1)the great canyon region of Yalung-zangbo River雅鲁藏布江大拐弯
英文短句/例句
1.Quantitative Terrain Analysis of the Great Canyon Region of Yalungzangbo River,Tibet and Discussion of Its Origin西藏雅鲁藏布江大拐弯地区量化地貌特征及其成因
2.A Historical and Geographical Examination of the Big Bend or Gorges of the Yaluzangbu River along with the Names come from of the Lower Reaches of Dihang River;雅鲁藏布江大拐弯峡谷至下游底杭河名称的由来及历史地理考察
3.A Research on Tourism Depth Development Based on Special Climate--Taking Yarlung Tsangpo Great Canyon as a Case特殊气候旅游资源的深度开发探析——以雅鲁藏布大拐弯地区为例
4.THE CHARACTERS AND ORIGIN OF THE FLORA FROM THE BIG BEND GORGE OF YALUTSANGPU (BRAHMABUTRA)RIVER, EASTERN HIMALAYAS喜马拉雅东部雅鲁藏布江大峡弯河谷地区植物区系的特点及来源
5.Aeolian landform on the Banks of River Valley--Case study in Yalutsangpo River Valley雅鲁藏布江河谷风沙地貌的初步观察
6.Design and Constructing in Transforming Simple Supported into Continuous System on Brahmaputra River Bridge in Gongga贡噶雅鲁藏布江大桥简支转连续梁的设计与施工
7.Study on Ophiolite and Chromitite in Western Yarlung Zangbo, Tibet;西藏雅鲁藏布江西段蛇绿岩及铬铁矿研究
8.Seismicity of the Yarlung Tsangpo Grand Canyon Region, China雅鲁藏布大峡谷地区地震活动性研究
9.Variety characteristics of the crustal stress field near the Brahmaputra fault zone雅鲁藏布江断裂带附近地应力场的变化特征
10.CLASSIFICATION AND DEVELOPMENT OF AEOLIAN SAND LANDFORM IN THE YURLUNG ZANGBO VALLEY雅鲁藏布江河谷风沙地貌分类与发育问题
11.Research on the Morphological Features of Yarlung Zangbo River Based on DEM;基于DEM的雅鲁藏布江河流地貌特征的研究
12.Multi-temporal Scales Analysis of Runoff Series in Yarlung Zangbo River Based on Hilbert-Huang Transform基于HHT变换的雅鲁藏布江径流多时间尺度分析
13.Trends in Daily Temperature and Precipitation Extremes over the Yarlung Zangbo River Basin during 1961-2005近45年雅鲁藏布江流域极端气候事件趋势分析
14.Famous rivers in China include the Yangtze River, the Yellow River, the Heilongjiang River, the Yarlung Zangbo River and the Huaihe River.中国主要的河流有长江、黄河、黑龙江、雅鲁藏布江、淮河。
15.Aeromagnetic Survey in Tibetan Plateau and the Characteristics of DAAZ Along Yarlung Zangbo River;青藏高原航磁测量及雅鲁藏布江双航磁异常带的性质研究
16.Discovery of mantle Ductile Shear Zone in Ophiolite along Yarlungzangbo River, Tibet and Its Significance雅鲁藏布江蛇绿岩中幔型韧性剪切带的发现及其意义
17.Yarlung Zangbo River Shui Yindao the Yellow River, solves the area south of Yellow River area to lack the water question the unsolved problem.把雅鲁藏布江水引到黄河，解决中原地区缺水问题的老问题。
18.On a Geochemistry Method of Hunting for Ores in the Banks of Yarlung Zangbo River Covering with Eolian Sand雅鲁藏布江两岸风成沙覆盖区地球化学找矿方法及效果
相关短句/例句
the great turn of Yaluzangbu雅鲁藏布大拐弯
1.Effect of water-rock interaction on the slope in the north of the great turn of Yaluzangbu;水岩作用对雅鲁藏布大拐弯北段滑坡的影响
3)the YarlungTsangpo Great Canyon雅鲁藏布大拐弯地区
4)Yaluzangbu River雅鲁藏布江
1.Cause analysis of environmental hazards in the middle reaches of Yaluzangbu River in Tibet;西藏自治区雅鲁藏布江中游地区环境灾害成因分析
2.The reproductive activities of Glyptosternum maculatum were investigated in the Yaluzangbu River in Tibet, China from September 2002 to August 2003.研究了西藏雅鲁藏布江中的黑斑原鮡个体生殖力及其与生物学指标的关系。
5)Yarlung Zangbo River雅鲁藏布江
1.Application of a Distributed Hydrological Model for the Yarlung Zangbo River and Analysis of the River Runoff;雅鲁藏布江流域的分布式水文模拟及径流变化分析
2.Characteristics and Driving Factors of the Runoff Variations in the Yarlung Zangbo River;雅鲁藏布江径流演变规律及其驱动因子分析
3.Deposition Features and Causes of Loess in Yarlung Zangbo River Valley Area;雅鲁藏布江河谷黄土的沉积特征及成因
6)Yalu Tsangpo river雅鲁藏布江
1.The phytogeographical affinities and florisitic nature of the big bend gorge (tropical and subtropical mountainous region below 2 500 m) of the Yalu Tsangpo River,S.中国西藏墨脱雅鲁藏布江大峡湾河谷地区（海拔2500m以下热带亚热带山地）属东喜马拉雅山地的一部分，在区系亲缘上属印度东北部阿萨姆喀西山和那加山以及尼泊尔等东喜马拉雅地区区系的一部分；其热带成分与我国云南南部的西双版纳也有较为密切的联系，这是第三纪以来印度－马来成分沿中南半岛迁移和交流的结果。
延伸阅读
雅鲁藏布江雅鲁藏布江世界上海拔最高的大河。位于西藏自治区南部。“雅鲁藏布”藏语意为“高山流下的雪水”。正源杰马央宗曲，源头海拔5590米，由喜马拉雅山脉中段北坡的一系列冰川融水汇成，在桑木张汇合南源库比藏布以后，向东流到萨嘎县的里孜，这一段称马泉河。从杰马央宗冰川的末端至里孜为上游段，河段长268千米，谷地开阔，河床比降小，水流平稳，江心洲和汊河发育，两岸有大片沼泽地分布。从里孜到派乡为中游段，河段长1293千米，两岸支流众多，主要有年楚河、拉萨河、尼洋河等，中游河段呈宽窄相间，水面宽100～200米，江中多沙洲，浅滩和汊流，曲水至泽当段，舟楫往来频繁，航运相当便利。派乡到巴昔卡附近为下游段，河段长496千米，河流在米林县里龙附近开始逐渐折向东北流，经派乡转为北东向，至帕隆藏布汇入后，急转南下，进入著名的底项大峡谷，河床下切2300多米，为世界上最大峡谷之一。出山口经巴昔卡流入印度，称布拉马普特拉河，进入孟加拉国称贾木纳河，注入印度洋的孟加拉湾。居中国段雅鲁藏布江全长2057千米，流域面积24.05万平方千米。水资源丰富，年径流量1400多亿立方米，径流年际变化幅度小。干流水力资源蕴藏量7611.6万千瓦，主要集中在下游底项峡谷区。雅鲁藏布江大拐弯
