1 Rock Forming Silicate Minerals. 2 Importance of the Silicates Abundance –~25% of all known minerals –Make up ~90% of earth’s crust –Composed of dominant.

Slides:



Advertisements
Similar presentations
A Tour of the Rock Forming Silicates
Advertisements

GOLDSCHMIDT’S RULES 1. The ions of one element can extensively replace those of another in ionic crystals if their radii differ by less than approximately.
Silicates are classified on the basis of Si-O polymerism
Back to silicate structures: nesosilicates inosilicates tectosilicates phyllosilicates cyclosilictaes sorosilicates.
Mineral Structures Silicates are classified on the basis of Si-O polymerism the [SiO 4 ] 4- tetrahedron.
Disilicates and Ring Silicates
Back to silicate structures:
Lecture 5 Crystal Chemistry Part 4: Compositional Variation of Minerals 1. Solid Solution 2. Mineral Formula Calculations.
Igneous Rocks. Classification of Igneous Rocks Most Abundant Elements: O, Si, Al, Fe, Ca, Mg, K, Na Calculate Elements as Oxides (Account for O) How Much.
Six-sided, pyramidal Quartz Crystals.
Mineral Chemistry and Crystallography. Definition of a Mineral All minerals: 1) Occur naturally 2) Are inorganic solids 3) Have a definitive chemical.
Systematic Mineralogy Description of how minerals are divided into groups Description of how minerals are divided into groups Groups based on anions Groups.
Introduction to Igneous Rocks IN THIS LECTURE –The basis of classification –Major versus trace versus REE –Classification of Igneous Rocks Plutonic Volcanic.
Ionic Coordination and Silicate Structures Lecture 4.
The Phase Rule in Metamorphic Systems
Mineral Structures From definition of a mineral:
Bridging oxygen Apical oxygen Non-bridging oxygen.
Atoms are the smallest components of nature
How Many Molecules? Pyrite Cube weighs 778 g – how many molecules is that?? About 4,000,000,000,000,000,000,000,000 Are they ALL Iron and Sulfur?
Feldspar Group Most abundant mineral in the crust  6 of 7 most common elements Defined through 3 end-members  Albite (Na), Anorthite (Ca), Orthoclase.
Distillation l l Start with a partially fermented product (containing some EtOH) l l Through a process of heating, vapor production, and condensation,
Feldspar Group Most abundant mineral in the crust  6 of 7 most common elements Defined through 3 end-members  Albite (Na), Anorthite (Ca), Orthoclase.
SiO 2 After Swamy and Saxena (1994) J. Geophys. Res., 99, 11,787-11,794.
How many molecules? Pyrite – FeS 2 Would there be any other elements in there???
Melt-crystal equilibrium 1 l Magma at composition X (30% Ca, 70% Na) cools  first crystal bytownite (73% Ca, 27% Na) l This shifts the composition of.
Lecture 17 Systematic Description of Minerals
Lecture 20 (12/06/2006) Systematic Description of Minerals Part 4: Silicates II: Cyclosilicates, Inosilicates, Phyllosilicates and Tectosilicates.
Atoms, Compounds, Minerals and Rocks. Atoms Atoms - the smallest unit of an element that retains the physical and chemical properties of that element.
Lecture 19 (12/04/2006) Systematic Description of Minerals Part 3: Silicates I: Introduction, Nesosilicates, and Sorosilicates.
Mineralogy Minerals and crystals. World’s largest crystals: A cave in the Naica Lead Zinc mine, Mexico.
Chapter 14 Classification and names of minerals. Mineral varieties: isomorphism Garnets Garnets Same crystal system and morphologySame crystal system.
