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Here we show that this statement remains true for extensions of finite complex reflection groups by elements in their normalizer.
      
Yau's original statement was improved or extended in various directions by a long list of authors.
      
We prove a corresponding statement for cross-ambiguity functions.
      
In this article, a closer look at the original statement reveals that the existence condition in fact follows from the smoothness condition which simplifies significantly the statement of the Gelfand-Levitan theory.
      
As an extension of Hoare logic, our pointer logic expresses the change of pointer information for each statement in its inference rules to support program verification.
      
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In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform,...

In recent years, the geotectonic problem of China engages the attentionof many Chinese and Soviet geologists, but different opinions are confessed by different authors. After studying the structural characters of the fundamentalfloor and its later geological development, theauthor of this paper agrees withthe statement of the Soviet geologist, B. M. Синицын. In 1952 he pointed outthat the Chinese platform in eastern China, may bs divided into: (1) theSine-Korean platform; and (2) the Southern-Chinese platform, consolidatedas a result of the Luliang movement. This Chinese platform especially in its southern part shows a very peculiarphenomenon as it is called "Activization" of the platform. During Sinian andPaleozoic, its sediments belonged to the pronounced epi-continental type, duringthe mesozoic the south-eastern part of the Southern-Chinese platform wasneither a stable shelf nor a geosyncline, but an intermediate type between them.Its characters were really not geosynclinal, but sometimes showed geosynclinalaffinities, as for instances, the immense granitic intrusions, the eruptions oflavas, and the rather strongly folded geosynclinal structures. These imply thelimited mobility or the incomplete consolidation of the underground. Accor-dingly, referred to the structural type of this region, P. Misch called it"Sinotype". Furthermore, in the Southern-Chinese platform, two strong "Activizingunits" are recognized as follows: 1) The Hunan-Kwangsi activizing andsubsiding region; 2) The Cathaysian activizing oldland. The "Activization"of these regions lasted for a long geological time. It began in Sinian, throughCaledonian, Variscian, Indo-Sinian, Yenshanian and even Himalayan. BeforeMesozoic, the Caledonian was the most intensive and widely distributed one.But as pointed out by A. H. Мазарович, the Caledonian of the Southern-Chineseplatform was merely a fold-belt within the platform. According to its geotectonic history, its character of sedimentation, itsregional metamorphism, its igneous activity and its geotectonic systems, suchas "Kwangsi ∈ system", "North-Kwangtung ∈ system", "Meso and Neo-Cathaysiansystem", and the "Nanling eastwest tectonic zone", it is the author's opinionthat the "Imtermediate type (Sinotype)" of the Southern-Chinese platform wasdeveloped gradually through a long "Activizing process". This "Sinotype" is anintermediate type between the stable shelf and the geosynclinal region.

作者同意B.M.西尼村的意见,认为中国地台是中国东部的一个大的构造单位,它是在吕梁运动后造成的。中国地台由两个主要部分构成,它的北部称中朝地台,南部称华南地台。中国地台有一很重要的特征,就是一个“活化”的地台。华南地台的东南部“活化”尤其强烈而显著,在中生代的太平洋运动时,差不多具有类似地槽的特征。但是它的“活化”是有悠久历史的,即开始於震旦纪,所以加里东运动给与很大的影响,但加里东运动只是地台内部的褶皱。地台“活化”直到中生代太平洋运动才得到高度发展,产生巨大的火成活动以及“中国式”的构造型式。新生代时地台还有中等强度的运动和火成活动。自第四纪冰期之后,地台仍在较弱的升降运动中。华南地台无论从沉积岩相、区域变质及火成活动,或从山字型、华夏式及南岭东西褶皱的构造体系等构造型式发育史的研究,都可以看到它的“活化”过程,在这过程里发育了“过渡类型”的构造形态,这都是不同放地槽或地台的构造形态的。本文是作为学习心得性质的初步尝试,文中不成熟和谬误之处尚多,希望得到大家的指正。如果能在集体的讨论和研究之下将我国大地构造研究清楚的话,这是作者所衷心期望的。

This paper discusses the statements of Mr. Peirce of America and of Mr. Leaf and Mr. Glaskin of England and of Prof. Daredobech of U.S.S.R., concerning the forms of loops, their lengths and the coefficients of density ratio of plain knitted fabric. An experiment undertaken reveals that the lengths of loops derived from their formulae are not far from the actual values, therefore they are of certain practical use. Upon experiment, it is found, however, that the coefficients of density ratio of plain knitted...

This paper discusses the statements of Mr. Peirce of America and of Mr. Leaf and Mr. Glaskin of England and of Prof. Daredobech of U.S.S.R., concerning the forms of loops, their lengths and the coefficients of density ratio of plain knitted fabric. An experiment undertaken reveals that the lengths of loops derived from their formulae are not far from the actual values, therefore they are of certain practical use. Upon experiment, it is found, however, that the coefficients of density ratio of plain knitted fabric do not correspond with what have been stated by Mr. Leaf and Mr. Glaskin, because the values of coefficients derived from their formulas sometimes become imaginary; and at the same time they do not appear to be the value of 0.8 as work out by Prof. Daredobech. Therefore the theoretical coefficients derived by these workers differ from what are obtained from our experiment. The actual coefficients of density ratio of plain knitted fabric still have to be derived.

本文阐述了美国的Peirce氏,英国的Leaf和Glaskin氏以及苏联Далидович教授对平针织物线圈形态、长度以及稳定对比系数的见解。作者的实验,说明他们的线圈长度公式和实际数据相差不远,有实用的价值,但是作者从实验中发现平针织物的稳定对比系数并不象Leaf和Glaskin氏所说的那样,因为用他们的公式求得的对比系数,有时可能为虚数;同时也不象Далидович教授所说的为0.8。这说明了他们从理论上探求得的平针织物稳定对比系数和实际是有出入的,而真正的平针织物稳定对比系数,尚有待于继续探讨或从实验中求得。

The conception of "inversion curve" is usually introduced in the discussion of the temperature effect for adiabatic throttling process of gases. However, the general features of an inversion curve are rarely discussed. It is the purpose of this paper to clarify the incorrect statements in certain text-books. As the results of such an analysis, the following conclusions are presented: 1. It is the following pair of equations that serves as the equation of an inversion curve: It is not exact to consider...

The conception of "inversion curve" is usually introduced in the discussion of the temperature effect for adiabatic throttling process of gases. However, the general features of an inversion curve are rarely discussed. It is the purpose of this paper to clarify the incorrect statements in certain text-books. As the results of such an analysis, the following conclusions are presented: 1. It is the following pair of equations that serves as the equation of an inversion curve: It is not exact to consider that the second equation of this pair of equations itself is the very equation of tile inversion curve. 2. The inversion temperature cannot be simply represented by v ( ). 3. The higher inversion temperature decreases with tile increase of pressure, while the lower inversion temperature increases with the increase of pressure. The higher inversion temperature and the lower inversion temperature must be treated seperately. 4. It is not correct to say that the lower inversion temperatures are all in the liquid region.

讨论气体绝热节流过程中的温度效应时,一般要引入“转变曲线”这一概念。但关于转变曲线的实质。在一般热力学书中则讨论得较少,并因此而使一些有失概念他得不到完善的理解。本文分析了转交曲线的实质,讨论了转交曲线的方程式,给出了转变曲线在p-v-T空间内的形状,并就转变温度随压力而改变的情况,澄清了由某些书中的错误阐述所引起的疑问。

 
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