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

A

Rare

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
Q

Kyanite birefringence in thin section

A

Weak 1st order red maximum

26
Q

Kyanite extinction in thin section

A

Oblique at 30 degrees, parallel in cross sections

27
Q

Kyanite Twinning in thin section

A

Frequent 100 and 001

28
Q

Kyanite distinguishing features in thin section

A

Strong cleavage, Cross parting

29
Q

Sillimanite form in thin section

A

acicular or fibrous, square in cross-sections

30
Q

Sillimanite cleavage in thin section

A

1 good cleavage normal to length of crystal - poorly visible

Transverse fractures are characteristic

31
Q

Sillimanite birefringence in thin section

A

2nd order blue maximum

32
Q

Sillimanite extinction in thin section

A

Parallel

33
Q

Sillimanite twinning in thin section

A

None

34
Q

Sillimanite distinguishing features in thin section

A

Fibrous and/or acicular habit. Distinctive transverse fracture.

35
Q

Structure of Aluminum Silicates

A

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
Q

Crystal Systems of Aluminum Silicates

A

Sillimanite - Orthorhombic
Andalusite - Orthorhombic
Kyanite - Triclinic

37
Q

Common rock they occur in

A

metapelites