Conversations with the Earth Tom Burbine
Lecture 16 Systematic Description of Minerals Part 3: Silicates I: Introduction to Silicates, Nesosilicates, and Sorosilicates Pyrope.
Chemistry of Igneous Rocks Characterization of different types (having different chemistries): –Ultramafic  Mafic  Intermediate  Felsic Composition.
EARTH MATERIALS III Rock-forming minerals: silicates Professor Peter Doyle
MOST IMPORTANT MINERAL SUITE: The Silicate Minerals
Rocks are aggregates of minerals. Many are silicate minerals. This granite, an igneous rock, has Quartz, an amphibole called Hornblende, a pink potassium.
MINERALS. Chemical composition of the Crust n Oxygen most abundant- 46.6% n Followed by silicon and aluminum n Iron, Calcium, Sodium, Potassium, Magnesium.
Another ‘picture’ of atom arrangement
Stoichiometry Chemical Analyses and Formulas Stoichiometry Chemical analyses of oxygen bearing minerals are given as weight percents of oxides. We need.
Ge 101. Introduction to Geology and Geochemistry Lecture 2 Crystal Structure of Minerals.
Ionic radius is related to the valence of the ion - ions that have lost electrons (cations) are smaller than their neutral state, ions that have gained.
List of 10 minerals (groups) you really want to know to be people Quartz, Olivine, Amphibole, Pyroxene, Feldspars, Garnet, Staurolith, Aluminosilicates,
  … is a naturally occurring, solid, with highly ordered atomic arrangement, homogeneous chemical composition.  Minerals are formed by inorganic processes.
Weathering -II.
Chapter 10 - B Identification of minerals with the petrographic microscope.
EPSC210 Introductory Mineralogy
Framework Silicates 2/3 of crust is framework silicates 2/3 of crust is framework silicates Quartz and feldspars are most common Quartz and feldspars are.
What if we had staurolite and andalusite together? What conditions would that indicate?
Metamorphic Rocks Francis, paragoniteNaAl 2 (AlSi 3 O 10 (OH) 2 muscoviteKAl 2 (AlSi 3 O 10 (OH) 2 pyrophylliteAl 2 Si 4 O 10 (OH) 2 andalusiteAl.
Minerlaogi II Average Composition of the Continental Crust Weight PercentVolume Percent Si O O Table 3.4.
Orthosilicates Isolated tetrahedron Isolated tetrahedron Common examples Common examples Olivine, garnet, and zircon Olivine, garnet, and zircon Al 2 SiO.
Introduction to Mineralogy Dr
Aluminosilicate Minerals
Pyroxene.
Magma Differentiate magma based on it’s chemical composition  felsic vs. mafic.
Introduction to Mineralogy, Second edition William D. Nesse Copyright © 2012, by Oxford University Press, Inc. CHAPTER 16 Orthosilicates.
Silicates JD Price. Silicate Structure (SiO2)
Structure of the Silicate Minerals Comparing Crystal Structures to Visible Mineral Properties.
III. Atoms, Elements and Minerals
BELL WORK: Define MINERAL:
Minerlaogi II Silikater.
Structure of the Silicate Minerals
Silicates are classified on the basis of Si-O polymerism
Minerals with isolated [SiO4]4- tetrahedra
Chemical Formulas Subscripts represent relative numbers of elements present (Parentheses) separate complexes or substituted elements Fe(OH)3 – Fe bonded.
MINERALOGY OF THE SILICATES
Silicates are classified on the basis of Si-O polymerism
Stoichiometry Some minerals contain varying amounts of 2+ elements which substitute for each other Solid solution – elements substitute in the mineral.
Crystal Structure and Crystallography of Materials
Presentation transcript:

