助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   构造旋回 的翻译结果: 查询用时:0.024秒
图标索引 在分类学科中查询
所有学科
地质学
石油天然气工业
矿业工程
更多类别查询

图标索引 历史查询
 

构造旋回
相关语句
  tectonic cycle
     Sedimentary formation and tectonic cycle of the Jurassic Northeastern Jiangxi continental basin
     赣东北侏罗纪陆盆的沉积建造及构造旋回
短句来源
     Latitic Series of the Yanshanian Tectonic Cycle in Beijing Region
     北京燕山构造旋回安粗岩系
短句来源
     The time limits of two grade Ⅱ sequences correspond to Early Permian and Late Permian and they are consistent with tectonic cycle and time limits of basin changing in southern China.
     2个 级层序的时限分别对应早二叠世和晚二叠世 ,这与中国南方二叠纪构造旋回盆地变更时限相一致。
短句来源
     Based on lithology, lithofacies, seismic reflection, log response, paleobiology, tectonic cycle, contact relationship and isotopic dating, the lower paleogene in the Liaohe Basin is divided into 4 sequences and 12 subsequences.
     根据岩性、岩相、地震反射、测井响应、古生物、构造旋回、接触关系及同位素年龄测定等,将辽河盆地下第三系划分为4个层序和12个亚层序。
短句来源
     The Yangtze panplate moved and subducted towards north and collided with the North China plate in the Hercynian tectonic cycle.
     海西构造旋回,泛扬子板块北上与华北板块俯冲碰撞。
短句来源
更多       
  tectonic cycles
     The geopulsation cycles are of different ranks which may form a hierarchy system. The cycles in the order of their length of time intervals are: Supercycle about 1 Ga, Megacycle 250—300 Ma, first order cycle 50—150 Ma, second order 5—50 Ma, and third order 1—5 Ma. All of them may be correlated with the different ranks of tectonic cycles, but higher order cycles above the third are without tectonic effect.
     地球脉动旋回可以分为不同的级次,构成级别体系:超级旋回约1Ga,巨旋回250~300Ma,一级旋回50~150Ma,二级旋回5~50Ma,三级旋回1~5Ma,均可与构造旋回相对应,更高的级次对构造不形成影响。
短句来源
     EPSODIC TECTONIC CYCLES AND INTERNAL ARCHITECTURES OF SEQUENCES IN CONTINENTAL BASIN
     陆相盆地幕式构造旋回与层序构成
短句来源
     The orust tectonic evolution in the research area could been divided into 8 large tectonic cycles, 7 times change of tectoni systems of organization, and subdivided it into tectonic evolution deformation series of 15 generations.
     研究区地壳构造演化大致经历了8个大的构造旋回、7次构造体制的转变和15个世代的构造演化变形序列
短句来源
     The tectonic cycles of Caledonia(440-445Ma ),Late Varascan(ca.350Ma )and Early Indosinia(250-230Ma )completed the transformation from p aleo-Asian Ocean to paleo-Tethys,a nd formed the paleo-Eurasian continent,which re sponded to the convergence of the Pan gea.
     加里东构造旋回(440~425Ma),早华力西构造旋回(350Ma),晚华力西—早印支构造旋回(250~230Ma),完成了古亚洲洋向古特提斯洋(海)的转换,实现了古欧亚大陆的形成,是对Pangea古陆聚合的积极响应.
短句来源
     With the six factors considered comprehensively,the stratigraphic framework of the Yi-Shu graben is set up based on biosequence and tectonic sequence and a integral and comparative program of the Yi-Shu graben is put forward. T5,T3,T1 seismic reflective layers represent tectonic cycles of different stages in the basin development and T4,T2 seismic reflective layers represent sedimentary and climatic sequence.
     在综合考虑6种因素的基础上,以生物层序和构造层序单元为基础,建立了依─舒地堑的整体地层格架,提出了依─舒地堑统一地层格架对比方案,指出T5、T3、T1地震反射层具有构造旋回意义,代表盆地演化的不同阶段,T4、T2地震反射层具有沉积学以及气候层序的意义。
短句来源
更多       
  structural cycle
     In Triassic,the evolution of this basin experienced a complete structural cycle from extended rift basin to compressed flexure one,then rising above the sea level.
     三叠纪 ,盆地演化经历了一个由拉伸作用形成的断陷盆、构造挤压形成的扰曲盆地和挤压隆升暴露于海面之上的完整构造旋回过程。
短句来源
  “构造旋回”译为未确定词的双语例句
     According to wave theory the east rift-subsidence zone is analyzed with 60Ma and 31Ma cyclic wave.
     提取 60Ma和 3 1Ma的周期波对东部断陷区进行沉积盆地波动理论分析 ,结果表明 ,60Ma周期波与盆地总体构造旋回一致 ;
短句来源
     Hydrocarbon generating history of the source rocks is built applying the technology of thermal simulation and biogas simulation by burial history curve and structural cyclic analysis.
     通过编制埋藏史曲线和构造旋回分析,采用烃源岩热模拟、生物气模拟技术,建立烃源岩的生烃史;
短句来源
     SWARMS OF EVENTS AND CLIMATIC-TECTONIC CYCLES WITH 0.4Ma QUASI-PERIOD
     具有0.4Ma准周期的事件群发性与气候-构造旋回刍论──以黄土区为对比区
短句来源
     and there is different mineralization in different granite structure cycle and differtent granite formation unit.
     不同花岗岩—构造旋回和不同花岗岩建造单元具有矿化的差异性。
短句来源
     By examination of Paishanlou gold deposit in Fuxin, Liaoning Province, it is concluded that the auriferous ductile or ductile-brittle shear zone is the specific result during the forming stage of supracrustal rock and basement rock series or the metamorphic-deformation stage of syntectonic cycle.
     提出了含金韧性或韧脆性剪切带是表壳岩、含金基底岩系形成期或同构造旋回变质变形期的特定产物,故可称之为含金同韧性剪切带.
短句来源
更多       
查询“构造旋回”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  tectonic cycle
An upper intercept age of 2,795 + 38 Ma, extends the known length of the otherwise tightly established, late Archaean tectonic cycle at Agnew from 250 Ma to 320 Ma.
      
