Silicate Minerals (I) Flashcards

(53 cards)

1
Q

Two broad classification of minerals.

A

Silicates and Non-silicates

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2
Q

When pertaining to Minerals Abundances, what is the percent abundance of Plagioclase Feldspars?

A

39%

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3
Q

When pertaining to Mineral Abundances, what is the percent abundance of Potassium Feldspar?

A

12%

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4
Q

When pertaining to MIneral Abundances, what is the percent abundance of Quartz?

A

12%

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5
Q

When pertaining to Mineral Abundances, what is the percent abundance of Pyroxenes?

A

11%

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6
Q

When pertaining to Mineral Abundances, what is the percent abundance of Amphiboles?

A

5%

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7
Q

When pertaining to Mineral Abudances, what is the percent abundance of Micas?

A

5%

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8
Q

When pertaining to Mineral Abudances, what is the percent abundance of Clays?

A

5%

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9
Q

When pertaining to Mineral Abudances, what is the percent abundance of all the Other Silicate Minerals?

A

3%

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10
Q

When pertaining to Mineral Abudances, what is the percent abundance of Non-silicates?

A

8%

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11
Q

Two bases for clasification of minerals.

A

Crystal Structure and Chemical Composition

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12
Q

Largest Group of Minerals.

Compounds Containing Silicon and Oxygen.

Building Block: Silicon Tetrahedron (SiO4)^-4.

A

Silicates

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13
Q

Determine the kind of Silicate:

Independent Silica Tetrahedron

Densely packed tetrahedra and bounded to one another via ionic bonds with interstitial cations.

Crystal habits are equidimensional and lack pronounced cleavage.

*Mostly ferromagnesian minerals

A

Nesosilicates

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14
Q

A nesosilicate mineral subgroup characterized by;

High relief, Relatively Strong Birefringence, Fair Cleavage, and Parallel Extinction

Can be confused with Pyroxenes, and alters to Serpentine Minerals

Common in Subsilicic, Mafic, Ultramafic, Metamorphic Limestones, and Contact Metamorphic Rocks

Rare in Pegmatites, Obsidians, and Ores

A

Olivine Group

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15
Q

Iron-rich member of the Olivine group.

A

Fayalite

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16
Q

Magnesium-rich member of the Olivine group.

A

Forsterite

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17
Q

What is the 2V angle of forsterite?

A

85 to 90 Degrees

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18
Q

What is the 2V angle of Fayalite?

A

47 to 54 Degrees

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19
Q

True or False:

Fayalite is the more common member of the Olivine Group.

A

False, Forsterite is more common, thus Fayalite is rarer.

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20
Q

A group under the nesosilicate minerals, which include the Aluminium and Calcium Silicates.

A

Garnet Group

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21
Q

Series of minerals under the Garnet group characterized by being the Aluminium Silicates.

A

Pyralspite Series (Pyrope, Almandine, Spessartine)

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22
Q

Series of minerals under the Garnet group characterized by being the Calcium Silicates.

A

Ugrandite Series (Uvarovite, Grossularite, Andradite)

23
Q

Which garnet series has the higher index of refraction, Pyralspite Series or Ugrandite Series?

A

Ugrandite Series

24
Q

Three Members of the Aluminosilicate Polymorphs.

A

Andalusite, Sillimanite, and Kyanite

25
Paired (“sister”) Silica Tetrahedra. Isolated Pyrosilicate Anions (Si2O6^−7). Consisting of double tetrahedra with a shared oxygen vertex.
Sorosilicates
26
Minerals under the Sorosilicate Category
Epidote Supergroup and Lawsonite Group
27
Ring Silica Tetrahedra 3-, 4-, 6-, 8-, 9-, or 12- Membered Rings of Si^4+ Tetrahedra Strongly linked bonds yield relatively dense and hard minerals.
Cyclosilicates
28
Members of the Cyclosilicate Category
Tourmaline Group, Beryl Group, Cordierite
29
Chained Silica Tetrahedra Have Interlocking Chains of Silicate Tetrahedra with SiO3. Pyroxenes
Single-chain Inosilicates
30
Which member of the Inosilicate category: Good to fair cleavages at ~93° Occasional simple twins Biaxial with large 2V angles Some are pleochroic large range of extinction angles for the Monoclinic members 6-50°) Most common members: augite, pigeonite Occurs in subsilicic igneous rocks, metamorphic rocks, meteorites
Pyroxene Group
31
Single-chain Inosilicate, short and stubby.
Pyroxenes
32
Two classifications of Pyroxenes.
Orthopyroxenes and Clinopyroxenes
33
Members of Orthopyroxenes include?
Estatite, Bronzite, Hypersthene, Ferrosiltite
34
Members of the Clinopyroxene group include?
Augite, Diopside, Pigeonite, Hedenbergite, Aegirine, Jadeite, Spodumene, Omphacite, Aegirine-Augite
35
Double-chain Inosilicates, long and slender.
Amphiboles
36
Two classifications of amphiboles.
Clinoamphiboles and Orthoamphiboles
37
Chained Silicon Tetrahedra Has interlocking Chains of Silicate Tetrahedra with Si4O11 Amphiboles
Double-chain Inosilicates
38
Pseudohexagonal cross-sections Perfect cleavage at 56-124° Simple twins common Common species: hornblende, basaltic hornblende: lamprobolite Colored and often pleochroic
Amphibole Group
39
Members of the Orthoamphibole group.
Anthophyllite
40
Members of the Clinoamphibole group.
Hornblende, Riebeckite, Cummingtonite, Crunerite, Tremolite-Actinolite, Nephrite, Lamprobolite, Glaucophane
41
Which kind of Amphibole minerals are more common?
Clinoamphiboles
42
Silicate minerals that are also called as chain silicates, that can be single-chain or double-chain, commonly monoclinic and orthorhombic.
Inosilicates
43
How to easily identify Pyroxenes or Amphiboles as Monoclinic or Orthorhombic?
Extinction Type/Angle: Monoclinic: Inclined Extinction Orthorhombic: Parallel Extinction
44
Garnet has ______ cleavage directions.
Zero
45
Olivine has _______ relief.
High
46
True or False: Amphiboles have inclined extinction.
Partially true. Generally, it exhibits inclined extinction, but not all the time. Orthoamphiboles are much rarer than Clinoamphiboles; Clinoamphiboles exhibit Inclined Extinction.
47
Ratio and Cation of Nesosilicates
1:4, (SiO4)^-4
48
Ratio and Cation of Sorosilicates
2:7 , (Si2O7)^-6
49
Ratio and Cation of Cyclosilicates
1:3, (Si6O18)^-12
50
Ratio and Cation of Single-chain Inosilicates
1:3, (Si2O6)^-4
51
Ratio and Cation of Double Chain Inosilicates
4:11, (Si4O11)^-6
52
Ratio and Cation of Phyllosilicates
2:5, (Si2O5)^-2
53
Ratio and Cation of Tectosilicates
1:2, SiO2