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dynamic evolution pattern
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  动态演化图像
     By tracing and analyzing the grouped strong earthquake activity and the dynamic evolution pattern of the earthquake precursor field in recent years in Xinjiang, the relation between the colonial evolution of precursor anomalies and 1996 1998 grouped earthquakes in Xinjiang was discussed.
     对新疆近几年来强震成组活动和地震前兆场的动态演化图像进行追踪分析 ,进一步探讨了前兆异常群体演化与 1996— 1998年新疆成组地震的关系。
短句来源
     When finishing the Project 95-04-04 from China Seismological Bureau, a new dimension-less geoelectric precursor factor, the degree of ground resistivity anisotropy (5) was investigated and proposed. Characteristic of dynamic evolution pattern of 5 reflects seismogenic process. The ability of predicting earthquake by the method of dynamic evolution patterns of S was inspected through a statistic test which was made in big North and Northwest part of China using the method of the R value.
     在完成中国地震局“九五”攻关项目(95-04-04)中,探索提出了新的无量纲地电前兆因子——地电阻率各向异性度(S),其动态演化图像特征反映了地震孕育过程,为考察地电阻率各向异性度(S)动态演化图像法预测地震的效能,对大华北、西北两个研究区利用许绍燮提出的R值法进行了统计检验。
  “dynamic evolution pattern”译为未确定词的双语例句
     CHARACTERISTICS OF PALEO PROTEROZOIC INTRUSIVE ROCKS AND CONTINENTAL DYNAMIC EVOLUTION PATTERN OF TECTONOMAGMA IN EAST LIAONING
     辽东地区古元古代侵入岩特征及构造岩浆大陆动力学演化
短句来源
  相似匹配句对
     DYNAMIC
     动态
短句来源
     Dynamic Evolution of Polyclinic Building
     综合医院建筑的动态演进
短句来源
     Dynamic
     地方科技动态
短句来源
     Dynamic Evolution of Hybrid Petri Nets
     一种混杂Petri网模型动态演变研究
短句来源
     DYNAMIC INTERACTING FORCE AND EVOLUTION OF COULOMB EXPLOSION PATTERNS FOR
     快速H_2~+在固体中穿行时产生的动力学相互作用力及库仑爆炸图形的演化
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  dynamic evolution pattern
Therefore, it would be possible to trace the process of earthquake generation and occurrence from the dynamic evolution pattern of S so as to service earthquake prediction.
      
The dynamic evolution pattern of S reflects the changes of the tectonic stress field during the seismogenic process.
      
Using this index and choosing the internationally accepted ground resistivity data before the Tangshan M=7.8 earthquake of July 28, 1976, the features of dynamic evolution pattern of Rρ(t) are studied.
      
Features and physical process of the dynamic evolution pattern of ground resistivity precursor front
      


In order to quantitatively describe the geoelectric precursor anomaly in the short-impending process of earthquakes, a new geoelectric precursor index — (monthly) relative change rate of ground resistivity, R ρ (t) , is designed. Using this index and choosing the internationally accepted ground resistivity data before the Tangshan M =7.8 earthquake of July 28, 1976, the features of dynamic evolution pattern of R ρ(t) are studied. The results show that: ① about 10~9 months before earthquake,...

In order to quantitatively describe the geoelectric precursor anomaly in the short-impending process of earthquakes, a new geoelectric precursor index — (monthly) relative change rate of ground resistivity, R ρ (t) , is designed. Using this index and choosing the internationally accepted ground resistivity data before the Tangshan M =7.8 earthquake of July 28, 1976, the features of dynamic evolution pattern of R ρ(t) are studied. The results show that: ① about 10~9 months before earthquake, the ground resistivity in a certain range around the epicentral region begins to display the anomaly of accelerating descent, and the rate of descent is higher in the epicentral region than in surrounding areas; ② with the shortening of countdown before earthquake, the R ρ(t) value in epicentral region increases gradually (ground resistivity value decreases at an increasing rate); ③ the R ρ(t) value has the epicentral area as a center and its contour lines propagate towards surrounding areas with the shortening of countdown before earthquake; ④after the R ρ(t) value in epicentral region has descended at increasing rate to reach an extremity [ R ρ(t) = (7.0], it turns to descend at decreasing rate (2~3 months) and earthquake occurs when it accelerates again. Meanwhile, earthquake occurs when the contour lines of R ρ(t) stop propagating towards surrounding areas and turn to shrink back (2~3 months later). Its physical process can be explained by the″ swollen hypothesis″ of Prof. Fu and the theory of ″Slip-weakening and rockmass instability″ of Mei, Niu, et al ..

