科马提石揭示了阿基亚深层地幔的水库
Alexander V Sobolev1,2, Evgeny V Asafov2, Andrey A Gurenko3
1Université Grenoble Alpes, Institute Science de la Terre (ISTerre), CNRS, F-38041 Grenoble, France.
Nature
|April 1, 2016
概括
在高温下爆发,新的研究表明它们的岩石含有0.6%的水. 这支持地球早期的羽毛起源和深层水分.
科学领域:
- 地质化学
- 石油学
- 地球的早期状况
背景情况:
- 古代的岩石是超岩, 表明地幔极度融化.
- 关于岩石含水量存在不确定性,影响喷发温度和起源模型 (羽毛与沉积).
研究的目的:
- 直接估计阿凯亚科马石的组成和结晶温度.
- 解决关于科马石含水量及其对地幔过程的影响的争论.
主要方法:
- 在酸中分析水,挥发性,主要和微量元素.
- 融化的地化学建模和来源特征.
主要成果:
- 在27亿年前的阿比蒂比岩石中,原始融含有30%的MgO,0.6%的H2O,并且在不相容的元素中被耗尽.
- 在降解条件下在1530°C开始结晶,通过分量结晶和微小的地同化进化.
- 高的H2O/Ce比率表明水性物质从地幔过渡区被入.
结论:
- 科马石的构成和低氧气流动性与潜水不一致,支持羽毛起源.
- 结果证实了高古地幔温度,并暗示了地球历史早期的深水地幔水库.
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