由大滑坡引起的喜马拉雅山峰的中世纪灭亡
Jérôme Lavé1, Cyrielle Guérin2, Pierre G Valla3
1CRPG, CNRS, Université de Lorraine, Vandœuvre-lès-Nancy, France. jlave@crpg.cnrs-nancy.fr.
Nature
|July 5, 2023
概括
巨大的岩石滑坡, 而不是典型的侵蚀, 可能会解释喜马拉雅山的高峰如何失去高度. 这种可能由永久土驱动的过程极大地改变了景观,
科学领域:
- 地形学
- 冰川学
- 构造学
背景情况:
- 在极高处的喜马拉雅侵蚀机制仍然不太清楚.
- 冰川侵蚀主导了山谷,但高海拔的冰川过程似乎不那么强烈.
- 这表明最高峰的侵蚀率有所下降, 质疑它们的长期地质稳定性.
研究的目的:
- 调查影响喜马拉雅高峰的侵蚀过程.
- 确定限制峰值增长的潜在机制.
- 了解高海拔物质浪费事件的地形和沉积物后果.
主要方法:
- 在安纳普尔纳山脉发生了巨大的山体滑坡事件.
- 岩石滑坡事件的放射测年.
- 分析岩石滑坡的体积和对山顶高度的影响.
主要成果:
- 在公元1190年左右发生了巨大的岩石滑坡,涉及约23立方公里的岩石.
- 这场山体滑坡摧毁了一座高达8000米的古山峰.
- 这一事件表明巨型山体滑坡是一个重要的高海拔侵蚀过程.
结论:
- 巨大的山体滑坡可能是侵蚀喜马拉雅高峰的主要机制,
- 高海拔的永久土可能有助于峰值基层的机械强度,促进大岩石滑坡.
- 这些事件产生大量沉积物,影响下游山谷和河流系统长时间.
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