Accessory Minerals

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    Minerals down the Microscope on Moodle(back to intro)

    Minerals down the Microscope on Moodle.

    Part 2: Accessory minerals

    These are typically very stable and commonly present as small crystals in a variety of igneous, metamorphic and

    sedimentary rocks but never present in large quantities. Hence they are not rock-forming minerals (i.e. the ca. 10

    minerals that form the vast majority of rocks).

    Minerals covered on these pages:

    Zircon

    Apatite

    Titanite

    Tourmaline

    Opaques(Fe-oxides, Fe-sulphides)

    Zircon

    Rock types in which zircon is commonly present: Granites, Intermediateigneousrocks , Sandstones, Schists,

    Gneisses

    (Generally present in all silicate rocks except ultrabasic igneous rocks)

    Zircon in mylonite

    Analyser out Analyser in

    Optical properties of zircon

    High relief

    High orderinterference colours

    Shape: Typically euhedral (igneous) or well rounded

    Formspleochroic haloes in biotite

    Minerals that might be confused with zircon

    Titanite (higher interference colours)

    Zircon shape, interference colours andpleochroic haloes

    Zircon in metasedimentary gneiss

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Reliefhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Pleochroichttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Pleochroichttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Reliefhttp://web2.ges.gla.ac.uk/~minerals/Intro.htm
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    Analyser out Analyser in

    Zircons in granite (note darker biotite adjacent to zircon)

    Analyser out Analyser in

    Zircon in schist Zircon in metasedimentary gneiss

    Analyser out Analyser in

    Note: Dark spots (pleochroic haloes) in biotite caused by radiation damage from small inclusions of

    zircon in the biotite. At high magnifications, some larger zircons may display internal zoning either picked

    out by small differences in relief or interference colours. In igneous rocks zircon typically has good crystal

    shape, in clastic sedimentary rocks and metasediments it tends to be well rounded.

    Apatite

    Rock types in which apatite is commonly present: Granites, Intermediate igneous rocks, Sandstones,

    Schists, Gneisses

    (Generally present in most silicate rocks except ultrabasic and basic igneous rocks)

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shape
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    Apatite inclusions in amphibole Apatite in orthogneiss

    Analyser out Analyser out

    Optical properties of apatite

    Colourless

    Moderate reliefLow orderinterference colours

    Shape: Typically euhedral slightly elongate prisms (hexagonal x-section)

    Minerals that might be confused with apatite

    Quartzand feldspar (low relief and typically abundant)

    Apatite shape and interference colours

    Apatite in granite

    Analyser out Analyser in

    Apatite in gneiss

    Analyser out

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Reliefhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Colour
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    Note: Higher relief that adjacent quartz, typical hexagonal; cross section and low interference colours.

    Hexagonal sections are typically completely dark in crossed polars.

    Titanite

    Rock types in which titanite is commonly present: Intermediate igneous rocks, Metabasic rocks, Calc-

    silicates

    Titanite in granite

    Analyser out Analyser in

    Optical properties of titanite

    High relief

    V. high orderinterference colours

    Shape: Diamond shaped in igneous rocks

    Minerals that might be confused with titanite

    Garnet(isotopic), Calcite (lower relief),Zircon (lower interference colours)

    Titanite shape and interference colours

    Titanites in metabasic rock

    Analyser out Analyser in

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Calcite.htmhttp://web2.ges.gla.ac.uk/~minerals/Garnet.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Relief
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    Note: Little change in colour of titanite when analyzer inserted due to very high interference colours.

    Metamorphic titanite tends to be less well shaped and may form a reaction rim around Fe-Ti oxides

    Tourmaline

    Rock types in which tourmaline is commonly present: Schists, Gneisses, some Granites

    Tourmaline in mica schist

    Analyser out Analyser in

    Optical properties of tourmaline

    Moderate relief

    Strongly coloured (often zoned)

    Moderate orderinterference colours

    Shape: Generally euhedral elongate with curved triangular cross section

    Elongate sections arepleochroic

    Minerals that might be confused with tourmaline

    Amphibole (Cleavage)Biotite (Cleavage, pleochroic scheme)

    Tourmaline shape and interference colours

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Biotite.htmhttp://web2.ges.gla.ac.uk/~minerals/Amphibole.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Pleochroichttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Colourhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Relief
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    Tourmaline in mica schists

    Analyser out Analyser out

    Note: Colour zoning indicative of compositional zoning. Both biotite and tourmaline are strongly

    pleochroic but elongate sections of tourmaline are dark N-S, biotite is dark E-W

    Opaques

    (Oxides and sulphides tend to be opaque minerals e.g. Magnetite, Ilmenite, Pyrite)

    Most rocks contain some opaque minerals.

    Ilmenite tends to form slightly tabular crystals, Pyrite often forms cubes.

    Optical properties... dark with analyser out.

    All images with analyser out

    Ilmenite in biotite schist Fine grained magnetite in basalt

    Magnetite in peridotite Fe-oxide cement in sandstone

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    Take the Accessory Minerals test

    Return to top

    Return to introduction

    http://web2.ges.gla.ac.uk/~minerals/Intro.htmhttp://web2.ges.gla.ac.uk/~minerals/Accessory_minerals.htm#Tophttp://web2.ges.gla.ac.uk/~minerals/Accessory_minerals_assessment.htm