These observations can be interpreted according to a volcanic-tectonic cycle in which volcanic eruptions and hydrothermal circulation are followed by a tectonic phase which includes fissuring and vertical movements.
      
Approximately the upper 60 km of the lithosphere is processed by the plate tectonic cycle.
      
However, in all cases substantial fraction of the mantle reservoir have been processed by the plate tectonic cycle.
      
The plate tectonic cycle is an inherent component of mantle convection.
      
更多          
  tectonic cycles
5 sequences represent 5 tectonic cycles and all the 6 sequence-bounds reflect tectonic activities.
      
We propose a model of volcano-tectonic cycles in which smooth volcanoes and lava flows are built during phases of high magmatic flux.
      
Glacial maximums predated the main final phases of tectonic cycles.
      
Tectonic cycles and the history of the Earth's biogeochemical and paleoceanographic record.
      
The glacial maximums were synchronous with early phases of tectonic cycles and peaks of subduction-related explosive volcanism.
      


There are three major fault blocks in China, i. e. the North China block province (consisting of six subblocks), the Yangtze block and the Tarim block. Their origin, development and consolidation are controlled by the pre-Sinian orogenies. One fault block may have been resulted from a single orogenic cycle or in most cases a few orogenic cycles because of the pre-Sinian orogeny was characterized by multiple cycles. Since the idea that an orogeny is occurred simultaneously all over the world was generally denied...

There are three major fault blocks in China, i. e. the North China block province (consisting of six subblocks), the Yangtze block and the Tarim block. Their origin, development and consolidation are controlled by the pre-Sinian orogenies. One fault block may have been resulted from a single orogenic cycle or in most cases a few orogenic cycles because of the pre-Sinian orogeny was characterized by multiple cycles. Since the idea that an orogeny is occurred simultaneously all over the world was generally denied by most geologists, we consider that the orogeny must also be diachronous" especially in non-metamorphic sequences. Moreover, we suggest that the Jinning orogeny in the Yangtze block is a good example of such diachronous orogenies.But in the metamorphosed sequences, an uncomformity which can be observed in geological section may generally represent a combinative expression of many orogenies.Oro'genic cycles in these three major fault blocks have been classified as follows:Sanggan cycle (>2500-2600 m.y.)Wutai cycle (>2000 m.y.)Zhongyue cycle (>1700 m.y.)Yinshan cycle (>1200-1300 m.y.)Jinning cycle (>1050-900 m.y.)An attempt to correlate them with other orogenies that occurred in the other continents of the world is made in this paper.

本文对我国三大断块(区)的前寒武纪地层的发育、建造类型、不整合及部分同位素年龄值进行了对比,划分出五个地壳构造运动旋回,即桑干旋回(2500—2600百万年前),五台旋回(2000百万年前),中岳旋回(1700百万年前),“阴山旋回”(约1200—1300百万年前)和晋宁旋回(1050—900百万年前)。指出在前震旦纪变质岩系中的不整合具有多次地壳构造运动的集合的性质,相当显生宙的一个构造旋回。同时指出晋宁运动具有明显的穿时性,与板块构造理论相符。

Based on the regional paleogeography, tectonic history and magmaticactivity, this paper deals with the Mesozoic tectonism and magmatism of thelower Yangtze Valley, and also discusses the relation between the mechanismand evolution of continental volcanism. After the beginning of Mesozoic time, the platform block of the lowerYangtze Valley was disintegrated. Under the influence of the northwardmovement of the Pacific Plate, a series of left-lateral deep faults were for-med in the eastern part of Chinese continent....

