Mineral Formulae

Note: know the formulas for those listed in your lab, marked $. If you cannot memorize a long formula, try to characterize it. Examples marked with an asterisk, *.

Secondary sedimentaryoccurrences are not mentioned for the silicates.

NESOSILICATES (alternate name Orthosilicates)

YSiO4

$ Olivines: simple solid solution Y2SiO4 or (Mg,Fe)2SiO4

Forsterite Mg2SiO4

Fayalite Fe2SiO4

OCC: Partial melting of mantle => Peridotites, Basaltic melt, Ol first to xtalz,

Basalts:1. MOR, Rift decompression melting of mantle; 2. Subduction Zone ~ 150 km, dewatering of subducted Ocean Lithosphere; 3. Partial melting of deep mantle at mantle – core boundary => Basaltic Plume

USE: 90% of Forsterite is used as a slag conditioner, 10% as a refractory.

Common Appearance: Tiny olive grains, weathers rusty.

$ Garnets: Y3Al2Si3O12

OCC: Metamorphism of Mudstones

Uses: abrasives

Common Appearance: rhombic dodecahedra or cubic, H ~7+, no consistent cleavages.

$ Zircon ZrSiO4

OCC: Common as tiny xtals in Granite, large in Alkaline Pegmatites

USE: ceramics;metamict: radiometric dating;source U, Th

Common Appearance: Tetragonal H 7.5, rarely metamict (black from radiation)

Aluminum Silicate Polymorphs

$ Sillimanite Al2SiO5Yellow-brown needles

$ KyaniteAl2SiO5Blue or white long Blades

$ AndalusiteAl2SiO5Dark, often cross in xsec

OCC: Metamorphism of Mudstones

UsesP,T index minerals, refractory

Common app: Given above

$ Staurolite (Fe,Mg)2Al9Si4O22(OH)2 *An Fe,Mg hydroxylated Aluminosilicate

OCC: Metamorphism of Mudstones

UsesP,T index minerals, refractory

Common App: brown Laths in side view, elongate diamond-shape or el. hexagon xsec

$ Topaz Al2SiO4(OH)2 * a hydroxylated Aluminosilicate

OCC: Late fractionation of magma (Granite & Rhyolites, Pegmatites)

Usesrefractory see:

Common App: H 8, Prismatic crystals with faces striated parallel to long dimension, wht-yellow

SOROSILICATES contain Si2O7

$ EpidoteCa2Al2(Fe3+;Al)(SiO4)(Si2O7)O(OH) * a Ca Fe+3 Al Sorosilicate

OCC: Retrograde Metamorphism and hydrothermal alteration of common minerals (feldspars, micas, pyroxenes, amphiboles, garnets).

UsesIndex mineral for low pressure (=shallow depth)

Common App: Usually Dark Green, with striated long Prismatic xtals, weathers to granular powder with distinctive light yellow-green color

$ HemimorphiteZn4(Si2O7)(OH)2.H2O* a Zinc Sorosilicate

OCC: Oxidation of the upper parts of Sphalerite ZnS bearing ore bodies, in the gossan of weathered Zinc Sulfide deposits.

UsesMined for Zinc

Common App: crystals are terminated by dissimilar faces.

CYCLOSILICATES 3,4 or 6-member rings. Ours all have 6-Silica rings

$ Tourmaline(Na,Ca)(Li,Mg,Al)3(Al,Fe,Mn)6(BO3)3(Si6O18)(OH)4* a hydroxylated Boron Cyclosilicate

OCC: in granite and granite pegmatites and in metamorphic rocks such as schist and marble.

Use: Refractory; Boron is used to dope quartz to make a semiconductor chip in computers

Common Appearance: Elongated crystals, trigonal to hexagonal xsec, usually black but sometimes colored, even multi-colored.

CHAIN SILICATES (INOSILICATES)

Pyroxenes (single chains) SiO3, thetetrahedra alternate direction in pairs.

Two prominent cleavages, meeting at angles near 90 degrees.

Cpx

$ Diopside CaMgSi2O6

OCC: In peridotite xenoliths from the Earth's mantle; contact metamorphism of Dolomites

Use: Ceramics, Geothermometer

Common Appearance: Usually medium green, two prominent cleavages, meeting at angles near 90 degrees, H 5-6

$ Augite (Ca,Na)(Mg,Fe,Al)(Si,Al)2O6. * a solid solution of Diopside and Hedenbergite, can also have Na and Al substituting

OCC: in mafic = basaltic rx, e.g. Basalt and Gabbro, most commonly at MORs and Rift Valleys.

