Neosilicates: Aluminum Silicates Flashcards

1
Q

Aluminium Silicates Formula

A

Al2SiO5

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2
Q

3 Polymorphs of Alluminum Silicates

A

Andalusite
Kyanite
Sillimanite

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3
Q

Polymorphs

A

Polymorphism describes the existence of a solid material in more than one form or crystal structure. Polymorphism is a form of isomerism.

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4
Q

Sillimanite

A

High-temperature form of Aluminium Silicate

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5
Q

Andalusite

A

Low temperature - Low pressure form of Aluminum Silicate

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6
Q

Kyanite

A

High pressure polymorph of aluminum silicate

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7
Q

Triple point of Aluminium Silicates

A

525 C

0.385 GPa

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8
Q

Invariant

A

Point where all 3 phases coexist

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9
Q

Importance of Aluminum Silicates

A

Their triple point is in the middle of common metamorphic conditions making them useful to determine the conditions at which the rock formed

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10
Q

Paragenisis of Aluminum Silicates

A

Metamorphic rocks formed in the conditions described be the triple point

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11
Q

Andalusite colour in thin section

A

Colourless

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12
Q

Kyanite colour in thin section

A

Colourless to pale blue

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13
Q

Sillimanite colour in thin section

A

Colourless to light yellow

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14
Q

Pleochroism in Aluminum Silicates

A

None / very weak

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15
Q

Relief in Aluminum Silicates

A

High

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16
Q

Aluminum Silicates colour in thin sections

A

Colourless / Pale

17
Q

Andalusite form in thin section

A

Euhedral crystals with dark CROSS

Dark inclusions of carbonaceous material is frequently arranged symmetrically to form a Maltese Cross.

18
Q

Andalusite Cleavage in thin section

A

Parallel to 110, in cross-sections intersection at 90 degrees

19
Q

Andalusite birefringence in thin section

A

weak up to 1st order yellow

20
Q

Andalusite extinction in thin section

A

Parallel but symmetric in cross sections

21
Q

Andalusite twinning in thin section

22
Q

Andalusite distinguishing features in thin section

A

Cross, weak birefringence

23
Q

Kyanite form in thin section

A

Tabular often deformed

24
Q

Kyanite cleavage in thin section

A

2 good cleavages parallel to 100 and 010 at 85 degrees

25
Kyanite birefringence in thin section
Weak 1st order red maximum
26
Kyanite extinction in thin section
Oblique at 30 degrees, parallel in cross sections
27
Kyanite Twinning in thin section
Frequent 100 and 001
28
Kyanite distinguishing features in thin section
Strong cleavage, Cross parting
29
Sillimanite form in thin section
acicular or fibrous, square in cross-sections
30
Sillimanite cleavage in thin section
1 good cleavage normal to length of crystal - poorly visible | Transverse fractures are characteristic
31
Sillimanite birefringence in thin section
2nd order blue maximum
32
Sillimanite extinction in thin section
Parallel
33
Sillimanite twinning in thin section
None
34
Sillimanite distinguishing features in thin section
Fibrous and/or acicular habit. Distinctive transverse fracture.
35
Structure of Aluminum Silicates
Half the Al is arranged in Straight chains of AlO6 are arranged parallel to the c axis The rest is arranged differently for each polymorph Sillimanite in 4 fold site, andalusite in 5 fold sites, kyanite in 6 fold sites These are linked along the c axis by SiO4 tetrahedra
36
Crystal Systems of Aluminum Silicates
Sillimanite - Orthorhombic Andalusite - Orthorhombic Kyanite - Triclinic
37
Common rock they occur in
metapelites