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Reflected Light Anisotrophism

Anisotrophism is an optical effect where certain minerals appear to change colors as they are rotated while illuminated by crossed polarized light.  These minerals are usually, but not always, opaque; typically have metallic or sub-metallic luster and . See more below.

Anisotropy is the variation in color or intensity of an opaque mineral viewed under crossed polarized light. Anisotropism is an optical effect where the mineral appears to change colors as it is rotated while illuminated by crossed polarized light.

Reflected light microscopy is used to examine opaque minerals to determine the paragenetic relationships between different mineral phases and their identification. Often, the same specimen which is viewed using the light microscope can be analyzed using advanced x-ray and ion microprobe techniques.

The sample (polished thin section, epoxy grain mount, or polished section) is placed in the appropriate reflected light microscope. Anisotrophism is an optical effect where the mineral appears to change colors as it is rotated while illuminated by crossed polarized light. The polarizers are not crossed as in the case to observe reflection pleochroism. 

Isotropic minerals (eg, galena, pyrite) and the basal sections of hexagonal, tetragonal, and trigonal minerals do not show any anisotrophism when rotated in cross polarized light. Minerals which are pleochroic or bireflectant are generally also anisotropic. Care must be taken when observing anisotrophy to follow these rules:

•  Sample is freshly polished and does not have any tarnish.
•  Illumination level is set generally high to view the muted colors under crossed polarizers.
•  Anisotropic colors, when obvious, are characteristic of the mineral.
• Some, but not all, isotropic minerals are anomalously anisotropic (eg. pyrite).