Use: Geothermometer, and major component of Basaltic Rx used as Trap rock.

Common Appearance: Usually Dark Green, , two prominent cleavages, meeting at angles near 90 degrees, H 5-6.5

Pyroxenoids also SiO3, but tetrahedra do not alternate direction in pairs

$ Rhodonite MnSiO3

OCC: Hydrothermal Deposits

Use: Minor ore of Manganese

Common Appearance: Rose-red, oxidizes brown.

Amphiboles (double chains)X2Y5Si8O22 (OH)2. Two cleavages at about 120 and 60 degrees.

$ HornblendeCa2(Mg,Fe,Al)5(Al,Si)8O22(OH)2a mixture of Amphiboles with Aluminum

OCC: The Mafic mineral in intermediate magmas, e.g. Andesite and Diorite

Use:

Common Appearance: Dark green, straight stringy appearance in one direction, two cleavages at about 124 and 56 degrees.

SHEET SILICATES (PHYLLOSILICATES)

Micas Phyllosilicates with (AlSi3O10)(OH)2

$ MuscoviteKAl2(AlSi3O10)(OH)2 Light Brown sheets

$ Biotite K(Mg,Fe)3(AlSi3O10)(OH)2 Dark Brown to Black Sheets

OCC: In Granites and Metamorphosed mudrocks

Use: Finishing of drywall, insulation, electrical insulator

Common Appearance: see above.

Clays *hydrated aluminosilicates

$KaoliniteGroup, polymorphs of Al2Si2O5(OH)4

OCC: Hydrolysis weathering of Feldspars

Use: Porcelain, paper, food, light bulbs. Kaopectate.

Common Appearance: Soft white powdery, swells when wet.

Miscellaneous Phyllosilicates

$ Talc Mg3Si4O10(OH)2

OCC: Metamorphism of ultramafic (mantle) rocks, and in blueschist provinces (metam. wet ophilites from subduction zones.)

Use: Paper, Paint, Electric Cable.

Common Appearance: White, greasy slippery feel, soft

FRAMEWORK SILICATES (TECTOSILICATES)

A. Feldspars

1. Plagioclase XAl (Al,Si)3O8

$ Anorthite CaAl2Si2O8 Note the coupled solid solution, Ca++ and Al+3

$ Albite NaAlSi3O8or Na+ and Si+4

OCC: Anorthite in Basaltic Rocks, Albite in Granitic Rocks

Use: glassmaking, ceramics

Common Appearance: Hardness ~6, 2 good cleavages at 90o , Anorthite is Gray, Albite white.

Plagioclase is often Striated

2. K-spars

$ Microcline KAlSi3O8Low T

OCC: Granitic Rocks and Pegmatites

Use: glassmaking, ceramics

Common Appearance: Hardness ~6, 2 good cleavages at 90o , Microcline is pink to tan with light often with streaks that are exsolved Albite.

B. SiO2 Group

$ Quartz SiO2

OCC: In Granitic Rocks

Use: glassmaking, ceramics, abrasives, semiconductor chips

Common Appearance: Hardness 7, NO CLEAVAGE just Conchoidal fractures, Many colors

Plagioclase is often Striated

C. Feldspathoids form when Silica SiO2 is not abundant.

$Sodalite Na8Al6Si6O24Cl2

OCC: Veins in Nepheline Syenites

Use: Carvings

Common Appearance: Royal Blue color is distinctive

OXIDES

$ Corundum Al2O3

OCC: Metamorphosed mudstones.

Use: abrasive

Common Appearance: Scratches Quartz, Center of crystals appear swollen

$ Hematite Fe2O3

OCC: most is weathered Magnetite

Use: Ore of Iron

Common Appearance: Black to red, RED STREAK

$ Magnetite Fe3O4

OCC: Common Acc Min in Igneous Rx

Use: Ore of Iron

Common Appearance: Black, MAGNETIC i.e. it diverts the needle of a cheap compass.

HYDROXIDES

$ Gibbsite Al(OH)3

OCC: usually as a component of the mixture ore “Bauxite”

an ore of Aluminum, from secondary enrichment of Al from laterites

Use: Aluminum is a light structural metal: aircraft, etc.

Common Appearance: Wavy opaque white, looks like white agate.

SULFIDES

$ Pyrite FeS2

OCC:

Use: Manufacture of Sulfuric Acid

Common Appearance: Shiny gold, NO CLEAVAGES

$ Chalcopyrite CuFeS2

OCC: Sulfide deposits from Hydrothermal cells, e.g. MORs

Use: Ore of Copper

Common Appearance: Like tarnished Pyrite, tarnish is rusty colored.

