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tectonic
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  构造
    TECTONIC CHARACTERISTICS OF TAIWAN AND ITS ADJACENT SEA AREAS
    我国台湾及其相邻海域构造特征
短句来源
    GEOLOGY AND PLATE TECTONIC MODEL OF TAIWAN
    台湾地质与板块构造模式
短句来源
    CHARACTERS OF THE TECTONIC SEQUENCE IN ZENGMU BASIN
    曾母盆地构造层特征
短句来源
    BASEMENT TECTONIC EVOLUTION AND BASIN FORMATION MECHANISM OF THE EAST CHINA SEA SHELF BASIN
    试论东海陆架盆地的基底构造演化和盆地形成机制
短句来源
    THE FEATURE OF THE EASTERN SHANDONG-NORTHERN JIANGSU TECTONIC ZONE AND ITS DYNAMICAL EVOLUTION
    胶东—苏北构造带特征及动力学演化
短句来源
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  “tectonic”译为未确定词的双语例句
    FORMATION OF MARGINAL BASINS AND ITS IMPLICATION TO THE TECTONIC EVOLUTION OF SOUTHEAST CHINA
    边缘海盆地的形成机制及其对中国东南地质研究的启示
短句来源
    The Proxy of Seabed Tectonic Process: CaCO_3/Fe_2O_3 and MgCO_3/Fe_2O_3 Ratios in Polymetallic Nodules
    海底构造运动的指示物——多金属结核中的CaCO_3/Fe_2O_3和MgCO_3/Fe_2O_3比值
短句来源
    A Study on Modern Tectonic Tension Fault in the Okinawa Trough
    冲绳海槽现代张裂特征研究
短句来源
    MODERN GEOPHYSICAL CHARACTERISTICS OF TECTONIC TENSION FAULT IN THE OKINAWA TROUGH
    冲绳海槽现代张裂的地球物理特征
短句来源
    Through the characteristics of geophysical field and the distribution of faults, especially by interpretation of seismic profiles and contrdsting well data, we compared and interpreted seven reflected interfases, Tl, T2, T3, T4, T5, T6 and Tg, of which Tg, T5 and T3 represent three regional unconfondties and are the reflections of three tectonic movements in the Cenozoic sediments of Wanan Basin.
    通过分析区域地球物理场特征及断裂分布,以及地震剖面的解释并结合钻井资料对比分析,在万安盆地新生代沉积中对比解释出T1,T2,T3,T4,T5,T6和Tg等7个地震反射界面。
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  tectonic
Studies in the past decade have proven the Shanita fauna to be an excellent marker of the northern peri-Gondwana tectonic blocks.
      
The thermal-rheological stratification structures of the lithosphere in the East Qinling orogenic belt present different features from each other within different tectonic units.
      
The North Qilian orogenic belt is an elongate tectonic unit that lies between the North China plate to the north and the Middle Qilian microplate to the south, and is formed by a collision of the two plates in the Caledonian.
      
The tectonic environment discrimination by trace element reveals that these igneous complexes formed in an island-arc setting.
      
Tectonic setting was stable during the Late Paleozoic, therefore there are obvious negative Ce anomalies.
      
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Based on the distribution of the Pre-Cambrian, the correspondence of the Paleozoic and Mesozoic sediments and their bearing fossils, the similarity of the granite intrusions and their metallogenic characteristics, the interconnection of the deep faults controlling the evolutions of regional geological regimes, the correlation of the regional tectonic linear features, anticlinoriums and synclinoriums and the consistance of the gravity and magnetic anomalies etc., it has been demonstrated that the ancient...

Based on the distribution of the Pre-Cambrian, the correspondence of the Paleozoic and Mesozoic sediments and their bearing fossils, the similarity of the granite intrusions and their metallogenic characteristics, the interconnection of the deep faults controlling the evolutions of regional geological regimes, the correlation of the regional tectonic linear features, anticlinoriums and synclinoriums and the consistance of the gravity and magnetic anomalies etc., it has been demonstrated that the ancient geotectonic evolutions of the southeastern China, including the Provinces of Jiangsu, Zhejiang, Fujian and Taiwan and the Municipality of Shanghai, are closely related with that of Southeast Japan.

本文从前寒武系的展布,古生界至中生界所含化石的共性,花岗岩类和矿化特征的类似,控制槽台体制深断裂带的延伸连接,区域构造线和复背斜、复向斜的相对应,以及深部构造和重、磁力场的一致性等,论证中国东南部的江苏、上海、浙江、福建、台湾等地与西南日本的古地质构造演化是紧密相连的。

In the gravitational field of the sun and the moon, the earth rotes onits own axis and revolves around the sun. And that results in an energyflow in different parts of the earth. According to the enegy flow vector, itcan be inferred that for a long time different parts of theearth vibrates latitutdinally rts whose direction is east-west. And it maybe the mechanical factor why the earth' s tectonic strnctures are south-north predominantly.

地球在日、月等星体的引力场中自转和绕日公转,地球内各部分之间必有能量流动,能流与应力张量的关系应为S=T·V,据此可推断地球各部分长期处于纬向振动中。这可能是地球大构造南一北向占绝对优势的力学因素。

The faults,mainly the NE,secondly the EW and NW,intersect the crustalong the coasts of Guangdong to form seven fault blocks with different activeintensity and twenty sub-fault blocks with different stability.The recent crus-tal movements on these fault blocks are dominated by vertical differential mov-ements.The geotherm-seismicity effect and energy-facies conversion of the fault-bl-ocks processes along the coasts have a close relationship with the deep-seatedtectonics.The recent fault-block subsidence areas...

The faults,mainly the NE,secondly the EW and NW,intersect the crustalong the coasts of Guangdong to form seven fault blocks with different activeintensity and twenty sub-fault blocks with different stability.The recent crus-tal movements on these fault blocks are dominated by vertical differential mov-ements.The geotherm-seismicity effect and energy-facies conversion of the fault-bl-ocks processes along the coasts have a close relationship with the deep-seatedtectonics.The recent fault-block subsidence areas with stronger earthquake andlower geotherm value are not only corresponding to the deep-seated uplift areaof the Conrad and Mohorovicic discontinuities,but it is also a area of highergravity value.The strong earthquakes of M>6 in Guangdong were all takingplace on the boundaries of the recent fault-block subsidence areas where thecrustal movements along the coast are stronger and the reginal stabilities arelower.The distribution of fault-block stress field and the style of the fault move-ment are different with the pattern of the block complex and the direction ofthe main stress in regional tectonic stress field.The regional stability is also influnced by the medium of the fault-blocks,the conditions of tectonic,the development of tectonic and the characteristic ofhydrogeology and engineering geology.There were about 70 percent earthquakesof M≥4(3/4) along the coasts took place in Cenozonic graben basins.

以北东向断裂为主干,迭加东西及北西向断裂,将沿岸地壳切割成活动强度不同的七个断块区及稳定性各异的二十个断块亚区.各断块近代以垂直差异运动为主.沿岸断块活动的热震效应、能态转换与深部构造密切相关.强震区,低热场区,近代拗陷区与深部莫、康氏面隆起区,重力高值区相对应.广东6级以上的强震都分布在沿岸活动性强、稳定性差的近代断陷区的边界上.断块应力分布和断裂活动方式随断块组合形态与分区构造应力场主压应力方位不同而异.区域稳定程度还受断块介质、结构条件、构造发育程度、水文工程地质特征制约.沿岸M≥4(3/4)的中强震70%发生在新生代断陷盆地内.

 
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