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major rock-forming minerals Sheet Silicates - Faculty web pages

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<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Serpentine Group – Mg 3 Si 2 O 5 (OH) 4<br />

Monoclinic; green; greasy, waxy, silky luster<br />

Antigorite- flaky, Lizardite*– fine-grained, Chrysotile*– asbestiform<br />

*true polymorphs<br />

Chrysotile – principal asbestos mineral, mined in southern Quebec<br />

Occurrence: Forms as alteration product of Mg silicates such as ol,<br />

px, amph; low grade metamorphism of sea floor basalts<br />

Used as ornamental and building stone


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Clay Mineral Group – Kaolinite - Al 2 Si 2 O 5 (OH) 4<br />

Triclinic; common mineral<br />

Chief constituent of kaolin or clay<br />

Occurrence: secondary mineral formed by weathering or<br />

hydrothermal alteration of Al silicates<br />

Used in brick making, fine pottery, china


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Clay Mineral Group – Talc – Mg 3 Si 4 O 10 (OH) 2<br />

Monoclinic; apple-green to white; greasy luster and feel<br />

Compact and massive variety called soapstone<br />

Occurrence: secondary mineral formed by alteration of Mg silicates<br />

Low grade metamorphic <strong>rock</strong>s such as schists


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Mica Group – Muscovite – KAl 2 (AlSi 3 O 10 )(OH) 2<br />

Monoclinic; light-colored, vitreous luster<br />

Tabular crystals w/prominent basal planes and diamond-shaped or<br />

hexagonal cross-section; perfect (001) cleavage<br />

Occurrence: granites, pegmatites, metamorphic <strong>rock</strong>s<br />

Used as insulating material, called isinglass, in furnaces, stove<br />

doors


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Mica Group – Biotite – K(Mg,Fe) 3 (AlSi 3 O 10 )(OH) 2<br />

Monoclinic; dark-colored, vitreous luster<br />

Tabular crystals w/prominent basal planes and diamond-shaped or<br />

hexagonal cross-section; perfect (001) cleavage<br />

Occurrence: granites, pegmatites, gabbros,metamorphic <strong>rock</strong>s


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

<strong>Sheet</strong> <strong>Silicates</strong> – (Si 2 O 5 ) 4-<br />

Chlorite – (Mg,Fe) 3 (Si,Al) 4 O 10 (OH) 2 (Mg,Fe) 3 (OH) 6<br />

Triclinic or Monoclinic; green, micaceous habit but not a mica<br />

Folia not elastic<br />

Composition of chlorite is t-o-t layers interlayered w/”brucite”<br />

layers<br />

Occurrence: common in metamorphic <strong>rock</strong>s, greenschists<br />

Associated w/actinolite and epidote


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – (SiO 2 ) Group<br />

Quartz – SiO 2<br />

Hexagonal; crystals commonly prismatic,w/striated faces<br />

Conchoidal fracture, vitreous luster<br />

Color variable<br />

Occurrence: common,ubiquitous abundant mineral in great<br />

variety of geologic environments<br />

All <strong>rock</strong> types, highly resistant to weathering


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – (SiO 2 ) Group<br />

Quartz – SiO 2 Varieties:<br />

Amethyst – purple; rose quartz, smoky quartz, milky quartz,<br />

citrine<br />

Microcrystalline varieties:<br />

Fibrous – chalcedony, agate, onyx<br />

Granular – flint, chert, jasper


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – (SiO 2 ) Group<br />

Quartz – SiO 2 Varieties:<br />

Amethyst – purple; rose quartz, smoky quartz, milky quartz,<br />

citrine<br />

Microcrystalline varieties:<br />

Fibrous – chalcedony, agate, onyx<br />

Granular – flint, chert, jasper


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspar Group<br />

K-Feldspar Group: KAlSi 3 O 8<br />

Microcline – Triclinic; 2 cleavages @ 90°; white to pale pink<br />

Amazonite – aqua colored, Pb 2+ substitutes for K + creating color<br />

Center<br />

Characteristic grid twinning – albite and pericline twins, may show<br />

perthite –exsolution bands<br />

Occurrence: slowly cooled igneous <strong>rock</strong>s, granites, pegmatites,<br />

