在orogenic生长过程中变形,降水和侵蚀之间的协调
Xiaoping Yuan1, Yuqiang Li2, Sascha Brune3,4
1State Key Laboratory of Biogeology and Environmental Geology, Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences, Wuhan, China. yuanxiaoping@cug.edu.cn.
源生长涉及变形,降水和侵蚀. 数字模型揭示了岩石升起,降水和高原形成期间侵蚀速率之间的强烈相关性.
科学领域:
- 地球科学 地球科学 地球科学
- 地质地质地质地质地质地
- 地质形态学 地质形态学
背景情况:
- 源生长导致地形高,增强降水和侵蚀.
- 人们还没有很好地理解形过程中变形,降水和侵蚀之间的相互作用.
研究的目的:
- 为了研究在orogenic增长过程中变形,降水和侵蚀的协调.
- 使用数值建模,探索不同侵蚀性对这些合过程的影响.
主要方法:
- 开发一个数字模型,将构造学,地表过程和地形沉结合起来.
- 模拟低,中,高侵蚀性气体的模拟.
主要成果:
- 对于中间侵蚀性,在高原形成过程中观察到强烈的相关性 (升降侵蚀的r≈0.9,降水侵蚀的r≈0.8).
- 证明了升起,降水和侵蚀率之间的相关性循环演变,与断层发展有关.
结论:
- 岩石升起和降水率与正在积极形成的高原的侵蚀率密切相关.
- 这些发现提供了关于活跃山脉侵蚀的构造学与气候驱动因素的见解,并解释了喜马拉雅山脉相互矛盾的数据.
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