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УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА. / Золотарев Мл., А. А.; Кривовичев, С. В.; Яковенчук, В. Н.

в: ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА, № 1, 2007, стр. 118-123.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Золотарев Мл., АА, Кривовичев, СВ & Яковенчук, ВН 2007, 'УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА', ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА, № 1, стр. 118-123. <http://elibrary.ru/item.asp?id=9474941>

APA

Золотарев Мл., А. А., Кривовичев, С. В., & Яковенчук, В. Н. (2007). УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА. ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА, (1), 118-123. http://elibrary.ru/item.asp?id=9474941

Vancouver

Золотарев Мл. АА, Кривовичев СВ, Яковенчук ВН. УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА. ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА. 2007;(1):118-123.

Author

Золотарев Мл., А. А. ; Кривовичев, С. В. ; Яковенчук, В. Н. / УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА. в: ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА. 2007 ; № 1. стр. 118-123.

BibTeX

@article{4734a95a5cd048eabfd38f80440d17c7,
title = "УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА",
abstract = "Refinement of crystal structure of mangan-neptunite, the manganese analogue of neptunitc, was carried out in the two space groups (Cc and C2/c). The mineral is monoclinic, the correct space group Cc; its unit cell parameters: a = 16.4821 (6), b = 12.5195(4), с = 10.0292 (3) A, p = 115.474( 1)°, V = 1868.31 A3. The crystal structure was refined to Д, = 0.0307 (wR2 = 0.0901) on the base of 4892 observed reflections with \Fhkl\ > 4o|fM;|. The most suitable model is acentric one, that is connected with the Ti- and (Fc, Mn, Mg)-ordering in the structure. Ti-octahcdra are strongly distorted and consist of one short bond Ti-О (1.7 A), one long bond (2.2 A) and four equal bonds (2.0 A). Fc-octahcdrons have regular shape, with all Fc-О bonds approximately equal.",
author = "{Золотарев Мл.}, {А. А.} and Кривовичев, {С. В.} and Яковенчук, {В. Н.}",
year = "2007",
language = "русский",
pages = "118--123",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "1",

}

RIS

TY - JOUR

T1 - УТОЧНЕНИЕ КРИСТАЛЛИЧЕСКОЙ СТРУКТУРЫ МАНГАННЕПТУНИТА

AU - Золотарев Мл., А. А.

AU - Кривовичев, С. В.

AU - Яковенчук, В. Н.

PY - 2007

Y1 - 2007

N2 - Refinement of crystal structure of mangan-neptunite, the manganese analogue of neptunitc, was carried out in the two space groups (Cc and C2/c). The mineral is monoclinic, the correct space group Cc; its unit cell parameters: a = 16.4821 (6), b = 12.5195(4), с = 10.0292 (3) A, p = 115.474( 1)°, V = 1868.31 A3. The crystal structure was refined to Д, = 0.0307 (wR2 = 0.0901) on the base of 4892 observed reflections with \Fhkl\ > 4o|fM;|. The most suitable model is acentric one, that is connected with the Ti- and (Fc, Mn, Mg)-ordering in the structure. Ti-octahcdra are strongly distorted and consist of one short bond Ti-О (1.7 A), one long bond (2.2 A) and four equal bonds (2.0 A). Fc-octahcdrons have regular shape, with all Fc-О bonds approximately equal.

AB - Refinement of crystal structure of mangan-neptunite, the manganese analogue of neptunitc, was carried out in the two space groups (Cc and C2/c). The mineral is monoclinic, the correct space group Cc; its unit cell parameters: a = 16.4821 (6), b = 12.5195(4), с = 10.0292 (3) A, p = 115.474( 1)°, V = 1868.31 A3. The crystal structure was refined to Д, = 0.0307 (wR2 = 0.0901) on the base of 4892 observed reflections with \Fhkl\ > 4o|fM;|. The most suitable model is acentric one, that is connected with the Ti- and (Fc, Mn, Mg)-ordering in the structure. Ti-octahcdra are strongly distorted and consist of one short bond Ti-О (1.7 A), one long bond (2.2 A) and four equal bonds (2.0 A). Fc-octahcdrons have regular shape, with all Fc-О bonds approximately equal.

M3 - статья

SP - 118

EP - 123

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 1

ER -

ID: 5069448