1) sturzstrom
(干)碎屑流
2) geological disaster of fragmentary flows(slack)
碎(煤)屑流
3) debris flow
碎屑流
1.
A supper debris flow had occurred on 9th Aril 2000,at the Zhamulongba gully of the down reach of Yigongzangbu River.
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。
2.
ith the further study on the high-speed landslide in recent years, a new form of geological hazard -debris flow which is often accompanying with the high-speed landslides hasdrawn more and more attention in the engineering geology field, particularly since the accurencesof Shalashan Maintain Front debris flow, Xintan Sanyogou debris flow and Shijiapou debris flow.
近十几年来，随着对崩滑灾害的研究深入，伴随高速滑坡的一种新形式的地质灾害－崩滑碎屑流已愈来愈引起工程地质与环境地质界的关注。
3.
At 11:45 On April 30,1994, a hazard-chain of lands1ide → collapse→debris flow→riverstoppage occurred at Jiguanling─Longguanzhui(107°29′ 27″E,29°28′06″N),located on the leftbank of Wujiang River in Wulong Couuty , Sichuan Provin ce, The volume of debris flow wasabout 5.
１９９４－０４－３０的１１：４５，四川省武隆县兴顺乡核桃坪村境内乌江左岸鸡冠岭一龙冠嘴（１０７°２９′２７″Ｅ，２９°２８′０６″Ｎ）发生了特大型滑坡→崩塌→碎屑流→堵江灾害链，其碎屑堆积物方量５３０万ｍ￣３。
4) Type A of debris flow
A型碎屑流
5) Lacustrine elastic flow
湖相碎屑流
6) pyroclastic flow
火山碎屑流
1.
Peridotite xenolith fragments from Late Quaternary pyroclastic flow in Weizhou Island,Beihai,Guangxi;
广西北海涠洲岛第四纪晚期火山碎屑流中橄榄岩包体碎块的发现及其地质意义
2.
This paper demonstrates the results of grain-size sieve analyses of the millennium pyroclastic flow deposits from Tianchi volcano.
火山碎屑流堆积因其巨大的危害性而成为火山学研究的重要课题之一。
3.
The author deeply studied cooling unit of pyroclastic flow in Luanping area and divided the volcanic rock into 12 cooling units.
笔者对滦平地区火山碎屑流冷却单元进行了深入的研究，划分出１２个冷却单元。
补充资料：由干
【由干】
（杂名）由乾陀罗之略。山名。
（杂名）由乾陀罗之略。山名。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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