[1]朱平一,王成华,唐邦兴.西藏特大规模碎屑流堆积特征[J].山地学报,2000,(05):453.
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西藏特大规模碎屑流堆积特征()
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《山地学报》[ISSN:1008-2186/CN:51-1516]

卷:
期数:
2000年05期
页码:
453
栏目:
山地学报
出版日期:
2000-10-28

文章信息/Info

作者:
朱平一;王成华;唐邦兴
中国科学院!水利部成都山地灾害与环境研究所四川成都610041;中国科学院!水利部成都山地灾害与环境研究所四川成都610041;中国科学院!水利部成都山地灾害与环境研究所四川成都610041
关键词:
雪崩; 滑坡; 碎屑流
文献标志码:
A
摘要:
20 0 0 -0 4 -0 9日由上游雪崩激发 ,导致中游地区的波密县境易贡藏布下游支沟扎木弄巴 (沟 )滑坡 ,沿程强烈侵蚀而暴发国内外罕见的特大规模碎屑流 ,并形成了气浪堆积、顶托江水堆积、反弹堆积、刨蚀堆积、寒冻风化堆积、地崩物质堆积等 6个不同于滑坡、泥石流的碎屑流堆积。

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更新日期/Last Update: 2000-10-28