1 Rock Forming Silicate Minerals

2 Importance of the Silicates Abundance –~25% of all known minerals –Make up ~90% of earth’s crust –Composed of dominant elements in earth’s crust (O, Si, Al, Fe, Mg, Ca, Na, K) –Rock-forming minerals Economic uses –Building construction (brick, stone, morter, glass) –Technology (silicon chips)

3 What Are Silicates? Frameworks based on the linkage of cation centered coordination polyhedron –The silica tetrahedra: the building block of the silicate minerals –SiO 4 -4 is the basic unit Si 2 O 7 SiO 4 Si 4 O 11 SiO 3 Si 2 O 5 SiO 2 Si 2 O 6

4 The Silicates Frameworks based on the linkage of SiO 4 -4 tetrahedra –Results in a structurally stable, anion complex –Suitable for the formation of polymers (two or more shared complex ions of the same type) Charge reaching the cation is exactly 1/2 the charge on the anion –Limited ways in which polymers can form (Pauling’s Rules) –Charge balance in minerals attained by: Sharing oxygen between adjoining tetrahedra Linking tetrahedra with other cations Si 2 O 7 SiO 4 Si 4 O 11 SiO 3 Si 2 O 5 SiO 2

5 Silicates Structure Ratio of Si to O determines structural configuration and is the criteria for silicate classification (subclasses) –Neso: SiO 4 -4, separate tetrahedra (1:4; Si:0) –Soro: Si 2 O 7 -6, double tetrahedra (1:3.5; Si:0) –Cyclo: Si 3 O 9 -6 (3 tetrahedra ring), Si 4 O (4 tetrahedra ring), Si 6 O (6 tetrahedra ring) (1:3; Si:0) SiO 4 Si 2 O 7 SiO 3 Si 4 O 11 Si 2 O 5 SiO 2 Si 2 O 6

6 More Silicates Structure Ratio of Si to O determines structural configuration and is the criteria for silicate classification (subclasses) –Ino: SiO 3 -2 (single chain of tetrahedra) (1:3; Si:0), Si 4 O (double chain of tetrahedra) (1:2.75; Si:0) –Phyllo: Si 4 O (OH) 2, sheets of tetrahedra (1:2.5; Si:0) –Tecto: SiO 2, three dimensional frameworks (1:2; Si:0) SiO 4 Si 2 O 7 SiO 3 Si 4 O 11 Si 2 O 5 SiO 2 Si 2 O 6

7 Silicate Subclasses Neso (a) Soro (b) Cyclo (c, d, e)

8 Silicate Subclasses Ino Phylo

9 Silicate Subclasses Tecto [SiO 2 ]

10 The Silicates Six silicate subclasses Name Structural linkage of SiO 4 -4 Silica Tetrahedra Geometry; Examples Nesosilicates SiO 4 independent silica tetrahedra; olivine, garnet Sorosilicates Si 2 O 7 double silica tetrahedra; epidote Cyclosilicates SiO 3 ring of silica tetrahedra; beryl (emerald), tourmaline Inosilicates Si 2 O 6 Si 4 O 11 chains of silica tetrahedra; pyroxene, amphibole Phyllosilicates Si 2 O 5 sheets of silica tetrahedra; mica, clay Tectosilicates Si0 2 frameworks of silica tetrahedra; quartz, feldspar

11 Structural Formulas and Silicate Group Minerals Where do the other cations fit? Coordination polyhedron with oxygen depends on ionic radius CationC.N.Polyhedron K+K+ 8-12Cubic Na + 8-6Cubic to octahedral Ca Cubic to octahedral Mn 2+ 6Octahedral Fe 2+ 6Octahedral Mg 2+ 6Octahedral Fe 3+ 6Octahedral Ti 4+ 6Octahedral Al Octahedral to tetrahedral Si 4+ 4Tetrahedral

12 Structural Formulas and Silicates Describes the structural and chemical relationship between related minerals (mineral groups) through a generalized description of the chemical formula Symbology –X = large, weakly charged cations, C.N. >6 (with oxygen) Na, K, & Ca (sort of) –Y = medium-sized, 2+ to 4+ cations, C.N. = 6 Mg, Fe +2, Fe +3, Al, Ti, & Ca (sort of) –Z = small cations, C.N. = 4 Mainly Si +4, but also Al +3 –W = additional anionic groups OH -, Cl -, F - Results in generic formula for all silicates: X m Y n (Z p O q )W r

13 T-X Phase Diagrams Diagrams showing the relationship between temperature, composition, and proportion of crystals and liquid in a melt –Liquidus: t-x at which first crystals form from a melt –Solidus: t-x at which the last melt crystallizes

14 The Solvus and Miscibility Gaps Miscibility gap (opposite of solid solution) –Defined by the solvus Outline of the miscibility gap Represents the area of a phase diagram where naturally occurring minerals do not occur

Mineral Families Nesosilicates Nesosilicates Olivine groupOlivine –Forsterite - Mg 2 SiO 4Forsterite –Fayalite - Fe 2 SiO 4Fayalite Garnet groupGarnet –Pyrope- Mg 3 Al 2 (SiO 4 ) 3Pyrope –Almandine - Fe 3 Al 2 (SiO 4 ) 3Almandine –Spessartine - Mn 3 Al 2 (SiO 4 ) 3Spessartine –Grossular - Ca 3 Al 2 (SiO 4 ) 3Grossular –Andradite - Ca 3 Fe 2 (SiO 4 ) 3Andradite –Uvarovite - Ca 3 Cr 2 (SiO 4 ) 3Uvarovite –Hydrogrossular - Ca 3 Al 2 Si 2 O 8 (SiO 4 ) 3-m (OH) 4mHydrogrossular Zircon group –Zircon - ZrSiO 4Zircon –Thorite - (Th,U)SiO 4Thorite Al 2 SiO 5 group –Andalusite - Al 2 SiO 5Andalusite –Kyanite - Al 2 SiO 5Kyanite –Sillimanite - Al 2 SiO 5Sillimanite –Dumortierite - Al BO 3 (SiO 4 ) 3 (O,OH) 3Dumortierite –Topaz - Al 2 SiO 4 (F,OH) 2Topaz –Staurolite - Fe 2 Al 9 (SiO 4 ) 4 (O,OH) 2Staurolite

