Chlo Rite

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  • 7/29/2019 Chlo Rite

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    22/5/13 Chlorite

    web2.ges.gla.ac.uk/~minerals/Chlorite.htm 1/5

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    Chlorite

    Mineral structure: Sheet silicate

    Common mineral in Pelites (Low grade), Metabasic rocks (low grade), or the alteration products of Fe-

    rich minerals

    Rock-forming minerals associated with Chlorite: Quartz, Muscovite, Amphibole, Biotite

    Chlorite in Schist

    Analyser out Analyser in

    Key optical features of chlorite in thin section:

    Green to Palegreen

    Pleochroic

    Single cleavage and straightextinction

    ModerateRelief

    Low order (almost isotopic) and anomalous interference colours (see below)

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

    Amphibole (typically strongly coloured, higher relief, two cleavages, inclined extinction),

    Chlorite replacing garnet (and biotite (low centre of image))

    Analyser out Analyser in

    http://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Biotite.htmhttp://web2.ges.gla.ac.uk/~minerals/Garnet.htmhttp://web2.ges.gla.ac.uk/~minerals/Amphibole.htmhttp://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#Extinctionhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Cleavagehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Pleochroichttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Colourhttp://web2.ges.gla.ac.uk/~minerals/Biotite.htmhttp://web2.ges.gla.ac.uk/~minerals/Amphibole.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Intro.htm
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    Chlorite replacing amphibole

    Analyser out Analyser in

    Note: Chlorite often forms as an alteration product of minerals (biotite,amphibole,pyroxene,garnet)

    Chlorite pleochroism and cleavage

    Analyser out Stage rotated by 90 0

    Distinguishing chlorite from amphibole

    Analyser out Analyser in

    http://web2.ges.gla.ac.uk/~minerals/Amphibole.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Cleavagehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Pleochroismhttp://web2.ges.gla.ac.uk/~minerals/Garnet.htmhttp://web2.ges.gla.ac.uk/~minerals/Pyroxene.htmhttp://web2.ges.gla.ac.uk/~minerals/Amphibole.htmhttp://web2.ges.gla.ac.uk/~minerals/Biotite.htmhttp://web2.ges.gla.ac.uk/~minerals/Amphibole.htm
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    Note: Chlorite is palergreen, has lowerreliefand lower orderinterference colours

    Anomalous interference colours in chlorite

    Analyser out Analyser in

    Note: Chlorite interference colours typically dark, anomalous blue or brown. Chlorite has straight

    extinction but due to the dark interference colours this is sometimes difficult to confirm.

    Chlorite in slate (fine grained) with colourless muscovite, quartz and plagioclase

    Analyser out Analyser in

    http://web2.ges.gla.ac.uk/~minerals/Plagioclase.htmhttp://web2.ges.gla.ac.uk/~minerals/Quartz.htmhttp://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Extinctionhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://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: Low order interference colours of chlorite tend to be difficult to pick out in fine grained low grade

    rocks. Due to chlorite fine grain size in low grade metamorphic rocks the green colourwith analyser out

    may be not obvious!

    Chlorite shape

    Analyser out Analyser in

    Note: As a sheet silicate with a single goodcleavage chlorite tends to form well shaped individual

    crystals. When chlorite forms as an alterationproduct of other large minerals stable at higher

    temperature it often forms clusters or clumps of finer grainsize.

    Folded chlorite-rich fabric (with high order interference colour muscovite)

    Analyser out Analyser in

    Note: Cleavage domains with muscovite in similar orientation

    Chlorite as a low temperature hydrothermal mineral often fills veins and amygdales

    (below)

    http://web2.ges.gla.ac.uk/~minerals/Muscovite.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interferencehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Alterationhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Cleavagehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Shapehttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Colour
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    Note: anomalous dark blue interference colours with analyser in

    Aligned flakes of chlorite in amygdales

    Analyser in

    Take the Chlorite test

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    Return to introduction

    http://web2.ges.gla.ac.uk/~minerals/Intro.htmhttp://web2.ges.gla.ac.uk/~minerals/Chlorite.htm#Tophttp://web2.ges.gla.ac.uk/~minerals/Chlorite_assessment.htmhttp://web2.ges.gla.ac.uk/~minerals/Basic%20Properties.htm#Interference