مواضيع المحاضرة: Silicates -major rock-forming minerals Isolated Tetrahedral Silicates –(SiO4)4-
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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Olivine - Mg

2

SiO

– Fe

2

SiO

4

Orthrhombic; pale yellow to olive green; vitreous luster
Usually as granular masses; Peridot – gemstone, nodules in basalt
Conchoidal fracture; H = 6.5 - 7, S.G. = 3.3-4.4
Structure – octahedra linked to isolated (SiO

4

)

4-

tetrahera

Occurrence:  mafic to ultramafic igneous rocks, basalt to peridotite
Dunite – all olivine rock


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Garnet Group – A

3

B

(SiO

4

)

(general formula)

Isometric; usually red, may be pink to green; vitreous luster
Dodecahedral xstals and massive; Conchoidal fracture; 
H = 6.5 – 7.5, S.G. = 3.5 - 4.3
Structure – A site = large divalent cations, Mg2+, Fe2+, Mn2+;
B site = smaller trivalent cations, Al3+, Fe3+, Cr3+
Pyrope (Mg-rich), Almandine (Fe-rich), Spessartine (Mn-rich),
Uvarovite (Cr-rich), Grossular (Ca-rich), Andradite (CaFe-rich) 
Occurrence:  metamorphic rocks, high P and high T


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Zircon – ZrSiO

Tetragonal; colorless to pink or brown; adamantine luster
Elongate xstals w/dipyramidal ends; 
H = 7.5, S.G. = 4.7
Zircon contains significant U and Th, radioactive, metamict
Used in radioactive age dating in U-Pb method; found in heavy
mineral fraction of sandstones, useful for provenance 
Occurrence:  widely distributed accessory mineral in all rock types,
especially common in granite


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Andalusite – Al

2

SiO

Group

Orthorhombic; white to pink; vitreous luster
Coarse square prisms w/chiastolite crosses – dark colored carbon
inclusions 
H = 7.5, S.G. = 3.2
Occurrence:  contact metamorphic rocks (pelitic schists) –
conditions of High T and Low P


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Kyanite – Al

2

SiO

Group

Triclinic; dark blue; vitreous luster
Long, bladed xstals; perfect cleavage in one direction 
H = 5 - 7, different along length and width; S.G. = 3.5
Occurrence:  High P metamorphic rocks (blueschists)
Used as an index mineral in defining metamorphic zones 


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Sillimanite – Al

2

SiO

Group

Orthorhombic; white to gray; vitreous luster
Long, slender xstals in parallel groups; frequently fibrous called
fibrolite
H = 6 - 7; S.G. = 3.2; one direction of cleavage
Occurrence:  High P and High T metamorphic rocks (pelitic
schists) - regional metamorphism
Used as an index mineral in defining metamorphic zones 


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Staurolite – Fe

2

Al

9

(Si

4

O

23

)(OH)

Monoclinic; brown; resinous to vitreous luster
Prismatic xstals with cruciform twins
H = 7 – 7.5; S.G. = 3.7; 
Occurrence:  Formed during regional metamorphismof Al-rich
rocks; found in gneisses and schists
Used as an index mineral medium grade metamorphic rocks 


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Silicates - major rock-forming minerals

Isolated Tetrahedral Silicates – (SiO

4

)

4-

Sphene (titanite) – CaTiO(SiO

4

)

Monoclinic; honey yellow to brown; resinous to adamantine luster
Wedged-shaped xstals
H = 5 – 5.5; S.G. = 3.4 
Occurrence:  Common in granites, gneisses, and chlorite schists
Used in radioactive age dating 


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Silicates - major rock-forming minerals

Paired Tetrahedral Silicates – (Si

2

O

7

)

6-

Epidote – Ca

2

(Al,Fe)Al

2

O(SiO

4

)(Si

2

O

7

)(OH)

Monoclinic; pistachio-green to black; vitreous luster
Elongate, prismatic xstals w/striations parallel to length; also
granular
H = 6 – 7; S.G. = 3.3-3.4 
Occurrence:  Common and widespread mineral; characteristic of
low to medium-grained metabasites and marbles
Associated w/actinolite, chlorite and albite in mafic rocks 


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Silicates - major rock-forming minerals

Ring Tetrahedral Silicates – (Si

6

O

18

)

12-

Beryl – Be

3

Al

2

(Si

6

O

18

)

