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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 />

Double refraction<br />

4.2.3 Double refraction<br />

In non-cubic, optically anisotropic crystals, light propagates in all directions as two sets <strong>of</strong><br />

orthogonally vibrating plane-polarized waves, except for directions parallel <strong>to</strong> an optic axis.<br />

The two waves have different velocities (and correspondingly different refractive indices n z '<br />

and n x ').<br />

The specific relation between crystal symmetry and indicatrix in each mineral species defines<br />

the orientation <strong>of</strong> the polarization plane and the refractive index <strong>of</strong> the two waves (Ch. 4.1.2;<br />

Figs. 4-6,7). For every crystal <strong>section</strong> seen in <strong>thin</strong> <strong>section</strong>, these parameters can be derived<br />

from the ellipse created by the inter<strong>section</strong> <strong>of</strong> the indicatrix and the <strong>thin</strong> <strong>section</strong> plane (Fig. 4-<br />

21).<br />

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

Figure 4-21. Relationship between crystal <strong>section</strong>, crystal orientation and indicatrix<br />

orientation using melilite as an example.<br />

80

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