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Earth's youngest known ultrahigh-temperature granulites discovered on Seram, eastern Indonesia

机译:在印度尼西亚东部的苏拉姆发现的地球上最年轻的已知超高温颗粒

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Episodes of ultrahigh-temperature (UHT, ≥900 °C) granulite metamorphism have been recorded in mountain belts since the Neoarchean. However, evidence for the tectonic mechanisms responsible for the generation of such extreme thermal conditions is rarely preserved. Here we report the discovery of 16 Ma UHT granulites-the youngest identified at the Earth's surface-from the Kobipoto Mountains of Seram in eastern Indonesia. UHT conditions were produced by a modern tectonic system in which slab rollback-driven lithospheric extension caused core complex-style exhumation of hot subcontinental lithospheric mantle. Overlying continental crust, heated and metamorphosed by exhumed lherzolites, developed spinel + quartz and sapphirine-bearing residual assemblages, shown by phase equilibria modeling to have required temperatures of ~950 °C at ~8 kbar pressure. Seram is therefore a possible modern analogue for ancient orogens that incorporate UHT granulites.
机译:自新archarean以来,在山区已记录了超高温(UHT,≥900°C)花岗石变质的事件。但是,几乎没有保存造成这种极端温度条件的构造机制的证据。在这里,我们报道了从印度尼西亚东部塞拉姆的科比坡托山发现的16 Ma UHT颗粒(在地球表面发现的最年轻)。 UHT条件是由现代构造系统产生的,在该构造系统中,板块回滚驱动的岩石圈伸展导致了核心的复杂样式的热次大陆岩石圈地幔发掘。相变平衡模型表明,上覆的大陆壳被发掘出的蛇绿石加热并变质,形成了尖晶石+石英和含蓝宝石的残余组合,在约8 kbar的压力下需要约950°C的温度。因此,对于结合了UHT颗粒的古代造山带,Seram是一种可能的现代类似物。

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