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Platinum-group elements for the Kudi ophiolite, western Kunlun

机译:昆仑西部古帝蛇绿岩的铂族元素

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摘要

The analyses of PGE characteristics for the Kudi ophiolite, western Kunlun, are reported in this note. The Ir-depleted anomalous ancient upper mantle represented by the Kudi mantle peridotites had been percolated and mixed by remelted oceanic crust material from a supra-subduction zoen, leaving the rocks relatively enriched in Pd. The PGE contents in the Kudi cumulate pyroxenites and gabbros vary from 2.4 to 23.94 ng/g, and the highest values are in pyroxenites. The Pd/Ir ratios increase from the pyroxenites to the gabbros.
机译:本文中对昆仑西部库迪蛇绿岩的PGE特征进行了分析。以库迪地幔橄榄岩为代表的贫铀异常上地幔被超俯冲带重熔的海洋地壳物质渗透和混合,使岩石中的钯相对富集。 Kudi中的PGE含量累积为辉石和辉长岩,变化范围为2.4至23.94 ng / g,最高值为辉石。 Pd / Ir比从辉石到辉长岩增加。

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