IntroductionSincethe1960′s,thedevelopmentofmodernscienceandtechnologyhasgradualymadeitposibletopredictearthquakesandhaspromot...

The dynamic pattern and transfer data matrix of the desertification trends of Yanchi Country in 1985-1995 which can indi-cate the dynamic evolution patterns of different phase in locating, qualitative and quantiative are obtained by explaining two-period desertification pattern of the remote sensing images in two phases and establishing spatial database with ARC/INFO. The evolution trends is simulated and forecasted by Markov chain model. The results show that Yanchi Country is...

The dynamic pattern and transfer data matrix of the desertification trends of Yanchi Country in 1985-1995 which can indi-cate the dynamic evolution patterns of different phase in locating, qualitative and quantiative are obtained by explaining two-period desertification pattern of the remote sensing images in two phases and establishing spatial database with ARC/INFO. The evolution trends is simulated and forecasted by Markov chain model. The results show that Yanchi Country is a de-veloping area of desertification, the desertification condition is aggravating with the dual phenomenon of treatment and con-trol abreast with destruction.

以2个不同时期遥感图像为主要信息源,分别解译编制2期土地沙漠化类型图,在ARC/INFO地理信息系统支持下,建立空间数据库,获得了盐池县1985—1995年土地沙漠化动态图和动态转移数据矩阵,可以定位、定性、定量地显示出前后两期间动态演变格局。并用Markov链模型对未来演变趋势进行模拟和预测。说明盐池县属于正在发展的沙漠化地区,沙漠化程度进一步加剧,同时存在着“一边治理,一边破坏”的双重现象。

Using three dimensional viscoelastic finite element simulation (FEM) we study th e dynamic evolution pattern of the coseismic change of Coulomb failure stress an d postseismic change, on time scale of hundreds years, of rheological effect ind uced by the M S=7.2 Xingtai earthquake on March 22, 1966. Then, we simulate the c oseismic disturbance of stress field in North China and dynamic change rate on o ne-year scale caused by the Xingtai earthquake and Tangshan earthquake during 1 5 years...

Using three dimensional viscoelastic finite element simulation (FEM) we study th e dynamic evolution pattern of the coseismic change of Coulomb failure stress an d postseismic change, on time scale of hundreds years, of rheological effect ind uced by the M S=7.2 Xingtai earthquake on March 22, 1966. Then, we simulate the c oseismic disturbance of stress field in North China and dynamic change rate on o ne-year scale caused by the Xingtai earthquake and Tangshan earthquake during 1 5 years from 1966 to 1980. Finally, we discuss the triggering of a strong earthqu ake to another future strong earthquake.

利用三维粘弹性有限元模型 ,首先研究了 1 966年 3月 2 2日邢台 7.2级地震所引起的库仑破裂应力的震时变化 ,以及百年时间尺度流变效应的动态演化图象及其特征 ,然后模拟了自该地震开始 ,经过 1 976年 7月 2 8日唐山 7.8级地震 ,直到 1 980年的 1 5年间 ,两次 7级以上强地震对华北地区应力场的震时扰动作用及其引起的 1年时间尺度的库仑破裂应力的动态变化速率 ,探讨了一次强地震对潜在的下一次强地震可能的加速触发作用

 
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