(Typomorphic features of celadonite structure.

The 1M celadonite from ferruginous metasomatic silicate rocks of the Krivoi Rog, Ukraine, has a high Fe3+ content in the octahedral layer, with a 5.21-5.23, b 9.03-9.05, c 10.10-10.15 A, beta 100o30'-100o50'. This presence of Fe3+ in the octahedral layer determines the unique structure of the dioctahedral phyllosilicates. The degree of structural perfection of celadonite is a sensitive indicator of the conditions of crystallization. -R.A.H.

Authors
Zhukhlistov A.P. 1 , Zvyagin B.B. 1 , Lazarenko E.K. 1 , Pavlishin V.I. 1
Journal
Zapiski Vsesoyuznogo Mineralogicheskogo Obshchestva
Number of issue
3
Language
Russian
Pages
348-353
Status
Published
Link
External link
Volume
108
Year
1979
Organizations
  • 1 Inst. Geologii Rudn. Mestorozliden Petrographii Mineralogii Geokhimiya, Moscow, USSR.
Date of creation
19.10.2018
Date of change
19.10.2018
Short link
https://repository.rudn.ru/en/records/article/record/1603/
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