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].
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Literature Cited
A. Deo, G. Finch, and F. Charpurey, Proc. Royal Soc. A236, 7, 1204 (1956).
H. van der Merve, New Investigations in Crystallography and Crystallochemistry [Russian translation] (1950).
P. A. Zemyatchenskii, Izv. Imp. Akad. Nauk 541 (1914).
I. E. Kamentsev, Kristallografiya 1, 2, 240 (1956).
D. E. Ovsienko, Problems of Physics of Metals and Metal Science [in Russian] (1953), No. 4.
A. E. Fersman, Selected Works [in Russian] vol. 1, p. 51.
K. P. Yanulov, Doklady Akad. Nauk SSSR 62, 813 (1948).
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Kamentsev, I.E. (1959). The Crystallization of KI in Contact with Biotite and Muscovite. In: Shubnikov, A.V., Sheftal’, N.N. (eds) Growth of Crystals. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-0471-6_8
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DOI: https://doi.org/10.1007/978-1-4757-0471-6_8
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