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烈度等震线
相关语句
  isoseismal of seismic intensity
     The isoseismal of seismic intensity for the 9.21 Taiwan Chi-Chi earthquake of 1999
     921台湾集集地震的烈度等震线
短句来源
     The isoseismal of seismic intensity is plotted based on the seismic damage to buildings in Nantou county、Taichung county、Taipei county and Miaoli county for the 9.21 Taiwan Chi-Chi Earthquake of 1999.A comparative study is conducted between the isoseismal of seismic intensity and the isoseismal of PGA recorded during this earthquake.
     根据收集到的9.21台湾集集大地震南投县、台中县、台北县和苗栗县的建筑物震害资料绘制了烈度等震线图,并与同一地震中记录到的地震动加速度峰值等值线图做了比较.
短句来源
  “烈度等震线”译为未确定词的双语例句
     As for this condition the study of physical measure of seismic intensity and damage potential of ground motion based on the abundant records and specified damage material from Chi-Chi earthquake is conducted in this paper.
     针对这种状况,本文利用台湾集集地震提供的同一地震中得到的丰富的地震记录和详尽的震害资料开展了烈度物理标准和地震动破坏势的研究,主要研究内容和成果有以下几个方面:(1)整理统计了集集地震的工程震害资料,并以此为基础采用平均震害指数方法绘制了集集地震的烈度等震线
短句来源
     The correlation between acceleration vectors of the ground motion and aspects of the seismals or the major-active fault has also been identified.
     比文中证明了地面运动加速度矢量峰值的衰减与烈度等震线或主发震断层走向的对应关系。
短句来源
     Their characteristics are shown clearly on the seismic deformation belts, isoseismal shapes, foreshocks and aftershocks distributions.
     其共轭破裂特征在地震形变带展布、烈度等震线形态、前震和余震分布等方面表现明显。
短句来源
     and the attenuation relationship of intensity differs manifestly. (3) In the Northwest China and North China,the ratios of long |axis to short |axis of the low-magnitude isoseismals are larger than those of big magnitude. Comparing with that phenomenon,the ratios in the Yunnan region are more complicated.
     (3)与我国西北、华北地区低震级档的各烈度等震线长、短轴之比值均高于高震级档的比值现象相比 ,云南地区这种比值关系要复杂得多。
短句来源
     In borrowing methods, actual distance is used generally as distance pa rameter in seismic ground motion attenuation relationship, which has different meaning from isoseismic distance.
     在借用法工作中,地震动衰减关系所用的距离参数一般采用实际距离,与烈度等震线距离的含义有所不同。
短句来源
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  相似匹配句对
     The isoseismal of seismic intensity for the 9.21 Taiwan Chi-Chi earthquake of 1999
     921台湾集集地震的烈度等震线
短句来源
     FUZZY EARTHQUAKE INTENSITY
     模糊烈度
短句来源
     The distortion of isoseismals was specially affected by the main control factor of intensity.
     尤其等震线图的畸形,是受烈度主要控制因素的影响。
短句来源
     THE ECONOMIO SIGNIFCANCE OF INTENSITY
     烈度的经济意义
短句来源
     DRAWING COMPREHENSIVE ISOSEISMAL LINES USEING THE TOPOLOGICAL OVERLAY PRINCIPLE OF GIS
     利用GIS绘制综合等震线
短句来源
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The authors used the information about five foreshocks (Ms>3.5) and eighteen aftershocks (Ms>3.0) of the Haicheng earthquake of February 1975 to determine the fracture directions of these shock faults and fracture speeds according to the method given in reference [2]. It was found that the distribution of the fracture directions in. the Haicheng shock area are basically consistent with the N-E and N-W strikes of local fracture tectonics,with the strikes of surface fissures created by the aftershocks and with...

