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central asian
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  中亚
     Its Sr(T)i values are between 0.704 and 0.71659,εNd(T) values between +1.3 and +2.8, and TDM-2 from 0.93 to 0.81 Ga, which are similar to those of high (positive)-εNd(T) value granites from the Central Asian Orogenic Belt.
     该岩体Sr初始值变化于0.704-0.71659之间。 εNd(T) 值为正值(+1.3-+2.8),模式年龄TDM-2为0.93-0.81Ga,与中亚造山带典型的高(正)εNd(T)值花岗岩相同。
短句来源
     AN IMPORTANT VECTOR PHLEBOTOMINE SANDFLY-Phlebotomus (Larroussius) smirnovi Perfiliew, 1941 of NORTH-WEST CHINA AND HER NEIGHBOURING CENTRAL ASIAN COUNTRIES AND MONGOLIA
     中国西北地区和毗邻中亚诸国以及外蒙的一个重要传播媒介—斯氏白蛉Phlebotomus (Larroussius) smirnovi Perfiliew, 1941
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     Analysis on Water Crisis and the Central Asian Security
     水危机与中亚安全分析
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     The Nature of 1916 Central Asian Uprising and its Historical Meaning
     1916年中亚起义的性质及其历史意义
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     The highest rate of sweet kernel(93.1%)was observed in the Central Asian eco-geographical group compared to Ili wild population(0.9%)and North China group(44.4%).
     ⑦伊犁野杏、中亚杏及华北杏甜仁比率分别为0.9%、93.1%和44.4%。
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     Nature, Common Character and Characteristics of Economic Transition in East European and Central Asian Countries
     Nature,Common Character and Characteristics of Economic Transition in East European and Central Asian Countries
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     Then we get the best lithospheric equilibrium compensation depth of 75 km in the Central Asian Region and the basic parameters of the lithospheric elastic slab in this region by linear inversion.
     求出了亚洲中部地区岩石圈均衡的最佳补偿深度为75km,通过线性反演得到该区岩石圈弹性板复合补偿模型的基本参数。
短句来源
     EQUILIBRIUM COMPENSATION DEPTH AND INVERSION ANALYSES FOR ELASTIC SLAB MODEL OF THE LITHOSPHERE IN THE CENTRAL ASIAN REGION
     亚洲中部地区岩石圈均衡补偿深度和弹性板模型反演结果分析
短句来源
     We conclude that the asthenolayer with the low cohesion in the depth of 75 km in the upper mantle of low cohesion coefficient may be the approximate position of the large-scale lithosphere equilibrium in this region. Moreover, we discuss the mechanism of the elastic slab of the Central Asian Region lithosphere.
     指出粘滞系数较低的上地幔75km附近存在的低粘滞度的软流层,可能是达到该区大范围岩石圈均衡的大体部位,并对亚洲中部地区大陆弹性板机制等问题进行了讨论。
短句来源
     This may provide an explanation for the relatively mass occurance of UHPM belts within central Asian zone and adjacent Qinling-Qilian-Kunlun zones.
     上述阶段和上述范围内集中形成了多条超高压变质带,这种这指示了古亚洲洋及邻区的独特构造背景与超高压变质事件之间的成因联系。
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  相似匹配句对
     Central Asian Community:Growth and Challenge
     中亚共同体:成长与挑战
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     Security Strategies of the Central Asian Countries
     中亚国家的安全战略
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     benefit for central;
     以效益为中心 ;
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     ASIAN ART
     亚洲艺术品
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     Asian Invasion
     亚洲大入侵
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  central asian
Independence of the Central Asian Faunistic Region (According to the Distribution of Lizards (Reptilia, Sauria))
      
Central Asian area above 2000 m was studied to test the independence of the Central Asian Mountain region in the herpetogeographical map of the Palearctic Region and the neighboring Sahara-Gobi Desert region.
      
The dominance (over 50% of the total number of species) of mountain Central Asian or other species groups allowed us to assign the studied area to either the Central Asian mountain region or Sahara-Gobi desert region.
      
Considering a large number of endemic species (28% of the total fauna), the Central Asian mountain area should be recognized as an independent region rather than a subregion of the Sahara-Gobi Desert region.
      
Some Aspects of the Genesis of Halogenic Sequences: Evidence from the Central Asian Halogenic Basin
      
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The Gurbantungut Sandy Desert in Northern Xinjiang occupies a transi-tional position between the Central-Asian and Kazakhstan Deserts in its floraas well as vegetation, yet has its unique characteristics. The vegetation of the sandy district of Gurbantungut consists mainly of9 communities and 3 congregations. Because of the differences in naturalconditions, flora and plant communities among different parts, the Gurbantun-gut may be subdivided into 3 phytogeographical subregions; Southwestern,Southeastern...

