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central south china
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  中南地区
     A cohort mortality study of 28453 subjects who employed in 1972-1974 and at least worked one year was conducted in central south China.
     对中南地区10个钨矿1972—1974年入矿(工龄至少1年)的在册职工28453人进行了队列研究。
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     Adhere to the Scientific Concept of Development and Facilitate Comprehensive, Coordinated Regional Development through Technology Innovation: Suggestions on the S&T Work in Central South China
     坚持科学发展观,以科技创新促进区域统筹协调发展——对中南地区科技工作的思考和建议
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     The Geo periodicals of the Central south China Area were mainly founded by the local geology organs, and the geographical periodical was mainly founded by advanced schools, while the periodical founded by learned society organs was emphasized on mining industry.
     中南地区的地质期刊主要由地方地质研究机构创办 ,地理期刊主要由高校创办 ,学会组织创办的期刊偏重于矿业 ;
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     Application Research of Evaporative Cooling Technique In Areas of central south China
     蒸发冷却技术在我国中南地区应用的可行性研究
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     The metamorphic deposits are those in the northeastern part of Central South China, the eastern part of East China, North China and Northeast China. The most typical of them are late Early Proterozoic sedimentometamorphic deposits.
     中国变质磷矿主要分布在中南地区的东北部、华东地区东部、华北及东北地区 ,早元古代晚期沉积变质磷矿最具代表性。
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     Robust evidencoes of the existence of the barrier layer(BL) in the central South China Sea(10°~19°N,108°~122° E) are provided,which occurs most frequently in summer(52.8%),and then autumn(41.0%) and spring(10.5%).
     南海中部海域(10°~19°N,108°~122°E)存在显著的季节变化的障碍层. 障碍层发生概率夏季最大(52.8%),秋季次之(41.0%),春季最小(10.5%).
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     The distribution and source of thorium in the sediment-section of 13°30'N, 113°-118°E in Central South China Sea are reported in this paper.
     本文通过测定沉积物中钍的含量,了解到在南海中部13°30′N,113°—118°E的沉积断面上,钍的分布特征是由113°E向118°E方向减少。
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     Seasonal and annual variations of marine sinking particulate flux during 1993~1996 in the central South China Sea
     1993~1996年南海中部海洋沉降颗粒通量的季节和年际变化
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     According to the results of 14C dating of 17 sediment samples from the central South China Sea, 14C dating method and procedure are discribed.
     本文根据南海中部海区17个样品的~(14)C年龄测定结果,叙述了深海沉积物的~(14)C测年方法和步骤;
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     The analyses of 18 elements in 91 surface sediments from the Central South China Sea (12-21℃, 110-118℃, 1983.9-1984.7) reveal the following geochemical characteristics: (1) its sediments are characterized by the geochemistry of semipelagic sediments;
     根据1983年9月—1984年7月所调查的南海中部91个表层沉积物中Fe,Mn等18种元素分析并结合其它资料的详细研究结果表明:(1)南海中部沉积物具有在近海—深海环境下形成的半深海沉积物的地球化学特征;
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  相似匹配句对
     CENTRAL CHINA AREA
     非物质文化遗产——我们的精神家园 华中地区
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     South China Area
     非物质文化遗产——我们的精神家园 华南地区
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     The Modernization in Central China
     我国中部地区的现代化浅析
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     Rangeland in South China.
     中国南方的牧野
短句来源
     CRETACEOUS NON-MARINE LAMELLIBRANCHIA FROM CENTRAL-SOUTH CHINA
     中南地区白垩纪淡水瓣鳃类
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  central south china
We show that the northeasternmost South China Sea basin, which may have undergone unique evolution since the late Mesozoic, is markedly different from the central South China Sea basin and the Huatung Basin, both geologically and geophysically.
      
Seasonal Variability of Thermohaline Front in the Central South China Sea
      
The Dengying Formation exposed at Sansha, Human Province, central South China, comprises unfossiliferous dolomitized platform carbonates and a solution-collapse breccia sequence.
      
Pinatubo produced an extensive, largely co-ignimbrite-derived airfall ash layer on Luzon Island and across the central South China Sea.
      
Tie-series sediment trap materials at different water depths and surface sediments in northern and central South China Sea (SCS) were analyzed for organic carbon, amino acids, amino sugars and carbohydrates.
      