The authors used the information about five foreshocks (Ms>3.5) and eighteen aftershocks (Ms>3.0) of the Haicheng earthquake of February 1975 to determine the fracture directions of these shock faults and fracture speeds according to the method given in reference [2]. It was found that the distribution of the fracture directions in. the Haicheng shock area are basically consistent with the N-E and N-W strikes of local fracture tectonics,with the strikes of surface fissures created by the aftershocks and with the configuration of the macroscopic isoseismic lines. Further,it was also found that not only the N-W fractures consistent with the fault strike of the major shock were strongly active,but also the N-E faults were evidently active before and after Ms 7.3 Haicheng mainshock,and that the faults striking N-E also played an important role in the seismogenic process. Therefore,the occurrence of the Haicheng earthquake seems to be the result of the activity of two nearly conjugate sets of faults.

本文利用海城地震的M_S>3.5的5个前震和M_S>3.0的18个余震资料,根据文献[2]提供的方法,确定了这些地震断层面破裂方向及破裂传播速度。在海城震区平面上展布结果表明,地震断层面破裂方向与北东向和北西向区域断裂构造走向、震后产生的地裂缝分布方位、地震烈度等震线形态相一致。进一步证明海城7.3级地震前后,不仅与大震断层走向一致的北西向断裂有强烈活动,而且北东向构造也有显著活动。说明后者对海城地震的孕育和发生也起了重要作用。因此,海城地震的发生是两组近于共轭构造活动的结果。

The interval between Hongdong and Linfen Earthquakes (M=8 ) was 392 years, but the distance between their macroscopic epicenters was only 40 km. This has aroused seismologists' attention. After studing thoroughly the seismic patterns and the aftershock distribution before the two events, and characteristics of the surface deformation and isoseismal during the time, it has been obtained that the focal volumes of the two events were coincided, with strikes of the seismogenic structures as NNE and NWW, respectively,...

The interval between Hongdong and Linfen Earthquakes (M=8 ) was 392 years, but the distance between their macroscopic epicenters was only 40 km. This has aroused seismologists' attention. After studing thoroughly the seismic patterns and the aftershock distribution before the two events, and characteristics of the surface deformation and isoseismal during the time, it has been obtained that the focal volumes of the two events were coincided, with strikes of the seismogenic structures as NNE and NWW, respectively, forminga "Locked Region" of the strong strain accumulation at their intersection. Finally, at the time of rupturing during the two events, they were to be two right-crossing nodal planes of a pair of conjugated faults.

洪洞和临汾八级地震,时间相隔392年,宏观震中仅相距40公里。这一问题引起地震工作者的关注。深入研究这两次地震的震前地震活动图象、余震分布情况、地震时的地表形变带、烈度等震线特点后得出:两次地震的震源体是重合的,发震构造的走向分别为北北东和北西西,它们相交形成能积累强大应变能的闭锁区,最后分别发震破裂时,则为一对共轭断层的两个成正交的节面。

Shanxi subsidence basin is an important area in North China, where strong earthquakes(M=6.0)always visit. This paper deals with the location of epicenters of the earthquakes, the isoseismal lines, the temporal sequences and the tectonic strike of all the strong earthquakes(M=6.0)in this area.The following preliminary results can be done in this paper:In the same subsidence basin, there are earthqakes of M=6.0 which occur repeatedly in the same spot with approximate magnitude, short interval, oblique or normal...

Shanxi subsidence basin is an important area in North China, where strong earthquakes(M=6.0)always visit. This paper deals with the location of epicenters of the earthquakes, the isoseismal lines, the temporal sequences and the tectonic strike of all the strong earthquakes(M=6.0)in this area.The following preliminary results can be done in this paper:In the same subsidence basin, there are earthqakes of M=6.0 which occur repeatedly in the same spot with approximate magnitude, short interval, oblique or normal strike and the different kinds of seismogenic structure.

山西的一些断陷盆地是华北地震区内6级以上地震活动的重要场所。本文在详细研究每个6级以上地震的震中部位、烈度等震线特点、时间序列特征、发震构造走向后得出:在同一盆地内,6级以上地震原地重复发生,而且震级相近,时间间隔较短,发震构造走向正交或斜交,发震构造的类型也有所不同。

 
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