Home > Classification of Minerals by Anionic Species How would you organize some 5000 species of minerals? Chemical Classification of M

Classification of Minerals by Anionic Species How would you organize some 5000 species of minerals? Chemical Classification of M

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Classification of Minerals by Anionic Species
(Anions are negative ions)
How would you organize some 5000 species of minerals?
Color? Hardness? Occurrence environment? Chemistry?
Positive ions? (cations) Negative ions? (anions)
Chemical Classification of Minerals Learning goals:
How are minerals classified by chemistry? Why is this useful?
Chemical Classification of Minerals Learning goals:
How are minerals classified by chemistry? By anionic species.
Chemical Classification of Minerals Learning goals:
Why is this useful? Because there is very little substitution at anion sites
Anions are Negative Ions
• May be single species
– O2-, F-, Cl-, S2-
• May be anionic group (polyanion):
– CO3
2-, SO4 2-, PO43-
• Silicates are classified by
polymerization of the silicate polyanion.
– Isolated tetrahedra – Chains – Sheets – Frameworks

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Chemical Classification
• Native Elements (no anions) • Halides (F, Cl, Br, I) (monovalent halogen) • Sulfides & arsenides (S, Ar) • Oxides (O) • Hydroxides (OH) • Sulfates & phosphates (SO4, PO4) • Carbonates (CO3) • Silicates:
– orthosilicates, sorosilicates, chain
silicates, layer silicates, framework silicates
Periodic Table Native Elements (no anions)
• Pure elements that occur as
minerals
– Graphite, diamond (C) – Sulfur (S) – Gold (Au), Silver (Ag), Copper (Cu) – Iron (kamacite) – Nickel (taenite) – As, Te, Se, Pt, Ir, Os, Pd, Ru, Rh
Native Elements
Halides: anion is F, Cl, Br, or I
• Halogens are the elements F, Cl, Br, I • Halogens are monovalent anions • Halite (NaCl), Sylvite (KCl) • Fluorite (CaF2) • Cryolite Na3AlF6
Periodic Table

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Sulfides: anion is S
• Sulfur is ��anion��, but is more covalent than
ionic (stoichiometry is less strict)
– Pyrite, marcasite (FeS2), chalcopyrite (CuFeS2) – Sphalerite ZnS, galena (PbS) – Chalcocite Cu2S, covellite (CuS), bornite (Cu5FeS4) – Realgar (AsS), orpiment (As2S3), cinnabar (HgS) – Stibnite (Sb2S3), molybdenite (MoS2)
• Sulfide minerals typically have
metallic luster, covalent bonding, and occur in hydrothermal veins.
• Only rarely do they occur at the
surface.
Elements in Sulfide Minerals
Oxides (Single): anion is O (no polyanion)
• Hemi-oxide Cuprite (Cu2O), Ice (H2O) • Monoxides
– Periclase group MgO, FeO, CaO, MnO – Zincite ZnO, Bromellite BeO
• Sesquioxides
– Corundum Al2O3, Hematite Fe2O3
• Dioxides
– Rutile TiO2, Cassiterite SnO2, Pyrolusite
MnO2
Oxides (Complex): anion is O
• Ilmenite FeTiO3 • Spinel Group
– Spinel MgAl2O4, Magnetite Fe3O4
• Perovskite CaTiO3
Hydroxides: anion is (OH)- Hydroxides: anion is OH
• Brucite Mg(OH)2 • Gibbsite Al(OH)3 • Diaspore AlOOH (Bauxite) • Goethite FeOOH

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Carbonates anion is (CO3)2- Carbonates Anion is (CO3)2-
• Calcite CaCO3, Rhodochrosite MnCO3 • Siderite FeCO3, Smithsonite ZnCO3 • Dolomite CaMg(CO3)2 • Aragonite CaCO3, Witherite BaCO3 • Strontianite SrCO3,Cerussite PbCO3 • Malachite and Azurite
Sulfates and Phosphates: (SO4)2- and (PO4)3- Sulfates and Phosphates: (SO4)2- and (PO4)3-
• Sulfur is 6+ • Phosphorus is 5+ • Contrast sulfide (S2-) and sulfate (S6+). • Phosphide (P3-) and phosphate (P5+). • Sulfates and phosphates are
oxidized!
Sulfates and Phosphates: (SO4)2- and (PO4)3-
• Barite (BaSO4), Celestine (SrSO4) • Gypsum CaSO4.2H2O • Anhydrite CaSO4 • Apatite Ca5(PO4)3OH • Turquoise CuAl6(PO4)4(OH)8·4H2O

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Silicates are classified by polymerization
• Orthosilicates (SiO4)4-: Isolated
tetrahedral O / Si = 4.0
• Sorosilicates (Si2O7)6- ��Bow-Ties�� 3.75 • Chain silicates
– (SiO3)2- : Infinite single chains 3.0 – (Si4O11)6- : Double Chains 2.75
• Sheet Silicates (Si4O10)4- sheets 2.5 • Framework Silicates (SiO2)
framework 2.0
Orthosilicates: (SiO4)4- Si/O: <~1/4 O / Si = 4
• Isolated SiO4 tetrahedra • Olivine Group (Mg2SiO4) • Garnet Group (Mg3Al2Si3O12) • Aluminosilicate Group (Al2SiO5) • Staurolite, Zircon, Titanite
Orthosilicates: Isolated Tetrahedra Sorosilicates and Cyclosilicates Si/O: 1/3 ~ ¼ O / SI = 3 – 3.5
• Epidote Group Ca2Al2FeSi3O12(OH) • Tourmaline NaMg3Al5B3Si6O27(OH)4 • Beryl Be3Al2Si6O18 • Cordierite (Mg,Fe)2Al(AlSi5)O18 •nH2O
Chain Silicates
• Single Chains Si/O ~ 1/3
– O / Si = 3.0 – Orthopyroxenes Mg2Si2O6 – Clinopyroxenes CaMgSi2O6 – Pyroxenoids Ca3Si3O9 • Double Chains Si/O 4:11
– O / (Si+Al) = 2.75
– Amphiboles (Mg,Fe)7Si8O22(OH)2

