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The crystal structure of averievite, Cu5O2(VO4)2·nMX : Comparison with related compounds. / Starova, G. L.; Krivovichev, S. V.; Fundamensky, V. S.; Filatov, S. K.

в: Mineralogical Magazine, Том 61, № 3, 01.06.1997, стр. 441-446.

Результаты исследований: Научные публикации в периодических изданияхОбзорная статьяРецензирование

Harvard

Starova, GL, Krivovichev, SV, Fundamensky, VS & Filatov, SK 1997, 'The crystal structure of averievite, Cu5O2(VO4)2·nMX: Comparison with related compounds', Mineralogical Magazine, Том. 61, № 3, стр. 441-446.

APA

Vancouver

Author

Starova, G. L. ; Krivovichev, S. V. ; Fundamensky, V. S. ; Filatov, S. K. / The crystal structure of averievite, Cu5O2(VO4)2·nMX : Comparison with related compounds. в: Mineralogical Magazine. 1997 ; Том 61, № 3. стр. 441-446.

BibTeX

@article{19040d8c043c49d4bd6334cae98e1cc4,
title = "The crystal structure of averievite, Cu5O2(VO4)2·nMX: Comparison with related compounds",
abstract = "The crystal structure of averievite, Cu5O2(VO4)2·nMX has been determined. Trigonal system, space group P3, a = 6.375(1), c = 8.399(1) {\AA}, V = 295.6(1) {\AA}3, Z = 1, Dx = 4.01(1) g/cm3. The atomic arrangement is characterized by infinite nets parallel to (001) composed of [OCu4]6+ tetrahedra linked via corners in hexagonal rings. The bases of neigbouring tetrahedra are in one plane and their non-shared corners are turned to the opposite sides. The [VO4]3- tetrahedra are attached to the bases of [OCu4] tetrahedra. There are large (R >3.2 {\AA}) channels in the structure where large molecular particles can enter. The comparison of the averievite structure with related compounds (in particular, copper oxovanadates) is given from the point of view of [OT4] polyion crystal chemistry.",
keywords = "Averievite, Crystal structure",
author = "Starova, {G. L.} and Krivovichev, {S. V.} and Fundamensky, {V. S.} and Filatov, {S. K.}",
year = "1997",
month = jun,
day = "1",
language = "English",
volume = "61",
pages = "441--446",
journal = "Mineralogical Magazine",
issn = "0026-461X",
publisher = "Mineralogical Society",
number = "3",

}

RIS

TY - JOUR

T1 - The crystal structure of averievite, Cu5O2(VO4)2·nMX

T2 - Comparison with related compounds

AU - Starova, G. L.

AU - Krivovichev, S. V.

AU - Fundamensky, V. S.

AU - Filatov, S. K.

PY - 1997/6/1

Y1 - 1997/6/1

N2 - The crystal structure of averievite, Cu5O2(VO4)2·nMX has been determined. Trigonal system, space group P3, a = 6.375(1), c = 8.399(1) Å, V = 295.6(1) Å3, Z = 1, Dx = 4.01(1) g/cm3. The atomic arrangement is characterized by infinite nets parallel to (001) composed of [OCu4]6+ tetrahedra linked via corners in hexagonal rings. The bases of neigbouring tetrahedra are in one plane and their non-shared corners are turned to the opposite sides. The [VO4]3- tetrahedra are attached to the bases of [OCu4] tetrahedra. There are large (R >3.2 Å) channels in the structure where large molecular particles can enter. The comparison of the averievite structure with related compounds (in particular, copper oxovanadates) is given from the point of view of [OT4] polyion crystal chemistry.

AB - The crystal structure of averievite, Cu5O2(VO4)2·nMX has been determined. Trigonal system, space group P3, a = 6.375(1), c = 8.399(1) Å, V = 295.6(1) Å3, Z = 1, Dx = 4.01(1) g/cm3. The atomic arrangement is characterized by infinite nets parallel to (001) composed of [OCu4]6+ tetrahedra linked via corners in hexagonal rings. The bases of neigbouring tetrahedra are in one plane and their non-shared corners are turned to the opposite sides. The [VO4]3- tetrahedra are attached to the bases of [OCu4] tetrahedra. There are large (R >3.2 Å) channels in the structure where large molecular particles can enter. The comparison of the averievite structure with related compounds (in particular, copper oxovanadates) is given from the point of view of [OT4] polyion crystal chemistry.

KW - Averievite

KW - Crystal structure

UR - http://www.scopus.com/inward/record.url?scp=0030698397&partnerID=8YFLogxK

M3 - Review article

AN - SCOPUS:0030698397

VL - 61

SP - 441

EP - 446

JO - Mineralogical Magazine

JF - Mineralogical Magazine

SN - 0026-461X

IS - 3

ER -

ID: 53955540