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Vol 37 Iss. 3
Pages:
105-108
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RUS
Article

X-ray study of deformed mica

Authors:
E. O. Shvaikovskaya
A. I. Nikolaeva
T. D. Shalyt
Date submitted:
1960-09-25
Date accepted:
1960-11-23
Date published:
1961-09-04

Abstract

Mica is an extensive group of minerals characterized by perfect {001} cleavage, i.e. the ability to easily split into very thin sheets with a flat surface parallel to the face of the third pinacoid. Muscovite and phlogopite have the most important industrial value. Mica have high electrical characteristics, incombustibility and great mechanical strength, they are also thermally and chemically stable, and are not very hygroscopic. Mica crystallize in a monoclinic system, approaching hexagonal . forms. Under the influence of mechanical effects mica deform, lose their properties and become unsuitable for industrial purposes, so, of course, the study of deformed mica is paid much attention.

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References

  1. Lashev E. К. Mica. Promstroizdat, 1948.
  2. Shvaikovskaya E. О. X-ray study of distortions of the crystal lattice of mineral fibers. Proc. AS USSR, series of physics, 1958, vol. XX, No. 6.
  3. Shvaikovskaya E. О. X-ray study of distortions of the crystal lattice of asbestos fibers. Journal of Mining Institute, 1958, vol. XXXVI, iss. 3.
  4. Pinnе T. Вег. Verharidl. Saxon. Academy of Sciences Leipzig. Math. natural science. KL, 1915, No. 17, S. 223.

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