青藏高原北缘,northern margin of the Qinghai-Tibet Plateau
1)northern margin of the Qinghai-Tibet Plateau青藏高原北缘
1.Uplift period of thenorthern margin of the Qinghai-Tibet Plateau:evidences from the Altyn Mountains and Qaidam Basin;青藏高原北缘的隆升时期——来自阿尔金山和柴达木盆地的证据
英文短句/例句
1.ISOSTATIC ANOMALY,REMAINDER ANOMALY AND EARTHQUAKES IN NORTH MARGIN OFQINGHAI-XIZANG PLATEAU青藏高原北缘均衡异常、剩余异常与地震
2.The mechanisms of different uplifts in the Yinshishan area, northern edge of Qinghai-Tibet plateau青藏高原北缘银石山地区差异隆升机制
3.Analysis on the Topographic Gradient and Geographical Meaning of Mt.Konggur,in the Northern Edge of Qinghai-Tibet Plateau青藏高原北缘公格尔山地区地形梯度的剖析
4.Tectonic Uplift and Cenozoic Sedimentary Evolution in the Northern Margin of the Tibetan Plateau;青藏高原北缘新生代沉积演化与高原构造隆升过程
5.Study on Eco-environment Degradation in the Northeastern Margin of the Qinghai-Tibetan Plateau;青藏高原东北边缘生态环境退化研究
6.The Tectonics Activity & Engineering Hazard Effects in the Northeast Margin of Qinghai-Tibet Plateau青藏高原东北缘构造活动及其工程灾害效应
7.On the boundary of Tethyan tectonic domain on northeastern margin of the Tibetan Plateau.青藏高原东北缘特提斯构造域界线的探讨
8.Cenozoic Uplift and Growth of Northwestern Margin of the Tibetan Plateau;青藏高原西北缘新生代构造隆升及扩展
9.Study on Late Cenozoic Geomorphic Processes of Typical Regions Along the Eastern and Northeastern Tibetan Margins青藏高原东缘、东北缘典型地区晚新生代地貌过程研究
10.Tectonic Deformation on Northwestern Margin of Tibetan Plateau during Pliocene-Pleistocene and Uplift of the Tibetan Plateau;青藏高原西北缘上新世—早更新世构造变形与高原隆升
11.Investigation of the Traditional Tibetan Medicine Plant Resources of Allium in the Eastern Area of Qinghai-Tibet Plateau青藏高原东缘葱属藏药植物资源调查
12.Investigation of the traditional Tibetan medicine plant resource of the Artemisia in the Eastern of Qinghai-Tibet Plateau青藏高原东缘蒿属藏药植物资源调查
13.Traditional Tibetan medicine plant resource of Polygonaceae family in eastern of Qinghai-Tibet plateau青藏高原东缘蓼科藏药植物资源调查
14.Traditional Tibetan medicine plant resources of Orchidaceae family in the Eastern Qinghai-Tibet Plateau青藏高原东缘兰科藏药植物资源调查
15.Studies on Population Ecology of Subalpine Birch Forests in the Northeast Border of the Qinghai-Xizang Plateau;青藏高原东北边缘亚高山桦木林种群生态学研究
16.The Seismic Tomography on the Velocity Structure of the Crust and Upper Mantle in the Northeastern Margin of the Qinghai-Tibetn Plateau青藏高原东北缘地壳上地幔速度结构的地震层析成像研究
17.An Integrated Study on Late Cenozoic Tectonic Deformation in the Liupanshan-Madongshan Area, Northeastern Margin of the Tibetan Plateau青藏高原东北缘六盘山—马东山地区晚新生代构造变形综合研究
