崩塌滑坡,collapse and landslide
1)collapse and landslide崩塌滑坡
1.In this paper,thewriter studies the regularities governing the density of collapse and landslide on the upperMing Jiang River Basin.岷江为长江—级支流,上游长330km,自1986年以来,发生崩塌滑坡200余处,体积约2。
2.Then using sensitivity coefficient analyzed the sensitivity of collapse and landslide to stratum lithology in research area,according to research area actual situation,the sensitivity coefficient is divided into four ranks which extremely sensitive area accounts for 29.35 km2,并分析了各地层岩性在各类立地类型组的分布关系;然后利用敏感性系数SC,分析了研究区内崩塌滑坡对地层岩性的敏感性,根据区域实际情况将敏感性系数划分为4个等级,其中极敏感区占研究区的29。
英文短句/例句

1.ANALYSIS ON THE NUMBER AND DENSITY OF LANDSLIDES TRIGGERED BY THE 2008 WENCHUAN EARTHQUANKE,CHINA汶川地震触发崩塌滑坡数量及其密度特征分析
2.Sensitivity Evaluation to the Earthquake-induced Landslide and Collapse:A Case Study of Beichuan County,Sichuan Province地震诱发崩塌滑坡敏感性评价——以北川县为例
3.Earth-fetching, sand-digging and quarrying shall be prohibited in areas in danger of land-collapsing or land-sliding or where mudrock flow is liable to occur.在崩塌滑坡危险区和泥石流易发区禁止取土、挖砂、采石。
4.The Characteristic and Evaluation of Collapse and Landslide Disaster Along Du-wen Highway in Wenchuan Earthquake Region汶川地震区都汶公路沿线崩塌滑坡灾害特征与评价
5.The scope of such areas shall be determined and announced by the local peop1e's governments at or above the county level.崩塌滑坡危险区和泥石流易发区的范围,由县级以上地方人民政府划定并公告。
6.Sensitivity Analysis of Collapse and Landslide on Stratum Lithology基于地层岩性的崩塌滑坡敏感性分析——以5·12震后都汶公路沿线为例
7.Distribution Characteristics and Impact Factors Assessment of Collapses and Landslides Caused by 5.12 Wenchuan Earthquake:Taking Dujiangyan-Wenchuan Highway as a Sample5.12汶川地震崩塌滑坡分布特征及影响因子评价——以都江堰至汶川公路沿线为例
8.A COLLAPSE LANDSLIDE OF MARCH 20.1904 AT BAIYA,GAOXIAN COUNTY,SICHUAN PROVINCE1994-03-20四川省高县白崖崩塌性滑坡
9.Hazard assessment of landslide and collapse in first-stage project of west line for water-transfer from south to north西线调水一期工程滑坡崩塌体灾害评价
10.The main kinds of hazards of road in Beijing mountain area are landslip, collapse, debris flow, karst and surface subsidence.北京山区公路所遭受的地质灾害主要有滑坡、滑(崩)塌、泥石流、岩溶、采空地面塌陷等。
11.A HAzARD-CHAIN OF LANDSLIO→COLLAPSE→DEBRIS FLOW→RIVER STOPPAGE IN WULONG COUNTY,SICHUAN PROVINCE ON APRIL 30,19941994-04-30四川省武隆县鸡冠岭滑坡→崩塌→碎屑流→堵江灾害链
12.Application of PPCE Based on RAGA in Collaps,Landslide and Debrits Flow Callaps,Hazard Evaluation--A case study of Jialing River,Beibei,ChongqingRAGA和PPCE在崩塌、滑坡、泥石流灾害评价中的应用——以重庆市北碚区为例
13.Spatial distribution of rockfall and landslide mass in disaster areas of Wenchuan earthquake汶川地震受灾严重区域崩塌与滑坡体空间分布研究
14.Landslides happen when large amounts of rock, mud and other loose materials are suddenly uprooted and sent sliding down a slope.大量的泥、石及其他堆积松散的物质突然坍塌,顺着山坡倾滑下来就形成了山崩。
15.We were concerned that the north slope of the volcano might slide away.我们关心的是,火山北坡将会崩塌。
16.Low-lying lands, steep slops, lands where landslip is likely to occur, and other environment-sensitive lands shall be avoided.九、避免低洼地、陡坡、易崩塌地或其他环境敏感地。
17.Stability Study of Talus Slides on the JinAnQiao Hydropower Station s Left Embank;金安桥水电站左岸边坡崩塌体稳定性研究
18.Theory of Block Rockmass Slope Collapse Monitoring and Prediction and Its Application;块裂岩质边坡崩塌监测预报理论及应用研究
相关短句/例句

landslide[英]['l?ndsla?d][美]['l?nd'sla?d]崩塌滑坡
1.Monitoring during construction of prevention works for landslides and the effect analysis;崩塌滑坡防治施工监测与治理效果
2.Areal landslides susceptibility analysis——A case study in Hong County, Sichuan Province;区域崩塌滑坡的易发性评价——以四川省珙县为例
3)landslide and collapse accumulation滑坡崩塌体
4)landslide and rockfall滑坡与崩塌
5)Collapse landslide崩塌性滑坡
6)slip and fall滑坡和崩塌
1.The authors discuss the main distribution of slip and fall in China and harm and reason analysis,put forward the measures of protection and control of geological disasters,in the hope that the protection of geological environment can become an important part of the process of the social development .论述了我国滑坡、崩塌的区域分布特征 ,滑坡和崩塌的危害程度 ,滑坡和崩塌类型和成因分析 ,并且提出了灾害的防御措施 ,以期达到环境保护成为社会发展过程中的一个重要组成部分。
延伸阅读

崩塌崩塌avalanche陡峻山坡上岩块、土体在重力作用下,发生突然的急剧的倾落运动。多发生在大于60°~70°的斜坡上。崩塌的物质,称为崩塌体。崩塌体为土质者,称为土崩;崩塌体为岩质者,称为岩崩;大规模的岩崩,称为山崩。崩塌可以发生在任何地带,山崩限于高山峡谷区内。崩塌体与坡体的分离界面称为崩塌面,崩塌面往往就是倾角很大的界面,如节理、片理、劈理、层面、破碎带等。崩塌体的运动方式为倾倒、崩落。崩塌体碎块在运动过程中滚动或跳跃,最后在坡脚处形成堆积地貌——崩塌倒石锥。崩塌倒石锥结构松散、杂乱、无层理、多孔隙;由于崩塌所产生的气浪作用,使细小颗粒的运动距离更远一些,因而在水平方向上有一定的分选性。科学家正在考察山坡崩塌情况