Based on the regional paleogeography, tectonic history and magmaticactivity, this paper deals with the Mesozoic tectonism and magmatism of thelower Yangtze Valley, and also discusses the relation between the mechanismand evolution of continental volcanism. After the beginning of Mesozoic time, the platform block of the lowerYangtze Valley was disintegrated. Under the influence of the northwardmovement of the Pacific Plate, a series of left-lateral deep faults were for-med in the eastern part of Chinese continent. Among them, the Tancheng-Lu-jiang deep fault is the largest one. From Isopach maps of different ages(Fig.2)we can see that the Tancheng-Lujiang deep fault hadn't any influence over all rock formations,except in Triassic time. Near the fault zone, atZhangbaling, Anhui, the upper Proterozoic schist has a radioactive age of 230-190 m. y., which denotes the age of dynamic metamorphism. In the studiedarea, the Tangcheng-Lujiang deep fault separates the Sino-Korea Plate onthe north-west from the South China Plate on the south-east. The Pre-Me-sozoic formations on both sides are from two quite different sedimentary ba-sins, and have a dislocation of several hundred kilometers. Late Jurassic vol-canics occur along the fault, while the Cretaceous sediments overlap thefault zone. The gravitational and magnetic fields (Fig. 3) suggest that theintrusion of basic and ultrabasic rocks occupy the fault zone. The fault planeis very steep and cuts deeply downwards. According to telluric measurement,it reaches to the upper mantle. Since Mesozoic time, Honshu-Taiwan island arc faced towards east, andobducted above the Pacific oceanic plate. A stretching sea, created behindthis area, i. e., the depression of epicontinental sea type, is attributive to theovercompensation of the upper mantle under southeast China. For the timebeing, this depression is enlarged. It is controlled by the NNE left-lateralfault and NEE spreading axis, we called it North Jiangsu-South Yellow SeaDepression. It is one of the epicontinental seas on the western Pacific. The Mesozoic tectonism of the lower Yangtze Valley is the combinationand interaction of these two kinds of movements. At first, the left-lateralmovement was dominant, and then the stretching (spreading in continent)gradually took place. So the shape and the cross-section of the depressionchanged with time (Fig. 5). Now, we divide the studied area into two parts: continental uplift andepicontinental depression, but as a whole, they are only a part of the conti-nental margin of western Pacific. Mesozoic magmatic activities spread widely over the area. Their locations,ages and rock compositions are closely related to their tectonic positions.They form a continuous evolutional series in space and time. Within thecontinental uplift, the main activities are batholitic intrusions, such as Huang-shan etc. They are intruded into the axial part of anticlinorium, composedmainly of granite or granodiorite. Small continental volcanics might occur inlocal downwarps. On the peripheral part of the continental uplift, there aresome stocks composed of granodiorite with clear differentiation.They are locat-ed at the axial part of folds. In the axial part of synclinorium, there is anotherkind of stocks with quite complex composition from granite to diorite andmonzonite. Upper Jurassic-Lower Cretaceous volcanics occur within local downwarps, such as Fanchang, etc. The main rock types are dacite, partlyrhyolite and rhyodacite, but andesite is very scarce. The volcanic series itselfconstitutes a synclinal downwarp, laid over by different pre-Mesozoic folds,mostly anticlines. On the peripheral part of epicontinental depression, intrusive activity isvery weak. There are some small stocks, mainly diorite. On the western partof the studied area, near Tancheng-Lujiang deep fault, there occur somesyenite batholiths. Continental volcanism spread widely over this area, form-ing large synclinal downwarps of more than thousand square kilometers. Themost famous ones are Nanjing-Wuhu and Lujiang-Zhongyang. Their mainrock types a

一、地质发育概况 长江下游地区在地质发育进程中历经了多次构造旋回,经受多期构造作用的迭加和改造。

There are various types of minor structures occurring in the Baiyin Open-pit Mine, Gansu. According to the deformation succession of the structures,it may be subdivided into two main phases and three subordinate stages,and all of them belong to the Caledonian cycle. For all the stages, the stylesof structure, dynamic characteristics, heat-flow values,strain-facies and meta-morphism that have been found in the minor structures,reveal certain regu-larities.

白银露天矿区小型构造十分发育,类型繁多,计有小褶皱,流劈(片)理、折劈理、破劈理、扭折、剪节理及拉长线理、皱纹线理等透入性构造。据初步解析可划分为二幕三期,均属加里东构造旋回。各变形期的构造样式、动力学特征、热流值、应变相及变质作用等都有一定的规律。研究这些规律,对于解决白银地区区域构造和成矿规律等方面都有实际意义。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关构造旋回的内容
在知识搜索中查有关构造旋回的内容
在数字搜索中查有关构造旋回的内容
在概念知识元中查有关构造旋回的内容
在学术趋势中查有关构造旋回的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社