IR, RU, PT, AND PD IN BASALTS AND KOMATIITES: NEW CONSTRAINTS FOR THE GEOCHEMICAL BEHAVIOR OF THE PLATINUM-GROUP ELEMENTS IN THE MANTLE

dc.contributor.authorRehkämper M.
dc.contributor.authorHalliday A.N.
dc.contributor.authorLee D.C.
dc.contributor.authorFitton J.G.
dc.contributor.authorWieneke M.
dc.contributor.authorArndt N.T.
dc.date.accessioned2021-01-12T11:09:46Z
dc.date.available2021-01-12T11:09:46Z
dc.date.issued1999
dc.description.abstractThe concentrations of the platinum-group elements (PGE) Ir, Ru, Pt, and Pd were determined in 18 mantle-derived basalts from a variety of tectonic settings and six komatiites from three locations. All analyses were performed using isotope dilution, Carius tube digestion, and the precise technique of multiple collector inductively coupled plasma mass spectrometry. Multiple analyses of two samples indicate external reproducibilities, based upon separate dissolutions, of approximately 2–9% in the ppt to ppb concentration range.
dc.identifierhttps://elibrary.ru/item.asp?id=13812238
dc.identifier.citationGeochimica et Cosmochimica Acta, 1999, , 22, 3915-3934
dc.identifier.issn0016-7037
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/22771
dc.titleIR, RU, PT, AND PD IN BASALTS AND KOMATIITES: NEW CONSTRAINTS FOR THE GEOCHEMICAL BEHAVIOR OF THE PLATINUM-GROUP ELEMENTS IN THE MANTLE
dc.typeСтатья

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