在喜马拉雅山脉,侵蚀和降雨的脱
D W Burbank1, A E Blythe, J Putkonen
1Department of Geological Sciences, University of California, Santa Barbara, California 93106, USA. burbank@crustal.ucsb.edu
Nature
|December 12, 2003
概括
山区的高侵蚀率不仅仅是由降雨梯度驱动的. 其他因素,如通道宽度和沉积物负载,平衡了降水差异,揭示了喜马拉雅山的均侵蚀.
科学领域:
- 地质形态学 地质形态学
- 构造学 构造学 构造学 构造学
- 气候科学 气候科学
背景情况:
- 数字模型表明,空间侵蚀梯度在活跃的原体中驱动高应变率.
- 这些模型经常使用"流动力"规则,将侵蚀与排放和通道斜率联系起来.
- 预计降水和斜率变化与侵蚀和地应变梯度相关.
研究的目的:
- 测试空间侵蚀梯度与大喜马拉雅地区降水梯度相关的假设.
- 为了研究侵蚀速率,降水和构造上升在一个主要的活跃的orogen之间的关系.
主要方法:
- 来自尼泊尔大喜马拉雅地区网络的综合气象数据.
- 使用低温热度计 (时间尺度>100,000年) 估计的地质侵蚀率.
- 分析了跨越喜马拉雅山脉顶部的~20公里区域的数据,降水量有显著差异.
主要成果:
- 在整个研究区内,没有发现地质侵蚀速率的显著空间变化.
- 降雨量减少并没有被的运河斜坡所补偿.
- 道宽度和沉积物度等因素似乎平衡了降水变化,影响了切口率.
结论:
- 大喜马拉雅地区的空间均侵蚀率尽管有显著的降水梯度,但仍被观察到.
- 河流切口受降水和斜率以外的因素的影响,包括通道宽度和沉积物负载.
- 均的侵蚀与岩石在地坡道上方的稳定上升的构造学运输是一致的.
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