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A Note on the Crystallography of Epidote

Published online by Cambridge University Press:  14 March 2018

J. Hornstra
Affiliation:
Kristallografisch Instituut, Rijks-Universiteit, Groningen, Holland
P. Terpstra
Affiliation:
Kristallografisch Instituut, Rijks-Universiteit, Groningen, Holland

Extract

In any monoclinic crystal, the zone–axis [uvw] is perpendicular to the plane (hkl) if u/(hc2–lac cos β) = v/(kc2a2sin2β) = w/(la2–hac cos β). In particular, the normal to the face (100) is quasi–parallel to the zoneaxis [r01̄] if c/(a cosβ) approximates to a rational number r.

Epidote has a:b:c = 1•5807:1:1•8057,β 115° 24', and is often twinned on a(100). G. Friedel describes and explains these twins in terms of a pseudo–normal zone–axis [301], with an obliquity of 3° and a twinindex 3. But the choice of a pseudo–normal zone–axis is necessarily arbitrary, since it is always possible to find a rational zone–axis making an angle with any given face–normal less than any assigned angle δ: though the indices of such an axis may involve large numbers.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1950

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References

Page 68 note 1. Friedel, G., Bull. Soc. Industrie Minérale, 1904, ser. 4, vols. 3-4, p. 399.Google Scholar

Page 68 note 2. O. Matthes, Neues Jahrb. Min., Abt. A, 1928, Beilage-Band 56, p. 418. [M.A. 4-88.]

Page 71 note 1. Bricking, H., Zeits. Kryst. Min., 1878, vol. 2, pp. 339 and 409 Google Scholar.