考古时期地的演变是通过分层和浅层潜水而发生的
Stephen F Foley1, Stephan Buhre, Dorrit E Jacob
1Institut für Geologische Wissenschaften, Universität Greifswald, Germany. sfoley@uni-greifswald.de
Nature
|January 17, 2003
概括
早期的地球地球.
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:
- 古代海洋地可能比现代地更厚,更富含,因为热流量更高.
- 之前的沉降实验只使用了现代的中海基岩,忽视了地球早期的条件.
研究的目的:
- 为了研究早期Archaean海洋地在沉降过程中的变态反应.
- 了解对地回收和大陆地形成的影响.
主要方法:
- 高压实验石油学.
- 分析来自超性积聚物和皮克里特的变态反应产物.
主要成果:
- 早期Archaean地材料的变形产生了pyroxenites,它们分层并融化为玄武岩.
- 大陆地的形成需要石榴石-两石的沉降和融化,这种石榴石从古老时代晚期开始流行.
- 早期阿基亚时代的浅层沉降只耗尽了一层薄薄的上层地幔层.
结论:
- 早期的阿凯纪地的沉降是浅的,导致了有限的地幔枯竭.
- 耗尽的地幔层的持续深化解释了地质化学和地质物理模型之间的差异.
- 大陆地的形成在阿古晚期开始显著,并有更深的沉降过程.
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