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加拿大西部
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  canadian western
     On the Status and Effect of the National Policy in Canadian Western Development
     论“国家政策”在加拿大西部开发中的地位与作用
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     By doing so, 1 would like to do something useful to the economic and cultural exchanges between the Chinese people and the people living in the Canadian west and show the experiences and the lessons of the Canadian Western Regionalism to the Chinese government to be used for reference to the Chinese western exploitation.
     从而加深我们对西部加拿大的了解,弄清西部离心主义与魁北克分离主义的区别,探索加拿大未来发展的道路,同时,推动我国与西部加拿大的经济文化交流,吸取加拿大西部发展的经验和教训,为我国西部的开发和建设提供借鉴。
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  “加拿大西部”译为未确定词的双语例句
     A Study of the Regionalism of Western Canada
     加拿大西部地方主义研究
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     A City for Living
     生活之城——加拿大西部城市印象
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     I try to pursue the reasons leading to the western Canadian regionalism, to follow its lines of development and to search for ways to help the west move out of this kind of difficult positions.
     本文即力图通过考察加拿大西部地方主义产生的历史背景和发展变化的历程,探讨西部地方主义长盛不衰的原因,并进而以西部地方主义为范例,研究整个加拿大地方主义盛行、联邦主义衰微的机制性因素,寻找西部乃至整个加拿大走出地方主义园囿之路。
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     The chemical laboratory of the Semiarid Prairie Agricultural Research Centre of Canada is very influential in western Canada.
     加拿大半干旱草原农业研究站化学实验室在加拿大西部很有影响。
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     Analysis of acid gas injection projects underway in North America, and in Western Canada in particular, show that disposal of H2S into depleted reservoirs may have already reached levels that begin to affect sulphur supply from that region.
     对北美,尤其是加拿大西部正在进行的酸性气体回注项目进行分析,结果表明,将H2S回注入耗竭的矿井已达到相当的规模,并开始影响该地区的硫磺供应。
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     A Study of the Regionalism of Western Canada
     加拿大西部地方主义研究
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     Introduction and Selection of Canada Forages in the West of Jilin Province
     吉林西部加拿大牧草引种及筛选试验
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     Boundary of Western China
     西部的界限
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     Sketches on Life in Canada
     倾情加拿大
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     Der Ring des Nibelungen In Canada
     加拿大的“指环”
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  canadian western
For the identification of the binding sites of glutathione (GS) in glutenins, flour of the wheat cultivar " Canadian Western Red Spring " was mixed with water containing 35S-labelled reduced GS as a tracer.
      
Numerical simulation of cold easterly circulations over the Canadian Western Plains using a mesoscale boundary-layer model
      
Arctic outbreaks over the Canadian Western Plains during the late spring period frequently take the form of a cold east-northeasterly flow over a warmer, sloping surface.
      
Comments on 'numerical simulation of cold easterly circulations over the Canadian Western plains using a mesoscale boundary-laye
      
Since 1994, progressively more protein grade increments have been added to existing standards for Canadian Western Red Spring (CWRS) wheat.
      
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In contrast with the Tertiary, the Late Cretaceous palynofloras of the China mainlandand its continental shelf are sparsely distributed in space and are discontinuous in time. Alto-gether 35 palynoferous stratigraphic units in 28 areas or basins have been recorded based onthe published data. The Songliao Basin in NE China and the W. Tarim Basin in NW Chinahave displayed a rather complete succession of Late Cretaceous palynofloras. Based on theevolution level of angiospermous pollen observed and correlation with...

In contrast with the Tertiary, the Late Cretaceous palynofloras of the China mainlandand its continental shelf are sparsely distributed in space and are discontinuous in time. Alto-gether 35 palynoferous stratigraphic units in 28 areas or basins have been recorded based onthe published data. The Songliao Basin in NE China and the W. Tarim Basin in NW Chinahave displayed a rather complete succession of Late Cretaceous palynofloras. Based on theevolution level of angiospermous pollen observed and correlation with Late Cretaceous paly-nofloras in some other areas of the world, four major evolutionary stages of the Late Creta-ceous palynoflora in China have been recognized as follows: 1)Prebrevaxonate pollen stage——Cenomanian Among angiospermous pollen, tricolpate forms with simple aperture occurring frequent-ly in Albian strata are still present, such as Psilatricolpites, Retitricolpites, Tricolpopollentiesand Cupuliferoidaepollenites. While forms of longaxonate tricolporate types are rarely seen,such as Tricolporopollenites, those brevaxonate tricolporate pollen grains, usually small insize, are occasionally present, such as Gothanipollis, Cupanieidites, Syncolporites, Retitricol-porites oblatus and Nyssapollenites? The cosmopolitan Asteropollis, Clavatipollenites and Lil-iacidites began to decline,sporadically occurring in this stage. Later, a triporate pollen ele-ment, Archaeotriporopollis with triangular outline has been seen in some areas. The Contentof angiospermous pollen is not over 10% in the stage. 2)Brevaxonate pollen stage——Turonian--Santonian As compared with the preceding stage, angiospermous pollen grains of this stage in-crease greatly both in diversity and in abundance. They often have complex aperture and ad-vanced structure with columellate exine. Brevaxonate tricolporate and/or tricolpate pollengrains with a larger body size have substantially increased, including such common elementsas Cranwellia, Borealipollis, Lythraites, Loranthacites, Beaupreaidites, Xinjiangpollis, andNyssapollenites. Together with Cupanieidites, Gothanipollis, Syncolporites, etc., the brevax-onate pollen grains play a more outstanding role in composition than other types of an-giospermous pollen grains, while triporate pollen grains are still not greatly developed sincetheir first occurrence in the preceding stage. Psilatricolpites and Retitricolpites became less important and meagre in this stage as compared with the first stage, while Clavatipollenitesand Asteropollis disappear in this stage. Some forerunners of Triprojectacites andNormapolles appear individually in the upper part, such as Aquilapollenites pyriformis andExtratriporopollenites. Although the angiosperm pollen grains become greatly developed dur-ing this stage, their content is no more than 30% of the total. 3)Advanced angiospermous pollen stage——Campanian This stage is characterized by the high diversity of angiospermous pollen and complexexine with advanced aperture. In addition to the continual presence of brevaxonate tricol-p(or)ate pollen which flourished in the second stage, some genera become relatively rich,such as Proteacidites, Callistopollenites, Cosoliduspollenites, Betpakdalina, Crassimargin-pollenites, Rugupolarpollenites, Jiangsupollis, Aquilapollenites, Jianghanpollis, Parvipro-jectus and Macicorpus. Normapolles pollen grains are still sparsely present, with a contentless than 1% of the total. Those angiospermous genera with a close affinity to the livingplants are the first to occur, although in small amounts. 4)Ulmoideipites stage——Maastrichtian In addition to the continuous flourishment of some characteristic genera, viz.,Aquilapollenites, Callistopollenites, Proteacidites, Betpakdalina, Jianghanpollis and Jiang-supollis in this stage, those pollen grains which are closely related to such families as Ul-maceae, Sapindaceae, Betulaceae, Juglandaceae and Fagaceae, etc., are more or less devel-oped, occurring in association with a few elements of Wodehouseia in some areas. After reviweing the literature published in the past 2 to 3 decades a