$ Sphalerite ZnS

OCC: Sulfide deposits from Hydrothermal cells, e.g. MORs

Use: Ore of Zinc

Common Appearance: Dark Brown YELLOW STREAK

$ Galena PbS

OCC: Sulfide deposits from Hydrothermal cells, e.g. MORs

Use: Ore of Lead, sometimes Silver and Gold.

Common Appearance:3 good cleavages at 90o, metallic luster.

$ Cinnabar HgS

OCC: a vein-filling mineral associated with recent volcanic activity and alkaline hot springs.

Use: Ore of Mercury. Mercury is used to make, for example, modern light bulbs

Common Appearance: Cinnabar is usually a bluish pink

$ Bornite Cu5FeS4

OCC: Sulfide deposits from Hydrothermal cells, e.g. MORs

Use: Minor ore of copper

Common Appearance: Dark, with a iridescent purple tarnish

$ Pyrrhotite Fe(1-x)S

OCC: a common trace constituent of mafic igneous rocks, and as sulfide “intrusions” with pentlandite, chalcopyrite and other sulfides

Use: Pyrrhotite does not have specific applications. It is mined primarily because it is associated with pentlandite, a sulfide mineral that can contain significant amounts of nickel and cobalt

Common Appearance: Looks like Chalcopyrite, but crystals are pseudo-hexagonal.

$ Realgar As4S4 or AsS

OCC: Hot Springs

Use: Ore of Arsenic; arsenic is used to dope quartz to make a semiconductor chip in computers

Common Appearance: amorphous red, with yellow Orpiment

$ Orpiment As2S3

OCC: Hot Springs above magma.

Use: Ore of Arsenic

Common Appearance: amorphous yellow, with red Realgar

SULFATES

$ Gypsum CaSO4

OCC: Evaporites

Use: Drywall = sheet rock; plaster of Paris

Common Appearance: two good cleavages at 90o , soft, hardness 2 so scratched by fingernail. Sometimes makes a “desert rose”

$ Anhydrite CaSO4

$ Barite BaSO4

OCC: Hot Springs for example in our own Rift Valley.

Use: Ore of Barium, used as drilling mud.

Common Appearance: Heavy, usually white. Sometimes makes a “desert rose”

CARBONATES

$ CalciteLow Pressure CaCO3

OCC: Limestone from fossil shells, also hot springs: seawater saturated in Ca++ and CO2

Use: Concrete, optics.

Common Appearance:

$AragoniteHigh Pressure CaCO3

OCC: Limestone from Seashells, caves.

Use: Pure source of CaCO3 for laboratory use, Concrete

Common Appearance: Cyclic Twins

$ AzuriteCu3(CO3)2(OH)2

OCC: From weathered Copper sulfides, due oxidation of Copper ions in the zone of aeration

Use: Pigment

Common Appearance: Dark Blue. Weathers to green Malachite, with which it is usually associated.

2 Cu3(CO3)2(OH)2 + H2O → 3 Cu2(CO3)(OH)2 + CO2

$ MalachiteCu2CO3(OH)2

OCC: From weathered Copper sulfides, due oxidation of Copper ions in the zone of aeration

Use: Pigment

Common Appearance: Green. Often from weathered Azurite.

$ DolomiteCaMg(CO3)2

OCC: Flooding of limestone islands, seawater infiltrates Calcite, some Ca++ replaced by Mg++

Use: concrete; source of magnesium( the Pidgeon process).

Common Appearance: Crystal masses look like pink rice or like maggots

PHOSPHATES

$ ApatiteCa5(PO4)3(F,Cl,OH)

OCC: Metamorphosed limestones (i.e. Marble)

Use: Fertilizer, source of Phosphorous; Ore of Rare Earth Minerals;Phosphorus is used to dope quartz to make semiconductor chips.

Common Appearance: Hardness 5,~ hex xsec, colors vary

HALIDES

$ Fluorite CaF2

OCC: In gangue of weathered sulfides.

Use: Made into Cryolite, a flux for Aluminum smelting. Also made into HF hydrofluoric Acid.

Common Appearance: 4 cleavages, hardness 4 so scratches copper in penny, many colors

$ Halite NaCl

OCC: Evaporites

Use: Food, preservative

Common Appearance: Clear to white, 3 good cleavages at 90o

$ Sylvite KCl

OCC: Evaporites

Use: Potassium Fertilizer

Common Appearance:Colorless to White to Red, Cubic, 3 good cleavages at 90o