The Gurbantungut Sandy Desert in Northern Xinjiang occupies a transi-tional position between the Central-Asian and Kazakhstan Deserts in its floraas well as vegetation, yet has its unique characteristics. The vegetation of the sandy district of Gurbantungut consists mainly of9 communities and 3 congregations. Because of the differences in naturalconditions, flora and plant communities among different parts, the Gurbantun-gut may be subdivided into 3 phytogeographical subregions; Southwestern,Southeastern and Northern. In a detailed scheme of division of Asian deserts, the Jungar Basinincluding Gurbantungut may be divided as an independent phytogeographicalunit, parallel with Central-Asian, Kazakhstan and Middle-Asian Deserts.

位于北疆准噶尔盆地中部的古尔班通古特沙漠,其植物区系和植被居于亚洲中部荒漠和哈萨克斯坦荒漠之间的过渡,但本身具有自己的特点。沙地植被主要由9个群落和3个群聚组成。由于各部分的自然条件、区系和群落性质的差别,沙漠本身在植被上又分异成三个不同的部分:西南区、东南区和北部区。在亚洲荒漠的详细划分方案中,包括古尔班通古特沙漠在内的准噶尔盆地荒漠可以作为独立的植物地理区划分出来。

East Xizang region belongs to Sino-Himalayan forest sukingdom of Horaltic Kindom. (Fig. 1 ) . The species of wild spermatophytes in this region amount to 2318 (Tab, 1 ),constituting 44.79% of the total number in Xizang. 32.66% of them, e.g. 757 species are the endemics to China, among which 49% (371 species) are distributed only in South Hengduan Mountains, such as Abies ern-estil, A. forrestii, Larix potaninii,Picea brachytula var. complanata, P. liki-angesis var. hirtella, Pinus densata, They are dominats...

East Xizang region belongs to Sino-Himalayan forest sukingdom of Horaltic Kindom. (Fig. 1 ) . The species of wild spermatophytes in this region amount to 2318 (Tab, 1 ),constituting 44.79% of the total number in Xizang. 32.66% of them, e.g. 757 species are the endemics to China, among which 49% (371 species) are distributed only in South Hengduan Mountains, such as Abies ern-estil, A. forrestii, Larix potaninii,Picea brachytula var. complanata, P. liki-angesis var. hirtella, Pinus densata, They are dominats of subalpine coniferous forest in East Xizang.There are 425 endemic species to Xizang, e. g. 18.33% of the total number. Among them 340 species represent the region's endemics, including 50 species of Compositae, 21 of Rosaceae, 20 of Gramineae, 16 of Papaveraceae and so on.Altogether 1182 species are attained including the endemics of Xizang and of the 0 her parts of China, that is, 50.99% of the total number of species. From this percentage we may see that flora in East Xizang is a young and quite flourishing species-endemism.The elements of East Asian distribution pattern occupy an important place in the flora of East Xizang and consist of 753 species, constituting 31. 7 % of the total number. Among them 311 species belong to East Himalayas and 195 to the whole Himalayas. There are a lot of common alpine Plants Himalayas, such as Cassippe selaginoides. Diplarche multiflora, Saxifraga (22 species) , Rholdod-endron (20) , Primula (24) , Gentiana (10) , Pedicularis (16) . It appears that the flora of East Xizang region, asapart of Sino-Himalayan forest flora of Horaltic Kingdom, is closely related to East Asiatic flora. The so-called relationship between East Xizang flora and Mediterranean-Central Asian flora is really next' to nothing.East Xizang region is subdivided into 2 subregions:A. Hengduan Mountains subregion with 64 endemic species of 37 genera of 21 families, including monotypic genus Salweenia of the primitive tribe Soph-oreae in Leguminosae. It was very probably a member of Gondwanaland flora which hed survived after finding a refuge in the midstream valleys of Nujiang River (Salween) and Lancang River (Mekong)B. Bomi-Gyaca subregion with 276 endemic species of 90 genera of 30 families includes Quercus tungmainsis, Brassiopsis Karmalaica, Agapetes praeclara, Aconitum (12 species) , Corydalis (14) , Pedicularis (14) and so on. The monotypic genus Parapteropyrum tibeticum is found in this sudregion and appears to be the definite Tethysian element during the drawing back of Tethys sea

本文分析了西藏东部植物地区的区系结构並划分两个亚地区,指出本地区是东亚植物区系的重要的物种分化中心。

The wenduermiao—Bailaimiao region in Inner Mongolia formed the trench—island is a system between the central Asian—Mongolia oceanic plate of Early palaeozoic and the North China continental platform. The subduction speed of the Wenduermiao subduction zone is 5.38 cm/year,and the extinction depth of this zone reaches 171.14kin,so this subduetion zone is a extra-lithospheric deep rift.

内蒙古温都尔庙—白乃庙地区是早古生代中亚—蒙古海洋板块与华北陆台之间的海沟—岛弧体系。温都尔庙板块俯冲带的俯冲速度为5.38厘米/年。俯冲消减的深度达171.14公里,是一条超岩石圈的深断裂带.

 
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