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Vol 38 Iss. 2
Pages:
150-181
Download volume:
RUS
Article
Geology

Simple edge forms of the cubic singony

Authors:
S. Sh. Gendelev
Date submitted:
1960-08-21
Date accepted:
1960-10-07
Date published:
1960-12-01

Abstract

The present communication completes the series of articles by V. I. Mikheev and I. I. Shafranovsky devoted to the complete derivation of all possible edge forms. In the derivation of simple edge forms of the cubic system, we first of all proceed from possible facet combinations. For this purpose we had to enumerate all possible pairwise combinations separately for each of the five kinds of symmetry. The symbols for such combinations are summarized in the table, where the upper horizontal line contains the symbols of the faces of the initial forms, in the planes of which lie the derived edges. The vertical line contains combinations of symbols of those faces, the intersection of which results in edge forms. A number of edge forms with a relatively small number of included edges are the result of intersection of faces of one simple form (from among those indicated in the upper horizontal row of the table); for example, the dodecahedron of the cube.

Область исследования:
Geology
Funding:

None

Go to volume 38

References

  1. Gendelev S. Sh., Shafranovsky I. I. Edge forms of the cubic system. Kristallografiya, 1958, vol. 3, iss. 4. (in Russian)
  2. Gendelev S. Sh. What is an edge form? Zapiski Vsesoyuznogo mineralogicheskogo obshchestva, 1959, issue 1. (in Russian)
  3. Mikheev V. I., Shafranovsky I. I. Edge forms of crystals. Mineralogicheskiy sbornik Lvovskogo geologicheskogo obshchestva, 1955, No. 9. (in Russian)
  4. Mikheev V. I., Shafranovsky I. I. Edge forms of crystals. Communication II. Sbornik “Kristallografiya”, issue 5, Metallurgizdat, 1956. (in Russian)
  5. Fischer E. Einfuhrung in die geometrische Kristallographie. Berlin, 1956.

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