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Chain Silicates Layer Silicates O / Si = 2.5
• Antigorite
Mg3Si2O5(OH)4
• Talc
Mg3Si4O10(OH)2
• Kaolinite
Al2Si2O5(OH)4
• Pyrophyllite
Al2Si4O10(OH)2
• Biotite
K(Mg,Fe)3AlSi3O10(OH)2
• Muscovite
KAl2(AlSi3)O10(OH)2
• Chlorite
(Mg,Fe)6AlSi3O10(OH)2
Layer Silicates Framework Silicates (Tektosilicates) O / Si = 2
• Silica Group SiO2 • Alkali Feldspar (Na,K)AlSi3O8 • Plagioclase NaAlSi3O8-CaAl2Si2O8 • Feldspathoids (Leucite, Kalsilite, etc) • Zeolites (open hydrous frameworks)
O / (Al + Si)IV
• Framework Silicates = 2.0 • Sheet Silicates = 2.5 • Amphiboles = 2.75 • Chain Silicate = 3.0 • Sorosilicates = 3.5 • Orthosilicates = 4
Tektosilicates (Framework Silicates)

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Chemical Classification
• Native Elements (no anions) • Halides (F, Cl, Br, I) • Sulfides & arsenides (S, Ar) • Oxides (O) • Hydroxides (OH) • Sulfates & phosphates (SO4, PO4) • Carbonates (CO3) • Silicates:
– orthosilicates, sorosilicates, chain
silicates, layer silicates, framework silicates
Chemical Classification of Minerals Learning goals:
How (why) are minerals classified by chemistry? Why is this useful? Why not by cations? How else might you classify minerals? Hardness? Color? Occurrence? Abundance?
Give Chemical Classification of Kamacite (Fe)
A. Native Element B. Sulfide C. Metal D. Extra-terrestrial E. Oxide
Give Chemical Classification of Kamacite (Fe)
A. Native Element B. Sulfide C. Metal D. Extra-terrestrial E. Oxide
Give Classification of Troilite (FeS)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide
Give Classification of Troilite (FeS)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide

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Give Classification of Pyrite (FeS2)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide
Give Classification of Pyrite (FeS2)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide
Give Chemical Classification of Barite (BaSO4)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide
Give Chemical Classification of Barite (BaSO4)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Oxide
Give Chemical Classification of Fluorite (CaF2)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Halide
Give Chemical Classification of Fluorite (CaF2)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Halide

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Give Chemical Classification of Apatite (Ca3(PO4)3F)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Halide
Give Chemical Classification of Apatite (Ca3(PO4)3F)
A. Native Element B. Sulfide C. Sulfate D. Phosphate E. Halide
Homework 1
Due Tuesday
Chemical Classification of Minerals Learning goals:
How (why) are minerals classified by chemistry? Why is this useful? Why not by cations? How else might you classify minerals? Hardness? Color? Occurrence? Abundance?
Geochemical Classification of the Elements
Lithophile - Ionic Siderophile - Metallic Chalcophile - Covalent Atmophile - Van der Waals
Geochemical Classification of the Elements
• How do the elements partition
between coexisting fluid (melt) phases?
– Gas Phase : Atmophile : Van der Waals – Oxide phase: Lithophile : Ionic – Sulfide Phase: Chalcophile: Covalent – Metal Phase: Siderophile: Metallic

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Geochemical Classification of the Elements
• How do the elements partition
between coexisting fluid (melt) phases?
– Gas Phase : Atmophile : Van der Waals – Oxide phase: Lithophile : Ionic – Sulfide Phase: Chalcophile: Covalent – Metal Phase: Siderophile: Metallic
Geochemical Classification of the Elements
• How do the elements partition
between coexisting fluid (melt) phases?
– Gas Phase : Atmophile : Van der Waals – Oxide phase: Lithophile : Ionic – Sulfide Phase: Chalcophile: Covalent – Metal Phase: Siderophile: Metallic
Geochemical Classification of the Elements
• How do the elements partition
between coexisting fluid (melt) phases?
– Gas Phase : Atmophile : Van der Waals – Oxide phase: Lithophile : Ionic – Sulfide Phase: Chalcophile: Covalent – Metal Phase: Siderophile: Metallic
Elements partition among immiscible fluids by bond type (!!)
Geochemical Classification of the Elements
Atmophile - Van der Waals Lithophile - Ionic Chalcophile - Covalent Siderophile - Metallic

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Geochemical Classification of the Elements
Atmophile - Van der Waals Lithophile - Ionic Chalcophile - Covalent Siderophile - Metallic
Geochemical Classification of the Elements
Atmophile - Van der Waals Lithophile - Ionic Siderophile - Metallic Chalcophile - Covalent

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