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谷冰川
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     Discussion on the Cross Section Features of Glacial Valley
     冰川横剖面形态特征探析
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     Glacier of the Qilian Mountain
     祁连山冰川
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     Glacier Masterpieces
     冰川杰作
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     The Morphological Character and Paleo climate Indication of the Cross Section of Glacial Valleys
     冰川横剖面形态特征的古环境标志再探讨
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     Kings Valley
     国王探幽
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  valley glacier
The ice thickness of the valley glacier sections, the surface of which was situated above the snow-line, amounted to 1000-1450 m.
      
These textures have been used to infer that a small valley glacier, overlain by snow, existed in the Santa Gertrudis Valley at the time of the eruption.
      
The ice thickness of the valley glacier sections, the surface of which was situated above the snow-line, amounted to 1000-1450?m.
      
Temporal and spatial variations in albedo on a valley glacier.
      
Ulf Jonsell, Temporal and spatial variations in albedo on a valley glacier, 2000.
      
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The authors propose the following arguments: 1) Da Ao is really cirque. Its landform was not crcated by periglacial snow erosion or solifluction; nor water flow. 2) "U" shaped valley of Wang Jia Po is a glacial trough. It was not formed from water flow or weathering under the control of the structure or nature of the uocks. 3) Ridges and hill locks in the mountain foot are the end moraine bars, not the "isolated islands" piled by the mudflow. 4) The climate of Lu Shau in the glacial stage was the cold one which...

The authors propose the following arguments: 1) Da Ao is really cirque. Its landform was not crcated by periglacial snow erosion or solifluction; nor water flow. 2) "U" shaped valley of Wang Jia Po is a glacial trough. It was not formed from water flow or weathering under the control of the structure or nature of the uocks. 3) Ridges and hill locks in the mountain foot are the end moraine bars, not the "isolated islands" piled by the mudflow. 4) The climate of Lu Shau in the glacial stage was the cold one which could cause the glacier. wet and hot climate exists in the interglacial stage, not in the glacial stage.

本文认为①大坳完全能归到冰斗之列,并非由冰缘雪蚀和融冻泥流作用拓宽、并经流水改造所成的地貌;②王家坡U谷是冰川槽谷,不必求助于构造和岩性控制下的流水、风化作用成因;③山麓的垅岗是终碛垅,并非泥石流“龙头”堆积的“孤岛”;④冰期庐山气候有发育冰川的寒冷冰期气候,而湿热气候并非冰期则是间冰期气候。

GPR is an active remote-sensing method,which includes Common Depth Point(CDP) and Wide Angle Reflection and Refraction(WARR).Different mode can be used to figure out different glaciology problem.GPR is applied to glaciology such as determining ice thickness,subice topography,basal crevasses, internal reflection horizons,and hydrological features etc.So it can provide abundant and authentic datum for the follow studies:subice valley,glacier structure,ice flow mechanism,water resource evaluation and variation...

GPR is an active remote-sensing method,which includes Common Depth Point(CDP) and Wide Angle Reflection and Refraction(WARR).Different mode can be used to figure out different glaciology problem.GPR is applied to glaciology such as determining ice thickness,subice topography,basal crevasses, internal reflection horizons,and hydrological features etc.So it can provide abundant and authentic datum for the follow studies:subice valley,glacier structure,ice flow mechanism,water resource evaluation and variation of climate and environment etc.

探地雷达技术是一种利用电磁波反射原理探测地下介质分布特征的地球物理勘探技术 ,其探测方式主要有剖面法 (CommonDepthPoint)和宽角法 (WideAngleReflectionandRefraction)两种。不同的探测方式可解决不同的冰川问题。探地雷达在冰川学中广泛应用于探测冰体厚度、冰下地形、冰裂缝、冰体内部沉积层位、冰川水文特征、划分冰川冰类型等 ,为冰下槽谷、冰川结构、冰川流动机制、水资源评估及气候与环境变化的研究提供丰富可靠的数据

An distinguashable ice-dammed lake formed during the Late Pleistocene at the Purlung Tsangpo River,a main downstream tributary of the Yarlung Tsangpo River,in the Songzong Basin of southeast Tibet has been recognized.The lacustrine deposit,more than 88 meters thick measured by Total Station(TCA2003),is disclosed after the Songzong landslide.The successional silty clay in the profile is 18.33 meters thick,clearly suggesting the formation of a lake.The Optical Simulated Luminescence(OSL)ages at the bottom and...

An distinguashable ice-dammed lake formed during the Late Pleistocene at the Purlung Tsangpo River,a main downstream tributary of the Yarlung Tsangpo River,in the Songzong Basin of southeast Tibet has been recognized.The lacustrine deposit,more than 88 meters thick measured by Total Station(TCA2003),is disclosed after the Songzong landslide.The successional silty clay in the profile is 18.33 meters thick,clearly suggesting the formation of a lake.The Optical Simulated Luminescence(OSL)ages at the bottom and top of the silty clay layer are 22.5±3.3kaB.P.,16.1±1.7kaB.P.,respectively,indicating that the lacustrine deposits were formed during the Last Glacial Maximum ranging from 25kaB.P.to 15kaB.P.It was discovered by field geological survey that the sediments were deposited in the outside of the moraine terrace of the Songzong Basin.Particularly,the high and large moraine terrace is outcropped in the front of the Dongqu Valley,a big tributary ravine at the south bank of the river.The Dongqu Valley upstream is one of the modern glacier centers of southeast Tibet.The special characteristics of the lacustrine sediment and the ancient lake line in the Songzong Basin indicate that the lacustrine sediment is related to the blocking of the Purlung Tsangpo River by the glacier in Last Glacial Maximum from Dongqu Valley.Moreover,the depositing velocity of the lacustrine reaches to 2.29~2.82mm/a,more quickly than other close lakes in Tibet.Evidence also shows that the Songzong ice-dammed lake might run through the Last Glacial Maximum.

青藏高原东南部帕隆藏布江松宗地区晚更新世期间发生了一次可以识别的支谷冰川阻江形成冰川堰塞湖———松宗古湖的事件。松宗滑坡处的湖相沉积剖面厚度≥88m,其中厚达18.33m并具湖相沉积代表性的连续粉质粘土层底部和顶部的光释光年龄分别为22.5±3.3kaB.P.和16.1±1.7kaB.P.,属末次盛冰期。松宗滑坡处河谷两侧冰碛台地与湖相沉积的接触关系和空间特征指示该湖相沉积与末次盛冰期董曲支谷冰川阻塞帕隆藏布江有关。湖相地层的剖面沉积特征揭示出这个冰川堰塞湖可能贯穿于整个末次盛冰期,但整个帕隆藏布并没有形成统一的山谷冰川

 
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