喜马拉雅造山带,Himalayan orogen
1)Himalayan orogen喜马拉雅造山带
1.Cenozoic tectonic evolution of theHimalayan orogen as constrained by along-strike variation of structural geometry,exhumation history,and foreland sedimentation;喜马拉雅造山带新生代构造演化:沿走向变化的构造几何形态、剥露历史和前陆沉积的约束
2.The uplift of theHimalayan orogen is an interesting geological problem.喜马拉雅造山带的隆升,在地质学研究中是一个非常让人感兴趣的问题,为了对其进行定量研究,揭示隆升历史及幅 度等相关问题,运用磷灰石、锆石裂变径迹法对研究区淡色花岗岩进行了分析,所取样品的裂变径迹年龄位于17。
3.The study area lying in the north slope of the middle part ofHimalayan orogen involves abundant representative tectonic landforms.研究区位于喜马拉雅造山带中段北坡,构造地貌丰富、典型。
英文短句/例句
1.DISCOVERY OF COESITE-BEARING ECLOGITE FROM WEST HIMALAYAN TECTONIC LINK AND ITS ENLIGHTENMENT喜马拉雅造山带西构造结含柯石英榴辉岩的发现及其启示
2.Evolution of Deformation and Metamorphism During the Tectono Emplacement of the Granulite in the Middle Himalaya Orogen喜马拉雅造山带中段麻粒岩构造侵位过程中变质变形演化
3.Alpine-Himalayan Belt阿尔卑斯－－喜马拉雅山带
4.The frequency dispersions of Rayleigh waves and 3-D velocity structures in Himalayan collision orogenic zone and Qiangtang basin喜马拉雅碰撞造山带和羌塘盆地的瑞雷波频散与三维速度结构
5.Himalayan giant喜马拉雅山脉中的大山
6.Darjeeling Himalayan Railway喜马拉雅山大吉岭铁路
7.The present thickenning of Northern Qilian orogenic belt is the result of himalayan reorogency.而现今的北祁连造山带的缩短和抬升则为喜马拉雅期再造山作用的产物
8.In South Asia, the Himalayan glaciers could retreat causing water scarcity.在南亚，喜马拉雅山冰河的倒退造成了水荒。
9.Stratiform Geomorphology and Himalayan Tectonic Movement on the North China Mountains;中国华北山地的层状地貌与喜马拉雅构造运动
10.The Himalayan orogenic belt has some important features that distinguish it from the Andean and Alpine orogenic belts.喜马拉雅山带不同于安第斯山和阿尔卑斯山，有其自己的特征
11.The ice on the top of the Himalayas never breaks up喜马拉雅山山顶的冰从来不化。
12.Truth is, the Himalayas are between you two, and China"s never coming over the Himalayas.事实是：喜马拉雅山就在你们中间，而中国是从不翻越喜马拉雅山的。
13.Geochemistry and petrogenesis of the Triassic volcanic rocks in the east-central segment of Tethyan Himalaya.特提斯喜马拉雅带中段东部三叠纪火山岩的地球化学和岩石成因
14.Volcanic Rocks in the Central Belt of Tethyan Himalayas Since the Late Paleozoic and Their Implications;特提斯喜马拉雅带中段晚古生代以来的火山岩及其意义
15.Intracontinent Orogen and Metallogenesis in Himalayan Epoch:Changdu Large Composite Basin, Eastern Tibet藏东缘昌都大型复合盆地喜马拉雅期陆内造山与成矿作用
16.INFERRING THE TECTONIC STRESS FIELD OF HIMALAYA ARCUATE STRUCTURE FROM THE MULTIPLE FOCAL MECHANISMS由多个地震的震源机制解推断喜马拉雅弧形山系的构造应力场
17.HIMALAYAN COLLISION OROGENESIS AND FORMATION OF THE LARGE ENRICHED MINERAL DISTRICT: SCIENTIFIC PROBLEMS AND THINKING喜马拉雅碰撞造山作用与(超)大型矿集区的形成:科学问题与思考
18.Attribution of the Qinghai-Tibet Plate and Himalayan Orogeny青藏板块属南大陆范畴及喜马拉雅现代造山运动
相关短句/例句
Himalayan Collision Zone喜马拉雅期碰撞造山带
1.Mantle source characteristics of magmatic carbonatites from theHimalayan Collision Zone in western Sichuan,SW China:Evidence of Pb-Sr-Nd isotopes.;川西喜马拉雅期碰撞造山带岩浆碳酸岩的地幔源区特征——Pb-Sr-Nd同位素证据
3)Himalayan-Tibetan orogen喜马拉雅-青藏高原造山带
4)Alpine Himalayan belt阿尔卑斯喜马拉雅造山带
5)Himalayas[英][,him?"lei?z][美][h?"mɑlj?z]喜马拉雅山
1.Alpine pasture study in the North WesternHimalayas using GIS and remote sensing;利用遥感技术对喜马拉雅山西北部高寒草地的研究(英文)
2.TheHimalayas is near the South Asian monsoon region,with a special local circulation system induced by its steep topography and complex terrains.喜马拉雅山区毗邻南亚季风区,其陡峭的地形和复杂的地表状态在强烈太阳辐射条件下形成了特殊的局地环流系统。
6)Himalayan collision orogenesis喜马拉雅碰撞造山作用
1.Large and super large ore deposits discovered to date in the plateau and its adjacent regions are spatially and temporally associated with theHimalayan collision orogenesis.青藏高原及邻区是中国唯一的一块具有世界规模级的成矿富集区 ,迄今所发现的大型、超大型矿床 /矿集区 ,在时间抑或空间上均与喜马拉雅碰撞造山作用有着密切的联系 ,反映了与喜马拉雅碰撞造山作用过程相伴随的青藏高原周边及内部岩石圈薄弱地带的壳幔置换过程、层圈交换作用、流体活动及其地球化学分馏过程 ,是控制大型、超大型矿床 /矿集区形成的主要因素。
延伸阅读
雅拉神山
雅拉神山
塔公景区内有数座被藏传佛教称为神山的山峰和丘原草山。其中著名的有4座。雅拉雪山，藏语全称为“夏学雅拉嘎波”（意为东方白牦牛山），系我国藏区四大神山之一。该山地跨道孚、康定、丹巴三县，其西北面与塔公草原相连，形成雪山与草原交相辉映的壮美景观。雅拉雪山主峰海拔5820米，终年积雪覆盖，盛夏时日，在如花似锦的塔公草原上观瞻雅拉雪峰，有如临仙界之感。雅拉雪山已被甘孜州列为全州18个生态旅游区之一，名为“雅拉雪山天然生态旅游区”。该区风景优美，观光旅游资源类型众多，而且组合紧凑绝妙。其中最引人入胜的是在金字塔形的雅拉雪峰下，有一个碧蓝的高山湖泊－－友措，湖水与冰川之间为冰瀑布连接，湖周山坡为红杉和杜鹃灌丛，构成一幅精妙绝伦的天然画卷。在塔公寺后面，依次排列着三座丘草山，山上由嘛尼经幡组成三角形或四方形众多旗阵，在风中招展，更增加了三座山的神秘色彩，其场面亦十分引人注目，十分壮观。这便是被称为藏传佛教密宗事部三怙主的三座神山。
