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First find of srilankite in the Urals

机译:在乌拉尔首次发现斯里兰卡人

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摘要

The first find of srilankite (very rare Zr and Ti oxide, Ti2ZrO6) in the Urals and the third find in Russia is reported. Srilankite forms very small (0.5-20 mu m) inclusions in some rutile grains. These minerals are observed in the rare rock variety, corundum-bearing spinel-saphirine hornblendite forming a block in serpentinized amphibolizied peridotite of the Ilmeny-Vishnevogorsk Complex, near the village of Taiginka, Chelyabinsk oblast. Srilankite has not been observed in such an association yet. The composition of the host rock provides evidence for its deep (the lowermost crust of the Earth) origin. Srilankites of the Urals are distinguished from all others by the high concentrations of UO2, ThO2, HfO2, and Nb2O5, which provides additional evidence for their crustal origin. Srilankite may indicate high-temperature and high-pressure conditions of rock formation.
机译:据报道,在乌拉尔发现了斯里兰卡沸石(非常稀有的Zr和Ti氧化物,Ti2ZrO6),在俄罗斯发现了第三次。斯里兰卡兰石在一些金红石颗粒中形成很小的夹杂物(0.5-20微米)。这些矿物可在车里雅宾斯克州Taiginka村附近的Ilmeny-Vishnevogorsk Complex的蛇纹化斜闪石橄榄岩中的稀有岩石品种,含刚玉的尖晶石-金缕石角闪石中观察到。尚未在这种关联中观察到斯里兰卡兰石。基质岩石的组成为其深层(地球的最低地壳)起源提供了证据。乌拉尔的斯里兰基特人与众不同,其高浓度的UO2,ThO2,HfO2和Nb2O5为其地壳起源提供了额外的证据。绢云母可能指示岩层的高温和高压条件。

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  • 来源
    《Doklady Earth Sciences》 |2016年第1期|957-960|共4页
  • 作者

    Korinevsky V. G.; Blinov I. A.;

  • 作者单位

    Russian Acad Sci, Ural Branch, Inst Mineral, Miass, Chelyabinsk Obl, Russia;

    Russian Acad Sci, Ural Branch, Inst Mineral, Miass, Chelyabinsk Obl, Russia;

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