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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 />

Conoscopy<br />

4.2.5.5 Practical hints for conoscopic observation<br />

Mineral grains that are <strong>to</strong> be investigated conoscopically should meet specific requirements:<br />

a. When using a strongly magnifying objective (M O = 40x, 50x, 63x or oil immersion 100x)<br />

with a large numerical aperture (>0.6), the mineral grain should cover the field <strong>of</strong> view<br />

completely.<br />

b. The mineral grain must not be twinned wi<strong>thin</strong> the observed frame, nor must it show<br />

alteration effects or exsolution phases.<br />

c. The mineral grain should have a suitable orientation.<br />

The procedure <strong>of</strong> obtaining the conoscopic interference figure is carried out as follows:<br />

a. Move the mineral grain in<strong>to</strong> the centre <strong>of</strong> the crosshairs, use a high-magnification objective<br />

(40x minimum) and focus.<br />

b. Open all diaphragms below the stage.<br />

c. Move the condenser in<strong>to</strong> the uppermost position and put the auxiliary condenser in<strong>to</strong> the<br />

light path.<br />

d. Put the analyzer in. Take out the ocular; use a pinhole if included with the microscope,<br />

observe the image in the ocular tube or use the Amici-Bertrand lens and observe the enlarged<br />

image through the ocular. In some microscopes, the Amici-Bertrand lens can be centred and<br />

focused separately, which is important for quantitative work.<br />

e. If the mineral grain is <strong>to</strong>o small <strong>to</strong> fully occupy the field <strong>of</strong> view, an upper diaphragm that<br />

is included in some microscopes can be used <strong>to</strong> reduce or eliminate the periphery around the<br />

grain. If there is no Amici-Bertrand lens with upper diaphragm, a sharp conoscopic interference<br />

figure may be obtained using a simple pinhole in place <strong>of</strong> the ocular.<br />

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

Minerals that are strongly coloured may cause problems for the determination <strong>of</strong> their optic<br />

sign if the first-order red plate is used. Therefore, the quartz wedge is recommended for<br />

compensation, which allows observing the direction <strong>of</strong> movement <strong>of</strong> the isochromes.<br />

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