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east southeast
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  “east southeast”译为未确定词的双语例句
     1 Review The rice frog Fejervarya limnocharis is one of the most common species in the south China, and distributed throughout the east, southeast and south of Asia.
     1 文献综述 泽蛙是我国南方的常见蛙类,广泛分布于亚洲东部、东南部和南部。
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     Bordering on the Huanghai Sea in the south, depends on Yalu River in the east, southeast of Donggang and Democratic People's Republic of Korea face each other across the river.
     南临黄海,东依鸭绿江,东南与朝鲜民主主义人民共和国隔江相望。
短句来源
     Principles of ecological system,natural preservation,landscape protection and making policy according to local actyak situation shoule be implemented. Different policies should be adopted to develop mountainous areas in west,east,southeast and southwest Dali.
     在未来的可持续发展中应依照生态系统原则、自然保护原则、景观保护原则和因地制宜原则, 分别对西部、东部、东南部和西南部山地的开发利用采取不同对策。
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     Three surveys were conducted on the this area in 1999 and 2000. Based on the first hand materials with the point of view of species population ecology, the conclusion can be drawn that there is a circle distribution of natural Ginkgo located in east, southeast and southwest Golden Buddha Mountains.
     在占充分资料的基础上 ,笔者运用植物群落学的理论和方法 ,对其进行慎重地群落学和种群生态学审查 ,得到下列结论 :以金佛山顶峰为核心的金佛山北部、东北、东部、东南和西南部 ,至今存在着一个孤形的银杏天然资源分布区 ,共有银杏天然资源约 180 0株 (~ 2 0 0 0株 )。
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     Regionally, the fault strike extended towards northeast in the west segment, towards east southeast in the middle segment and towards southeast in the east segment.
     在区域尺度上 ,主干边界断层总体走向西段为北东向、中段为近东西向、东段为北西西向 ;
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  相似匹配句对
     SOUTHEAST MONSOON AND RAINFALL IN EAST CHINA
     东南季风与我国东部的降水
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     The Model of East Asia and the Financial Turbulence in Southeast Asia
     东亚模式与东南亚金融动荡
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     in the Southeast of Hubei Province
     鄂东南职业教育存在的问题及对策
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     TRAVELING ALONE IN THE SOUTHEAST OF GUIZHOU
     独行黔东南
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     LOOKING AT THE SEA AT SOUTHEAST OF CHINA
     东南看海
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  east southeast
Adolescents came from six ethnic groups: White, African, Mexican, Other Latino, Filipino, and East/Southeast Asian Americans.
      
One species, Argulus japonicus, has been introduced from east/southeast Asia to all other continents, except Antarctica.
      
Three of the four individuals foraged east/southeast of the colony, over the middle continental shelf and the shelf break, between 43° and 51°S.
      
First-degree trend surfaces revealed that the deeper tubular wells occur towards east/southeast and exploit Paleozoic sediments as well fractured/fissured diabases/basalts, whereas the tubular wells in the west/northwest region are shallower.
      
When the upper-level winds are from the east-southeast, the surface winds fall into the inversion wind regime.
      
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This paper analyses the relationship between the first appearance of Culex tritaeniorhynchus in the early spring and the different wind directions on the ground and 850 HPA (about 1500 m heigh) by the continual observation of the appearance in the early spring of Culex tritaeniorhynens and the meteorological data in the years of 1982-1989, as compared with that of Anopheles sinensis. It was found that the percentage of the first appearance of Culex tritaeniorhynchus coinciding with the simulta- neous appearance...

This paper analyses the relationship between the first appearance of Culex tritaeniorhynchus in the early spring and the different wind directions on the ground and 850 HPA (about 1500 m heigh) by the continual observation of the appearance in the early spring of Culex tritaeniorhynens and the meteorological data in the years of 1982-1989, as compared with that of Anopheles sinensis. It was found that the percentage of the first appearance of Culex tritaeniorhynchus coinciding with the simulta- neous appearance of south to east-southeast winds (S-ESE) on the ground level and south-south west to west winds (SSW-W) at 850 HPA was signific- antly higher than that of Anopheles sinensis. The result demonstrated that the first appearane c of Culex tritaeniorhynchus in the early spring was related to both the S-ESE winds on the ground level and SSW-W winds at 850 HPA. It suggested that the pest origin of Culex tritaeniorhynchus in the early spring probably was immigrated from southern somewhere with the southern component weather system, But Anopheles sinensis has no such phenomenon.

本文根据1982~1989年对三带喙库蚊早春出现情况的连续观察结果,结合气象资料,分析了上海海滨三带喙库蚊首次出现与地面风和高空风的关系,并与中华按蚊进行比较。结果发现三带喙库蚊首次出现日与地面S-ESE风向和高空SSW-W风向的吻合率显著高于中华按蚊,说明三带喙库蚊早春首次出现与地面S-ESE风向和高空SSW-W风向有关,提示该蚊早春虫源随南支天气系统由外地迁入的可能性。

This paper provides a foundation for studying dynamics of marginal sea on the southeast of China mainland. It is based on the data from GPS observation metwork of China continent and Fujian region as well as the data of IGS (International GPS Service) tracing stations around China continent during the years of 1994 to 1997. Two mechanics models of blocks movement and intra-block deformation are established. Velocity and strain rate fields of present-day crustal horizontal movement in Fujian and its neighbouring...

