Principles of Mineral Behaviour (L7-13) Flashcards

1
Q

What does a phase diagram show?

A

Which structure is stable at a given P, T

Which structure has lowest free energy = eq^m state

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2
Q

What causes a phase transition?

A

Change in P, T
Change in eq^m state
Phase transition

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3
Q

For SiO2, which phase transitions are displacive and which are reconstructive?

A

Displacive: α-β Qz, high-low crist, high-low trid
Reconstructive: Qz-trid, trid-crist, Qz-coesite

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4
Q

Where does β cristobalite occur?

A

Rarely

In volcanic ash

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5
Q

Where does high P tridymite occur?

A

Thermal aureoles around granite/gabbro intrusions

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6
Q

What form is Si in, in α quartz?

A

Si in tetrahedra

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7
Q

What form is Si in, in stishovite?

A

Si in octahedra

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8
Q

Where does coesite occur?

A

As inclusions in garnet in ultrahigh pressure metamorphic rocks

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9
Q

What can be said about the properties of an individual tetrahedron of SiO2?

A

Si-O bonds are strong

Rigid tetrahedron

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10
Q

How do tetrahedra link?

What can be said about the angle?

A

Sharing corner oxygen, forming chains, sheets, or frameworks
θ = 180 = purely ionic, θ = 109 = purely covalent
θ observed 140-180: partly covalent

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11
Q

What can be said about the variation of bond energy w.r.t Si-O bond length and Si-O-Si bond angle?

A

Si-O bond length has a narrow range

Changing θ doesn’t change energy by much, allowing variety in frameworks

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12
Q
High β quartz:
Crystal system?
Space group?
When is it stable?
What does a view down the c axis show?
A

Hexagonal
P6_2 22
Stable above 573°C
Spirals of tetrehedra around screw nodes

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13
Q

Low α quartz:
Crystal system?
Space group?
When is it stable?

A

Trigonal
P3_2 21
Stable below 573°C

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14
Q

How can the structures of tridymite and cristobalite be described?

A

Sheets of tetrahedra stacked in different ways

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15
Q

High tridymite:
Crystal system?
Space group?
Stacking of layers?

A

Hexagonal
P 6_3 /mmc
ABAB

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16
Q

High cristobalite:
Crystal system?
Space group?
Stacking of layers?

A

Cubic
Fd3m
ABCABC

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17
Q

Define polytypes

A

Different structure of identical layers

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18
Q

Coesite:
Crystal system?
Space group?
Framework?

A

Monoclinic
C2/c
3D, contains 4-fold rings of tetrahedra

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19
Q
Stishovite:
Crystal system?
Space group?
Structure?
When is it stable?
Why so dense?
A
Tetragonal
P4_2 /mnm
Chains of edge sharing SiO6 octahedra
Stable at v high P
Dense as increased coordination of Si
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20
Q

Displacive transition of quartz from β to α:
How many orientations?
What happens to screw hexad?
What name is given to the product?

A

2
Becomes screw triad
Dauphiné twins

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21
Q

How can the SiO2 variants be told apart in thin section?

A

Quartz: uniaxial positive, dusty inclusions, undulose extinction
Tridymite: biaxial positive, arrow-head twinning
Cristobalite: uniaxial negative, fish scale texture

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22
Q

What happens in a displacive transition?

A

A high-symmetry structure transforms to a closely-related low-symmetry structure via small displacements of atoms
Displacements often described in terms of rotations of structural units

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23
Q

Displacive transitions:
Quenchable?
What happens if there’s a change in crystal system?

A

No, transition is too fast

Transformation twins appear

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24
Q

What happens in a reconstructive transition?

A

One polymorph transforms to another polymorph with an unrelated structure

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25
Q
Reconstructive transitions:
Why is activation energy large?
Quenchable?
Any twins?
Why does it cause seismic anomalies?
A

Bonds broken and reformed, diffusion of atoms, very slow process
Easily, because transformation is slow, metastability is possible
No since structures are unrelated
Because all physical properties change

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26
Q

What is the equation to determine free energy?

