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 />
Optical properties: basic principles<br />
4.1.2 Isotropy and anisotropy<br />
Isotropic materials<br />
Optically isotropic substances such as gases, liquids, glasses and the highly symmetric cubic<br />
minerals show optical behaviour that is independent <strong>of</strong> the direction <strong>of</strong> light propagation.<br />
This means, their optical properties (light velocity, refractive index and colour) are identical<br />
in all directions.<br />
The three-dimensional propagation <strong>of</strong> light in an isotropic material can be presented<br />
graphically as 3-D models for wave or ray velocity and for refractive index, both <strong>of</strong> which are<br />
spheres (Fig. 4-3). The model preferred by mineralogists is the optical indicatrix, which<br />
describes the refractive index as a direction-dependent variable.<br />
Figure 4-3. Isotropic substances; 3D surfaces <strong>of</strong> v and n<br />
Raith, Raase & Reinhardt – February 2012<br />
A. Ray velocity surface: For each ray direction, the velocity value is represented by a specific distance<br />
from a chosen origin (v = 0). The geometric form representing all directions <strong>of</strong> ray propagation is a<br />
sphere with radius v.<br />
B. Indicatrix: For each ray direction, the refractive index is represented by a specific distance from a<br />
chosen origin and is marked <strong>of</strong>f parallel <strong>to</strong> the vibration direction and perpendicular <strong>to</strong> the ray<br />
propagation direction. The geometric form representing the refractive index for all ray propagation<br />
directions is a sphere with radius n. Each ray propagation direction has an infinite number <strong>of</strong> potential<br />
vibration directions.<br />
In <strong>thin</strong> <strong>section</strong> <strong>microscopy</strong>, glasses and cubic minerals generally show a single specific<br />
refractive index and colour independent <strong>of</strong> orientation (Fig. 4-4). An indication <strong>of</strong> crystal<br />
orientation in <strong>thin</strong> <strong>section</strong> can therefore only be derived from morphological properties, for<br />
example, crystal outlines or cleavage (Fig. 3-9). Another important characteristic <strong>of</strong> optically<br />
isotropic materials is that light waves do not experience any change in vibration direction.<br />
This means that E-W vibrating plane-polarized light waves maintain their E-W orientation<br />
after passing through the isotropic materials (glass, mineral). Therefore, they are blocked by<br />
the analyzer, which is a N-S oriented polarizer (Fig. 4-4 A,E).<br />
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