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台湾花莲海域强震的同震响应特征

Analysis on Coseismic Response to Strong Earthquake in Taiwan’s Hualien Sea Area

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【作者】 杨婕刘水莲卓群陈伟张文男

【Author】 YANG Jie1,LIU Shui-lian2,ZHUO Qun3,CHEN Wei4,ZHANG Wen-nan5(1.Xiamen Seimostation,Xiamen 361003,China;2.Yong’an Seimostation,Yong’an 366000,China;3.Xiamen Seismic Digital Telemetering Centre,Xiamen 361003,China;4.Fujian Seismic and Geological Investigating Institute,Fuzhou 350003,China;5.Xiaxian Seismological Station,Xiaxian 044400,China)

【机构】 厦门地震台永安地震台厦门市地震遥测中心福建省地震局地震地质工程勘察院夏县中心地震台

【摘要】 从面波延迟时间、最大变形幅度、同震持续时间3个方面研究厦门地震台数字化观测仪器对2009年台湾花莲海域2次强震的同震响应特征,结果表明:对同一地点的地震,同震响应面波的延迟时间相同,持续时间与观测仪的分辨率有关;同震响应幅度与地震的震级正相关,与地震发生的方位有关:同震响应的形态以高频脉冲为主,有时伴有阶跃。为今后解释形变短临前兆现象、提取短临前兆信息及依据短临前兆信号对潜在地震的定位等提供基础。

【Abstract】 In this paper,three aspects of coseismic response to two strong earthquakes in Taiwan’s Hualien area in 2009 are studied: delay time of surface wave, maximum deformation amplitude and lasting time of coseismic response.The result shows that the time delay of surface wave is the same to earthquakes at the same place;the lasting time of the coseismic response is relate to the resolution ratio of the observation instrument;the amplitude of the coseismic response is positive correlated with the magnitude of the earthquake.The coseismic responses are mostly high-frequency impulse and sometimes accompanied with phase step.The result may helps us get a better understanding of the performance of digital observation instruments,provides us a way to study short-impending anomaly prior to earthquakes.

【基金】 福建省地震局地震科研基金(闽震科函[2008]9号)
  • 【文献出处】 华北地震科学 ,North China Earthquake Sciences , 编辑部邮箱 ,2011年03期
  • 【分类号】P315.72
  • 【被引频次】3
  • 【下载频次】34
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