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glacier
相关语句
  冰川
    Comments on 《The Problems of Quaternary Glacier and Environment in the East China《
    读《中国东部第四纪冰川与环境问题》
短句来源
    Comments on 《The Problems of Quaternary Glacier and Environment in the East China》
    读《中国东部第四纪冰川与环境问题》
短句来源
    APPLICATION SOFTWARE DESIGN AND OPERATIONOF GLACIER INVENTORY DATA BASE
    冰川目录数据库软件设计及其应用
短句来源
    A Traverse Expedition to the Lambert Glacier Basin,Eastern Antarctica
    东南极Lambert冰川流域路线考察
短句来源
    The Development and Evolution of Landscape in Front of Alpine Glacier──A Case Study from the Front Area of No. 1 Glacier in Tianshan Mountain
    高山冰川前缘地带景观生态的发育与演替──以天山1号冰川前缘为例
短句来源
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  “glacier”译为未确定词的双语例句
    The latest one was the Little Ice Age,including three phases of glacier advancing and shrinking. The two older phases were in about(1 720±60) a BP and(250±60) a BP. The Neoglaciation included three times of ice advancing and shrinking,of which the first and the last one respectly occurred in(4.2±0.4) ka BP and (2.9±0.3) ka BP.
    冰碛丘陵组地层属于新冰期沉积,3次冰进结束年代分别为:(4.2±0.4)ka BP,(2.9±0.3)ka BP,(1 720±60)a BP;
短句来源
  相似匹配句对
    in the form of piedmont glacier.
    之前,形成山麓冰川。
短句来源
    A Diary of Investigation of Glacier in Tibet
    西藏冰川考察日记
短句来源
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  glacier
Microorganisms Found in the Basal Horizons of the Antarctic Glacier above Lake Vostok
      
Problems of such kind arise in glaciology when one estimates the stability of snow on mountain slopes or determines the catastrophic movement of a glacier; the results can also be applied to solifluction phenomena [2, 3].
      
It was assumed that the temperature at the bed of the glacier could reach the melting point due to nonstationary heating and that the conditions would be produced for motion of the glacier.
      
Here we examine the nonstationary response of a glacier to small deviations of the system parameters from critical values corresponding to the stationary state.
      
Numerical investigation and self-similar solutions of the glacier-ocean interaction problem
      
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On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming...

On the Tibetan Plateau, remnants of the quaternary glaciation are of general oc-curence. Cirques, U-shape valleys, glacial-scoured lakers, till plains, terminal moraines, and drift boulders are wide spread features down to 4200 m in altitude. The authors believe that there was once a fairly continuous ice cover on the Tibetan plateau in late pleistocene. Here after the snow-line was raised, and the glaciers retreated gradually to their present positions. The reasons are two-fold: (a) a general warming of the world climate, (b) dessication of Tibet due to further uplift. The latter is evidenced by the obvious shrinkage of many lakes on the plateau. By correlating the moraines of this glaciation with the terrace of Zi-Ling Tsangpo and Yamdrok, we reach at the conclusion that this great Ice Cover was of late pleistocene in age. Since that time the glacier retreated in three recessional stages:

王明业等同志这篇论文提供了不少西藏高原上古冰川沉积以及其他遗迹的资料。从这些遗迹的分布来看,肯定有一个时期冰川的范围远比现代为大,那时冰川会从一些山谷通过一些低的山口漫溢到另一些山谷中,会覆盖广大的山麓地区,甚至达到盆地的中心。也可以想见某些宽平的山顶上可能有平顶冰川或所谓冰帽覆盖。在这种情况下,冰川的厚度一定也比现代为大,冰川的类型也更复杂的多。但是对于西藏高原这样一个广大的地区来说,作者等的观察范围以及获得的资料究竟还是非常有限,在达到的地区内也未见到有巨厚的,延续很广的冰碛物存在,所以据此即说除雅鲁藏布江谷地和金沙江、澜沧江、怒江的峡谷外西藏高原断续出现的冰盖是相当普遍的(虽然作者等也声明说和格林兰、南极洲的冰盖不一样),结论似乎下得太早。所引waxler的关于晚更新世雪线下降随的资料仅适用于一般海洋性气候的冰川作用区,是否能用到象西藏这样大陆性很强的地区是值得怀疑的。但是无论如何,作者等的资料是很宝贵的,关于西藏高原古冰川覆盖类型的问题,目前也确实还难说孰是孰非,所以我们还是把本文发表出来,以供对西藏古冰川研究的参考。

The valleys, basins, and sediments of the Lushan ( 29° N, 116°E ) were first interpreted as the product of pleistocene glaciers by J.S. Lee in 1933. Following similar conclusions on massifs throughout subtropical S.E. China the hypothesis was re-iterated in 1947.Similar views were expressed in the late 1960's and there is still a strong body of opinion in China that mountain glaciation was widespread south of the Chang Jiang.The Lushan has become the critical site, for some of the few foreign scientists...