18.Late Neogene Geology and Environment Evolution at Zoig(?) Basin of Northeast Margin of Qinghai-Tibet Plateau;青藏高原东北缘若尔盖盆地晚新近纪地质及其环境演化
相关短句/例句
northeastern margin of the Qinghai-Tibet Plateau青藏高原东北缘
1.Geochemistry of hydrocarbon source rocks in the Liupanshan basin at thenortheastern margin of the Qinghai-Tibet Plateau;青藏高原东北缘六盘山盆地烃源岩的地球化学特征
2.Tertiary Duofuton Na-rich mafic volcanic rocks,onnortheastern margin of the Qinghai-Tibet Plateau and their tectonic implications;青藏高原东北缘多福屯第三纪钠质基性火山岩及构造启示
3)northwestern margin of the Qinghai-Tibet Plateau青藏高原西北缘
1.Characteristics of late Miocene A-type granite on thenorthwestern margin of the Qinghai-Tibet Plateau and its significance.;青藏高原西北缘中新世晚期A型花岗岩的特征及意义
4)northeastern border of the Qinghai-Tibet plateau青藏高原东北边缘
1.Population age structure of birch forests in the subalpine of thenortheastern border of the Qinghai-Tibet plateau;青藏高原东北边缘亚高山桦木林种群年龄结构
5)Northeastern margin of Tibet Plateau青藏高原东北缘地区
6)Eastern margin of the Tibetan Plateau青藏高原东缘
1.Based on Digital Elevation Model(DEM) analysis,the large-scaled geomorphology of eastern margin of the Tibetan Plateau can be divided into four zones,the Tibetan Plateau,the Longmen Mountain,the Chengdu Basin,and the Uplift Zone of Eastern Sichuan Basin.文章利用数字高程剖面将青藏高原东缘分为4个大尺度地貌单元,即青藏高原地貌区、龙门山高山地貌区、山前冲积平原区(成都盆地)和四川盆地东部隆起区。
2.This research provides morphological evidences for further study on tectonic activities in the eastern margin of the Tibetan Plateau.本研究为进一步研究青藏高原东缘的活动构造提供了重要的地貌证据。
延伸阅读
青藏高原.20世纪后半叶，有关青藏高原的各种科学研究不断升温，青藏高原也成了各国科学家和探险家所向往的“圣地”。年轻而古老的青藏高原它是世界屋脊……在中国的西南边陲，有一片海拔平均在4000米以上，面积达230万平方公里的土地，这就是号称“世界屋脊”和“地球第三极”的青藏高原。它东连云贵高原和四川盆地，西达万山之宗的帕米尔高原，北邻中国内陆沙漠地带，南眺热带亚热带风光的印度大平原。它雄奇高峻、傲视四方，以奇异的地理构造和地貌景观，以及独特的文化积淀和历史皱褶，堪称世界一绝。它是年轻的……青藏高原原本是全球发展最年轻的高原，这里曾经是波涛汹涌的“古特提斯海”，南北两侧分别盘踞着地球上两个巨大的大陆。直到距今4000万年前后，印度板块向北漂移，在这里与欧亚板块产生碰撞而形成南北方向的撞压，从而使这一地区迅速隆升，以高出其周围地区5000米的巨大高差突兀于大气流层中，从而成为全球瞩目的“第三极”。它也是古老的……青藏高原是我国及至亚洲几大河流，如长江、黄河、印度河、恒河、雅鲁藏布江、怒江（萨尔温江），澜沧江（湄公河）的发源地。这里的地理环境造就了青藏高原极富特色的自然资源。动物资源：国家一级保护动物白唇鹿、野牦牛、云豹、雪豹、藏野驴、藏羚羊；国家二级保护动物马鹿、马麝、岩羊、白腹锦鸡、雉鸡、藏马鸡等；植物资源：虫草、贝母、松茸等等。当您走上青藏高原……预防高原适应不全症：在海拔4000米以上的地段，约60—100的人均发生急性缺氧反应或者疾病。症状：头痛、头昏、心慌、气短、食欲不振、恶心呕吐、腹胀、胸闷、胸痛、疲乏无力、面部轻度浮肿、口唇干裂等。危重时则会血压增高、心跳加快，甚至出现昏迷状态。治疗：食物应以易消化、营养丰富、高糖、含多种维生素的最好，多食蔬菜、水果、严禁饮酒，以免增加耗氧量。睡眠时枕头要垫高，半卧姿势最佳。如症状严重，即使在静息时也十分明显时，则应立即吸氧，然后送医院就诊。
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