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三幕
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  three-act
     As one of the masterpieces, the three-act comedy, the issue of face, attacks the problem of face, a typical Chinese spirit profoundly, thus make it unique in the history of modern Chinese comedies.
     三幕喜剧《面子问题》就是其中历史文化意蕴最为丰厚的一部,它对"面子问题"这一"中国精神的纲领"进行了深刻的解剖,从而成为老舍的喜剧代表作,也是中国现代喜剧史上一部耐人寻味、具有独特艺术魅力的佳作。
短句来源
     During Hemingway’s long literary career, the three-act play The Fifth Column——the only play he wrote, against the background of Spanish Civil War, told the story of an American journalist who confidentially served the Republic Government and participated in the war against the fascist spies——“the fifth column”.
     海明威在其漫长的创作生涯中所完成的唯一的一部三幕剧《第五纵队》以西班牙内战为背景,写一位美国新闻记者秘密为共和政府服务,与几位反法西斯斗士并肩作战粉碎敌人在马德里城内间谍网“第五纵队”的戏剧性故事。
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  “三幕”译为未确定词的双语例句
     Three-scene drama Savage of Gao Xingjian's can be said to be the classic of the eco-drama in the Chinese drama history of the 20th century.
     高行健的三幕戏剧《野人》,可以说是20世纪中国戏剧史上生态戏剧的经典之作。
短句来源
     Twenty-eight deformation temperature were obtained from gneissic granite in Early Proterozoic Liaohe Group, which can be derided into three series, 645—690℃, 550—610℃ and 485℃±. They record three episodes of deformation.
     辽南早元古代辽河群中片麻状花岗岩的变形温度显示出645—690℃,550—610℃和485℃±三组温度值,表明花岗岩遭受了三幕构造变形。
短句来源
     There are obvious differences among the directions,features and mechanism of the tectonic movements with three stages.
     三幕构造运动的方向、特征和动力机制明显不同,运动方向的多次改变导致海槽内多种走向构造地貌的存在。
短句来源
     Multidisciplinary analysis of data on the neotectonism, natural earthquake mechanism, oil drilling, artificial earthquake, variation in the forms of structural traps and their intersect, reservoir pressure, interpretation of satellite image indicates that the direction of the regional principal compressive stress during the Himalayan movement in the Sichuan Basim and its neighbourhood was variable: the direction in the early and late episodes was NE-SW, in the middle - NW-SE.
     根据四川盆地及邻区的新构造运动,天然发震机制、石油钻探、人工地震,构造圈闭形态变异及交切关系、储层或油气藏压力、卫星遥感信息解译等多方面资料综合分析得出,喜马拉雅三幕构造运动区域主压应力方向变化很大,早幕和晚幕运动为NE-SW向,中幕运动为NW-SE向。
短句来源
     ③ the second reservoiring period: the third stage of Himalayan orogeny.
     ③第二成藏期,对应于喜山运动三幕
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  相似匹配句对
     Three.
     .
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     3) T.
     ()T.
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     The latter three episodes were recorded in the calcareous cements.
     后记录于钙质胶结物中。
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     Experimental Analysis of Environmental Description in Act 3, Thunderstorm
     试析《雷雨》第环境描写
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  three-act
You will explore the function and application of story design, dialogue, and character and three-act structure.
      
This three-act one-woman show depicts the lives of a trio of Arab American women and their individual and communal struggles.
      
The first decision was to turn the three-act play into a two act musical.
      
The screenwriting experience is a three-act process that can be improved upon each time.
      


The most intense neotectonic activities in Sichuan province occurred at least three times in the history. The first episode occurred during the time between Eogene and Neogene, the second between Neogene and early Pleistocene and, the third between early Pleistocene and middle Pleistocene. They control the activities of various types of structural zones and structural systems respectively, and through complex evolutions they finally take complicated forms of structural contours and mountains and rivers. The...

The most intense neotectonic activities in Sichuan province occurred at least three times in the history. The first episode occurred during the time between Eogene and Neogene, the second between Neogene and early Pleistocene and, the third between early Pleistocene and middle Pleistocene. They control the activities of various types of structural zones and structural systems respectively, and through complex evolutions they finally take complicated forms of structural contours and mountains and rivers. The structural patterns formed in Neiod are as follows: east-west structural zone, north-south structural zone, chess-board structures, Neocahaysian system, Qinghai-Xizang system, rotational shear structures and so on. The structural stress fields and their trasitional models reflected by the generations and evolutions of all the structural zones and their genetic sequences occurred with good regularity. As a whole, the north-south trending compression was earlier than the east-west trending compression. Active structures occur within Sichuan province from middle pleistocene up to present with north-south trending compression fractures and the related large-seale chess-board structures composed of north-east and northwest trending fractures as the main part and, with folded fractures in western Sichuan province of Neocathaysian system and Qinghai-Xizang system as the secondary part, it is of instructive significance to select the active structures to the study of seismogeology and engineering geology.

