STRUCTURAL FEATURES AND NMR195PT SPECTROSCOPY OF COOPERITE MONOCRYSTALS (NATURAL PTS)

Ivanov A.V.; Palazhchenko V.I.; Strikha V.E.; Antzutkin O.N.; Forsling W.

dc.contributor.author	Ivanov A.V.
dc.contributor.author	Palazhchenko V.I.
dc.contributor.author	Strikha V.E.
dc.contributor.author	Antzutkin O.N.
dc.contributor.author	Forsling W.
dc.date.accessioned	2024-11-02T11:07:59Z
dc.date.available	2024-11-02T11:07:59Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13524332
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1141-1144
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46387
dc.description.abstract	Cooperite (natural PtS)—a platinum group mineral—is a main platinum source in Cu–Ni sulfide ores. Cooperite commonly crystallizes in two morphological modifications: (i) irregular grains; (ii) less frequent micrometric and submicrometric prismatic crystals associated with Fe-platinum and Os–Ir minerals, which could be formed at high temperatures and, consequently, high chemical activity of sulfur. In this work, cooperite monocrystals (natural PtS) are characterized in detail with X-ray diffraction, microprobe, and high-resolution scanning electron microscopy. For the first time, we demonstrate the possibility of the application of static and MAS 195Pt spectroscopy for the study of natural platinum minerals.
dc.subject	cooperite
dc.title	STRUCTURAL FEATURES AND NMR195PT SPECTROSCOPY OF COOPERITE MONOCRYSTALS (NATURAL PTS)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070312