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First, the spatial distribution of rainfall anomalies of Central-South China (23-34°N, 100-113°E) was examined by means of the empirical orthogonal function analysis. The data used in this paper are collected from 60 stations, monthly mean rainfall observations from April to October during the last 27 years (1953-1979). The monthly mean rainfall anomalies in Central-South China have been classified into fourteen types. The first four types ane characterized by the seasonal...

First, the spatial distribution of rainfall anomalies of Central-South China (23-34°N, 100-113°E) was examined by means of the empirical orthogonal function analysis. The data used in this paper are collected from 60 stations, monthly mean rainfall observations from April to October during the last 27 years (1953-1979). The monthly mean rainfall anomalies in Central-South China have been classified into fourteen types. The first four types ane characterized by the seasonal migration of the rain-belt,and each of the other types reflects a definite structure which can be easily interpreted with synoptic-climatological knowledge.Secondly, the correlation coefficients were calaulated to show the relationships between the rainfall and the discharge at the upper Changjiang for every month from April to October. The results show that regions in which correlation coefficients are higher than 0.37 (at 5% significant level) shift obviously with the season. The region or the socalled key region, in which rainfall is more important for the discharge, sometimes coincides with the variance centers of the first eigenvector and sometimes not. In most cases this key region is in accordance with the second eigenvector, or even the third eigenvector. It turns out that in spite of the close relation between the rainfall and the discharge at the upper Chang-Jiang, both of then are somewhat independent in their variations. So, we must pay more attention to the difference between them in studying the formation of discharge anomolies and in making long-range forecast of droughts and floods at the upper Chang-Jiang.

本文分析了23—34°N,100—113°E所包围地区内汎期(4—10月)月雨量的分布特征,及其对长江上游流量的影响。在上述范围内选取了60个雨量站,资料年代从1953到1979年计27年。采用特征向量分析,把这一地区汎期月雨量的分布归纳为14种型,并讨论了各型的特征。同时计算了长江上游各月平均流量与同期各站雨量的相关,根据相关分布图,探讨了各月雨量分布对长江上游流量的影响。

A map of sediment types in scale of 1:3,000,000 is compiled on the analytical data including grain size, the composition of sand fraction, the light and heavy detrital minerals, clay minerals, the fauna identification of foraminifera, calcareous nannoplankton, radiolarian, diatom and spore-pollen, chemical quantitative analysis and 14C dating et al of 130 surface sediment samples from the central South China Sea involving water depth of 480-4400 m in two cruises of October 1983 and June 1984. Based on...

A map of sediment types in scale of 1:3,000,000 is compiled on the analytical data including grain size, the composition of sand fraction, the light and heavy detrital minerals, clay minerals, the fauna identification of foraminifera, calcareous nannoplankton, radiolarian, diatom and spore-pollen, chemical quantitative analysis and 14C dating et al of 130 surface sediment samples from the central South China Sea involving water depth of 480-4400 m in two cruises of October 1983 and June 1984. Based on the map main types and distribution of the sediments as well as deep sea sedimentation are discussed.

本文以1983年10月和1984年6月两个航次期间在南海中部海域内采集的130个站位的沉积物组分全面鉴定(粒度、砂级全组分、轻重碎屑矿物、粘土矿物、有孔虫、钙质超微、放射虫、硅藻和孢粉等生物鉴定、化学定量分析、少量~(14)C测年等)为基础,以1∶300万南海中部沉积物类型图为依据,讨论了沉积物主要类型、分布和沉积作用特点。

Six assemblages and five subassemblages of benthic foraminifera are established on the basis of 53 surface sediment samples from the central South China Sea. Planktonic foraminifera in surface sediments of this area can be divided into four assemblages of different water depths. The main factors controlling the distribution of foraminifera in the area are dissolution of deep-sea carbonate, water masses, sea-floor relief and relict sediment.

本文根据南海中部海区53个表层沉积物样的有孔虫分析,初步确定了六个底栖有孔虫组合和五个亚组合,而浮游有孔虫可分为四个不同水深的组合。控制本区有孔虫分布的主要因素是深海碳酸盐溶解作用、水团、海底地形以及残留沉积。

 
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