Hexagonal; blue-green to light yellow to green; vitreous luster
Prismatic xstals w/hexagonal cross-sections vertically striated
H = 7.5 – 8; S.G. = 2.65 -2.8 
Occurrence:  Common and widely distributed in granitic rocks
and pegmatites
Gem beryl – emerald, aquamarine, morganite (pink), golden beryl
Harder than apatite; softer than corundum


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Silicates - major rock-forming minerals

Ring Tetrahedral Silicates – (Si

6

O

18

)

12-

Tourmaline –

(Na,Ca)(Li,Mg,Al)(Al,Fe,Mn)

6

(BO

3

)

3

(Si

6

O

18

)(OH)

4

Hexagonal; vitreous luster; color varies w/composition
Prismatic xstals w/trigonal cross-sections vertically striated
H = 7 -7.5; S.G. = 3 
Occurrence:  Common accessory in igneous and metamorphic 
rocks and granite pegmatites
Schorl- black, Fe-rich form, most common
Dravite – brown; rubellite – pink, elbaite - watermelon


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Silicates - major rock-forming minerals

Single Chain Silicates – Pyroxenes – (Si

2

O

6

)

4-

Tourmaline –

(Na,Ca)(Li,Mg,Al)(Al,Fe,Mn)

6

(BO

3

)

3

(Si

6

O

18

)(OH)

4

Hexagonal; vitreous luster; color varies w/composition
Prismatic xstals w/trigonal cross-sections vertically striated
H = 7 -7.5; S.G. = 3 
Occurrence:  Common accessory in igneous and metamorphic 
rocks and granite pegmatites
Schorl- black, Fe-rich form, most common
Dravite – brown; rubellite – pink, elbaite - watermelon


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Silicates - major rock-forming minerals

Single Chain Silicates – Pyroxenes – (Si

2

O

6

)

4-

Orthopyroxene – Opx -

orthorhombic

Enstatite – Ferrosilite (Mg,Fe)SiO

3

Hypersthene- int. composition

Stout prisms, 90° cleavage, no H

2

O in structure 

Color varies w/composition; more Fe-rich = darker color
Occurrence:  Gabbros, peridotite, basalt, andesite; very high 
grade metamorphic rocks – granulite facies

Enstatite

Hypersthene


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Silicates - major rock-forming minerals

Single Chain Silicates – Pyroxenes – (Si

2

O

6

)

4-

Clinopyroxene – Cpx -

monoclinic

Diopside – Hedenbergite: CaMgSi

2

O

-CaFeSi

2

O

6

Augite- most common; Stout prisms, 90° cleavage, no H

2

O

Color varies w/composition; more Fe-rich = darker color
Occurrence:  Gabbros, basalt, andesite, marble; very high 
grade metamorphic rocks – granulite facies

Diopside

Augite

Augite


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Silicates - major rock-forming minerals

Double Chain Silicates  - Amphiboles – (Si

4

O

11

)

6-

Tremolite – Actinolite: 

Ca

2

Mg

5

Si

8

O

22

(OH)

2

-

Ca

2

Fe

5

Si

8

O

22

(OH)

2

Monoclinic; contain H2O, elongate xstals, often acicular, 
color varies w/composition; white to green
2 cleavages @ 60° & 120°
Occurrence:  Tremolite – metamorphosed limestones
Actinolite – greenschist facies, metamorphosed igneous rocks

Tremolite

Actinolite


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Silicates - major rock-forming minerals

Double Chain Silicates  - Amphiboles – (Si

4

O

11

)

6-

Hornblende: (

Ca,Na)

2-3

(Mg,Fe,Al)

5

Si

6

(Si,Al)

2

O

22

(OH)

2

Monoclinic; contain H2O, black prismatic xstals
most common amphibole; 2 cleavages @ 60° & 120°
Occurrence:  Important mineral in both igneous and metamorphic
rocks


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Silicates - major rock-forming minerals

SIngle Chain Silicates – Pyroxenoids– (SiO

3

)

2-

Wollastonite –

CaSiO

3

Triclinic; vitreous luster, white
Bladed xstals w/high aspect ratio (length to width)
Twisted tetrahedral chains – lower symmetry than pyroxenes 
Occurrence:  Contact metamorphic mineral formed by fluid
Metamorphism (metasomatism)
CaCO

3

+ SiO

2

= CaSiO

3

+ CO

2




رفعت المحاضرة من قبل: Medoo Chan
المشاهدات: لقد قام 5 أعضاء و 111 زائراً بقراءة هذه المحاضرة








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