REFINEMENT OF THE MANGAN-NEPTUNITE CRYSTAL STRUCTURE
| dc.contributor.author | Zolotarev Jr.A.A. | |
| dc.contributor.author | Krivovichev S.V. | |
| dc.contributor.author | Yakovenchuk V.N. | |
| dc.date.accessioned | 2026-10-19T05:21:34Z | |
| dc.date.issued | 2007 | |
| dc.description.abstract | The crystal structure of mangan-neptunite, a manganese analogue of neptunite, has been refined in two space groups (Cc and C2/c). The mineral is monoclinic, with the correct space group Cc; the unit-cell dimensions are: a = 16.4821(6), b = 12.5195(4), c = 10.0292(3) Å, β = 115.474(1)°, and V = 1868.31 Å3. The crystal structure has been refined to R 1 = 0.0307 (wR 2 = 0.0901) on the basis of 4892 observed reflections with |F hkl | ≥ 4σ|F hkl |. The most plausible acentric model is caused by the Ti- and (Fe, Mn, Mg)-ordering in the structure. Ti-octahedrons are strongly distorted and consist of short bond Ti-O (1.7 Å), one long bond (2.2 Å), and four equal bonds (2.0 Å). Fe-octahedrons are regularly shaped, with all Fe-O bonds being approximately identical. | |
| dc.identifier | https://elibrary.ru/item.asp?id=13551781 | |
| dc.identifier.citation | Geology of Ore Deposits, 2007, 49, 8, 835-838 | |
| dc.identifier.doi | 10.1134/S1075701507080181 | |
| dc.identifier.issn | 1075-7015 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/55081 | |
| dc.title | REFINEMENT OF THE MANGAN-NEPTUNITE CRYSTAL STRUCTURE | |
| dc.type | Статья |
Файлы
Оригинальный пакет
1 - 1 из 1