Above reactivated faults
In host igneous/salt instructions

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
79
Q

Where does deformation take place for active buckling folding?

A

at the layer scale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
80
Q

What affects the deformation pattern of active buckling folding?

A

strength of layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
81
Q

What is buckling folding?

A

Compressive stress parallel to layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
82
Q

Where does buckling folding occur?

A

Parallel to orogeny

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
83
Q

Where does buckling instability develop?

A

sites of irregularity on the layer interface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
84
Q

TRUE or FALSE: relative viscosity of layers of rock involved control folding

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
85
Q

Define vicsoity

A

the ability of a material to resist flowing

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
86
Q

What does no mechanical contrast between layers generate?

A

Only thickening of material, no folding

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
87
Q

What does mechainal contrast between layers generate?

A

creates folds, which vary in ar length as a function of thickness of layer

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
88
Q

TRUE or FALSE: the thicker the strongest layer the broader the wavelength of the fold

A

TRUE

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
89
Q

TRUE or FALSE: Thickness of layers control wavelength (where competency contrast exists)

90
Q

What is the mathematical expression of the relationship between wavelength and layer thickness?

A

Biot-Ramberg equation

91
Q

What are the asumptions of the Biot-Ramberg model?

A

No volume loss, isn’trelaistic

92
Q

What can create volume loss in the feild that constrats the bio-ramberg model?

A

Compression reducing pore space, can cause ~30 - 40% volume loss

93
Q

What does mechanical or thickness contrast between successive layers causes?

A

Change in fold geometry

94
Q

What does high viscosity and thickness of layers create

A

Large wavelengths (km scale)

95
Q

What forms when a layer has a lower viscosity than the matrix?

A

Mullion structures

96
Q

What are mullion strcutures

A

High viscoity material makes bulbous folds and the lower viscoity mater is pushed into the cusp

97
Q

What controls the wavelength of bigs folds when there are multi-layers?

A

The thicker layers

98
Q

What do the thing layers in a multilayer fold create?

A

Parasitic folds

99
Q

What forms when folding multilayers which have scpaed apar competent layers?

A

Disharmonic folds

100
Q

What is the distint features of disharmonic folds?

A

The axial surfaces is discontinues with dissimilar fold axial plan and amplitude

101
Q

What trumps layer thickness in fold control?

102
Q

Where do parasitic fold form?

A

The back of larger folds

103
Q

What is fomred is multilayers scpaed togther are close?

A

they behave as a single layer and form harmonic folds

104
Q

Define Pumpelly’s Rule

A

the fold axes and aial surfaces of minor folds of an area are congrugent of the major fold structures of the same phase of deformation

105
Q

What is the orientation of the small fold structures representative off?

A

The orientation of regional structures

106
Q

What does the horizon with lower and high visocity do when stres is imparted?

A

lower; compresses
higher; folds

107
Q

Define fold envelope

A

Macroscale fold geology defined by connecting all the crests of the parasitic folds

108
Q

Define Vergence

A

the rotation of axial surface from a symmetrical fold into a asymmetrical fold without changing orientation of enveloping surface

109
Q

Define Fold vergence

A

Sense of shear towards a geographic direction

110
Q

How are asymmetrical folds formed?

A

Symmetrical folds are bent and distorted by larger scale fold envelope

111
Q

What are fold vergence types indicators of?

A

area of a fold

112
Q

Define S wave

A

Long limb and short limb with a asymmetrical fold and is verging

113
Q

TRUE or FALSE: Fold vergence is on all scales and is formed by competent constraints between successive layers

114
Q

What can vergence be applied to?

A

parasitic folds and asymmetrical folds in shears zones

115
Q

What can fold vergence be determined by?

A

cleavage-bedding structure

116
Q

What can be used to how if a folded is refolded or a disharmonic fold?

A

Stereonets and map patterns

117
Q

Define faults

A

fractures along which there is a visible offset (physical discontiniuty) by shear displacemnt parapllel to the fracture surface

118
Q

What are faults denominated by?

