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

dc.contributor.authorDistler V.V.
dc.contributor.authorKryachko V.V.
dc.contributor.authorYudovskaya M.A.
dc.contributor.authorBityutskaya L.A.
dc.contributor.authorGrechkina M.V.
dc.contributor.authorBogatikov E.V.
dc.date.accessioned2024-11-02T11:07:58Z
dc.date.available2024-11-02T11:07:58Z
dc.date.issued2006
dc.description.abstractParquet-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.identifierhttps://www.elibrary.ru/item.asp?id=13524329
dc.identifier.citationDoklady Earth Sciences, 2006, 407, 2, 335-338
dc.identifier.doi10.1134/S1028334X06020413
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46384
dc.subjectisoferroplatinum
dc.titleTHE NANOBLOCK STRUCTURE OF NATURAL ISOFERROPLATINUM (PT3FE) AND PROBLEM OF QUASICRYSTALLINE STATE OF SOME PLATINUM GROUP MINERALS
dc.typeСтатья

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