24 Orth Silicatezxs

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    Lecture 24:Lecture 24:

    OrthosilicatesOrthosilicates && SorosilicatesSorosilicates

    ReadRead ChptChpt 1010

    ORTHOSILICATES:

    !Structure: isolated [SiO4] tetrahedraheld together by interstitial

    cations

    !Distinguishing characteristics: high specific gravity(dense

    packing); high hardness; isotropic structure(no pronounced

    cleavage)

    !3 Important Groups: Olivines, Garnets, Al2SiO5polymorphs

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    3 Important Groups:

    (1) Olivine (M2VI

    SiO4)

    Most important:

    Fayalite Forsterite

    Fe2SiO4"Mg2SiO4

    Complete solid solutionbetween these two endmember

    minerals

    Nearly ideal(linear physical properties) solid solution

    (Fe"Mg) between two endmembers

    Also occurs:

    Monticellite Kirschteinite

    CaMgSiO4"CaFeSiO4

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    3 Important Groups:

    (1) Olivine ((Mg,Fe)2

    VISiO4)

    ! Occurrence: ultrabasic igneous rocks(peridotite, gabbro,

    basalt, dunite); metamorphosed serpentinites

    !Physical properties: glassy luster, conchoidalfracture, greencolor, granular, high melting point, H-6.5-7, easily altered

    ! Structure: 2 M sites for cations; M1= slightly distorted

    tetrahedron, M2=slightly larger, more distorted tetrahedron; at

    high T there is solid soln. between the two series

    ! Symmetry: Orthorhombic

    ! Uses: refractory sands, peridot (semiprecious gem)

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    3 Important Groups:

    (2) Garnet (A3

    VIIIB2

    VI(SiO4)

    3)

    Lots of solid solutionin the A and B sites

    Ugrandite series has A=Ca+2

    Uvarovite: Ca3Cr2(SiO4)3Grossular: Ca3Al2(SiO4)3Andradite: Ca3Fe2(SiO4)3

    Pyralspite series has B=Al+3(and ! Ca+2)

    Pyrope: Mg3Al2(SiO4)3Almandine: Fe3Al2(SiO4)3Spessartine: Mn3Al2(SiO4)3

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    3 Important Groups:

    (2) Garnet (A3VIIIB2VI(SiO4)3)

    ! Occurrence: accessory mineralin igneous rocks; common

    index mineral(indicative of P,T conditions of formation) in

    metamorphic rocks

    ! Physical properties: brown-red(due to Fe, Mn, Cr);

    dodecahedral(12-sided) shape with diamond-shaped faces is

    common

    Some colors: pyrope (pink/purple), spessartine (brownish

    red), almandine (deep red)

    ! Symmetry: Isometric

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    Almandine

    Salida, ColoradoPhoto by Mary Sutherland

    James Madison U.

    Grossular

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    Uvarovite

    Mineral Galleries

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    3 Important Groups:

    (3) Al2SiO5Group

    3 polymorphs: Kyanite, Andalusite, Sillimanite

    KYANITE

    SILLLIMANITE

    ANDALUSITE

    P

    T

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    3 Important Groups:

    Al2SiO5Group: Kyanite (AlVIAlVISiO5)

    !Occurrence: common in metamorphic rocks, often associatedwith garnet, corundum, staurolite, high pressure, dense phase

    !Physical properties: bladed crystals, blue color,hardness

    varieswith direction (H=5 parallel to crystal; H=7 perp to crystal);

    good {100} cleavage; vitreous to pearly luster

    !Symmetry: triclinic

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    KyaniteNamibia

    University of Bristol

    Kyanite

    Brazil

    Mineral Galleries

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    Andalusite, variety Chiastolite

    Brazil

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    Andalusite

    Brazil

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    3 Important Groups:

    Al2SiO5Group: Sillimanite (AlIVAlVISiO5)

    !Occurrence: common in high Tmetamorphic rocks (rarest of the3 polymorphs)

    !Physical properties: slender crystals or fibrous aggregates;

    white, brown or green color; perfect {010} cleavage

    !Symmetry: orthorhombic

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    Sillimanite

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    Sillimanite

    Brazil

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    Other important orthosilicate minerals:

    Zircon (ZrSiO4):used for radiometric dating; source of Zr

    Topaz (Al2SiO4(OH,F)2):blue gem

    Staurolite:high grade metamorphic index mineral

    Chloritoid:low grade metamorphic index mineral

    Titanite (sphene):common accessory mineral in igneous rocks

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    ZirconZircon

    StauroliteStaurolite

    TopazTopaz

    Keivy, Kola Peninsula Russia

    Photo Mary Sutherland, James Madison U.

    Marambaia Mina Gerais, Brazil

    Photo Mary Sutherland, James

    Madison U.

    Quebec, Canada

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    SOROSILICATES

    !from [SiO4] joined to form dimers!Example:

    Epidote(Ca2(Al,Fe) Al2OSiO4Si2O7(OH)): typically occurs in

    metamorphic rocks; distinguished by pistachio- or apple-green

    color

    Epidote

    Peru

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