The valleys, basins, and sediments of the Lushan ( 29° N, 116°E ) were first interpreted as the product of pleistocene glaciers by J.S. Lee in 1933. Following similar conclusions on massifs throughout subtropical S.E. China the hypothesis was re-iterated in 1947.Similar views were expressed in the late 1960's and there is still a strong body of opinion in China that mountain glaciation was widespread south of the Chang Jiang.The Lushan has become the critical site, for some of the few foreign scientists to visit it have accepted the glacial hypothesis.

李四光于1933年首次将庐山的谷地、盆地以及沉积物解释为更新世冰川作用的产物,并进而对中国整个东南部亚热带山地作了雷同的阐述,此后他又在1947年和六十年代后期重申了上述观点。这样,在中国便形成了一种见解,认为长江以南曾经历过广泛的山岳冰川作用,加之某些考察过庐山的外国学者亦接受了这一观点,就使得庐山成了具有关键性的地区。 用以支持冰川作用的证据有“冰斗”、“U谷”、“擦痕面”、“漂砾”、“栖歇石”、“冰碛垅”与“鼓丘”。对谷首形态的测量分析证明,没有一个“冰斗”深得足以产生冰川或能引起冰川基底滑动。“U谷”的大小和形状与冰川作用的成因不一致:一些是单向斜构造,另一些则是由流水作用形成的谷地,后者具有由重力作用形成的呈链状交错的横断面。也没有发现真正的岩盆。“栖歇石”是多节理的砂岩经差别风化之后形成的类似于羊背岩的产物。“冰碛”是由砂、粘土填充的巨砾所组成,次生粘土矿物是丰富的。深度风化、富含粘土的剖面可广泛分布到海拔1,300米处。不存在有意义的粉砂填质与带有冰川擦面的碎屑。沉积物的组构表明它们与当地的斜坡及扇形地表面形态有很好的相关关系。“冰碛垅”和“冰砾阜”可以看作是不同切割阶段的扇积砾。所谓的冰川动力...

李四光于1933年首次将庐山的谷地、盆地以及沉积物解释为更新世冰川作用的产物,并进而对中国整个东南部亚热带山地作了雷同的阐述,此后他又在1947年和六十年代后期重申了上述观点。这样,在中国便形成了一种见解,认为长江以南曾经历过广泛的山岳冰川作用,加之某些考察过庐山的外国学者亦接受了这一观点,就使得庐山成了具有关键性的地区。 用以支持冰川作用的证据有“冰斗”、“U谷”、“擦痕面”、“漂砾”、“栖歇石”、“冰碛垅”与“鼓丘”。对谷首形态的测量分析证明,没有一个“冰斗”深得足以产生冰川或能引起冰川基底滑动。“U谷”的大小和形状与冰川作用的成因不一致:一些是单向斜构造,另一些则是由流水作用形成的谷地,后者具有由重力作用形成的呈链状交错的横断面。也没有发现真正的岩盆。“栖歇石”是多节理的砂岩经差别风化之后形成的类似于羊背岩的产物。“冰碛”是由砂、粘土填充的巨砾所组成,次生粘土矿物是丰富的。深度风化、富含粘土的剖面可广泛分布到海拔1,300米处。不存在有意义的粉砂填质与带有冰川擦面的碎屑。沉积物的组构表明它们与当地的斜坡及扇形地表面形态有很好的相关关系。“冰碛垅”和“冰砾阜”可以看作是不同切割阶段的扇积砾。所谓的冰川动力构造可用局部构造活动来解释

Huanglong Temple Scenic Spot is located in the Min Mountains in northwest Sichuan and is blessed with beautiful scenery.Its precipitous mountains, steep valleys, elegant forestry, graceful lakes, picturesque caves and precious animals, dotted with a few ancient temples, are a high mountain tourists' resort worth exploiting,especially for its colourful terraced lake,which has as its name the Goddess" Lake.This scenic spot finds its origin in one of the ancient glacier paths to the north of Xuebaoding.It...

Huanglong Temple Scenic Spot is located in the Min Mountains in northwest Sichuan and is blessed with beautiful scenery.Its precipitous mountains, steep valleys, elegant forestry, graceful lakes, picturesque caves and precious animals, dotted with a few ancient temples, are a high mountain tourists' resort worth exploiting,especially for its colourful terraced lake,which has as its name the Goddess" Lake.This scenic spot finds its origin in one of the ancient glacier paths to the north of Xuebaoding.It has been formed under the combined influence of specific geological, topographical and geographical environment in the high mountains ever since the Quaternary Developmental process, such as moraine-erosive features, high mountain climate, radiation, karst effect and primeval forestry.

黄龙寺位于川西北的岷山之中,风景十分优美.它以峻峰、莽谷、香树、瑰湖、奇洞、异兽和配置得体的几座古老寺庙为特点,龙其是它的五彩梯湖,被称之为“瑶池仙景”.是一处可供开发的高山旅游胜地. 该自然风景发育在大雪宝顶北坡一条古冰川故道中.由于特殊的地质、地貌、第四纪发育史和高山自然地理环境:冰碛——冰蚀特性,高山气候、阳光,岩溶效应和原始森林等的综合作用,造就了这种奇特的自然美景.

 
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