Anisotropism

 

 

 

Anisotropism is an optical effect where certain minerals appear to change colors as they are rotated while illuminated by cross polarized light.  These minerals are often, but not always, opaque and typically have a metallic or sub-metallic luster. The gems below are all anisotropic. See more information below.

 

Arsenic

 

Arsenopyrite

 

Cassiterite

 

Covellite
Arsenic

 

Arsenopyrite

 

Cassiterite

 

Covellite

 

 

 

 

 

 

 

Cuprite

 

Ferberite

 

Hematite

 

Hubnerite
Cuprite

 

Ferberite

 

Hematite

 

Hübnerite

 

 

 

 

 

 

 

Ilmenite

 

Lapis-Lazuli

 

Lepidicrocite inclusions in Quartz

 

Marcasite
Ilmenite

 

Lazurite

 

Lepidocrocite (incl.)

 

Marcasite

 

 

 

 

 

 

Orpiment

 

Pyrargyrite

 

Pyrrhotite

 

Realgar
Orpiment

 

Pyrargyrite

 

Pyrrhotite

 

Realgar

 

 

 

 

 

 

 

Rutile

 

Tenorite

 

Zincite

 

 

Rutile

 

Tenorite

 

Zincite

 

 

 

Anisotropy is the variation in color or intensity of an opaque mineral viewed under cross polarized light. Anisotropism is an optical effect where the mineral appears to change colors as it is rotated while illuminated by cross 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 cross 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 cross polarizers.
  •  Anisotropic colors, when obvious, are characteristic of the mineral.
  • Some, but not all, isotropic minerals are anomalously anisotropic (eg. pyrite).

 


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