ON THE FORMATION OF PERIDOTITE-DERIVED OS-RICH PGE ALLOYS

dc.contributor.author	Brenker F.E.
dc.contributor.author	Meibom A.
dc.contributor.author	Frei R.
dc.date.accessioned	2021-12-02T03:58:08Z
dc.date.available	2021-12-02T03:58:08Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=14467638
dc.identifier.citation	American Mineralogist, 2003, 88, 11-12 Part 1, 1731-1740
dc.identifier.issn	0003-004X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/32644
dc.description.abstract	Osmium-rich Pt group element (PGE) alloys occur worldwide in association with chromite in ultramafic (peridotite) complexes. It has been suggested that these Os-rich alloys formed under extreme P-T conditions in the lowermost mantle, before the metallic core of the Earth formed, or later, in the outer core, and have been transported to the upper mantle as xenoliths in deep-rooted mantle plumes.
dc.title	ON THE FORMATION OF PERIDOTITE-DERIVED OS-RICH PGE ALLOYS
dc.type	Статья

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