在挪威,一个古老的orogenic peridotite巨层的深层起源和热化
Dirk Spengler1, Herman L M van Roermund, Martyn R Drury
1Faculteit Geowetenschappen, Universiteit Utrecht, Budapestlaan 4, 3584CD Utrecht, The Netherlands. spengler@geo.uu.nl
Nature
|April 14, 2006
概括
这项研究揭示,来自地球深处的古老地幔岩石,通过一次融化事件形成了克拉顿的保护根. 这一发现澄清了这些岩根的起源,以及它们在保存古代大陆地中的作用.
科学领域:
- 地质科学是地球科学.
- 石化学 石化学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 亚大陆的石质层地幔提供浮力和强度,保护古老的大陆地 (cratons).
- 石层在坑下面的起源是有争议的,但它被认为是大量炼后的残留物.
- 现有的融化枯竭,石榴石岩的模型表明复杂的,多阶段的形成过程.
研究的目的:
- 调查克拉石层地幔的起源和形成过程.
- 为了分析orogenicperidotites作为地的碎片融入地.
- 了解这些地幔碎片的融化历史和石化过程.
主要方法:
- 来自挪威西部奥特罗伊的质矿的分析.
- 对岩石样本进行地质化学和石矿学检查.
- 融化过程和地幔上游的建模.
主要成果:
- 石在从超过350公里的深度上升时经历了广泛的融化.
- 在一次融化事件中形成了带花石的石根.
- 这些矿石代表了古老时期的贫化矿石岩的残留物.
结论:
- Kratonic 根可以通过一个单一的大规模融化事件在地幔上升过程中形成.
- 这些发现挑战了石榴石承载石岩层形成的多阶段模型.
- 这项研究提供了对早期地球过程的洞察,这些过程形成并保存了石坑.
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