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中国地震
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  earthquakes in china
     The statistical analysis of the day and night and the season distribution of earthquakes in China
     中国地震昼夜分布和季节分布的统计分析
短句来源
     A COMPARISON BETWEEN CALIBRATION FUNCTIONS OF SURFACE-WAVE MAGNITUDES OF EARTHQUAKES IN CHINA
     中国地震面波震级量规函数的比较研究
短句来源
     The authors apply the Morishita index I δ to analyze the features of the day nigh and seasonal distribution of earthquakes in China. They found that: I δ for earthquakes with M ≥8 is 1.40 and 1.20, showing swarm distribution;
     采用 Morishita(森下 )指数 Iδ 方法分析中国地震昼夜和季节分布特点 ,结果表明 ,M≥ 8地震的 Iδ值分别为 1 .40和 1 .2 0 ,具有明显的丛集特点 ;
短句来源
     TEMPORAL AND SPATIAL STATISTICAL CHARACTERISTICS OF EARTHQUAKES IN CHINA BY SINGLE-LINK CLUSTER METHOD
     用单键群方法研究中国地震时空分布的统计特征
短句来源
     According to 30 year's examination, it is thought that the celestial phenomenon combination period and the solar activity have cer-tian triggering action on earthquakes in China, especially in North China.
     据30年的检验,认为天象组合期及太阳活动性对于中国地震,特别是华北地震有一定的触发作用。
短句来源
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  china earthquake
     The system is based on CEDASGrid(China Earthquake Disaster Alleviation and Simulation Grid), combines the excellent accomplishments and applies these results to the work.
     本系统是建立在“中国地震减灾仿真网格试验系统CEDASGrid(China Earthquake Disaster Alleviation and Simulation Grid)”的基础上,整合了网格项目已经取得的优秀成果,使这些成果能够更好的应用于实际工作之中。
短句来源
     As part of the project named "CEDASGrid (China Earthquake Disaster Alleviation and Simulation Grid)", this paper deals with grid computing platform and seismic observation data service for Internet release based on Web GIS.
     本论文以“中国地震减灾仿真网格试验系统CEDASGrid(China Earthquake Disaster Alleviation and Simulation Grid)”项目为背景,对网格计算平台和地震信息基于Web GIS的网络发布进行了研究和应用开发。
短句来源
     Design and Development of China Earthquake Simulation Grid Application System
     中国地震仿真网格应用系统的设计与开发
短句来源
     By using orthogonal regression method, a systematic comparison is made between surface wave magnitudes determined by Institute of Geophysics of China Earthquake Administration (IGCEA) and National Earthquake Information Center of US Geological Survey (USGS/NEIC) on the basis of observation data collected by the two institutions between 1983 and 2004. A formula is obtained which reveals the relationship between surface wave magnitudes determined by China seismograph network and US seismograph network.
     采用正交回归方法,利用中国地震局地球物理研究所(IGCEA)和美国地质调查局国家地震信息中心(USGS/NEIC)1983—2004年的观测资料,对这两个机构测定的面波震级进行了系统的比较,得到了中国地震台网与美国地震台网面波震级之间的关系式.
短句来源
     RESOURCE MANAGEMENT AND JOB SCHEDULING OF CHINA EARTHQUAKE GRID EXPERIMENT SYSTEM:CONSTRUCTION OF RESOURCE MANAGEMENT AND JOB DYNAMIC SCHEDULING MODEL ProRMJS
     中国地震网格试验系统中资源管理与作业调度研究——资源管理和作业动态分配模型ProRMJS的建立
短句来源
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  “中国地震”译为未确定词的双语例句
     The paper based on the observation report of seismological net of China selected 109earthquakes data from 1983 to 1986 (5.5≤Ms≤8.5; 110°≤Δ≤105°).
     根据《中国地震台网观测报告》,选取1983—1986年期间的109次地震(5.5≤Ms≤8.5;10°≤Δ≤105°)资料。
短句来源
     Journal Related to earthquakes Study in China
     中国地震科技期刊动态研究与思考
短句来源
     Evaluating on Earthquake Relief and Rescue Efforts in 2003 in China
     2003年中国地震救灾评价
短句来源
     ANALYSIS ON THE SEISMIC GREAT TREND IN CHINA BY 7.3 EARTHQUAKE IN TAIWAN STRAITS
     由台湾海峡7.3级地震分析中国地震大形势
短句来源
     Summing-up of the Work in 2000 and the Program of Academic Activities in 2001 of the Seismological Society of China
     中国地震学会2000年工作总结暨2001年学术活动计划
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  earthquakes in china
The second stage marked with the occurrence of quite a few strong earthquakes in China, from which many lessons were learned and corresponding considerations were specified in our design codes and followed in construction practice.
      
