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china mainland
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  中国大陆
    Study on Activity and Mechanism of Group Strong Earthquake in China Mainland
    中国大陆强震的成组活动特征及发生机制研究
短句来源
    STATE OF MODERN TECTONIC STRESS FIELD IN EAST CHINA MAINLAND
    中国大陆东部现今构造应力状态
短句来源
    DISCUSSION ON SYCLIC CHARACTER OF EARTHQUAKES WITH M_(s)≥7.0 IN CHINA MAINLAND IN THIS CENTURY
    本世纪来中国大陆M_s≥7.0地震的轮回性探讨
短句来源
    ANALYSIS ON CLUSTERING FEATURES OF STRONG EARTHQUAKES IN CHINA MAINLAND
    中国大陆6级地震丛式活动特性分析
短句来源
    DETERMINATION OF PLATE MOVEMENT DIRECTION ADJACENT TO CHINA MAINLAND
    与中国大陆相邻的板块运动方向的确定
短句来源
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  我国大陆
    TECTONIC BACKGROUND OF MIDDLE-STRONG EARTHQUAKES IN CHINA MAINLAND IN 2001
    2001年我国大陆中强地震活动的构造背景
短句来源
    In the Paper,seismicity is generally discussed by using the fundamentals of disspa- tive structure of nonlinear thermodynamics,and the surface activities of the three seis- mically active areas of North China,Central China and South China in the eastern parts of China Mainland are briefly analyzed.
    本文运用非线性热力学的耗散结构基本原理对地震活动作了一般性讨论,并对我国大陆东部地区的华北、华中和华南三个地震活动区的地表活动作了一些简要分析。
短句来源
    However, during the last seismic activity climax in China mainland in 1966-1976, this region is quite quiet.
    但在1966—1976年我国大陆上一个地震活动高潮中该区却十分平静,预测在下一强震活动幕中西北地区可能成为强震的主体活动地区。
短句来源
    The spatial-temporal variations of seismicity based on the analysis of twentt two earthquakes with M≥5. 5 during 1970-1984 in the China Mainland and the vicinity,it is shown that during several months to two years prior to the events, regional seismic activity tended to concentrate on the band where the eventual main shock was located, while the seismicity in the wide area around the band became very calm at the same time.
    本文分析了1970—1984年间我国大陆及邻近地区22次5.5级以上的地震震例,结果表明:(1)地震条带与大范围平静伴生这一结论具有普遍意义,在上述研究基础上本文给出了条带判别标志。 (2)条带形成于主震前几个月—2年的时间段内,主要就发生在条带上;
短句来源
    By comparing with 9 large shocks in China mainland, it can be seen that a and b-values of the Hualian M7.6 earthquake are relatively similar to those strong shocks in Southwest China, and the attenuation coefficient, f, lies between those in eastern and western China mainland.
    进一步对比我国大陆九次大震,可见花莲7.6级地震a值和b值较接近西南地区强震,而地震衰减系数P值介于东部和西南地区强震之间。
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  “china mainland”译为未确定词的双语例句
    S-WAVE SPLITTING AND SEISMIC ANISOTROPY OF UPPER-MANTLE IN CHINA MAINLAND
    中国陆区S波分裂与上地幔地震各向异性
短句来源
    Crustal structure of China mainland and its adjacent regions
    中国及邻近地区地壳结构
短句来源
    The exposed crust of the North China platform and the Qinling-Dabie orogenic belt to its south has lower μ(238U/204Pb) values (<8),but other regions of China mainland exhibit much higher μ values,which implies that the low μ feature of the North China platform and its adjacent regions does not have global significance.
    华北地台及其南缘的秦岭-大别山造山带出露地壳具低μ(238U/204Pb)值(<8)特征,但其他地区μ值较高,暗示华北地台及其周边地区出露地壳的低μ值特点不具备全球意义。
短句来源
    A COMPARISON BETWEEN THE SEISMOTECTONICS IN THE EASTERN PARTS OF CHINA MAINLAND AND NORTH AMERICA
    中美大陆东部地震构造的比较
短句来源
    ANALYSIS OF FORESHOCKS BEFORE SOME STRONG EARTHQUAKES WITH M≥6.0 IN CHINA MAINLAND
    我国某些六级以上地震前震的分析
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  china mainland
Distribution characteristics of Rayleigh wave group velocity in China mainland and its adjacent sea areas
      
Butterworth band-pass filter has been applied to S-wave data recorded at 8 stations in China mainland, and S-wave splitting at different frequency bands is analyzed.
      
