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青海-西藏高原稳定滑坡水的分布模式和形成机制:一项初步研究
Liang Song1,2,3,4, Liqiang Ma5,6,7, Zhiguo Chang1,8,9
1Key Laboratory of Xinjiang Coal Resources Green Mining (Xinjiang Institute of Engineering), Ministry of Education, Urumqi, 830023, China.
Scientific reports
|February 3, 2026
概括
研究人员在青海-西藏高原绘制了348座稳定的天然水,确定岩石雪崩和海是主要原因. 的结构是它们长期稳定的关键.
科学领域:
- 地质地质地质地质地质地
- 地质形态学 地质形态学
- 天然危害 天然危害
背景情况:
- 青海 - 西藏高原的东边缘在构造上活跃,有深深的峡谷,有利于天然水的形成.
- 关于该地区天然水的稳定性和分布的研究有限.
研究的目的:
- 在青海-西藏高原绘制稳定的天然水分布图.
- 确定这些水的起源和对这些水的长期稳定性有助于的因素.
主要方法:
- 远程传感绘制地图.
- 详细的实地调查.
- 建立一个稳定的水库存.
主要成果:
- 总共有348座稳定的天然水被确定:294座当前水和54座古水.
- 主要的起源包括岩石雪崩 (36.5%),海 (32.8%),岩石落 (23%) 和岩石滑坡 (7.7%).
- 总结了六种稳定的水的地形类型,结构配置对稳定性至关重要.
结论:
- 该研究提供了该地区稳定的天然水的全面清单.
- 了解大的起源和结构配置对于评估山体滑坡大的稳定性至关重要.
- 这项研究有助于对构造性活跃地区的危险评估和风险管理.
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