Sorosilicates Cyclosilicates Epidote group (has both (SiO 4 ) 4− and (Si 2 O 7 ) 6− groups) –Epidote - Ca 2 (Al,Fe) 3 O(SiO 4 )(Si 2 O 7 )(OH)Epidote –Zoisite - Ca 2 Al 3 O(SiO 4 )(Si 2 O 7 )(OH)Zoisite –Clinozoisite - Ca 2 Al 3 O(SiO 4 )(Si 2 O 7 )(OH)Clinozoisite –Tanzanite - Ca 2 Al 3 O(SiO 4 )(Si 2 O 7 )(OH)Tanzanite –Allanite - Ca(Ce,La,Y,Ca)Al 2 (Fe 2+,Fe 3+ )O(Si O 4 )(Si 2 O 7 )(OH)Allanite –Dollaseite-(Ce)- CaCeMg 2 AlSi 3 O 11 F(OH)Dollaseite-(Ce) 3-member ring –Benitoite - BaTi(Si 3 O 9 )Benitoite 6-member ring –Axinite - (Ca,Fe,Mn) 3 Al 2 (BO 3 )(Si 4 O 12 )(OH)Axinite –Beryl/Emerald - Be 3 Al 2 (Si 6 O 18 )BerylEmerald –Cordierite - (Mg,Fe) 2 Al 3 (Si 5 AlO 18 )Cordierite –Tourmaline - (Na,Ca)(Al,Li,Mg) 3- (Al,Fe,Mn) 6 (Si 6 O 18 (BO 3 ) 3 (OH) 4Tourmaline

Inosilicates SiO 3, 1:3, Si 4 O 11, 4:11 ratio Single chain Pyroxene groupPyroxene –Enstatite - orthoferrosilite series Enstatite - MgSiO 3Enstatite Ferrosilite - FeSiO 3Ferrosilite –Pigeonite - Ca 0.25 (Mg,Fe) 1.75 Si 2 O 6Pigeonite –Diopside - hedenbergite series Diopside - CaMgSi 2 O 6Diopside Hedenbergite - CaFeSi 2 O 6Hedenbergite Augite - (Ca,Na)(Mg,Fe,Al)(Si,Al) 2 O 6Augite –Sodium pyroxene series Jadeite - NaAlSi 2 O 6Jadeite Aegirine (Acmite) - NaFe 3+ Si 2 O 6AegirineAcmite –Spodumene - LiAlSi 2 O 6Spodumene Pyroxenoid group –Wollastonite - CaSiO 3Wollastonite –Rhodonite - MnSiO 3Rhodonite –Pectolite - NaCa 2 (Si 3 O 8 )(OH)Pectolite Double chain Amphibole groupAmphibole –Anthophyllite - (Mg,Fe) 7 Si 8 O 22 (OH) 2Anthophyllite –Cumingtonite series Cummingtonite - Fe 2 Mg 5 Si 8 O 22 (OH) 2Cummingtonite Grunerite - Fe 7 Si 8 O 22 (OH) 2Grunerite –Tremolite series Tremolite - Ca 2 Mg 5 Si 8 O 22 (OH) 2Tremolite Actinolite - Ca 2 (Mg,Fe) 5 Si 8 O 22 (OH) 2Actinolite –Hornblende - (Ca,Na) 2- 3 (Mg,Fe,Al) 5 Si 6 (Al,Si) 2 O 22 (OH) 2Hornblende –Sodium amphibole group Glaucophane - Na 2 Mg 3 Al 2 Si 8 O 22 (OH) 2Glaucophane Riebeckite (asbestos) - Na 2 Fe 2+ 3 Fe 3+ 2 Si 8 O 22 (OH) 2Riebeckiteasbestos

