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Vol 119
Pages:
89-95
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RUS
Article

Mineral formation processes and mineral facies

Authors:
S. A. Rudenko
V. Yu. Ashkin
Date submitted:
1988-08-21
Date accepted:
1988-10-02
Date published:
1989-08-15

Abstract

The history of the formation of the doctrine of facies, in the development of which such a significant role belongs to D. V. Nalivkin, is marked, on the one hand, by the expansion of the range of objects covered by this doctrine, and, on the other hand, by a wider and deeper consideration of their features

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References

  1. Geranicheva G. K., Marin Yu B. Causes of morphological variability of zircon // Zap. of the Leningr. Mining Institute. 1968. V. 54, vol. 2. P. 56-67.
  2. Grodnitsky L. L. Evolution of the chemical composition of biotite during the formation of muscovite and muscovite-redcometal pegmatites of Karelia and the Kola Peninsula // Mineral. and Geochemistry of the Precambrian of Karelia / Karelian Branch of the USSR Academy of Sciences. Petrozavodsk, 1970. p. p. 25-40.
  3. Evzikova N. Z. Prospecting crystallomorphology. M.: Nedra, 1984, 143 p.
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  10. Rudenko S. A. Typomorphic features of pegmatite minerals // Minerals - indicators of the peculiarities of their host environment. L.: Nauka, 1975. P. 9-34.
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  17. Ashkin V. Yu., Bogdanova G. N., Persinen A. A. Thermoluminescence of quartz and its practical significance // Physics of Minerals and Problems of Typomorphism: Conference Proceedings / Leningr. Mining Institute. L., 1976. P. 16-30.
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