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guide to thin section microscopy - Mineralogical Society of America

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Guide <strong>to</strong> Thin Section Microscopy<br />

Scheme for mineral identification<br />

5. Routine mineral determination<br />

Mineral colour<br />

Observations in plane-polarized light mode<br />

Colour <strong>to</strong>ne and intensity,<br />

Colour distribution<br />

Pleochroism<br />

Ch. 4.2.1<br />

Light refraction<br />

Relief, chagrin,<br />

Becke-Line:<br />

Refractive index n<br />

Ch. 4.2.2<br />

Pleochroism, changing relief/chagrin = anisotropic<br />

non-cubic minerals<br />

Morphological<br />

characteristics<br />

Grain form, twins,<br />

fractures, cleavage,<br />

zoning, inclusions,<br />

decomposition, alteration<br />

Ch. 3.1 – 3.4<br />

Observations in crossed polarizers mode<br />

Mineral <strong>section</strong> remains black during rotation <strong>of</strong> stage<br />

a. isotropic<br />

no optic axis interference figure<br />

Glasses; cubic minerals<br />

b. anisotropic: Section ⊥ optic axis<br />

optic axis interference figure:<br />

uniaxial, biaxial; Ch. 4.2.5<br />

non-cubic minerals<br />

Mineral <strong>section</strong> changes from bright <strong>to</strong> dark during stage rotation = anisotropic<br />

Interference colour<br />

low, high<br />

normal, anomalous<br />

Ch. 4.2.3<br />

Sections <strong>of</strong> maximum<br />

interference colour<br />

Sections with low<br />

interference colour<br />

Morphological features<br />

Twins and intergrowths;<br />

Subgrains, undulose extinction;<br />

Zoning, unmixing;<br />

Brewster crosses in spherulites<br />

Ch. 3.3, 3.4, 4.2.3<br />

Raith, Raase & Reinhardt – February 2012<br />

birefringence<br />

Ch. 4.2.3<br />

orthorhombic<br />

monoclinic<br />

Extinction<br />

straight<br />

symmetrical<br />

inclined<br />

a. optically uniaxial, optic sign<br />

Sections ~ ⊥ opt. axis<br />

b. optically biaxial, optic sign<br />

Sections ~ ⊥ acute bisectrix, or ⊥ optic axis<br />

Ch. 4.2.5<br />

hexagonal<br />

trigonal<br />

tetragonal<br />

triclinic<br />

Sign <strong>of</strong> elongation: l (+), l (-)<br />

Ch. 4.2.4<br />

Extinction angle ε<br />

Ch. 4.2.4<br />

127

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