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Native minerals
Elements found in their pure form without chemical combination with other elements.
Halides
Cl, Br, F,
Oxides
O
Sulfates
SO4
Sulfides
S
Phosphates
PO4
Carbonates
CO3
Silicates
SiO2
Apatite
phosphate: Ca5(PO4)3(OH,F,Cl)
Aragonite
carbonate: CaCO3
Bornite
sulfide: Cu5FeS4
Calcite
carbonate CaCO3
Chalcocite
sulfide: Cu2S
Chalcopyrite
sulfide: CuFeS2
Cinnabar
sulfide: HgS
Corundum
oxide: Al2O3
Crocoite
oxide: PbCrO₄.
Diamond
native element: C
Fluorite
halide: CaF2
Galena
sulfide: PbS
Graphite
native element: C
Gypsum
sulfate: CaSO4-2H2O
Halite
halide: NaCl
Hematite
oxide: Fe2O3.
Magnesite
carbonate: MgCO3
Magnetite
oxide: Fe3O4.
Malachite
carbonate: Cu₂CO₃(OH)₂
Molybdenite
sulfide: MoS2
Pyrite
sulfide: FeS2
Rhodochrosite
carbonate: MnCO3
Rutile
oxide: TiO2
Sulfur
native: S
Siderite
carbonate: FeCO3
Sphalerite
sulfide: ZnS
Stibnite
sulfide: Sb2S3
Topaz
silicate: Al₂SiO₄(F, OH)2
Orthosilicates
Silicate minerals in which the silicate tetrahedron is independent.
General formula for olivine
orthosilicates: (Mg, Fe)2SiO4
General formula for garnet
orthosilicates: X3Y2(SiO4)3
Single chain silicates
Silicates where tetrahedra link in chains, such as pyroxenes.
General pyroxene formula
single chain silicates: XYZ2O6.
Double chain silicates
Silicates where tetrahedra link in double chains, such as amphiboles.
General amphibole formula
double chain silicates: A0-1B2C5T8022W2.
Sheet silicates
Silicate minerals with layered structures, such as micas and clays.
Framework silicates
Silicate minerals with interconnected frameworks of tetrahedra, such as quartz and feldspar.
Almandine
garnet, orthosilicate: Fe3Al2(SiO4)3
Andalusite
orthosilicate: Al2SiO5
Fayalite
orthosilicate: Fe2SiO4
Forsterite
orthosilicate: Mg2SiO4
Grossular
garnet, orthosilicate: Ca3Al2(SiO4)3
Kyanite
orthosilicate: Al2SiO5
Pyrope
garnet, orthosilicate: Mg3Al2(SiO4)3
Sillimanite
orthosilicate: Al2SiO5
Spessartine
garnet, orthosilicate: Mn3Al2(SiO4)3
Topaz
orthosilicate: Al2SiO4(F, OH)2
Zircon
orthosilicate: ZrSiO4
General formula for pyroxene
single chain silicates: XYZ2O6
Distinguishing orthopyroxene and clinopyroxene
Orthopyroxene (e.g., enstatite and ferrosilite) typically exhibits a single prism crystal habit and has a higher Mg/Fe ratio, while clinopyroxene (e.g., diopside and augite) shows a more complex crystal structure with two distinct cleavage angles and a greater variation in composition.
Enstatite
single chain silicate: Mg2Si2O6
Ferrosilite
single chain silicate: Fe2Si2O6
Hedenbergite
single chain silicate: CaFeSi2O6
Diopside
single chain silicate: CaMgSi2O6
Augite
single chain silicate: (Ca,Na)(Mg,Fe,Al)(Al,Si)2O6.
General amphibole formula
double chain silicates: A0-1B2C5T8022W2
Tremolite
double chain silicates: Ca2(Mg,Fe)5Si8O22(OH)2
Actinolite
double chain silicates: Ca2(Mg,Fe)5Si8O22(OH)2
Hornblende
double chain silicates: (Na, K)0-1Ca2(Mg, Fe, Al)5(Si,Al)8O22(OH)2
Glaucophane
double chain silicates: Na2Mg3Al2Si8O22(OH)2
Sheet silicates
Silicate minerals with layered structures, such as micas and clays.
Kaolinite
sheet silicate: Al2(Si2O5)(OH)4.
Serpentine
sheet silicate: Mg3(Si2O5)(OH)4.
Talc
sheet silicate: Mg3(Si4O10)(OH)2.
Muscovite
sheet silicate: KAl2(AlSi3O10)(OH)2.
Biotite
sheet silicate: K(Mg,Fe)3(AlSi3O10)(OH)2.
Chlorite
sheet silicate: Mg3([Si,Al]4O10)(OH)2 . (Mg,Al)3(OH)6.
Classification of sheet silicates
Classified as TOT (Tetrahedral-Octahedral Tetrahedral), TOT+C (Tetrahedral-Octahedral Tetrahedral + Cation), and TOT+O (Tetrahedral-Octahedral Tetrahedral + Octahedral).
Dioctahderal vs Trioctahedral
Dioctahderal has two octahedral cations per unit cell while trioctahedral has three octahedral cations per unit cell.
Framework silicates
Silicate minerals with interconnected frameworks of tetrahedra, such as quartz and feldspar.
Quartz
framework silicate: SiO2
Chrysotile
framework silicate: SiO2
Opal
framework silicate: SiO2.nH2O
Plagioclase feldspar
framework silicate: CaAl2Si2O8 to NaAlSi3O8
Alkali feldspar
framework silicate: NaAlSi3O8 to KAlSi3O8