Rupture velocity, faulting mode, and fault trend have been determined from the seismic intensity maps of the 1964 Niigata and the 1983 Japan Sea earthquakes in China by matching theoretical isoseismals.
      
Through checking its function in practice, it is found that the spatial distribution of precursor information is not an isolate window or belt, but a broad precursor information field before theMs≥7.0 earthquakes in China and its nearby regions.
      
Patterns and regularity of ring distribution of seismic activity before great earthquakes in China
      
Maximum entropy spectral characteristics of seismic activity for great earthquakes in China
      
更多          
  china earthquake
Prevalence of psychiatric disorder following the 1988 Yun Nan (China) earthquake
      
From April, 2003 to September, 2004, a passive broadband seismic array consisting of 60 stations was deployed over the Tianshan orogenic belt by State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration.
      
We analyzed the North China earthquake catalogue from 1970 to 1986 (from 1965 to 1986 for Huabei, the North China, plain region) and identified forty-two bursts of aftershock.
      
Focal mechanism of the October 19, 1989 Datong, China earthquake
      
Research on the correlation between North China earthquake and global regional strong earthquakes
      
更多          


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在弹性应力以最大速度进行积累的地区,地震活动性最强.强烈的地震活动性可以表現为两种形式:或者是不很强的地震常常发生,或者是发生少数毁灭性的地震.前者相当于那些具有大量断裂或岩石强度較小的地区,后者相当于岩石强度較大的地区.任何地震区內,弹性应力或应变的平均积累速度、一定时期內的平均地震頻度与地震能量就是地震活动性的定量指标. 本文的任务是根据近代的地震仪器賽料和三千年的地震历史資料,全面地研究中国的地震活动性.

Starting from the frequently adopted formula h=△_i/(10~((I_0-I_i)/S)—1)~(1、2),where h is the focal depth, Ai is the mean radius of the ith isoseismal, I_0 is the epicentral intensity and s is a parameter and taking the common logarithm, we have log h=log△_i—1/2log (10~(I_0-I_i)/S)—1),A graticule can be constructed on the basis of this formula with s as a variable parameter. By use of this graticule, the values of s and h for 19 Chinese earthquakes were determined and it was found that the s-values for Eastern...

Starting from the frequently adopted formula h=△_i/(10~((I_0-I_i)/S)—1)~(1、2),where h is the focal depth, Ai is the mean radius of the ith isoseismal, I_0 is the epicentral intensity and s is a parameter and taking the common logarithm, we have log h=log△_i—1/2log (10~(I_0-I_i)/S)—1),A graticule can be constructed on the basis of this formula with s as a variable parameter. By use of this graticule, the values of s and h for 19 Chinese earthquakes were determined and it was found that the s-values for Eastern China are lower than those for Western China. According to the material for 61 earthquakes, it was found that the value of s increases with the focal depth; however, its relation with the low-velocity layer is not evident.

根据常用公式 h=Δ_i/10~((I_0-I_i)/s)-1~(1/2), 式中h为震源深度,Δ_i为烈度为I_i的等震綫半径,I_0为震中烈度,S为一系数;取(1)式的对数得 logh=logΔ_i-1/2log[10~((I_0-I_i)/s)-1], 按(2)式可以作成一量版,以同时測定h和s。利用这个量版測定了19个中国地震的s和h,結合文献[4]的資料,指出中国东部的s系数比西部的偏低;且当深度加大时,s系数加大。采用文献[1,5]的資料測定了61个地震的s系数,結果表明s的数值随深度的增加而加大,占与低速层的关系并不明显。

Basing on the following aspects: 1) the correlation of the macroreiiei and distribution characteristics of the great continental earthquakes in china; 2) the fault plane solution of 127 events; 3) data on 18 great earthquakes of fractured zone; 4) the rate of slip motion along the earthquake fault zones, a dynamical cause of the great continental earthquakes in China was studied, a dynamical model of their stress field adjustment has been presented and is also used to explain the continental seismicity of china....

Basing on the following aspects: 1) the correlation of the macroreiiei and distribution characteristics of the great continental earthquakes in china; 2) the fault plane solution of 127 events; 3) data on 18 great earthquakes of fractured zone; 4) the rate of slip motion along the earthquake fault zones, a dynamical cause of the great continental earthquakes in China was studied, a dynamical model of their stress field adjustment has been presented and is also used to explain the continental seismicity of china.

本文根据强震区域分布特征与大地貌的相关性,127个地震断层面解,18个大地震破裂带资料和地震断裂带的平均滑动速度等方面的资料,提出了中国大陆地震应力调整场动态模型。最后,基于此模型讨论了中国地震活动性问题。

 
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