seismograms信息详情
震动图
seismographs service───地震仪服务
seismic surveys───地震测量
attenuation relationships seismic───地震衰减关系
few seismograms showing motion near to the source are available.───可以利用的记录震源附近运动的地震图很少。
Theoretical reflection seismograms in dynamite source condition are formed by using anisotropic reflectivity method.───用各向异性反射率法计算爆破源反射地震的理论地震图。
Let's guess an origin time of 10 seconds, measured on the same clock that made the time scale at the bottom of the figure and timed the seismograms.───让我们猜测地震的起源时间为10秒,在同一个钟上测量,使得时间刻度在图表的底部,让地震图同步时控。
Spectral seismograms are introduced as a means to recognize the morphology of the seismic signal, as arriving at the point of observation.───为了识别到达观测点的地震信号的形态,我们引入谱地震图的方法。
Bouchon and colleagues hunted through the rest of the seismograms to see if they had missed other occurrences of that waveform.───布乔及其同事仔细寻找其他震动图中是否也出现那种波形。
Seismograms are the records (paper copy) produced by seismographs used to calculate the location and magnitude of an earthquake.───震动图是地震仪的测量结果的纸质记录,是用来确定地震发生的地区和震级。
With modern instrumentation, energy can be measured directly from velocity seismograms and converted to a magnitude.───现代测量仪器可以直接由速率震动图测量出地震能量,然后转算为地震等级。
Layers need to be fractionized to get high precision synthetic seismograms, whereas its computation complexity is beyond the capability.───为得到高精度合成地震记录,需将地层细分,但地层层数很多时,计算量较大;
Among all the seismic methods, surface wave testing is easiest to perform since surface wave contains most of the energy in the seismograms.───表面波亦为地表震测法中最容易产生且震幅亦最大之震波,因此在施测上较容易且快速。
The principal deficit in making synthetic seismograms is that the input data commonly are incomplete.
Based on 249 horizontal-component digital seismograms recorded on 14 stations of Guangdong Telemetered Network, the attenuation of ground motion and site response of each station is investigated.
Then the azimuth of formation fractures is estimated; and with the joint use of zero offset P wave source VSP data, fast and slow shear wave seismograms are obtained to have fracture density.
Local attenuation in western Nagano, central Japan, estimated from seismograms recorded in three boreholes.
Michel Bouchon at the University of Grenoble, France, and a team of French and Turkish geologists studied seismograms recorded before the Izmit earthquake, which killed some 17, 000 people.
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