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- W2032296911 abstract "Les mineraux du groupe du platine provenant du complexe de Konder, ultrabasique, alcalin et zone, situe a l'est du bouclier d'Aldan, en Russie orientale, sont surtout representes par l'isoferroplatine, formeen deux generations, les deux ayant des teneurs en fer allant de 7.5 a 11.5% (poids). Une generation de haute temperature est saturee avec les autres elements du groupe du platine sous forme d'impuretes: jusqu'a 5.3% Ir, 2.9% Os, et 1.8% Rh (base ponderale). En revanche, l'isoferroplatine tardif contient moins de 1.9% Ir, 1.0% Os, et 0.6% Rh. Parmi les mineraux accessoires du groupe du platine, on trouve une grande variete de solutions solides faisant partie du systeme Os-Ir-Rh-Pt, tetraferroplatine, tulameenite, hongshiite, mineraux des series erlichmanite-laurite et irarsite-hollingworthite, sperrylite, bismuthures, antimoniures, tellurures, stannures, et hydroxydes. Les assemblages contiennent possiblement de nouvelles especes minerales: ruthenium natif, l'analogue palladifere de la hongshiite, Pt 2 As 3 , et l'analogue platinifere de la konderite et de l'inaglyite, entre autres, qui forment des liseres autour des grains d'isoferroplatine et des inclusions dans cette phase. Nous observons pour l'or une morphologie et une distribution semblables a celles de l'isoferroplatine; l'or est lie a de rares lentilles de sulfures et des impregnations dans la dunite (or de haute temperature, porteur de Cu, Pt, et Pd), et des venues de monzodiorite recoupant la dunite (or en moyenne ou faible teneurs, a faible contenu en impuretes)." @default.
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- W2032296911 date "2005-04-01" @default.
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- W2032296911 title "COMPOSITIONAL VARIATIONS IN PLATINUM-GROUP MINERALS AND GOLD, KONDER ALKALINE-ULTRABASIC MASSIF, ALDAN SHIELD, RUSSIA" @default.
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- W2032296911 doi "https://doi.org/10.2113/gscanmin.43.2.637" @default.
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