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The Crystallization of KI in Contact with Biotite and Muscovite

  • I. E. Kamentsev

Abstract

Deo et al. [1] have recently studied how oriented crystals are formed on calcite and mica. They found that oriented crystals that formed on one surface continued to grow with the same orientation even if they encountered another surface with a different orientation. However, they concluded that in epitactic growth the surface determined the orientation of the initial nucleus, but that the subsequent growth was not influenced; this contradicts certain experimental data [3].

Keywords

Russian Translation Growth Mechanism Saturated Solution Contact Line Direction Parallel 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

Literature Cited

  1. [1]
    A. Deo, G. Finch, and F. Charpurey, Proc. Royal Soc. A236, 7, 1204 (1956).Google Scholar
  2. [2]
    H. van der Merve, New Investigations in Crystallography and Crystallochemistry [Russian translation] (1950).Google Scholar
  3. [3]
    P. A. Zemyatchenskii, Izv. Imp. Akad. Nauk 541 (1914).Google Scholar
  4. [4]
    I. E. Kamentsev, Kristallografiya 1, 2, 240 (1956).Google Scholar
  5. [5]
    D. E. Ovsienko, Problems of Physics of Metals and Metal Science [in Russian] (1953), No. 4.Google Scholar
  6. [6]
    A. E. Fersman, Selected Works [in Russian] vol. 1, p. 51.Google Scholar
  7. [7]
    K. P. Yanulov, Doklady Akad. Nauk SSSR 62, 813 (1948).Google Scholar
  8. [8]
    M. Royer, Bull. Soc. France Min. 77, 1004 (1954).Google Scholar

Copyright information

© Consultants Bureau, Inc. 1959

Authors and Affiliations

  • I. E. Kamentsev
    • 1
  1. 1.Department of CrystallizationZhdanov State UniversityLeningradRussia

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