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计算地震学
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  computational seismology
     It may include most- part of the contents of statis-tical seismology and fuzzy seismology,and part of the contents of computational seismology,theo- retical seismology,experiment seismology and non-linear seismology,but with emphasis onmathematical methods,modellings and calculations.
     它可以包括统计地震学和模糊地震学的大部分内容和计算地震学、理论地震学、实验地震学、非线性地震学等的一部分内容,侧重于数学方法与模型研究和计算。
短句来源
  “计算地震学”译为未确定词的双语例句
     Though using the integral instrument-recorded catalogue in Sichuan-Yunnan regi on , the seismic parameters which are relatively independent and of explicit physic al meaning such as b value, frequency, strain energy, total area o f fracture pla ne, C value, D value and M f value etc.
     利用川滇地区具有完整仪测的地震目录 ,重点对云南地区及可能发生大震的地震带 (区 ) ,计算地震学相对独立、且具有明确物理意义的参数 :b值、频度、应变能、断层面总面积、C值、D值与Mf值等 ;
短句来源
  相似匹配句对
     We also give a new correction factor to simplify the calculation of the Unstatistic.
     的计算
短句来源
     non-linear seismology;
     非线性地震学
短句来源
     Mobile Computing
     移动计算
短句来源
     SUBSEAFLOOR SEISMOLOGY
     海底地震学
短句来源
     onception and calculation and application of the prediction method of seismological anomalyness
     地震学异常度预测法的概念、计算与应用
短句来源
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There are four major factors that influence the magnitude of deviatoric, stress in the upper lithosphere, based on the data of three-dimensional finite element caloulation, seismology, microstructure and in-situ stress measurements. These factors are, (1)mechanical properties of rock medium (the magnitude of deviatoric stress bigger in the hard rocks, and smaller in the soft rocks); (2)tectonic positions(the magnitude of deviatoric stress is bigger within the plate, and smaller at the plate boundary); (3) depth...

There are four major factors that influence the magnitude of deviatoric, stress in the upper lithosphere, based on the data of three-dimensional finite element caloulation, seismology, microstructure and in-situ stress measurements. These factors are, (1)mechanical properties of rock medium (the magnitude of deviatoric stress bigger in the hard rocks, and smaller in the soft rocks); (2)tectonic positions(the magnitude of deviatoric stress is bigger within the plate, and smaller at the plate boundary); (3) depth (deviatoric stress increases with the increase of depth); (4) latitude (the magnitude of deviatoric stress is bigger in the midlatitude areas, and smaller in the low-or high-htitude areas),

通过上部岩石圈应力状态的三维有限元计算、地震学资料分析,显微构造分析和原地应力测量结果表明,上部岩石圈偏应力值大小与岩石介质的力学性质(硬质岩石介质中偏应力值较大,软质岩石中偏应力值较小)、所处的构造位置(板内偏应力值较大,板间较小)、所处深度(偏应力值随深度的增加而增加)、所处纬度(中纬度地区偏应力值较小,两极和赤道地区较大)有着密切的关系。

Mathematical seismology is a new branch of seismology.Its main research contents consist ofthe applications of various applied methematical methods and some methods of theoretical and ex-perimental analysis to seismological researches.It may include most- part of the contents of statis-tical seismology and fuzzy seismology,and part of the contents of computational seismology,theo- retical seismology,experiment seismology and non-linear seismology,but with emphasis onmathematical methods,modellings and calculations....

Mathematical seismology is a new branch of seismology.Its main research contents consist ofthe applications of various applied methematical methods and some methods of theoretical and ex-perimental analysis to seismological researches.It may include most- part of the contents of statis-tical seismology and fuzzy seismology,and part of the contents of computational seismology,theo- retical seismology,experiment seismology and non-linear seismology,but with emphasis onmathematical methods,modellings and calculations. This paper gives a brief description of the ad-vances in mathematical seismology in recent years,the Sino- Japan Joint Symposium on Mathemat-ical Seismology held in Hangzhou,China,on May 3 to 6, 1995 and the Post-Symposium Courseof Lectures on Mathematical Seismology given in the Hangzhou Cadre Training Center SSB,aswell as the monographs “Advances in Mathematical Seismology” recently published both in Eng- lish and Chinese.

数理地震学是地震学的一个分支,其主要研究内容是把各种应用数学方法及某些理论与实验分析方法应用于地震学研究当中。它可以包括统计地震学和模糊地震学的大部分内容和计算地震学、理论地震学、实验地震学、非线性地震学等的一部分内容,侧重于数学方法与模型研究和计算。本文简要介绍近年来数理地震学研究的某些新进展,1995年5月3—6日在杭州召开的中日数理地震学学术研讨会,会后于5月7—15日在国家地震局杭州干部培训中心举办的数理地震学新进展培训班,以及新出版的中、英文版专著《数理地震学进展》。

Taking the seismic data from the centric-south section of the south-north seismic zone, China as an example, according to analysis of the ten parameters of N-value, C-value, E-value, b-value, seismoless-value, η-value, GL-value, Rm-value, C-value and D-value obtained in space scanning by CAPseis softwar and using the average and modulus methods, seismological anomalyness is calculated. It is proved that the efficacy of probabilistic prediction of future seismic images in the studied area is probably better than...

Taking the seismic data from the centric-south section of the south-north seismic zone, China as an example, according to analysis of the ten parameters of N-value, C-value, E-value, b-value, seismoless-value, η-value, GL-value, Rm-value, C-value and D-value obtained in space scanning by CAPseis softwar and using the average and modulus methods, seismological anomalyness is calculated. It is proved that the efficacy of probabilistic prediction of future seismic images in the studied area is probably better than ones from above mentioned single parameters.

以我国南北地震带中南段的地震学资料为例 ,基于CAPSeis软件对N值、蠕变值、能量值、b值、缺震值、η值、GL值、Rm值、C值、D值等十项地震学预报指标进行空间扫描所得出的数据 ,以平均法和模数法计算地震学异常度 ,对研究区未来的地震学图象进行概率性的预测 ,其预报效能明显高于各单一参量的统计概率。

 
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