A

G = H_0 - TS + PV

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27
Q

Enthalpy:
What is it?
When does it dominate free energy?
What causes high enthalpy?

A

Bond energies + kinetic energy from atomic vibrations
When P and T are low
Electrostatic repulsion, unfavourable bond angles, strain, cation size mismatch, charge mismatch

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28
Q

Entropy:
What is it?
When does it dominate free energy?
What causes high entropy?

A

Measure of disorder in a crystal
When T is high
Large vibrational degree of freedom, configurational disorder

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29
Q

Volume:
What is it?
How is molar volume determined?
What does high P favour?

A

Efficiency with which atoms in structures fill space
Volume of unit cell and the number of formula units in it
Structures with small molar volume

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30
Q

Why is it unnecessary that H, S and V are a function of P, T?

A

ΔH, ΔS, ΔV are usually constant for solid-solid reactions

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31
Q

Temperature dependence of free energy:
Which phases are stable at low T and high T?
dG/dT = ?
Change at Ttr = ?

A

Low enthalpy phase stable at low T
High entropy phase stable at high T
dG/dT = -S
ΔS

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32
Q

Pressure dependence of free energy:
Which phases are stable at low P and high P?
dG/dP = ?
Change at Ptr = ?

A

Low enthalpy phase stable at low P
Low volume phase stable at high P
dG/dP = V
ΔV

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33
Q

How do first-order and second-order phase transitions differ?

A

First-order: discontinuous dG/dT at transition point

Second-order: continuous dG/dT, discontinuous d2G/dT2 at transition point

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34
Q

What kind of phase transition is Qz-trid?

A

Reconstructive

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35
Q

What determines the transition point in a phase transition?

A

ΔG = 0

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36
Q

Geological importance:
What is the SiO2 polymorph present indicative of?
What does the presence of transformation twins indicate?
How do reconstructive transitions relate to seismics?
How do displacive transitions relate to seismics?

A

PT conditions of formation
The cooling history
Reconstructive transitions -> Δρ -> Δv shear + body wave
Displacive transitions -> elastic property changes -> changes in v_s + v_p

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37
Q

Olivine:
General formula
Crystal system
Space group

A

R2SiO4
Orthorhombic
Pbnm

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38
Q

Where is olivine common?

A

Upper mantle

Basic igneous rocks

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39
Q

What is the structure of olivine?

A

Isolated SiO4 tetrahedra
Linked by cation sites (m1, m2) with 6 fold coordination
O(2-) arranged in close packed layers

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40
Q

What are the Goldschmidt rules for solid solution?

A

Cation differs in size by < 15%

Cations differ in charge by =< +/- 1

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41
Q

When is solid solution viable for olivine compositions, and when is it not?

A

Complete s.s. between Forsterite (Mg2SiO4) and Fayalite (Fe2SiO4)
No s.s. between Monticellite (CaMgSiO4) and Forsterite (Mg2SiO4)

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42
Q

Why can some structures containing octahedra not do displacive transitions?

A

Shared edges = not flexible

43
Q

Outline the olivine-spinel reconstructive transition

A

Both have O(2-) in c.p. layers
Olivine layers ABABAB, spinel layers ABCABC
Olivine hcp, spinel ccp

44
Q

How do the m1 and m2 cation sites differ in olivine’s structure?

A

M1 sites form a chain sharing edges
M2 sites attached to sides of chains
M2 sites are on mirror planes
M1 sites are between mirror planes

45
Q

What is the best way to distinguish forsterite and fayalite in thin section?

A

Forsterite: biaxial positive
Fayalite: biaxial negative

46
Q

What are the distinguishing features of olivine in thin section?

A

Moderate/high relief
Moderate/high birefringence
Often has curvy serpentine cracks

47
Q

Why does Fo and Fa form a s.s.?