A

brittle deformation mechanisms

119
Q

what is the scale of displacement for faults?

A

shear fracture (micro-fault) cm’s or less

120
Q

name the two main features of faults

A

hanging wall and footwall

121
Q

Define Net slip

A

Total amount of displacement

122
Q

Define heave

A

The anount of hoziontal displace ment

123
Q

Define throw

A

the amount of vertical displacemnt

124
Q

What do faults represent?

A

Physical discontinuty and discontinuty in velocity feild

125
Q

what is limited concenous regarding plate-boundary fault zones?

A

the width and structure below seismigenic layer

126
Q

What is the fault zone widths in the lower crust?

A

<10 - 10’s km

127
Q

What is the fault zone widths in the lithospheric mantle?

A

<100 - 100’s km

128
Q

TRUE or FALSE: faults aren’t continuous planar surfaces and the magnitude of displacement across the fault plane isn;t consant

129
Q

Are these terms for faults areas?

Maximum displacement zone
Tip Point
Tip Line

130
Q

What decreases from the maximum displacement zone to tip point?

A

decreasing displacement

131
Q

What rule does the Anderson model explain?

A

fault propagation

132
Q

What do faults do?

A

Particular orientation and well-defined angles

133
Q

What are the assumptions of the anderson model?

A
  1. Earth is a prinipal plane with a principal stress direction perpendicular to gravity
  2. two sets of shear planes (conjugate faults) develop at ~25-30o to O1
  3. If O1 =/= O2 =/= O3, there are three possible configurations for the prinipal stresses (min, mas and intermediate) relative to the earths surface
134
Q

Are normal dip-slip faults more steep than thrust dip-slip faults?

135
Q

Which faults are generally low angle?

136
Q

What do anderson’s rule form the basis of?

A

The basis of structural analysis of faults

137
Q

What does anderson’s rules not explain?

A

all possible fault types

138
Q

Examples of faults outwith the anderson model

A

When O1 is vertical, its assumed normal fault will drip 60 -65o ut <60o faults do form

When O3 is vertical its assumed thrust fault will dip 25-30o but >35o faults form

139
Q

What are the explanations for reverse faults and low angle normal faults?

A

Reactivation, stress-trajectories and listric faults

140
Q

What is the exaplation for reactivation?

A

reverse faults are reactered normal faults
(compression fafter extension)

low angle normal faults are reactiveated thrust faults
(extension after compression)

141
Q

Define stress -trajectories

A

Fault angles reprentthe curvature of stress strajectores with depth in the arths crust

142
Q

What is an issue with the anderson model and stress trajectories?

A

some faults from at depth where elevated T & P plus changing differential stress exists so the application of the simiplifed anderson model doesn’t work

143
Q

If the crust was homogenous what would the stress trajectories be?

A

Planar at all levels in rock body

144
Q

As the crust is hertorgenous what will the orinetation of stress trajectores do?

145
Q

What assumption can be made about cauving stress jacterotes and faults?

A

If prinipal stress directions vary in orinetaion then the angle of faults relative to the earth’s surface will not conform to predictions made by anderson model

146
Q

What is listric fault?

A

A fault surface which is concave upwards with dip that decreases with depth

147
Q

Where are litric faults common?

A

extened (strecthed) crust

148
Q

What could explain listric faults?

A

variation in the stress trajectories caused by heterogenous rock

149
Q

Define strain envelope

A

area around fault where strain is concentrated

150
Q

Where is the area of lowest stress in a fault?

A

The area of max strain

151
Q

What does the fault tip do as stress is released in low stress areas

A

Bend towards each other

152
Q

What happens to a ramp when the rocks have compressive stress?

A

Becomes the damage zone

153
Q

What is fault geometry dependent on?

A

Host rock structural and rheological hemogeneity

154
Q

What are the three types of faults joining?

A

uniform, basement and variation

155
Q

What is a uniform fault?