Phyllosilicates Si 2 O 5 or a 2:5 ratio Clay mineral groupClay mineral –Halloysite - Al 2 Si 2 O 5 (OH) 4Halloysite –Kaolinite - Al 2 Si 2 O 5 (OH) 4Kaolinite –Illite- (K,H 3 O)(Al,Mg,Fe) 2 (Si,Al) 4 O 10 [(OH ) 2,(H 2 O)]Illite –Montmorillonite- (Na,Ca) 0.33 (Al,Mg) 2 Si 4 O 10 (OH) 2 ·nH 2 OMontmorillonite –Vermiculite - (MgFe,Al) 3 (Al,Si) 4 O 10 (OH) 2 ·4H 2 OVermiculite –Talc - Mg 3 Si 4 O 10 (OH) 2Talc –Palygorskite - (Mg,Al) 2 Si 4 O 10 (OH)·4(H 2 O)Palygorskite –Pyrophyllite - Al 2 Si 4 O 10 (OH) 2Pyrophyllite Mica groupMica –Biotite - K(Mg,Fe) 3 (AlSi 3 )O 10 (OH) 2Biotite –Muscovite - KAl 2 (AlSi 3 )O 10 (OH) 2Muscovite –Phlogopite - KMg 3 (AlSi 3 )O 10 (OH) 2Phlogopite –Lepidolite - K(Li,Al) 2- 3 (AlSi 3 )O 10 (OH) 2Lepidolite –Margarite - CaAl 2 (Al 2 Si 2 )O 10 (OH) 2Margarite –Glauconite - (K,Na)(Al,Mg,Fe) 2 (Si,Al) 4 O 10 (OH) 2Glauconite Chlorite group –Chlorite - (Mg,Fe) 3 (Si,Al) 4 O 10 (OH) 2 (Mg,Fe) 3 (OH) 6

Tectosilicates Quartz group –Quartz - SiO 2Quartz –Tridymite - SiO 2Tridymite –Cristobalite - SiO 2Cristobalite Feldspar familyFeldspar –Alkali-feldspars Potassium-feldspars –Microcline - KAlSi 3 O 8Microcline –Orthoclase - KAlSi 3 O 8Orthoclase –Sanidine - KAlSi 3 O 8Sanidine Anorthoclase - (Na,K)AlSi 3 O 8Anorthoclase –Plagioclase feldsparsPlagioclase Albite - NaAlSi 3 O 8Albite Oligoclase - (Na,Ca)(Si,Al) 4 O 8 (Na:Ca 4:1)Oligoclase Andesine - (Na,Ca)(Si,Al) 4 O 8 (Na:Ca 3:2)Andesine Labradorite - (Na,Ca)(Si,Al) 4 O 8 (Na:Ca 2:3)Labradorite Bytownite - (Na,Ca)(Si,Al) 4 O 8 (Na:Ca 1:4)Bytownite Anorthite - CaAl 2 Si 2 O 8Anorthite Feldspathoid familyFeldspathoid –Nosean - Na 8 Al 6 Si 6 O 24 (SO 4 )Nosean –Cancrinite - Na 6 Ca 2 (CO 3,Al 6 Si 6 O 24 ).2H 2 OCancrinite –Leucite - KAlSi 2 O 6Leucite –Nepheline - (Na,K)AlSiO 4Nepheline –Sodalite - Na 8 (AlSiO 4 ) 6 Cl 2Sodalite Hauyne - (Na,Ca) 4- 8 Al 6 Si 6 (O,S)24(SO 4,Cl) 1-2Hauyne –Lazurite - (Na,Ca) 8 (AlSiO 4 ) 6 (SO 4,S,Cl) 2Lazurite Scapolite groupScapolite –Marialite - Na 4 (AlSi 3 O 8 ) 3 (Cl 2,CO 3,SO 4 )Marialite –Meionite - Ca 4 (Al 2 Si 2 O 8 ) 3 (Cl 2 CO 3,SO 4 )Meionite Zeolite groupZeolite –Natrolite - Na 2 Al 2 Si 3 O 10 2H 2 ONatrolite –Chabazite- CaAl 2 Si 4 O 12 6H 2 OChabazite –Heulandite - CaAl 2 Si 7 O 18 6H 2 OHeulandite –Stilbite - NaCa 2 Al 5 Si 13 O 36 17H 2 OStilbite

Pyroxene Amphibole Biotite Mica Mafic Minerals Igneous Rock-Forming Minerals Felsic Minerals Orthoclase Feldspar Muscovite Mica Quartz Plagioclase Feldspar (Ca/Na) Olivine