概括
来自板块沉降的动态地形导致快速的大陆沉降. 数字模型显示,这些速度与北美板块边缘沿北美板块边缘的罗纪沉积堆积相匹配.
科学领域:
- 地力学是什么?地力学是什么?
- 构造学 构造学 构造学 构造学
- 沉积物学的沉积物学
背景情况:
- 活跃边缘过程,包括动态地形,影响大陆石化层.
- 以前对沉降的解释往往集中在地上加载上.
研究的目的:
- 调查动态地形在海洋盆地关闭期间大陆沉降中的作用.
- 为了比较动态沉降与沉积积的速度.
主要方法:
- 动态地形的数值建模启动和演变.
- 分析与板块浅化和海洋盆地关闭有关的沉降率.
主要成果:
- 动态沉降率可以超过每百万年100米.
- 这些速度与罗纪沿着汇聚边缘的沉积积累相似.
结论:
- 动态地形是活跃大陆边缘快速沉降的重要驱动因素.
- 数字建模为以前仅归因于表面负荷的构造过程提供了关键的见解.
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