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I. Ansheles
I. Ansheles

Articles

Article
Geology
  • Date submitted
    1914-06-27
  • Date accepted
    1914-08-25

On the dispersion of idocrase

Article preview

In the third issue of Fedorov's "Universal Method," in Chapter VII — "Study of Dispersion" — V. V. Nikitin describes idocrase exhibiting sharp dispersion of birefringence. Furthermore, it possesses the property that within a single grain, in its various sections, the magnitude of birefringence varies. As a result, the interference color is not uniform across the entire extent of the idocrase grains. In sections close to parallel to the optical axis — the fourfold axis of symmetry of the crystal — the colors are arranged in bands parallel to each other: the central part of the grain shows white interference color, followed by a band with a mastix-yellow color, then a purple-red one, and finally, the edges of the grain are colored purple-violet.

How to cite: Ansheles I. On the dispersion of idocrase // Journal of Mining Institute. 1914. Vol. 5. Iss. 2-3. p. 224-226.