A

Free energy of mixing is at a minimum between the two pure compositions

48
Q

How can the proportion of melt or xal be determined in a T against X plot?

A

Lever rule

49
Q

What develops if crystallisation is too fast for equilibrium compositions to develop?
How would it look for olivine?

A

Zoning

Mg rich core, Fe rich rim

50
Q

G-X curves for liquid and s.s. stability are a function of what?

A

T

51
Q

What is exsolution?

A

Lowering of energy by phase separation into two phase compositions

52
Q

When does exsolution typically occur?

Why?

A

Low T

ΔH(mix) value makes intermediate compositions unstable

53
Q

Define binary system

A

A chemical system which can be described in terms of 2 chemical components

54
Q

How do phase diagrams underpin petrology and geophysics?

A

Melting of mantle -> basalt

Melting of seds -> granite

55
Q

What are pyroxenes important in?

A

Basic igneous

High/med grade matemorphic

56
Q

What is the general formula for pyroxenes?

What can fill each role?

A
W(1-p) (x,y)(1+p) Z2O6
W: Ca, Na
x: Mg2+, Fe2+
y: Al3+, Fe3+
Z: Al3+, Si4+
57
Q

What is the structure of pyroxenes?

A

Single chains of SiO4 tetrahedra

Linked laterally by cations in 6 or 8-fold coordination

58
Q

What are the three main pyroxenes, and what are their space groups and crystal systems?

A

Diopside, C2/c, monoclinic
Orthopyroxene, pbca, orthorhombic
Pigeonite, p2(1)/c, monoclinic

59
Q

What does the quadrilateral of pyroxenes look like?

A
Trapezium shape
Top left: diopside CaMgSi2O6
Top right: hedenbergite CaFeSi2O6
Bottom left: enstatite Mg2Si2O6
Bottom right: ferrosilite Fe2Si2O6
Hypersthene = midpoint of enstatite and ferrosilite
Augite along the top
Opx along the bottom
Pigeonite a bit above opx
60
Q

Sodic pyroxenes:
Important in what?
Typically undergo what conditions of metamorphism?
Typical metamorphism product?
How do they differ from quadrilateral pyroxenes?

A

Important in alkali granites
High P, low T
Blueschists
Na+ instead of Ca2+, Al3+/Fe3+ instead of Mg/Fe2+

61
Q

What are the distinguishing features of all pyroxenes?

A

2 cleavages at 90°
Colourless (expect for 3 rare types)
Moderate relief

62
Q

How would cpx, opx and pig be distinguished in thin section?

A

cpx has inclined extinction, opx has straight
opx has low birefringence, cpx and pig have moderate
pig has inclined extinction + low 2V

63
Q

How do pyroxene chains adjust to the different sizes of cation?

A

Rotation of tetrahedra

64
Q

How do the structures of opx and cpx differ?

A

Cpx: all m1 site octahedra are in the same orientation
Opx: different orientations of m1 octahedra

65
Q

How does high and low pigeonite differ?

A

High: C2/c space group, extended chains almost 180° between tetrahedra
Low: P2(1)/c, 2 types of chains with different tetrahedral rotation angles

66
Q

Where does the large miscibility gap arise from between opx + pig and augite in the pyroxene quadrilateral?

A

Different cation sizes:
Ca2+ 1.00Å, Mg2+ 0.72Å, Fe2+ 0.78Å
Large ΔH(mix)

67
Q

Why is Ca2Si2O6 not a pyroxene?

A

Can’t substitute Ca on m1 sites

68
Q

What does the sodic pyroxene triangle look like?

A

Top: Aegerine NaFeSi2O6
Bottom left: Jadeite NaAlSi2O6
Bottom right: Augite Ca(Mg,Fe)Si2O6
Complete s.s. between Aegerine and Jadeite
Complete s.s. between Aegerine and Augite
Not a complete s.s. between Jadeite and Augite
Stable omphacite phase between Jadeite and Augite

69
Q

What is the structure of omphacite w.r.t. cation sites?