A

Uniform extension generating a population of incipient faults of which some grow, interact and link up to longer faults

156
Q

What is a basement fault?

A

Basement controlled extension generating an achelon faults in the cover that link up to a non-planar large fault

157
Q

What is a variation fault?

A

Variation of basement controlled extension where the preexisting fault is inclined with respect to the extension direction

158
Q

What happens to the ramp as the fault tips propagate?

A

It twists as the relay lengthens

159
Q

What is ramp length on average?

A

3 - 3.5x the width

160
Q

What does rock flour do?

A

Act as seal against fluid movement

161
Q

What is a fabric?

A

minerals and mineral aggregates with a preferred orientation that penetrate the rock at the microscopic to cm spacing scale

162
Q

What is a Primary Fabric?

A

Fabric formed during sedimentary deposition or igneous crystallisation

163
Q

What fabric does igneous crystallisation create?

A

A random crystalline fabric

164
Q

What are secondary fabrics?

A

Fabrics are well developed in strongly deformed rocks e.g. metamorphic rocks

165
Q

What is Tectonite?

A

Rocks with fabric that clearly display coordinated geometric features that indicate continuous solid (ductile) flow during formation

166
Q

What is lineation?

A

a linear fabric

167
Q

examples of lineation

A

elongate minerals, worms burrows, cigar shaped i.e. prolate

168
Q

What is the term for Tectonite with lineation?

A

L - Tectonite

169
Q

What is foliation?

A

a planar fabric

170
Q

examples of foliation

A

mica; grains are pancake shape, e.g. oblate

171
Q

What is the term for tectonite with foliation?

A

S - Tectonite

172
Q

What is the term for tectonite with foliation and lineation?

A

L - S Tectonite

173
Q

What is the increasing order of change with metamorphic grade?

A

Slaty cleavage (fine) -> Schistosity (intermediate) -> Gneissic foliation (Coarse)

174
Q

Whats the difference between Schistosity and Gneissic foliation?

A

Schistosity is grain size visible to naked eye while Gneissic foliation has light - dark banding

175
Q

Why do crystals tend towards hexagonal shape when recrysallsing?

A

its a very energy efficient shape which is thermodynamically stable

176
Q

What are the two types of protolith?

A

Orthogneiss and Paragneiss

177
Q

Which protolith is igneous and the other is pelitic?

A

Ortho = igneous
Para = pelitic

178
Q

What is an order of protolith to high grade metamorphism?

A

Shale -> slate -> schist -> gneiss
(proto) (LG) (HG)

179
Q

Define cleavage?

A

The ability of a rock to spilt or cleave into ~parallel surfaces along foliation

180
Q

When does cleavage form?

A

At temps <350oC, below greenschist facies conditions

181
Q

What happens to grain size as metamorphic grade increases?

182
Q

What happens to minerals during deformation?

A

grow in a preferred alignment according to the stress feild

183
Q

What happens during schistosity grade metamorphism?

A

Other metamorphic minerals may grow, depends one composition of protolith e.g. garnet

184
Q

What must the schistose foliation do with non-elongate xls?

A

curve around it which forms wavy foliation

185
Q

How is gneissic foliation defines?

A

compositional banding

186
Q

What happens to muscovite in high grade metamorphic rocks?

A

breakdowns and reacts to form K-feldspar

187
Q

Rocks can contain more than one foliation, where?

A

Areas which have experiences polyphase deformation

188
Q

How are foliations labelled?

A

So = primary
S1, S2 = subsequent foliation-forming deformation events

189
Q

What is the development of tectonic foliation depend on?

A

composition parent lithology, metamorphic grade and magnitude of deformation

190
Q

What does the specific requirements for faliation development create?

A

characteristic foliation types

191
Q

What are the stages of cleavage development?

A

compaction -> pencil -> slaty -> crenulation

192
Q

What stages of cleavage development is diagenetic or tectonic?

A

Diagenetic; compaction
Tectonic; pencil, salty, crenulation

193
Q

How is diagenetic foliation created?

