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Plagioclase and Apatite from Exsolution Structures in Minerals from Mantle Xenoliths

机译:地幔异岩中矿物溶出结构的斜长石和磷灰石

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Chlorine- and alkali-bearing minerals unusual for the kimberlitic matrix from nonserpentinized kimber-lite of the Udachnaya pipe (Yakutia) with an anomalously low concentration of water [ 1 ] were described in the groundmass [2|, as chloride-carbonate nodules [3], and in melt inclusions in olivines from this kim-berlite [4]. Phlogopite, apatite, calcite, djerfisherite [5], and sodalite [5, 6] were observed in xenoliths of deformed lherzolites from the Udachnaya pipe; tetra-ferriphlogopite, halite, sylvite, alkaline carbonates, and sulfates were registered in melt inclusions from all primary minerals of these xenoliths [5]. Graphite-
机译:在地面质量[2 |]中,Udachnaya管(雅库特)的非蛇形化金伯利岩的含金刚石基质中异常含氯和碱的矿物[1]被描述为氯化碳酸盐结节[3]。 ],以及金伯利岩[4]中橄榄石中的熔融包裹体。在Udachnaya管道中,在变形形锂铁矿的异岩中观察到了金云母,磷灰石,方解石,硬水铝石[5、6]。在这些异岩的所有主要矿物的熔融包裹体中都记录了四亚铁金云母,盐岩,钾盐,碱式碳酸盐和硫酸盐[5]。石墨-

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    《Doklady Earth Sciences》 |2011年第2期|p.483-485|共3页
  • 作者单位

    Sobolev Institute of Geology and Mineralogy,Siberian Branch, Russian Academy of Sciences,Novosibirsk, Russia;

    Sobolev Institute of Geology and Mineralogy,Siberian Branch, Russian Academy of Sciences,Novosibirsk, Russia;

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