THE NANOBLOCK STRUCTURE OF NATURAL ISOFERROPLATINUM (PT3FE) AND PROBLEM OF QUASICRYSTALLINE STATE OF SOME PLATINUM GROUP MINERALS

Distler V.V.; Kryachko V.V.; Yudovskaya M.A.; Bityutskaya L.A.; Grechkina M.V.; Bogatikov E.V.

dc.contributor.author	Distler V.V.
dc.contributor.author	Kryachko V.V.
dc.contributor.author	Yudovskaya M.A.
dc.contributor.author	Bityutskaya L.A.
dc.contributor.author	Grechkina M.V.
dc.contributor.author	Bogatikov E.V.
dc.date.accessioned	2024-11-02T11:07:58Z
dc.date.available	2024-11-02T11:07:58Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524329
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 335-338
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46384
dc.description.abstract	Parquet-type nanoblock structure of isoferroplatinum crystals was first discovered with atomic force microscopy (AFM). Fourier and wavelet transforms were applied to the AFM topographic data to reveal the characteristic scales and self-similarity of elements of nanoblock structure, indicating a quasicrystalline structure of isoferroplatinum.
dc.subject	isoferroplatinum
dc.title	THE NANOBLOCK STRUCTURE OF NATURAL ISOFERROPLATINUM (PT3FE) AND PROBLEM OF QUASICRYSTALLINE STATE OF SOME PLATINUM GROUP MINERALS
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06020413