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第二幕
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  the second phase
     The Gongchangling granite was emplacedabout 2600 Ma ago and slightly later the second phase of ductile deformation happened, givingrise to NNW reverse shear zones and ENE strike -slip shear zones and producing schistosity S_2 ofparallel ductile shear zones in iron -bearing rock series The third phase of ductile deformationtook place 2000 Ma ago.
     2600Ma左右弓长岭花岗岩侵位,稍后又发生第二幕韧性变形,产生了NNW逆向剪切带和NEE走滑剪切带,这时含铁岩系中形成平行韧性剪切带的片理S_2。
短句来源
     The characters of ENE and NNW shear zones formed in this phase arecontrary to those of the second phase.
     2000Ma发生第三幕韧性变形,其中NEE和NNW向剪切性质与第二幕恰好相反。
短句来源
     The longest principal axis of strain had two azimuths of NW SE and NE SW,which showed that the fault had two obvious different types of strain states. The longest principal axis of strain,which was formed in the second phase of Yanshanian movement and earlier,is in NW SE azimuth. The longest principal axis of strain,formed in the period of Mesozoic fault basins,is in NE SW azimuth.
     该断裂存在两种明显不同的应变状态,NW-SE向最大主应变轴反映了燕山运动第二幕及其以前的应变状态,NE-SW向最大主应变轴反映出辽西中生代断陷盆地形成时的应变状态.
短句来源
     the second phase (Beiliu movement) resulted in northwestward advance of the Yunkai anticlinorium and the foreland basin also migrated toward the northwest side;
     第二幕(北流运动)使云开复式背斜向西北推进,前陆盆地亦向西北侧迁移。
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  “第二幕”译为未确定词的双语例句
     the second is NW(310°—330°)closed similar or congruous folds and fracture cleavages superposing on the first formations under the state of quasi-plastic;
     第二幕为叠加在第一幕之上的北西向(310°—330°)紧闭相似或同斜褶皱及破劈理等,属准塑性状态下的变形;
短句来源
     (1997) concluded on the basis of two Rb-Sr isochron ages that the Jiande Group volcanism (124 Ma) in western Zhejiang should be grouped into the first mag-matic event of Episode I , the Moshishan Group volcanism (97 Ma) in eastern Zhejiang into the second magmatic event of Episode I ,and the Yongkang Group volcanism (<97 Ma) in eastern Zhejiang into Episode I .
     Lapierre等(1997)的一文中据两条Rb-Sr等时线年龄,给出了如下论断:浙西火山活动(建德群)时代为124Ma,划归为第一幕第一次岩浆事件; 浙东(磨石山群)时代为97Ma,划归为第一幕第二次岩浆事件,而第二幕岩浆事件(指永康群)时代<97Ma。
短句来源
     (2) the second episode of the Songyang orogeny (about 2.2 Ga); (3) the Zhongyue orogeny (about 1.9 Ga). The p T t D path shows that the deformation and metamorphism of the granite greenstone terrane were closely related to the process of the continental crustal collision and uplift.
     新太古代岩石经历了嵩阳运动第一幕(约2.5Ga)、第二幕(约2.2Ga)和中岳运动(约1.9Ga)3个重要变质变形期,据此建立的p—T—t—D轨迹显示花岗岩—绿岩地体变质变形与陆壳碰撞隆升过程有密切关系
短句来源
     The alkali rich porphyries in central Yunnan were formed by separated melting of the basic or ultrabasic source rocks in the deep crust during the structural relaxed stage between the first and second epoches of the Himalayan movement.
     云南省中部富碱斑岩形成于喜马拉雅山运动第一幕与第二幕之间的构造松弛阶段,由地壳深部的基性-超基性源岩经分离熔融而成。
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     Its second act was the establishment of the Hata's minority government.
     细川宣布辞职,羽田少数派政权正式成立是日本政界改组的第二幕
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  相似匹配句对
     Secondly, the process of drafting utilizing foreign capital
     第二
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     Secondly, legalization.
     第二
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     SCENE TWO:THE HOSPITAL WAITING ROOM
     第二:医院候诊室
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     THE SECOND ACT OF THE RESHUFFLING IN JAPAN'S POLITICS
     日本政界改组的第二
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  the second phase
The control, based on the ExpoDense algorithm, should be predetermined at the first phase and adaptive in the second phase of the two-phase process of high-density culture production.
      