四川最强烈的挽近构造活动时期至少有三次。第一幕在新、老第三纪之间,第二幕在新第三纪与早更新世之间,第三幕在早、中更新世之间。它们各控制多种构造带或构造体系的活动,经过错综复杂的演变过程,最后铸成四川复杂的地质构造轮廓和山川地貌景观。挽近时期进一步活动的构造型式有:东西向构造带、南北构造带、棋盘格式构造、新华夏系、青藏系及旋扭构造等。各构造带的发生演变及成生顺序所反映的构造应力场及其转变方式颇有规律。总体看来,南北向挤压作用在先,东西向挤压作用在后。

Based on applying the techniques of structural analysis to rocks involved in the so-called "Yingtaoyuan Formation" near Anshan city, Liaoning province, structural sequence and thus the tectonic style of this formation have been discerned and clarified. Rocks belonging to the "Yingtaoyuan Formation" have undergone at least three phases of deformation during Proterzoic time. The first phase of deformation produced folds ranging in size from intrafolial to regional scale and generally exhibiting tightly appressed...

Based on applying the techniques of structural analysis to rocks involved in the so-called "Yingtaoyuan Formation" near Anshan city, Liaoning province, structural sequence and thus the tectonic style of this formation have been discerned and clarified. Rocks belonging to the "Yingtaoyuan Formation" have undergone at least three phases of deformation during Proterzoic time. The first phase of deformation produced folds ranging in size from intrafolial to regional scale and generally exhibiting tightly appressed to isoclinal forms of nearly N-S trend. F1 folds have a best development and exercise the major control on the disposition of rock units within entire area. S1, a newly formed planar element which is an axial plane to F1 folds, is defined by the preferred orientation of platy minerals such as,mica and chlorite in pelitic rocks and by parallel banding in ore-bearing quartzite. It shows transposition relationship with preexisting So, the origional bedding of rocks. Linear structures including boudins, mullions and Si/So intersections are found in various rock types. Mullions are always occurred in the hinge protions of folds (particularly in antiform) and this may be taken as an indication to identify folds in thick-bedded and even massive rocks. Structures by which the second phase deformation was denoted are S2, F2 and L2. S2 is a set of typical crenulation cleavage that overprinted on an anisotropic background of rocks which already contained earlier structures S0, S1 and F1 etc.. It is an axial plane to F2 folds, a series of folds of mainly mesoscopic in size except those distributed in the Yanqianshan domain. Fine wrinkles, the surface expression of S2/S1 intersections, labelled L2, are widely distributed on S1 (≈S0) surface within pelitic rocks and run parallel to axial trends of folds nearby. Third phase deformation is marked by the spasmodically developed kink-bands. All of these indicate a general evolution tendency of decrease in both metamorphic temperature and plasticity of rocks during this tectonic cycle. On the basis of considering the geometrical homogeneity of the S1 fabric, 9 domains were divided throughout the area occupied by this formation. Data obtained from field survey have been plotted on equal-area stereogram (lower hemisphere) for each domain. Preferred orientation and trend determination of the ambiguous fabric patterns are determined by means of computer treatment using the eigenvalue method. By comparing the structural sequence and tectonic style in the "Yingtaoyuan Formation" to those in the underlying granulite association of the Archean Anshan Group, it is obvious that a great difference exists between these two rock units and that it is improper to regard the "Yingtaoyuan Formation" as one unit of the Archean Anshan Group as was proposed previously by many geologists. However, there is a great resemblance between this formation and the overlying Liaohe Group (Upper Proterozoic) in two aspects, i.e. the structural sequence and the metamorphic facies, so it is reasonable to correlate the time of this formation to Ferrian of Early Proterozoic.

本文区分了“樱桃园组”岩石在元古主构造旋回的三幕变形,详细描述了各幕SFL组合和按区段进行了投影。主变形幕D_1的构造最发育,F_1控制着本区的岩性分布。构造序列及样式变化显示由高塑性向脆性的变形格式。本组与下伏的太古鞍山群变粒岩在构造序列、样式和变质相上都有显著差异,过去许多地质学家把二者混划为一个单位,统名“鞍山群”,属太古宙。但本组与上覆的辽河群(上元古)的构造样式和变质相却相似,故其时代相当于早元古Ferrian期。

There were seven important tectogeneses, two episodes of Indosinian movement and five of Yanshanian, occurring in the Southeast China diwa region in Mesozoic. This paper presents some maps showing that the stratigraphic contact relation caused by each of the tectogeneses changes from SE to NW regularly from unconformity to disconformity to conformity. This indicates that the tectonic force of the diwa activity came from the Pacific Ocean.The largest tectogenesis in the diwa region in Mesozoic is the third episode...

There were seven important tectogeneses, two episodes of Indosinian movement and five of Yanshanian, occurring in the Southeast China diwa region in Mesozoic. This paper presents some maps showing that the stratigraphic contact relation caused by each of the tectogeneses changes from SE to NW regularly from unconformity to disconformity to conformity. This indicates that the tectonic force of the diwa activity came from the Pacific Ocean.The largest tectogenesis in the diwa region in Mesozoic is the third episode of Yanshanian movement occurring between late Jurassic and early Cretaceous. The scale of the tectogeneses increases wavily before Cretaceous and deoreases gradually after Jurassic.

根据地层接触的区域性横向变化,讨论了东南地洼区及其邻区,中生代主要构造运动的强度、规模和动力来源。结果表明,中生代七次较重要的构造运动所造成的地壳变形,均是东强西弱,相应的地层接触关系自东南向北西显示出:角度不整合→平行不整合→整合的变化序列。证实地洼活动的构造动力来自于太平洋方向,其中以发生在晚侏罗世和早白垩世之间的燕山第三幕规模最大。在此之前,地壳运动强度总体波动上升,此后逐渐下降。

 
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