1) Lacustrine elastic flow
湖相碎屑流
2) Pyroclasic flow facies
火山碎屑流相
3) basal-clastic phase
底碎屑相
5) geological disaster of fragmentary flows(slack)
碎(煤)屑流
6) 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。
补充资料：等流相续
【等流相续】
（术语）一类者不变更其性质而相续为一类也。
（术语）一类者不变更其性质而相续为一类也。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条