震中区震前的高频地声
HIGH FREQUENCY GEOSOUNDS IN THE EPICENTRE REGION PRIOR TO EARTHQUAKE
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摘要: 在近震区建立地声观测站,利用地听器的高频响应特征和对信号的抗干扰处理,结果发现了震前高频地声的存在。进一步分析表明,这些信号是一些能量较弱的脉冲型信息。其持续时间仅为ms的数量级,而最高的优势频率则超过1000Hz。该信息可能是震中附近地区地声的重要特征。Abstract: The geosound observation station has been set up near the epicentre region. High frequency geosound signals have been found by means of geophone for its high frequency response characteristic and some processing of anticlutter. Further analysis iudicates that these signals are impulsive informations with weak energy. The duration of geosound impulses is only of the order of millisecond and the highest dominat frequency is higher than 1 kHz. It is the important features near the epicentre region probably.