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The crystal structure of tetraferriphlogopite and tetraferribiotite. / Semenova, T. F.; Rozhdestvenskaya, I. V.; Frank-Kamenetsky, V. A.; Pavlishin, V. I.

в: Mineralogicheskii Zhurnal, Том 5, № 1, 01.01.1983, стр. 41-49.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Semenova, TF, Rozhdestvenskaya, IV, Frank-Kamenetsky, VA & Pavlishin, VI 1983, 'The crystal structure of tetraferriphlogopite and tetraferribiotite.', Mineralogicheskii Zhurnal, Том. 5, № 1, стр. 41-49.

APA

Semenova, T. F., Rozhdestvenskaya, I. V., Frank-Kamenetsky, V. A., & Pavlishin, V. I. (1983). The crystal structure of tetraferriphlogopite and tetraferribiotite. Mineralogicheskii Zhurnal, 5(1), 41-49.

Vancouver

Semenova TF, Rozhdestvenskaya IV, Frank-Kamenetsky VA, Pavlishin VI. The crystal structure of tetraferriphlogopite and tetraferribiotite. Mineralogicheskii Zhurnal. 1983 Янв. 1;5(1):41-49.

Author

Semenova, T. F. ; Rozhdestvenskaya, I. V. ; Frank-Kamenetsky, V. A. ; Pavlishin, V. I. / The crystal structure of tetraferriphlogopite and tetraferribiotite. в: Mineralogicheskii Zhurnal. 1983 ; Том 5, № 1. стр. 41-49.

BibTeX

@article{30415d26f4b74e6bbc23590b399dff4c,
title = "The crystal structure of tetraferriphlogopite and tetraferribiotite.",
abstract = "The structures of natural intermediate tetraferriphlogopite from the Kovdor iron-ore deposit and tetraferribiotite from the Krivoi Rog Basin (both in the Ukrainian Shield) have been refined. A three-dimensional set of intensities has been obtained using an automatic single-crystal diffractometer. The structure of intermediate tetraferriphlogopite has been refined to R 0.059, from 1059 observed reflections, and that of tetraferribiotite to R 0.079, from 534 reflections. The average bond lengths in intermediate tetraferriphlogopite are: T-O 0.1665, M1-O,OH = M2- O,OH 0.2085, and inner K-O 0.2973 nm; the angle of rotation of the tetrahedra alpha = 9.24o. In tetraferribiotite, T-O 0.1679, M1-O,OH 0.2111, M2-O,OH 0.2098, K-O 0.2974 nm and alpha 8.96o. In both structures, the OH group is situated along the c* axis; the bond length in the two minerals is 0.0792 and 0.0887 nm. The pattern of distortions in the tetraferribiotite structure is analogous to that identified in phlogopite.-D.A.B.",
author = "Semenova, {T. F.} and Rozhdestvenskaya, {I. V.} and Frank-Kamenetsky, {V. A.} and Pavlishin, {V. I.}",
year = "1983",
month = jan,
day = "1",
language = "русский",
volume = "5",
pages = "41--49",
journal = "МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ",
issn = "0204-3548",
publisher = "Институт геохимии, минералогии и рудообразования НАН Украины",
number = "1",

}

RIS

TY - JOUR

T1 - The crystal structure of tetraferriphlogopite and tetraferribiotite.

AU - Semenova, T. F.

AU - Rozhdestvenskaya, I. V.

AU - Frank-Kamenetsky, V. A.

AU - Pavlishin, V. I.

PY - 1983/1/1

Y1 - 1983/1/1

N2 - The structures of natural intermediate tetraferriphlogopite from the Kovdor iron-ore deposit and tetraferribiotite from the Krivoi Rog Basin (both in the Ukrainian Shield) have been refined. A three-dimensional set of intensities has been obtained using an automatic single-crystal diffractometer. The structure of intermediate tetraferriphlogopite has been refined to R 0.059, from 1059 observed reflections, and that of tetraferribiotite to R 0.079, from 534 reflections. The average bond lengths in intermediate tetraferriphlogopite are: T-O 0.1665, M1-O,OH = M2- O,OH 0.2085, and inner K-O 0.2973 nm; the angle of rotation of the tetrahedra alpha = 9.24o. In tetraferribiotite, T-O 0.1679, M1-O,OH 0.2111, M2-O,OH 0.2098, K-O 0.2974 nm and alpha 8.96o. In both structures, the OH group is situated along the c* axis; the bond length in the two minerals is 0.0792 and 0.0887 nm. The pattern of distortions in the tetraferribiotite structure is analogous to that identified in phlogopite.-D.A.B.

AB - The structures of natural intermediate tetraferriphlogopite from the Kovdor iron-ore deposit and tetraferribiotite from the Krivoi Rog Basin (both in the Ukrainian Shield) have been refined. A three-dimensional set of intensities has been obtained using an automatic single-crystal diffractometer. The structure of intermediate tetraferriphlogopite has been refined to R 0.059, from 1059 observed reflections, and that of tetraferribiotite to R 0.079, from 534 reflections. The average bond lengths in intermediate tetraferriphlogopite are: T-O 0.1665, M1-O,OH = M2- O,OH 0.2085, and inner K-O 0.2973 nm; the angle of rotation of the tetrahedra alpha = 9.24o. In tetraferribiotite, T-O 0.1679, M1-O,OH 0.2111, M2-O,OH 0.2098, K-O 0.2974 nm and alpha 8.96o. In both structures, the OH group is situated along the c* axis; the bond length in the two minerals is 0.0792 and 0.0887 nm. The pattern of distortions in the tetraferribiotite structure is analogous to that identified in phlogopite.-D.A.B.

UR - http://www.scopus.com/inward/record.url?scp=0021034432&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0021034432

VL - 5

SP - 41

EP - 49

JO - МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ

JF - МИНЕРАЛОГИЧЕСКИЙ ЖУРНАЛ

SN - 0204-3548

IS - 1

ER -

ID: 50027137