本文根据我国已发表的资料,综合分析研究了我国各地晚白垩世及早、晚白垩世时限前后的孢粉植物组合,特别对其中的被子植物花粉演进序列进行了探索,并和北半球五个主要的晚白垩世孢粉植物发育地区(加拿大西部,美国东部、中西部,东欧,前苏联远东地区)连续的晚白垩世被子植物花粉演化序列进行了对比研究,提出我国晚白垩世孢粉植物群发展基本上可分为四个主要阶段,即(1)前短轴类被子花粉发育期,(2)短轴类被子花粉发育期,(3)进化被子花粉发育期,(4)脊榆粉发育期,它们发育的时限分属于赛诺曼期(Cenomanian),土仑期至桑托期(Turonian-San-tonian),坎佩尼期(Campanian)和马斯特里赫特期(Maastrichtian)。根据孢粉植物群特征和其所反映的古气候,将我国晚白垩世孢粉植物群分为两个孢粉植物地理区,即;东北中生孢粉植物区和西北—东南旱生孢粉植物区,后者又分为西北亚区和东南亚区。

The chemical laboratory of the Semiarid Prairie Agricultural Research Centre of Canada is very influential in western Canada. In this paper, its management and operation were introduced and analysed.

加拿大半干旱草原农业研究站化学实验室在加拿大西部很有影响。本文介绍并分析了它的管理与运作机制。

The Faro and Tom deposits in the Selwyn basin and the Cirque and Driftpile deposits in the Kechika Trough of western Canada are massive sulphide deposits occurring in Cambrian phyllites (Faro) and Devonian marine clastics, black shales and carbonates(Tom, Cirque and Driftpile), respectively. Sulphide minerals as well as gangues in these deposits have suffered intense pressure solution, and the sulphides have undergone multi_stage overgrowth. Overgrowths can be divided into syntaxial and antitaxial ones based...

The Faro and Tom deposits in the Selwyn basin and the Cirque and Driftpile deposits in the Kechika Trough of western Canada are massive sulphide deposits occurring in Cambrian phyllites (Faro) and Devonian marine clastics, black shales and carbonates(Tom, Cirque and Driftpile), respectively. Sulphide minerals as well as gangues in these deposits have suffered intense pressure solution, and the sulphides have undergone multi_stage overgrowth. Overgrowths can be divided into syntaxial and antitaxial ones based on the compositions of overgrown minerals, or into static and dynamic ones based on the environments for overgrowth processes. Triple junction textures can also be formed under the condition of nonorientable stress, and hence are not unique products of annealing equilibrium. Pressure solution of gangue minerals will raise the ore grades, and can hence be applied to account for the appreciably higher metal quantity in ore mylonites than in surrounding massive ores within some deposits. Pressure solution of sulphide minerals will induce remobilization of metals, which are likely to be precipitated in other locations to form new orebodies. Overgrowth is capable of facilitating the unloading of ore materials from fluids. The overgrowth of sulphide crystal seeds is a possible mechanism for sulphide_bearing strata to act as geochemical barriers, which will be overprinted preferentially by late_stage fluids to produce stratabound mineral deposits.

加拿大西部块状硫化物矿石普遍地发生过硫化物的压溶和增生。增生作用根据增生体的成分可以分为同质增生和异质增生 ,根据动力环境可以分为静态增生和动态增生。三晶嵌接结构可以是静态增生的产物。压溶和增生是块状硫化物矿床成岩和变质过程中的重要作用。脉石矿物的压溶可使原生矿石就地加富 ,硫化物的压溶可使成矿物质发生再活化。增生可促进矿质沉淀。富含硫化物的地层之所以能成为地球化学障而有利于后期热液叠加和层控矿床的形成 ,硫化物晶芽的增生是一种重要机制

 
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