guide to thin section microscopy - Mineralogical Society of America
guide to thin section microscopy - Mineralogical Society of America
guide to thin section microscopy - Mineralogical Society of America
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Guide <strong>to</strong> Thin Section Microscopy<br />
Double refraction<br />
4.2.3.2 Observation with analyzer inserted (crossed-polarizers mode)<br />
Extinction behaviour: The rotation <strong>of</strong> a birefringent crystal <strong>section</strong> between crossed<br />
polarizers involves a periodic change between a bright image and a dark image. A full<br />
rotation <strong>of</strong> the stage involves four extinction positions separated by 90˚ and four bright<br />
images in between (Fig. 4-23). The four orientations <strong>of</strong> maximum brightness are also referred<br />
<strong>to</strong> as diagonal positions.<br />
Figure 4-23. Extinction positions and diagonal positions <strong>of</strong> a quartz grain during a 360˚<br />
rotation <strong>of</strong> the stage.<br />
Raith, Raase & Reinhardt – February 2012<br />
In the extinction position the E-W vibrating waves leaving the polarizer are exactly parallel<br />
<strong>to</strong> one <strong>of</strong> the two possible vibration directions <strong>of</strong> the crystal (Fig. 4-23). Hence, the waves are<br />
not split up and pass the mineral without any change in vibration direction as E-W vibrating<br />
waves which propagate with the velocity specific <strong>to</strong> that direction in the crystal. Taking the<br />
optically uniaxial quartz as an example, either the E- or the O-waves with the refractive<br />
indices n e ' resp. n o are parallel <strong>to</strong> the polarizer. In the general case <strong>of</strong> an anisotropic mineral,<br />
the waves are those that relate <strong>to</strong> the refractive indices n z ' and n x '. After leaving the crystal,<br />
the E-W vibrating waves are blocked by the N-S-oriented analyzer, and the crystal appears<br />
black.<br />
If the crystal is rotated out <strong>of</strong> the extinction position, the plane <strong>of</strong> polarisation <strong>of</strong> the light<br />
entering the crystal is no longer parallel <strong>to</strong> any <strong>of</strong> the principal vibration directions in the<br />
crystal (n o , n e ', n z ', n x '). The E-W vibrating waves leaving the polarizer are therefore split up<br />
in the crystal in<strong>to</strong> two orthogonally vibrating waves with refractive indices n e ' and n o resp. n z '<br />
and n x ' in the general case <strong>of</strong> an anisotropic mineral (Fig. 4-23,24). As light enters the crystal,<br />
the relative amplitudes a 1 and a 2 <strong>of</strong> the two newly generated waves depend entirely on the<br />
orientation <strong>of</strong> n x ' and n z ' (or n o and n e ') with respect <strong>to</strong> the polarizer (Fig. 4-24, bot<strong>to</strong>m row).<br />
At small angles, one <strong>of</strong> the two waves very much dominates in terms <strong>of</strong> light intensity. In<br />
the 45° diagonal position the a 1 and a 2 amplitudes are identical. However, without the analyzer<br />
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