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METHOD FOR MONITORING NETWORK REGION seismic stations

机译:网络区域地震台站的监测方法

摘要

FIELD: physics.;SUBSTANCE: network of seismic stations which use pressure sensors as primary velocity sensors are placed in an earthquake-prone region. The ratios of velocities of longitudinal and transverse waves in the earth's crust are determined at different azimuth angles of the route of each of the network of stations. Discrete samples of measurements are obtained for each of the routes in the same time intervals. The Fourier spectra of the obtained samples are determined with determination of weighted average frequencies. The moment of change in weighted average frequencies is identified with the occurrence of an anomalous zone of an imminent earthquake on the measured route. Bearings of the anomalous zone are taken as points of intersection of the radius vectors of velocities of several stations on the measured routes. Signal energy of the calculated spectra is determined and the behaviour of its variation is monitored. The size of the anomalous zone is calculated. The time and magnitude of the expected seismic impact are predicted.;EFFECT: longer time interval for preventive forecast, high accuracy of determining forecast parameters of a seismic impact.;6 dwg
机译:领域:物理学;实体:将压力传感器用作主要速度传感器的地震台网放置在地震多发地区。地壳中纵向波和横向波的速度比是在每个站点网络的路径的不同方位角下确定的。在相同的时间间隔内为每条路线获取离散的测量样本。通过确定加权平均频率来确定获得的样品的傅立叶光谱。加权平均频率的变化时刻由所测路线上即将发生地震的异常区域的发生来识别。异常区域的方位被视为测量路线上多个站点的速度半径矢量的交点。确定计算频谱的信号能量,并监视其变化行为。计算异常区域的大小。预测了预期地震影响的时间和强度。效果:预防性预测的时间间隔更长,确定地震影响的预测参数的准确性很高; 6 dwg

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