A

Ordered arrangement of alternating Al/Mg on m1

Ca/Na on m2

70
Q

How could omphacite be identified in thin section?

A

2 cleavages at 90°

Green in ppl

71
Q

There are three types of processes in quadrilateral pyroxenes, state and outline them

A

Entropy associated with thermal motions:
Open structures at high T, collapsed at low T
C2/c P2(1)/c displacive transition in pigeonite
Entropy associated with distribution of cations in structure:
Favours s.s. at high T, limited s.s. at low T
-> miscibility gap
-> exsolution of pig from aug and reverse, exsolution of opx from aug and reverse
Reconstructive transition pig opx:
-> expect distinctive textures in thin section
indicative of cooling rates

72
Q

Exsolution of pig from aug:
When do lamellae of pig grow?
Why is the interface planar?
What is the interface plane?

A

When xal cools below solvus by diffusion of Ca & Mg/Fe2+
Minimise strain energy
// (001)

73
Q

How can exsolution lamellae be used to determine cooling rate?

A
x^2 = D*t
x = diffusion distance ~ thickness of lamellae
D = diffusion coefficient
t = time
74
Q

What does the diffusion coefficient depend on?

What does this mean for exsolution rate?

A

Strong T dependence

Faster at high T

75
Q

How do exsolution lamellae depend on T besides growth rate?

A

Orientation of growth

76
Q

Fast cooling:
Which rock types?
Which phase transitions?

A

Volcanics: basalt/andesite
Too fast for reconstructive transition or exsolution
Displacive transitions occur

77
Q

What would be the result of fast cooling of:
Augite?
Pigeonite?

A

Augite: homogeneous augite xals
Pigeonite: homogeneous pig xals, displacive transition from high pig to low pig

78
Q

Intermediate cooling:
Typical settings?
Which phase transitions?

A

Thick lava flow or thin sill
Too fast for reconstructive transition
Time for Ca/Mg diffusion -> exsolution

79
Q

What would be the result of intermediate cooling of:
Augite?
Pigeonite?

A

Augite: exsolution of pig // (001)
Pigeonite: exsolution of aug // (001)

80
Q

What’s the typical setting of slow cooling?

A

Large intrusions of basic magma

81
Q

What would be the process of slow cooling pigeonite?

A

Twinned xal of pigeonite
Cool to pig+aug solvus: exsolve aug // (001)
Cool to eutectoid point: exsolution lamellae coarsen + reconstructive transition pig -> opx (+ aug)
Further cooling: aug exsolving from opx // (100)
“inverted pigeonite” texture

82
Q

What would be the result of slow cooling of augite?

A

Aug crystals with pig // (001)

83
Q

What would be the result of slow cooling opx?

A

Opx crystals with aug // (100)

84
Q

What is the chemistry of the alkali feldspar s.s.?
What is the extent at various T?
Why?

A

NaAlSi3O8 - KAlSi3O8
Complete s.s. at high T
Limited s.s. at low T
K+ Na+, large Δr, Δz = 0

85
Q

What is the chemistry of the plagioclase feldspar s.s.?
What is the extent at various T?
Why?

A

NaAlSi3O8 - CaAl2Si2O8
Complete s.s. at all T
Na+ + Si4+ Ca2+ + Al3+, Δr small, Δz = 1

86
Q

What is the structure of feldspars?

A

3D framework of corner sharing AlO4 & SiO4 tetrahedra

Na, K, Ca in large cavity sites

87
Q

What kind of phase transitions are seen in feldspars?

A

Displacive
Exsolution textures
Al/Si ordering

88
Q

Displacive transition in Na-rich feldspar:
What happens?
Space group change?
Crystal system change?

