大陆分裂期间的边和内部的共同演变
Thomas M Gernon1, Thea K Hincks2, Sascha Brune3,4
1School of Ocean & Earth Science, University of Southampton, Southampton, UK. T.M.Gernon@soton.ac.uk.
Nature
|August 7, 2024
概括
曾经被认为是独立的巨大的斜坡和高原, 机械地与大陆裂变联系在一起. 在冈多瓦瓦瓦解期间的地幔过程驱动着地形演化和 Kraton 升起.
科学领域:
- 地力学和构造学
- 景观的演变
- 大陆裂变
背景情况:
- 巨大的斜坡和高原是分散的形大陆碎片的突出特征.
- 传统上,这些地形因其广的空间分离而被认为是不同的.
研究的目的:
- 开发一个物理模型,将坡和高原形成与大陆裂变联系起来.
- 挑战地质稳定地带的概念.
主要方法:
- 综合地质观测和统计分析.
- 应用地力学模拟和景观演变模型.
- 热时间学数据分析.
主要成果:
- 悬崖开始于裂边界断层,并通过向前侵蚀 (约1公里) 退缩.
- 地幔的对流不稳定向石坑 (~15-20公里) 迁移,去除了岩层的根源,并推动了高原的升起.
- 一个跨越克拉顿的同步排泄波记录了这些不断演变的地球动力学过程.
结论:
- 大陆裂变和冈德瓦纳分裂为坡和高原的起源提供了一个统一的模型.
- 观察到的景观演变反映了 Kratons 下的动态地幔过程.
- 克拉顿在地质上不是静态的,而是在大陆的分裂过程中显著地演变.
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