The stationary probability distribution of a two-phase queueing system with a finite or an infinite buffer for the first phase and a finite buffer for the second phase is derived.
      
The service time distribution is arbitrary for the first phase and of phase-type for the second phase.
      
If the buffer of the second phase is full at the instant of completion of service at the first phase, the first server is blocked until the buffer is freed.
      
The second phase, vasoconstriction, was blocked by naloxone.
      
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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。

Two main deformations in Taihuai Tectonic Cycle of the late Archaean(2700-2500 Ma.)in high-grade supracrustals in the Northern China Craton are identified by a case study led in Shachang,Miyun, Beijing where are recognized two generations of four structural elements,i.e.fault, fold,foliation and lineation. The first deformation (D1) produced recumbent fold(F1)with strong transposition of lithological layers,on their surfaces, and distinct foliation (S1) and lineation with nearly SN horenzantal occurrence as...

Two main deformations in Taihuai Tectonic Cycle of the late Archaean(2700-2500 Ma.)in high-grade supracrustals in the Northern China Craton are identified by a case study led in Shachang,Miyun, Beijing where are recognized two generations of four structural elements,i.e.fault, fold,foliation and lineation. The first deformation (D1) produced recumbent fold(F1)with strong transposition of lithological layers,on their surfaces, and distinct foliation (S1) and lineation with nearly SN horenzantal occurrence as that of the axes of F1. In the second deformation(D2) the structure of the supracrustals was moulded into coaxially superposed large-medium scale open folds (F2) with vertical axial planes and vertically sheared ductile faults.The minerals with preferred orientation,by which the foliations,S1 or S2,are showed, are of two phases,the active phase,formed syntectonicly,and the passive phase,crys-talized before or after deformation.The active phase representing syntectonic metamor-phism shows that the first deformation occurred in an amphibolite facies and the second deformation in green-schist facies rather than in granulite or amphibolite facies. The distribution of the active phases, both in D1 and D2, as well as the distribution of foliation S1 and S2, shows that all the two metamorphisms proceeded strongly only at places where the then synchronous deformations, D1 and D2, were strong.The granulite facies metamorphism taking place around 3000 Ma. ago had been expected to have some particular structural elements but now only banded structures are recognizable.

沙厂铁矿区上壳岩在太古宙时期经历了麻粒岩相、角闪岩相和绿片岩相的多相变质作用,这种多相变质作用的发生及其分布特点是与本区台怀运动旋回的两幕构造变形的形成有密切关系。本文根据不同变质相的矿物组合与不同变形幕构造片理的相互关系的研究得出角闪岩相退变是与台怀变形序列的第一幕变形相对应,而绿片岩相退变是与第二幕变形有联系的结论。退变质作用的不均匀性,即其强弱的表现与不同变形幕的构造变形有直接关系。

Considering features of geomorphic structure and its evolution in time and space, the horizontal landform pattern in China coas essentially established by the Yanshan Tectonic Movement, the relief differences were founded by Himalaya Tecfouic Movemeut, espits secoud stageThe ex-sisting lendforms are the result of the interaction of exogenic and endo-genic agents in gedogic history

从中国地貌结构特点及其时空演变过程来看,中国地貌的平面格局是燕山运动奠定的,地势高差是喜马拉雅运动,特别是喜马拉雅运动第二幕造成的,与太平洋板块和印度板块活动有着密切的生成联系。现存地貌是地质历史上内外力相互作用的结果。

 
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