A

Framework collapses around Na+
C2/m C(-)1
Monoclinic triclinic

89
Q
Displacive transition in Na-rich feldspar:
What develops?
What is this known as?
What are the two types of interfaces?
Combining the two interface types gives?
A

Shear orientations of equal proportions
Transformation twinning
// old m plane = Albite twin, // old diad = pericline twin
Cross hatched twins, albite + pericline 90° apart

90
Q
Exsolution in alkali feldspars:
What occurs?
Under what condition?
Thermodynamics + effect?
Product?
A

Na+ K+ diffusion
Intermediate cooling rate
Large +ve ΔH(mix) -> solvus, peak T = 700°C
Exsolution textures

91
Q

Al/Si ordering (alkali feldspar):
Cooling rate?
What happens at high T?
What happens at low T?
Where is the transition between high and low T?
How can the high and low T transition be visible?

A

Very slow cooling rate
Configurational entropy favours disordered distribution of Al & Si among tetrahedral sites
Enthalpy reduction due to removal of local strains favours ordered distribution of Al & Si
Transition at 480°C
Sanidine -> microcline in contact metamorphic aureoles

92
Q

Al avoidance:
Other name?
What is it?
Purpose?

A

Loewenstein’s rule
Al & Al try to avoid occupying adjacent tetrahedra
Reduces elastic energy

93
Q

What catalyses Al/Si diffusion?

What conclusion can be drawn from this?

A

H+

Wet granite Al/Si ordering faster than dry granite

94
Q

What would be the process of intermediate cooling of sanidine?

A

Cools until solvus hit
Exsolution of Na-rich feldspar begins
Exsolution continues until eutectoid point hit
Na feldspar transformation: mono -> tri + twinning within lamellae (only albite twins)
“perthite texture” = irregular lamellae of albite in K feldspar

95
Q

What is the product of slow cooling of an intermediate alkali feldspar composition?

A

Low albite + microcline showing coarse scale exsolution

96
Q

Al/Si ordering (plag feldspar):
Purpose?
Problem?

A

Lowers enthalpy by reducing elastic energy

Al:Si ratio changes across s.s.

97
Q

Feldspar names:
NaAlSi3O8
CaAl2Si2O8
KAlSi3O8

A

NaAlSi3O8: albite
CaAl2Si2O8: anorthite
KAlSi3O8: sanidine/orthoclase/microcline

98
Q
Plag composition in rocks:
Basalt?
Anorthosite?
Granite?
Andesite/granodiorite?
Metamorphic?
A

Basalt: An 65-70%
Anorthosite: An 80-90%
Granite: Ab-rich
Andesite/granodiorite: complex zoning at intermediate compositions
Metamorphic: An content increases with grade

99
Q

Why do andesites & granodiorites have complex zoning of plag feldspars compositions?

A

Effect of p(H2O) on liquidus/solidus temperatures

100
Q

What are the characteristic features of plag feldspars in thin section?

A

Abundant lamellar twinning (growth twins)
Low relief
Low birefringence

101
Q

What is the effect of having 2 Al in anorthite compared to albite’s 1 Al:

w. r.t structure
w. r.t Al avoidance

A

An has doubled c repeat in comparison with Ab
Add Al to ordered Ab: puts Al next to Al, unfavourable
-> get alternative ordering schemes & miscibility gaps

102
Q

How many miscibility gaps are there in plag feldspar s.s.?

Why?

A

3: peristerite, Boggild, Huttenlocher

4 ordered structures

103
Q

Why does the peristerite miscibility gap exist for plag feldspars?

A

Increasing Al/Si order -> decreased free energy
Narrow G curve because ordered Ab can’t accept much Al in s.s.
-> coexisting ordered Ab and disordered An_27

104
Q

How can plag composition be determined from extinction angles?

A

Find a twinned crystal with sharp twin boundaries
Align twins N-S: same colour in both twins
Check twin interface is vertical: use medium power, twin plane doesn’t move on focus change
Extinction angle symmetrical for both twins
Measure two extinction angles for 5 crystals
Use maximum value
Compare to chart