THE CRYSTAL STRUCTURE OF FENAKSITE K2NA2FE2SI8O20

dc.contributor.author	Rozhdestvenskaya I.V.
dc.contributor.author	Bannova I.I.
dc.contributor.author	Nikishova L.V.
dc.contributor.author	Soboleva T.V.
dc.date.accessioned	2022-08-14T03:31:08Z
dc.date.available	2022-08-14T03:31:08Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13470616
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 1029-1033
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38524
dc.description.abstract	Fenaksite K2Na2Fe2Si8O20 was discovered by M.D. Dorfman in Khibiny in 1959. Its crystal structure was determined and refined with the application of photomethod up to R = 0.148. We studied the stucture of synthetic fenaksite based on XRD data. The results obtained made it possible to refine the structure of this mineral and compare it with the topologically similar structures of agrellites.
dc.title	THE CRYSTAL STRUCTURE OF FENAKSITE K2NA2FE2SI8O20
dc.type	Статья

Files in this item

Files	Size	Format	View
There are no files associated with this item.