This paper provides a foundation for studying dynamics of marginal sea on the southeast of China mainland. It is based on the data from GPS observation metwork of China continent and Fujian region as well as the data of IGS (International GPS Service) tracing stations around China continent during the years of 1994 to 1997. Two mechanics models of blocks movement and intra-block deformation are established. Velocity and strain rate fields of present-day crustal horizontal movement in Fujian and its neighbouring sea region are firstly studied. The results indicate that Fujian and its neighbouring sea region as a whole horizontally moves towards southeast or east-southeast namely towards sea, not only in China continent frame-work or in around China continent frame work, but also relative to Taiwan. The average velocity is 11.2 + 3.0mm/ a (by Fujian GPS network) or 14.0 ± 4.0mm / a (by China GPS network). Meanwhile, in Fujian area there is a northwest movement directing from sea to hinterland. The average velocity is 3.0 ± 2.6mm / a. The principal compressive axis of regional strain rate field lies in NW (NWW)-SE (SEE). The collision of indian plate and Euro-Asian plate affects Fujian and its neighbouring sea region by several blocks' side-transferring in China continent. The obduction and jam of Philippines-sea plate to Taiwan (southeast margin of Euro-Asia continent) also affects this region. The jointly affection still exists today. The former is stronger than the latter while the velocity field of the former is homogeneous and the one of the latte is not homogeneous.

为研究中国大陆东南部的边缘海动力学,基于中国大陆和福建区域的GPS观测网 以及环绕中国大陆的IGS(International GPS Service)跟踪站在1994—1997年间的测量数据, 建立块体运动和块内变形两种力学模型,研究了福建及其邻近海域现今地壳水平运动速度场 和应变率场.结果表明:无论在中国大陆还是在中国大陆周边框架内,或相对于台湾而言,福 建及其邻近海域均整体地向着东南或东偏南方向,即指向海洋的方向作水平运动.运动平均 速率为11.2±3.0mm/a(福建网)或14.0±4.0mm/a(全国网).然而在福建区域内还存在着 一种由海洋指向大陆内部的北西向运动,其运动平均速率为 3.0± 2.6mm/ a.区域应变率场 主压应变方位为NW(NWW)-SE(SEE).印度板块对欧亚板块的碰撞通过中国大陆内部各 块体间的侧向传递和菲律宾海板块对台湾(欧亚大陆东南沿)的仰冲与挤压,同时作用到福建 及其邻近海域。此种联合作用现今仍在继续进行中,前者的影响比后者更强烈,但前者形成的 速率场均匀,而后者不均匀。

HTThe distribution of velocity field of crustal horizontal movement and apparent strain field in the northeast margin of Qinghai-Xizang block is studied on the basis of GPS data in 1993 and 1999. A method for directly solving the parameters of block rotation and deformation from displacement observation is presented. The characteristics of tectonic motion and deformation in this area are studied preliminarily. The results show that (1) There exists a whole motion toward east-southeast with a velocity...

HTThe distribution of velocity field of crustal horizontal movement and apparent strain field in the northeast margin of Qinghai-Xizang block is studied on the basis of GPS data in 1993 and 1999. A method for directly solving the parameters of block rotation and deformation from displacement observation is presented. The characteristics of tectonic motion and deformation in this area are studied preliminarily. The results show that (1) There exists a whole motion toward east-southeast with a velocity of 9mm/a; (2) Gansu-Qinghai block in the south of this area moves faster, while Alashan block in the north of this area moves slower, the difference of the velocity between two blocks is near 6mm/a, the sinistral strike slip movement of Qilian-Haiyuan fracture zone is much more remarkable; (3) There exists NNE-NEE compressional movement from west to east; (4) Inside Alashan block and Gansu-Qinghai block, there exist NWW tensional deformation, the whole tensional deformation of Alashan block is even more obvious. In the meeting region of blocks in the west side of Ordos block, there exists compressional movement. HTH

利用青藏块体东北缘地区 1 993、1 999年GPS观测资料 ,给出了本区地壳水平运动速度场及视应变场分布图 ,提出了由位移观测值直接求解块体旋转和变形参数的方法 ,初步研究了本区构造块体运动与变形特征 .结果表明 :①本区存在整体性向东—东南方的运动(速率约 9mm/a) ;②南部的甘肃—青海块体的运动较快 ,而北部的阿拉善块体的运动较慢 ,二者运动速率相差近 6mm/a,祁连—海原断裂带左旋走滑运动显著 .③自西向东存在北北东—北东东向压性运动 ;④阿拉善块体、甘肃—青海块体内部存在北西西向张性变形 ,阿拉善块体的整体张性变形更显著 ,鄂尔多斯块体西侧的块体交接地带为压性运动 .

 
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