A

Thin elongated detritcal mica grains rotate passively into parallel orientation

194
Q

How are tectonic foliation created?

A

Pressure solution

195
Q

define pressure solution

A

wet diffusion where qtz dissolves and micas grow in response the orientation of the stress feild

196
Q

Where does tectonic cleavage pronouced and cross cut primary foliation?

A

Pencil cleavage

197
Q

How does pencil cleavage create elongated shards?

A

shale fractures along both primary and secondary foliations
or
fracturing along 2 tectonic foliations e.g. thrust ramp,formed during same deformation event

198
Q

What happens between pencil and slaty cleavage?

A

Continued tectonic shortening and tectonic foliation development

199
Q

What is slaty cleavage?

A

metamorphosed low greenschist grade

200
Q

What does salty cleavage create?

A

quartz and Mica rich domains

201
Q

What does Q & M domain create with compression?

A

Axial-planar cleavage; dine planar fabric parallel to the axial planes of the folds

202
Q

What is axial planar cleavage like in mudstones and sandstones?

A

mudstone: strong
sandstone: weak/absent

203
Q

What can axial planar cleavage tell you about?

A

fold struture where folding is obsercue

204
Q

What can axial planar cleavage and competece contrats create?

A

Cleavage refraction

205
Q

define cleavage refraction

A

contrast in competence between folded layers of rock

206
Q

Formation created by cleavage refraction?

A

cleavage fan

207
Q

How is cleavage fan formed?

A

more ductile horizon slides when folding creating contrast in cleavage orientation

208
Q

Names of sedimentary protoliths?

A

Psammite; sandy protolith
Pelite; muddy protolith

209
Q

What happens in transition to crenulation?

A

tectonic foliation develops at high angle to earlier tectonic foliation and new minerals form in preferred alignment

210
Q

Define difference between symmetric and asymmetric crenulation cleavage?

A

Sym; o1 parallel to pre-existing foliation

Asy; o1 not parallel to pre-existing foliation

211
Q

In crenulation cleavage, what does the axial planes to the microfolds create?

A

new foliation

212
Q

What is the physical shapes fromed by crenulation cleavage?

A

quatrz hinges; older tectontic foliation
mic limbs; younger tectonic foliation

213
Q

What terms used to classify fault rock?

A

Brittle, cohesive (incohesive) and ductile

213
Q

What promotes ductile deformation?

A

temp increase with depth

214
Q

What promotes brittle deformation?

A

strain rate increa

215
Q

Where are brittle incohesive fault rocks formed?

A

earth’s surface, and is subdivided based on the volume of angualur clasts vs powdery matrix

216
Q

What is the subdivision of brittle incohesive?

A

Fault breccia >30% frags.
shattered with visible angular fragments

Fault gouge <30% frags.
ground down to fine powder and ofter hydrothermally altered to clays

217
Q

What is brittle cohesive fault rock defined as?

A

Deformation accomplished by crushing (fracturing, rotation and frictional sliding)

  • fine grained, almost glassy with angular clasts
218
Q

What does brittle cohesive under go which defines subdivsions?

A

cataclastic and contains angular porphyroclasts in finer matrix

219
Q

What are the subdivisions of brittle cohesive?

A

Protocataclasite; crushed matrix 10-50%

Cataclasite; C.m 50-90%

Ultracataclasite; C.m >90%

220
Q

What is ductile cohesive fault rocks define by?

A

rocks produced by ductile reduction of initial grain size which develop penetrative foliation and mineral stretching lineation

221
Q

What are the subdivisions of ductile cohesion?

A

Protomylonite; 10-50% grain size reduction

Mylonite; 50-90% grain size reduction

Ultramylonite; <90% grain size reduction (few to no porphyroclasts remain)

222
Q

What is brittle and ductile cohesion called?

A

Brittle: cataclasite
Ductile: Mylonite

223
Q

Where was mylonite first applied?

A

Moine thrust, scotland