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纪气候变化是安第斯山脉起的可能原因
1Department of Earth Sciences, Parks Road, Oxford, OX1 3PR, UK. simon.lamb@earth.ox.ac.uk
Nature
|October 24, 2003
概括
气候变化可能通过影响流区动态推动了安第斯山脉的升起. 由气候驱动的沉积物饥饿,增加了剪切应力,支持高安第斯山脉.
科学领域:
- 地质地质地质地质地质地
- 气候科学 气候科学
- 构造学 构造学 构造学 构造学
背景情况:
- 传统上,山脉升起与气候变化有关,而不是相反.
- 安第斯山脉的形成是复杂的,涉及岩层力量.
研究的目的:
- 提出一个机制,其中Cenozoic气候变化导致安第斯山脉的上升.
- 为了研究潜伏区动态在山地建筑中的作用.
主要方法:
- 分析南美石化层的力量平衡.
- 检查沉积沉积物,剪切应力和山峰高度之间的关系.
主要成果:
- 安第斯山脉的高度和构造学由俯冲区剪切应力和浮力对比控制.
- 俯冲区的剪切应力取决于俯冲沉积物的体积.
结论:
- 气候驱动的侵蚀和沉积物沉积控制潜水和山地形成.
- 南美洲受气候控制的沉积物饥饿导致高剪压,支持安第斯山脉的升高.
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