metamorphic <strong>rock</strong>s - gneisses


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspar Group<br />

K-Feldspar Group: KAlSi 3 O 8<br />

Orthoclase – Monoclinic; 2 cleavages @ 90°; white to pale pink<br />

Short prismatic crystals<br />

Carlsbad penetration twins common, also Baveno and Manebach<br />

twins<br />

May show perthite –exsolution bands<br />

Occurrence: moderately cooled igneous <strong>rock</strong>s, granites,<br />

pegmatites, high grade metamorphic <strong>rock</strong>s - gneisses


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspar Group<br />

K-Feldspar Group: KAlSi 3 O 8<br />

Sanidine – Monoclinic; 2 cleavages @ 90°; white to pale pink<br />

tabular crystals; Carlsbad penetration twins common<br />

Difficult to impossible to tell from orthoclase in hand specimen<br />

Need optical or X-ray techniques<br />

High T form, rapid cooling in volcanics<br />

Occurrence: volcanic igneous <strong>rock</strong>s, rhyolites, dacites, SiO 2 -rich<br />

volcanics


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspar Group<br />

Cleavlandite<br />

Albite<br />

Plagioclase Group: NaAlSi 3 O 8 –CaAl 2 Si 2 O 8<br />

Solid solution series – albite to anorthite end members<br />

Triclinic; 2 cleavages @ 90°; white to gray<br />

Tabular crystals; Albite polysynthetic twins common<br />

Labradorite may have play of colors<br />

Occurrence: mafic and felsic igneous <strong>rock</strong>s, metamorphic <strong>rock</strong>s,<br />

sedimentary <strong>rock</strong>s


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspar Group<br />

Labradorite<br />

Labradorite<br />

Plagioclase Group: NaAlSi 3 O 8 –CaAl 2 Si 2 O 8<br />

Solid solution series – albite to anorthite end members<br />

Triclinic; 2 cleavages @ 90°; white to gray<br />

Tabular crystals; Albite polysynthetic twins common<br />

Labradorite may have play of colors<br />

Occurrence: mafic and felsic igneous <strong>rock</strong>s, metamorphic <strong>rock</strong>s,<br />

sedimentary <strong>rock</strong>s


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspathoid Group<br />

Feldspathoid Group: Framework silicates similar to feldspars<br />

Contain 2/3 as much SiO 2 as feldspars, lower SG – 2.1-2.5<br />

Nepheline – (Na,K)AlSiO 4 , hexagonal<br />

Usually massive, compact, greasy luster, colorless to white<br />

Occurrence: SiO 2 -poor, alkali-rich igneous <strong>rock</strong>s<br />

NEVER FOUND WITH QUARTZ


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspathoid Group<br />

Feldspathoid Group:<br />

Sodalite –Na 8 AlSiO 4 Cl 2 , isometric<br />

Usually massive, blue, vitreous luster<br />

Rare mineral, associated w/nepheline<br />

Occurrence: SiO 2 -poor, alkali-rich igneous <strong>rock</strong>s<br />

NEVER FOUND WITH QUARTZ


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Feldspathoid Group<br />

Feldspathoid Group:<br />

Leucite – KAlSi 2 O 6 , isometric to tetragonal depending on T<br />

Trapezohedron crystals, white to gray, vitreous luster,<br />

Rare mineral<br />

Occurrence: Certain K-rich volcanics and shallow intrusives<br />

NEVER FOUND WITH QUARTZ


<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Zeolite Group<br />

Chabazite Chabazite<br />

Zeolite Group: Hydrous aluminosilicates w/Na, Ca, K and<br />

Variable amounts of water in large voids of framework which are<br />

interconnected spaces or channels<br />

Occurrence: Found in cavities in basalt, alterations of volcanic<br />

glass and tuff<br />

Defines low grade regional metamorphic facies – zeolite facies


Heulandite<br />

<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Zeolite Group<br />

Natrolite<br />

Zeolite Group:<br />

Natrolite – Na 2 Al 2 Si 3 O 10 2H 2 O<br />

Chabazite – Ca 2 Al 2 Si 4 O 12 2H 2 O<br />

Heulandite – CaAl 2 Si 7 O 18 6H 2 O<br />

Stilbite – NaCa 2 Al 5 Si 13 O 36 14H 2 O<br />

Stilbite


Heulandite<br />

<strong>Silicates</strong> - <strong>major</strong> <strong>rock</strong>-<strong>forming</strong> <strong>minerals</strong><br />

Framework <strong>Silicates</strong> – Zeolite Group<br />

Natrolite<br />

Stilbite<br />

Used commercially as molecular sieves – molecules too large to<br />

pass through channels excluded<br />

Catalytic cracking of hydrocarbon molecules<br />

Water softeners –cation exchange properties – hard water w/high<br />

Ca made soft by exchanging Ca 2+ for Na +

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