首页> 外国专利> METHOD FOR OBSERVING ELECTROMAGNETIC FIELD RELATED TO PREMONITORY SYMPTOMS OF AN EARTHQUAKE AND DEVICE THEREFOR

METHOD FOR OBSERVING ELECTROMAGNETIC FIELD RELATED TO PREMONITORY SYMPTOMS OF AN EARTHQUAKE AND DEVICE THEREFOR

机译:观察与地震预警症状有关的电磁场的方法及其装置

摘要

PROBLEM TO BE SOLVED: To transmits low frequency earthquake electromagnetic field signals, local characteristic value signals and improved local characteristic value signals of a plurality of observing stations to a base station, determine delay time, half-value width and main characteristic value signal of an electromagnetic field signal from the correlation function of each station, and estimate the generating time, place and magnitude of an earthquake from them with high precision. ;SOLUTION: In a plurality of observing stations, the electromagnetic field signal accompanying a minute breakage of earth crust is observed by a sensor 1 and made into an earthquake electromagnetic signal free from noise by a local discriminating part 3, and local characteristic value and improved local characteristic value are formed by a local characteristic value calculating part 4. A transmitting part 5 transmits them to the receiving part 6 of a base station, a correlation processing part 7 finds the delay time and half-value width from the correlation function between the data of each observing station, and a tomographic part 8 finds the spatial distribution and extension of an earthquake electromagnetic field signal generating source. A main station discriminating part 9 extracts the electromagnetic field signal within an arrival allowable time width from the delay time, and a main station characteristic value calculating part 10 finds the main station characteristic value. A three-factor estimating part 11 synthetically estimates the earthquake generating time, generating place, and magnitude from them.;COPYRIGHT: (C)1997,JPO
机译:要解决的问题:为了将多个观测站的低频地震电磁场信号,局部特征值信号和改进的局部特征值信号传输到基站,确定天线的延迟时间,半值宽度和主要特征值信号。通过每个站的相关函数获得电磁场信号,并从中精确估算出地震的发生时间,地点和震级。 ;解决方案:在多个观测站中,伴随着地壳微小破裂的电磁场信号由传感器1观测,并由局部判别部分3变为无噪声的地震电磁信号,并改善了局部特征值局部特征值由局部特征值计算部分4形成。发送部分5将它们发送到基站的接收部分6,相关处理部分7从信号之间的相关函数中找到延迟时间和半值宽度。断层摄影部8求出各观测站的数据,并求出地震电磁场信号发生源的空间分布及扩展。主站辨别部9从延迟时间提取到达允许时间宽度内的电磁场信号,并且主站特征值计算部10求出主站特征值。三因素估算部分11从中综合估算地震发生的时间,发生的地点和震级。版权所有:(C)1997,日本特许厅

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