Frequency band-dependence of S-wave splitting in China mainland and its implications
      
Recent advances in structural control research and applications in China mainland
      
The China mainland Ayu is a new subspecies, Plecoglossus altivelis chinensis Wu >amp;amp; Shan, the establishment of which and its forming causes are discussed.
      
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Having compared the seismic activities of the shallow strong earthquake sequences and the aftershock characters of the strong earthquake sequences with observation data of regional seismic networks and the field investigation results in recent years in China mainland, it can be considered that they belong in the late strong aftershock,and their characteristics are as follows:1. The probability of earthquake occurrence is not high.2. The epicentral intensity is usually lower.3. The pattern of seismic activity...

Having compared the seismic activities of the shallow strong earthquake sequences and the aftershock characters of the strong earthquake sequences with observation data of regional seismic networks and the field investigation results in recent years in China mainland, it can be considered that they belong in the late strong aftershock,and their characteristics are as follows:1. The probability of earthquake occurrence is not high.2. The epicentral intensity is usually lower.3. The pattern of seismic activity probably differs from the previous.4. The precursory signals are few.The method how to estimate the late strong aftershock is studied, and its formation mechanism is also discussed in this paper.

本文比较了中围大陆近年来发生的浅源强震序列活动及有区域地震台网观测资料和地震现场实地考察结果的强震序列余震性质。认为它们属于晚期强余震的范畴,有以下四个特点:1.发震率不高;2.震中烈度一般偏低;3.地震活动的形态可能与前不同;4.前兆信息量小。 本文还探讨了估测晚期强余震的方法,并讨论了其形成机理。

To set up the homogenious magnitude system of local earthquakes is an effective way to uniformize the magnitudes of near earthquake in China mainland. In this paper, the average attenuation patterns of maximum seismic phase of near earthquakes in this region is described, the calibrating function of the average magnitudes has been estimated, and the preliminary effectiveness in practice application is also studied.

建立地方性均匀震级系统是统一我国近震震级的可能途径之一。本文对建立华北南部地方性均匀震级系统进行了尝试,论述了该区近震最大震相的平均衰减形态,估算了均匀震级的量规函数,初步考察了其应用效果。

The continental earthquakes are seriously imperilling the lives of mankind. The continental earthquakes in the world are concentrated in a wide ring between 20°-50°N.lat., which can be divided into four similar seismic regions. The comparison between China-Mongolia and North America may very well release then similarities. The eastern parts of the two seismic regions in China mainland and North America are both seismically inactive, main seismotectonics in NE and intersected with discontinual seismotectonics...

The continental earthquakes are seriously imperilling the lives of mankind. The continental earthquakes in the world are concentrated in a wide ring between 20°-50°N.lat., which can be divided into four similar seismic regions. The comparison between China-Mongolia and North America may very well release then similarities. The eastern parts of the two seismic regions in China mainland and North America are both seismically inactive, main seismotectonics in NE and intersected with discontinual seismotectonics in NW, forming a intersecting pattern. On the other hand, according to the strength and number of earthquakes, both regions can be divided into several latitudinal laths. Between the laths, there are significant differences in seismicity, crustal deformation, newtectonics,gravity, geomagnetism, crustal structure and structure of lithosphere. However, the behaviors of the two regions under the integrated function of a seismicaily intersecting pattern and cutting laths are similar; Under such contral, some source structures within the two regions are also similar, e.g. the Xingtai and New Madred earthquakes, the Quanzhou and Charleston earthquakes.

大陆地震对人类威胁最重。全球大陆地震集中在北纬20°—50°地带,它们可分为四个相似的地震区。中蒙地震区和北美地震区的对比,能很好地揭示其相似的特征。中、美两个地震区的东半区都是相对的少震区,以北东向地震构造为主,均穿插北西向断续的地震构造,构成交叉的网络。此外,根据两地区地震强度和数量的分布,都可以分成几个近东西向的板条,每条之间在地震活动、地壳形变、新构造活动、重力、地磁、地壳结构、以及岩石圈结构等方面都表现了明显的差异。然而地震网络和岩石圈的板条分割这两种构造格局的综合作用,两个区域的表现都是相似的。在此控制下,也表现了某些震源构造的相似,如邢台地震与新马德里地震,泉州地震与查理斯顿地震。

 
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