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作 者:陈棋福[1] 李丽[1] 李纲[1] 陈凌[2] 彭文涛 汤毅[3] 陈颙[1] 王夫运[4]
机构地区:[1]Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China [2]Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China [3]Institute of Geophysics, China Earthquake Administration, Beijing 100081, China [4]Research Center of Exploration Geophysics, China Earthquake Administration, Zhengzhou 450002, China
出 处:《地震学报》2004年第6期651-659,共9页Acta Seismologica Sinica
基 金:National Natural Science Foundations of China (No. 40234038 and 40174014).
摘 要:Based on schematically formulation of the vibrations induced by moving trains, this paper analyses the waveforms along the Datong-Qinhuangdao railroad in Northern China recorded in the suburban Huairou district of Beijing on March 8, 2003. It is illustrated that vibrations induced by train, except traditional recognized noises and interfer- ence effects, could be used as a seismic source to detect crustal structures with its advantage of abundant frequency spectrum, repeatability and no additional harm to the environment. It will bring lights to the traditional exploration seismology with the further studies of signal processing and interpretation methods, and related models and new observing systems.Based on schematically formulation of the vibrations induced by moving trains, this paper analyses the waveforms along the Datong-Qinhuangdao railroad in Northern China recorded in the suburban Huairou district of Beijing on March 8, 2003. It is illustrated that vibrations induced by train, except traditional recognized noises and interference effects, could be used as a seismic source to detect crustal structures with its advantage of abundant frequency spectrum, repeatability and no additional harm to the environment. It will bring lights to the traditional exploration seismology with the further studies of signal processing and interpretation methods, and related models and new observing systems.
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