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  • 7/29/2019 Cordier It e

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    22/5/13 Cordierite

    web2.ges.gla.ac.uk/~minerals/Cordierite.htm 1/4

    Return to index minerals Return to introduction

    Cordierite

    Mineral structure: Cyclosilicate

    Common mineral in Pelites (Schists & Gneisses), some GranitesAssociated with low pressure metamorphism

    Rock-forming minerals associated with Cordierite: Biotite, Muscovite, Quartz

    Other index minerals commonly associated with Cordierite: Andalusite, Sillimanite

    Cordierite in Hornfels

    Analyser out Analyser in

    Key optical features of cordierite in thin section:

    Colourless

    Low relief

    No cleavage

    Low orderinterference colours

    Very readily altered, along fractures or at edges of grains

    Simple or multiple twinning

    Yellow pleochroic haloes

    Common minerals that might be confused with cordierite and occur in similar rocks:

    Quartz(no twinning, no alteration, few inclusions)

    Plagioclase(more regular multiple twinning, dusty brown homogeneous alteration)

    K-feldspar(cross-hatched twinning, exsolution, homogeneous alteration)

    Cordierite pleochroic haloes around radioactive accessory minerals

    Analyser out Analyser out

    http://web2.ges.gla.ac.uk/~minerals/Accessory_minerals.htm#Tophttp://web2.ges.gla.ac.uk/~minerals/Plagioclase.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Twinninghttp://web2.ges.gla.ac.uk/~minerals/Adv.htmhttp://web2.ges.gla.ac.uk/~minerals/Intro.htmhttp://web2.ges.gla.ac.uk/~minerals/Accessory_minerals.htm#Tophttp://web2.ges.gla.ac.uk/~minerals/K-Feldspar.htmhttp://web2.ges.gla.ac.uk/~minerals/Plagioclase.htmhttp://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Twinninghttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Alterationhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Cleavagehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Reliefhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Colourhttp://web2.ges.gla.ac.uk/~minerals/Sillimanite.htmhttp://web2.ges.gla.ac.uk/~minerals/Andalusite.htmhttp://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Biotite.htmhttp://web2.ges.gla.ac.uk/~minerals/Intro.htmhttp://web2.ges.gla.ac.uk/~minerals/Adv.htm
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    Cordierite twinning

    Cordierite may show a variety of different types of twinning, from sector twinning of cordierite porphyroblasts,

    simple twinning and multiple twinning of recrystallised matrix porphyroblasts. Twin boundaries often poorly

    defined.

    Analyser in Analyser in

    Note: Sector twinned porphyroblast Note: Simple twinning and marginalalteration

    Analyser in Analyser in

    Note: Multiple TwinningNote: Inclusion-rich occasionally twinned cordierite with more

    regular multiple-twinned smallerplagioclase

    Cordierite alteration to pinite (muscovite and chlorite mix)

    Alteration very common, typically yellow-brown, focussed at margins of cordierite or along fractures.

    Analyser out Analyser in

    http://web2.ges.gla.ac.uk/~minerals/Chlorite.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Alterationhttp://web2.ges.gla.ac.uk/~minerals/Plagioclase.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Alterationhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Twinning
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    22/5/13 Cordierite

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    Note: Alteration along fractures and at margins of cordierite

    Analyser out Analyser in

    Note: Marginal alteration of cordierite porphyroblast

    Analyser in

    Note: Complete alteration of cordierite porphyroblasts produces fine-grained aggregate of muscovite

    and chlorite.

    Cordierite shape

    Analyser out Analyser out

    http://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shape
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    Note: At high grade cordierite forms a matrix phase in gneisses

    Analyser out

    Note: At medium grade cordierite porphyroblasts are common and mineral inclusions typically far more

    abundant than within quartzand feldspar.

    Return to top

    Return to index minerals introduction

    Return to introduction

    http://web2.ges.gla.ac.uk/~minerals/Intro.htmhttp://web2.ges.gla.ac.uk/~minerals/Adv.htmhttp://web2.ges.gla.ac.uk/~minerals/Cordierite.htm#Tophttp://web2.ges.gla.ac.uk/~minerals/Quartz.htm