地球上的板块构造由羽毛诱导的沉积启动
T V Gerya1, R J Stern2, M Baes3
1Department of Earth Sciences, ETH-Zurich, Sonneggstrasse 5, 8092 Zurich, Switzerland.
Nature
|November 13, 2015
概括
地球的早期
科学领域:
- 地质学
- 构造学
- 地球科学
背景情况:
- 地球板块构造和沉积的起源仍然不太清楚.
- 浮沉开始的板块前构造机制可能与现代过程有很大的不同.
研究的目的:
- 作为板块构造开始的机制,研究羽毛诱导的沉降启动的可行性.
- 确定控制自主潜伏的关键物理因素.
主要方法:
- 使用高分辨率的三维数值热力学建模.
- 模拟探索了地幔羽毛与海洋岩层的相互作用.
主要成果:
- 需要一个强大的,负面浮动的海洋岩层.
- 岩层上方的岩层减弱和水化地的滑是关键因素.
- 在一个更热的早期地球上,对于旧的海洋板块来说,羽诱导的沉降是可行的.
结论:
- 在早期地球上,地幔羽毛可能是第一个潜伏区的开端.
- 较年轻的海洋板块倾向于岩层滴水而不是持续的沉积,阻碍了全球板块构造的开始.
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