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fault failure
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     According to the hypothesis of fault failure of earthquake genesis, this paper concerns with a stress pattern describing qualitatively the process of genesis o'f earthquakes by means of a three-dimensional stress circle and Navier-Coulomb strength theory.
     本文遵循地震发生的断层成因说,应用三维应力圆和纳维-库伦强度理论,提出一种定性描述孕震过程的应力图象。
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     The acceleration record of the pricipai axis direction is controled by fault failure direction.
     对于断裂带附近的记录,其主轴方向受断层破裂方向的控制。
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     Both the arrival time difference and the virtual wave velocity during and before the earthquake are almost equal to each other,the RT waves during the earthquake were emitted by the fault failure,and the RT waves appearing 2 days before the earthquake were emitted by the early failure of the fault in the hypocenter region of the earthquake.
     峰值异常尖锐,Q≈8.3。 与地震同时从震源发出的RT波为断层破裂所激发,故推断地震前2天所出现的RT波系MW9.0地震震源区断层前期破裂所致。
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  fault failure
The diagnosis module of our BIST circuit can capture the error syndromes as well as fault locations for the purposes of repair and fault/failure analysis.
      
Numerous cycles of fluid pressure build-up, fault failure, jog dilation, fluid flow, phase separation of low salinity H2O-CO2-CH4(-N2) fluids, and sealing took place.
      
Unlike an oil filled recloser, SF6 and solid epoxy reclosers will not create a fire hazard in the unlikely event of an internal arc fault failure.
      
The nal assumption in the derivation of the model is that the per-fault failure density has an exponential distribution.
      
Further tectonic loading will reduce the fault strength until the next fault failure criteria are reached and the cycle repeats.
      
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According to the hypothesis of fault failure of earthquake genesis, this paper concerns with a stress pattern describing qualitatively the process of genesis o'f earthquakes by means of a three-dimensional stress circle and Navier-Coulomb strength theory. This pattern can be used to estimate the tendency of rise and fall of earthquake risk of an area and to show the heteromorphic character of earthquake precurosry phenomena which in turn explains certain problems arising 'from earthquake prediction practice....

According to the hypothesis of fault failure of earthquake genesis, this paper concerns with a stress pattern describing qualitatively the process of genesis o'f earthquakes by means of a three-dimensional stress circle and Navier-Coulomb strength theory. This pattern can be used to estimate the tendency of rise and fall of earthquake risk of an area and to show the heteromorphic character of earthquake precurosry phenomena which in turn explains certain problems arising 'from earthquake prediction practice.

本文遵循地震发生的断层成因说,应用三维应力圆和纳维-库伦强度理论,提出一种定性描述孕震过程的应力图象。这种图象可用来估计地震危险性的增长和减退,并可用它说明地震前兆异常规律应该多种多样,从而可以解释地震预报实践中曾经出现的若干疑问。

This paper discusses the mechanical process of earthquakes from its preparation to occurrence by the method of numerical analysis, taking the 1976 Tangshan strong earthquake as an example. We have analysed the mechanism of the causative fault failure in Tangshan region using the nonlinear finite element method.The mechanical process from the preparation to occurrence of the causative fault and the rock system around the fault are approximately simulated according to the time-sequence by the...

This paper discusses the mechanical process of earthquakes from its preparation to occurrence by the method of numerical analysis, taking the 1976 Tangshan strong earthquake as an example. We have analysed the mechanism of the causative fault failure in Tangshan region using the nonlinear finite element method.The mechanical process from the preparation to occurrence of the causative fault and the rock system around the fault are approximately simulated according to the time-sequence by the increment analysis method. The results are analysed and compared with the observed real earthquake data.

本文用数值分析方法探讨了地震从孕震到发震的力学过程,以76年的唐山地震为实例,用非线性有限元方法,分析唐山发震断层破坏的力学机制,用增量分析的方法,近似地按时间序列模拟发震断层和周围岩石从孕震到发震的力学过程,并与实测资料进行分析比较。

Surface motion characteristics of the Wugia earthquake(Ms=7. 4,Aug. 23,1985)are analysed in this paper We adopted covariances matsix to get the principal axis direction of surface motion based on strong aftershock records,the acceleration records(SN,EW)are synthesized as one time interval along the direction of principle axis. The result shows that the principle axis directions of surface motion are basically pointing towards the epicenter when the different time in tervals are laken,the priciplal axis direction...

Surface motion characteristics of the Wugia earthquake(Ms=7. 4,Aug. 23,1985)are analysed in this paper We adopted covariances matsix to get the principal axis direction of surface motion based on strong aftershock records,the acceleration records(SN,EW)are synthesized as one time interval along the direction of principle axis. The result shows that the principle axis directions of surface motion are basically pointing towards the epicenter when the different time in tervals are laken,the priciplal axis direction of major peak time interval is very close to the priciple axis direction of whole records. The acceleration record of the pricipai axis direction is controled by fault failure direction. The acceleration time history of surface motion was synthesized along the prnicipal axis direction, its response spectrum was similar with the near principal axis direction record. The peak value of synthesizeds were basically consistant with the station records,but the energy somewhat increased.

本文对1985年8月23日乌恰强震(W_s=7.4)的强余震运动特征进行了分析。采用协方差矩阵由强震记录求得地面运动的主轴方向,并将台站记录(南北、东西)两个方向的加速度记录沿主轴方向合成为一条时程。 结果表明,地面运动的主轴方向基本都指向震中。当取不同时段计算主轴方向时,记录上的主峰时段的主轴方向与整条记录的主轴方向十分接近。对于断裂带附近的记录,其主轴方向受断层破裂方向的控制。沿主轴方向合成的加速度时程反应谱,与接近主轴方向的记录时程反应谱形状相似。合成记录与台站记录的峰值加速度值基本相等,而能量有所增大。

 
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